北苏鲁乳山辉长—闪长岩及其基性岩石包体的锆石U-Pb年代学和地球化学研究
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摘要
华北克拉通东部显生宙岩石圈破坏及其深部过程研究是我国固体地球科学的重要议题。近年的许多资料表明,将华北东部南缘岩石圈地幔演化与扬子大陆向华北地块的深俯冲进行有机联系可以为探讨华北克拉通的改造、破坏等深部过程提供有意义的约束。造山带内火成岩的地球化学特征是它们形成时地球动力学背景信息的最直接载体,能揭示出块体结合部位丰富而复杂的壳幔相互作用信息。本文以北苏鲁乳山市宫家辉长—闪长岩、上口辉石闪长岩及其中的基性岩石包体为研究对象,同时兼顾邻区同时代的三佛山花岗岩,在对它们进行详细的锆石U-Pb年代学、岩相学、地球化学和同位素地质学分析的基础上,细致讨论了它们的岩石成因、源区性质及所揭示的壳幔相互作用及岩石圈地幔演化信息,反演了华北东部南缘中生代—新生代岩石圈减薄等深部过程。获得了如下的主要认识:
1.宫家辉长—闪长岩和上口辉石闪长岩是分别位于乳山市东南部宫家村和东北部上口村的两个独立小岩体。宫家岩体从早到晚由中—细粒黑云母辉长岩、中—粗粒黑云母辉长岩、细粒黑云母辉石闪长岩和中—细粒黑云母辉石闪长岩构成,以细粒黑云母辉石闪长岩为主体。上口岩体出露不完整,仅见到偏中性的辉石闪长岩单元。宫家岩体中的基性岩石包体类型包括黑云母橄榄辉石岩、含长单斜辉石岩、单斜辉石岩及黑云母辉长岩等四种类型,以黑云母辉长岩为主,主要分布在第三期侵位的细粒黑云母辉石闪长岩之中。
2.宫家辉长—闪长岩中四个相带岩石的形成时代较接近,为114±1Ma～111±1Ma,上口辉石闪长岩的侵位结晶年龄为110.5±1Ma,它们同属早白垩世晚期岩浆活动的产物。宫家岩体中的黑云母橄榄辉石岩包体也获得了111.5±1Ma的~(206)pb/~(238)U加权平均年龄。
3.宫家辉长—闪长岩和上口辉石闪长岩均显示出高钾钙碱性—钾玄岩系列的特点,具有高Al_2O_3、低MgO,富集轻稀土、大离子亲石元素和Pb,强烈亏损Nb、Ta、Zr、Hf,Ti等高场强元素和类似EMII型地幔的Sr-Nd同位素组成,这些特征相似于华北东部南缘中生代幔源火成岩。宫家和上口岩体与富集的大陆岩石圈地幔在软流圈上涌的伸展背景下减压熔融有关,并伴随着橄榄石、单斜辉石、磷灰石及铁钛氧化物等矿物的分离结晶。其地幔源区以相对富单斜辉石的尖晶石相为主,深度小于80kin,并具有亲华北南缘的特点。该地幔源区不同于华北古生代金伯利岩中橄榄岩捕掳体所代表的以方辉橄榄岩为主的难熔型地幔,也与新生代碱性玄武岩中橄榄岩捕掳体指示的主元素饱满、同位素亏损的新生大洋型地幔有差别,是遭受了来自俯冲的扬子大陆板片释放的熔/流体交代改造而演化的产物,但改造程度弱于华北南缘早白垩世早期方城玄武岩和沂南辉长代表的岩石圈地幔,显示俯冲的扬子陆壳物质对上覆岩石圈地幔的交代改造自下而上是不均匀的。
4.宫家辉长—闪长岩中基性岩石包体的显微结构和岩石组合不同于邻区太古代或元古代超镁铁质岩块和华北克拉通东部中生代闪长岩中捕获的来自岩石圈地幔或壳幔过渡带的深源捕掳体。相反,它们具有的火成结构、与寄主岩相似的岩石化学和同位素组成,说明其成因与寄主岩浆在侵位上升时发生高压分异结晶或析离有关。四类包体各不相同的主元素、微量元素组成,显示其可能为寄主岩浆演化的不同阶段产物。
5.对三佛山花岗岩的研究主要集中在王家口和潘家含斑二长花岗岩和尚岭正长花岗岩,它们形成于早白垩世晚期(～110Ma),是一套高钾钙碱性系列的岩浆,具有高SiO_2、低FeO_t、MgO的特点,Na_2O/K_2O均小于1,富集轻稀土、大离子亲石元素(如Sr、Ba),Sr-Nd同位素组成与邻区幔源岩石十分接近。它们是早白垩世软流圈上涌和华北东部岩石圈减薄的伸展背景下古老的陆壳物质发生重熔,形成的酸性熔体与幔源岩浆混合后再经历分离结晶的演化产物。它们具有中稀土下凹、重稀土富集的稀土配分模式,表明酸性岩浆的熔融源区残留相以含有角闪石为特征,基本无加厚地壳的必要矿物相石榴子石,揭示～110Ma时该地区地壳已恢复到正常厚度,暗示此时的岩石圈减薄已达到峰期。
6.结合已有的研究成果和本文资料,华北克拉通东部南缘中—新生代岩石圈地幔演化的过程可能可以解释为:早中生代扬子大陆向华北深俯冲,破坏了华北南缘原有的地幔对流体系,加剧了软流圈的活动性能,引起岩石圈地幔的热—机械侵蚀和化学侵蚀减薄;苏鲁超高压变质带折返时释放的流体和俯冲板片熔融形成的硅质熔体不断地穿透并交代改造上覆华北古老岩石圈地幔楔,使之转变为高度富集的地幔;在中晚侏罗世时,软流圈继续抬升,引起原先的交代富集地幔熔融,形成的幔源岩浆或底侵在下地壳、壳幔过渡带,并同时诱发俯冲的扬子陆壳发生重熔形成花岗质岩浆;早白垩世郯庐断裂带的大幅左行平移走滑引起软流圈物质以郯庐断裂带为中心大幅上涌,导致上覆岩石圈地幔和地壳的强烈伸展,伴随岩石圈地幔的侧向挤出减薄,富集的岩石圈地幔同时发生大规模熔融而被消耗,岩石圈地幔减薄达到峰期,幔源岩浆同时烘烤地壳,诱使地壳发生重熔形成酸性岩浆,在合适的部位还形成壳幔混合花岗质岩浆。晚白垩世—新生代,太平洋板块快速向华北陆内斜向俯冲导致含深海远洋沉积物的俯冲洋壳软流圈发生混熔,加快了岩石圈地幔减薄,软流圈地幔于古近纪开始趋于冷却回沉,形成现今新生的大洋型地幔,实现对原有的富集型岩石圈地幔的置换。这一模式在华北东部南缘具有普遍意义。
The nature and evolution of the North China lithosphere have attracted many attentions in the past few years,because of considerable losing of the Archean keels during the Phanerozoic. Recent published data indicated that the Dabie-Sulu orogenic belt has become one of the most ideal regions for the studies on deep subduction of continental lithosphere,and its affections to the destruction of North China Craton.Mesozoic igneous rocks from the Dabie-Sulu orogenic belt are considered to be the products of subduction-induced and post-collisional extension-related magmatism and thus can provide constraints on the processes involved in the lithosphere evolution.In this paper,we present geochronological and geochemical investigations for the Gonajia and Shangkou intermediate-mafic intrusive complex,and their mafic xenoliths, as well as the coeval Sanfoshan granites from the northern Sulu orogen,with the aim of constraining the petrogenesis and origin of these rocks and mantle processes involved in their generation,and will further discuss the crust-mantle interaction that occurred underneath the collision zone and its implication for the lithosphere evolution.In addition,the evolution crust-mantle interaction occurred underneath the southern wedge of the North China lithosphere have also been discussed.
1.The Gongjia and Shangkou complexes are two independent small intermediate-mafic plutons that located at the southeastern and northeastern part of the Rushan city,respectively. The Gonajia complex comprises of four phases including(1)medium- to fine-grained biotite gabbro;(2)medium-grained biotite gabbro;(3)medium- to coarse-grained biotite gabbro;(4) fine-grained pyroxene-beafing diorite.The pyroxene-bearing diorite predominates in the outermost part of the Gongjia complex.The Shangkou pluton has relative poor occurrence and only the intermediate phase been found.Mafic xenoliths captured in the Gongjia complex include olivine-pyroxenite,plagioclase-bearing clinopyroxenite,clinopyroxenite and biotite-bearing gabbro,all of which mainly distributed in the third phase of the host rocks.
2.The Gongjia complex has rather uniform zircon U-Pb ages of 114±1Ma-111±1Ma, whereas the Shangkou pyroxene-bearing diorite has an emplacement age of 110.5±1Ma, indicating that they were both intruded in the late of the Cretaceous.Zircons extracted from an olivine-pyroxenite xenoliths give a weighted mean ~(206)pb/~(238)U age of 111.5±1 Ma.
3.The Gongjia and Shangkou complexes have high Al_2O_3 and low MgO,and show high-K calc-alkaline to shoshonitic affinities.They are highly enriched in large ion lithophile elements (LILE)and light rare earth elements(LREE),depleted in high field strength elements(HFSE) and Pb,and exhibit EMII-like Sr and Nd isotopes.These complex are interpreted to originate from decompression melting of spinel-facies cratonic mantle that metasomatized by the subducted Yangtze crustal materials and the melts experienced fractionation of olivine, clinopyroxene,apatite and Fe-Ti oxides.Such mantle is not only different from the Palaeozoic refractory lithosphere,but also contrasts with the fertile one in Cenozoic.These complexes are similar in composition to other Early Cretaceous mafic-intermediate complexes from the southern margin of the North China Craton,implying the mantle source of the Rushan intrusion is tectonically affiliated to the southern wedge of the North China Craton.We infer that the Gongjia and Shangkou complexes formed in an extensional regime corresponding to the asthenosphere upwelling during gradual erosion and replacement of the cratonic mantle by the fertile lithosphere beneath the eastern North China Craton.
4.The petrographic and rock assemblages of the mafic xenoliths are not only different from that of the Archean or Proterozoic ultramafic bodies from the adjacent regions,but also contrast with the deep-seated xenoliths entrained in the Mesozoic diorites from the eastern North China Craton.On the contrary,the magmatic textures and similar elemental and isotopeic compositions to the host rocks demonstrate that the xenoliths were most probably represented high pressure fractionational products of the host magmas.The different major and trace element compositions of the four kinds of xenoliths indicate that they might form during the different evolutional periods of the magma intrusion.
5.For the Sanfoshan granites,we mainly focused on the Wangjiakou and Panjia monzonite granites,and Tongling alkali-granite.They were both emplaced in late Cretaceous(～110Ma),and display high-K calc-alkaline affinities,have high SiO_2,low FeO_t and MgO,with Na_2O/K_2O ratios lower than 1.They are enriched in LILE(such as Sr and Ba)and LREE,and with Sr and Nd isotopic compositions very closed to the nearest mantle derived igneous rocks such as the Gonajia complex and lamprophyres.These Cretaceous granitic rocks were formed by crustal-derived acid magma mixed with mantle originated basic magma,and the mixed magmas experienced minerals fractionation during their followed evolution.The concave-up chondrite-normalized REE patterns suggest that the precursor magma from a garnet-free source and the depletion of the MREE may be an indication of amphibole as residual in the melting source of the acid magma.These imply that the crust was thinned to a normal thickness and the lithospheric mantle thinning peaked around 110Ma underneath the studied regions.
6.The lithosphere evolution beneath the southern wedge of the eastern North China Craton during the Mesozoic to Cenozoic may have achieved in the following processes:The Early Mesozoic deep subduction of the Yangtze block at the southern part of the North China Craton destroyed the physical integrity of the North China lithosphere,and then triggered the thin of the North China lithosphere through thermo-mechanical erosion and chemical erosion caused by the asthenosphere upwelling.Those fluids and melts released from the subducted Yangtze slab would progressively migrate up,perturbate and metasomatize the overlying lithospheric mantle wedge and finally account for the formation of the highly enriched Mesozoic lithospheric mantle beneath the North China Craton.During the middle-late Jurassic,the pre-metasomatized enriched lithospheric mantle would begin to melt due to the upwelling of the hot asthenosphere,these mantle-derived magmas would underplate at the base of the lower crust or crust-mantle transition zone,causing the partial melting of the subducted Yangtze crust and giving the formation of the granitic rocks.The left-laeral strike-slip fault of the Tanlu fault in the Early Cretaceous triggered the strong upwelling of the asthenosphere,and simultaneously caused the intensive extension of the lithospheric mantle and crust,accompanied by splited apart of the lithosphere;the majority of the enriched lithospheric mantle was then considerably thinned by partial melting,these mantle-derived magmas may mixed with the crustal acid magmas and formed granitic rocks and certain environments.From late Cretaceous to Cenozoic,the oblique subduction of the pacific plate caused the oceanic crustal materials adequately mingled with the asthenosphere,and then the progresive asthenospheric cooling lowered the boundary between the lithosphere and the asthenosphere and created new oceanic-type lithospheric mantle.
1.宫家辉长—闪长岩和上口辉石闪长岩是分别位于乳山市东南部宫家村和东北部上口村的两个独立小岩体。宫家岩体从早到晚由中—细粒黑云母辉长岩、中—粗粒黑云母辉长岩、细粒黑云母辉石闪长岩和中—细粒黑云母辉石闪长岩构成,以细粒黑云母辉石闪长岩为主体。上口岩体出露不完整,仅见到偏中性的辉石闪长岩单元。宫家岩体中的基性岩石包体类型包括黑云母橄榄辉石岩、含长单斜辉石岩、单斜辉石岩及黑云母辉长岩等四种类型,以黑云母辉长岩为主,主要分布在第三期侵位的细粒黑云母辉石闪长岩之中。
2.宫家辉长—闪长岩中四个相带岩石的形成时代较接近,为114±1Ma～111±1Ma,上口辉石闪长岩的侵位结晶年龄为110.5±1Ma,它们同属早白垩世晚期岩浆活动的产物。宫家岩体中的黑云母橄榄辉石岩包体也获得了111.5±1Ma的~(206)pb/~(238)U加权平均年龄。
3.宫家辉长—闪长岩和上口辉石闪长岩均显示出高钾钙碱性—钾玄岩系列的特点,具有高Al_2O_3、低MgO,富集轻稀土、大离子亲石元素和Pb,强烈亏损Nb、Ta、Zr、Hf,Ti等高场强元素和类似EMII型地幔的Sr-Nd同位素组成,这些特征相似于华北东部南缘中生代幔源火成岩。宫家和上口岩体与富集的大陆岩石圈地幔在软流圈上涌的伸展背景下减压熔融有关,并伴随着橄榄石、单斜辉石、磷灰石及铁钛氧化物等矿物的分离结晶。其地幔源区以相对富单斜辉石的尖晶石相为主,深度小于80kin,并具有亲华北南缘的特点。该地幔源区不同于华北古生代金伯利岩中橄榄岩捕掳体所代表的以方辉橄榄岩为主的难熔型地幔,也与新生代碱性玄武岩中橄榄岩捕掳体指示的主元素饱满、同位素亏损的新生大洋型地幔有差别,是遭受了来自俯冲的扬子大陆板片释放的熔/流体交代改造而演化的产物,但改造程度弱于华北南缘早白垩世早期方城玄武岩和沂南辉长代表的岩石圈地幔,显示俯冲的扬子陆壳物质对上覆岩石圈地幔的交代改造自下而上是不均匀的。
4.宫家辉长—闪长岩中基性岩石包体的显微结构和岩石组合不同于邻区太古代或元古代超镁铁质岩块和华北克拉通东部中生代闪长岩中捕获的来自岩石圈地幔或壳幔过渡带的深源捕掳体。相反,它们具有的火成结构、与寄主岩相似的岩石化学和同位素组成,说明其成因与寄主岩浆在侵位上升时发生高压分异结晶或析离有关。四类包体各不相同的主元素、微量元素组成,显示其可能为寄主岩浆演化的不同阶段产物。
5.对三佛山花岗岩的研究主要集中在王家口和潘家含斑二长花岗岩和尚岭正长花岗岩,它们形成于早白垩世晚期(～110Ma),是一套高钾钙碱性系列的岩浆,具有高SiO_2、低FeO_t、MgO的特点,Na_2O/K_2O均小于1,富集轻稀土、大离子亲石元素(如Sr、Ba),Sr-Nd同位素组成与邻区幔源岩石十分接近。它们是早白垩世软流圈上涌和华北东部岩石圈减薄的伸展背景下古老的陆壳物质发生重熔,形成的酸性熔体与幔源岩浆混合后再经历分离结晶的演化产物。它们具有中稀土下凹、重稀土富集的稀土配分模式,表明酸性岩浆的熔融源区残留相以含有角闪石为特征,基本无加厚地壳的必要矿物相石榴子石,揭示～110Ma时该地区地壳已恢复到正常厚度,暗示此时的岩石圈减薄已达到峰期。
6.结合已有的研究成果和本文资料,华北克拉通东部南缘中—新生代岩石圈地幔演化的过程可能可以解释为:早中生代扬子大陆向华北深俯冲,破坏了华北南缘原有的地幔对流体系,加剧了软流圈的活动性能,引起岩石圈地幔的热—机械侵蚀和化学侵蚀减薄;苏鲁超高压变质带折返时释放的流体和俯冲板片熔融形成的硅质熔体不断地穿透并交代改造上覆华北古老岩石圈地幔楔,使之转变为高度富集的地幔;在中晚侏罗世时,软流圈继续抬升,引起原先的交代富集地幔熔融,形成的幔源岩浆或底侵在下地壳、壳幔过渡带,并同时诱发俯冲的扬子陆壳发生重熔形成花岗质岩浆;早白垩世郯庐断裂带的大幅左行平移走滑引起软流圈物质以郯庐断裂带为中心大幅上涌,导致上覆岩石圈地幔和地壳的强烈伸展,伴随岩石圈地幔的侧向挤出减薄,富集的岩石圈地幔同时发生大规模熔融而被消耗,岩石圈地幔减薄达到峰期,幔源岩浆同时烘烤地壳,诱使地壳发生重熔形成酸性岩浆,在合适的部位还形成壳幔混合花岗质岩浆。晚白垩世—新生代,太平洋板块快速向华北陆内斜向俯冲导致含深海远洋沉积物的俯冲洋壳软流圈发生混熔,加快了岩石圈地幔减薄,软流圈地幔于古近纪开始趋于冷却回沉,形成现今新生的大洋型地幔,实现对原有的富集型岩石圈地幔的置换。这一模式在华北东部南缘具有普遍意义。
The nature and evolution of the North China lithosphere have attracted many attentions in the past few years,because of considerable losing of the Archean keels during the Phanerozoic. Recent published data indicated that the Dabie-Sulu orogenic belt has become one of the most ideal regions for the studies on deep subduction of continental lithosphere,and its affections to the destruction of North China Craton.Mesozoic igneous rocks from the Dabie-Sulu orogenic belt are considered to be the products of subduction-induced and post-collisional extension-related magmatism and thus can provide constraints on the processes involved in the lithosphere evolution.In this paper,we present geochronological and geochemical investigations for the Gonajia and Shangkou intermediate-mafic intrusive complex,and their mafic xenoliths, as well as the coeval Sanfoshan granites from the northern Sulu orogen,with the aim of constraining the petrogenesis and origin of these rocks and mantle processes involved in their generation,and will further discuss the crust-mantle interaction that occurred underneath the collision zone and its implication for the lithosphere evolution.In addition,the evolution crust-mantle interaction occurred underneath the southern wedge of the North China lithosphere have also been discussed.
1.The Gongjia and Shangkou complexes are two independent small intermediate-mafic plutons that located at the southeastern and northeastern part of the Rushan city,respectively. The Gonajia complex comprises of four phases including(1)medium- to fine-grained biotite gabbro;(2)medium-grained biotite gabbro;(3)medium- to coarse-grained biotite gabbro;(4) fine-grained pyroxene-beafing diorite.The pyroxene-bearing diorite predominates in the outermost part of the Gongjia complex.The Shangkou pluton has relative poor occurrence and only the intermediate phase been found.Mafic xenoliths captured in the Gongjia complex include olivine-pyroxenite,plagioclase-bearing clinopyroxenite,clinopyroxenite and biotite-bearing gabbro,all of which mainly distributed in the third phase of the host rocks.
2.The Gongjia complex has rather uniform zircon U-Pb ages of 114±1Ma-111±1Ma, whereas the Shangkou pyroxene-bearing diorite has an emplacement age of 110.5±1Ma, indicating that they were both intruded in the late of the Cretaceous.Zircons extracted from an olivine-pyroxenite xenoliths give a weighted mean ~(206)pb/~(238)U age of 111.5±1 Ma.
3.The Gongjia and Shangkou complexes have high Al_2O_3 and low MgO,and show high-K calc-alkaline to shoshonitic affinities.They are highly enriched in large ion lithophile elements (LILE)and light rare earth elements(LREE),depleted in high field strength elements(HFSE) and Pb,and exhibit EMII-like Sr and Nd isotopes.These complex are interpreted to originate from decompression melting of spinel-facies cratonic mantle that metasomatized by the subducted Yangtze crustal materials and the melts experienced fractionation of olivine, clinopyroxene,apatite and Fe-Ti oxides.Such mantle is not only different from the Palaeozoic refractory lithosphere,but also contrasts with the fertile one in Cenozoic.These complexes are similar in composition to other Early Cretaceous mafic-intermediate complexes from the southern margin of the North China Craton,implying the mantle source of the Rushan intrusion is tectonically affiliated to the southern wedge of the North China Craton.We infer that the Gongjia and Shangkou complexes formed in an extensional regime corresponding to the asthenosphere upwelling during gradual erosion and replacement of the cratonic mantle by the fertile lithosphere beneath the eastern North China Craton.
4.The petrographic and rock assemblages of the mafic xenoliths are not only different from that of the Archean or Proterozoic ultramafic bodies from the adjacent regions,but also contrast with the deep-seated xenoliths entrained in the Mesozoic diorites from the eastern North China Craton.On the contrary,the magmatic textures and similar elemental and isotopeic compositions to the host rocks demonstrate that the xenoliths were most probably represented high pressure fractionational products of the host magmas.The different major and trace element compositions of the four kinds of xenoliths indicate that they might form during the different evolutional periods of the magma intrusion.
5.For the Sanfoshan granites,we mainly focused on the Wangjiakou and Panjia monzonite granites,and Tongling alkali-granite.They were both emplaced in late Cretaceous(～110Ma),and display high-K calc-alkaline affinities,have high SiO_2,low FeO_t and MgO,with Na_2O/K_2O ratios lower than 1.They are enriched in LILE(such as Sr and Ba)and LREE,and with Sr and Nd isotopic compositions very closed to the nearest mantle derived igneous rocks such as the Gonajia complex and lamprophyres.These Cretaceous granitic rocks were formed by crustal-derived acid magma mixed with mantle originated basic magma,and the mixed magmas experienced minerals fractionation during their followed evolution.The concave-up chondrite-normalized REE patterns suggest that the precursor magma from a garnet-free source and the depletion of the MREE may be an indication of amphibole as residual in the melting source of the acid magma.These imply that the crust was thinned to a normal thickness and the lithospheric mantle thinning peaked around 110Ma underneath the studied regions.
6.The lithosphere evolution beneath the southern wedge of the eastern North China Craton during the Mesozoic to Cenozoic may have achieved in the following processes:The Early Mesozoic deep subduction of the Yangtze block at the southern part of the North China Craton destroyed the physical integrity of the North China lithosphere,and then triggered the thin of the North China lithosphere through thermo-mechanical erosion and chemical erosion caused by the asthenosphere upwelling.Those fluids and melts released from the subducted Yangtze slab would progressively migrate up,perturbate and metasomatize the overlying lithospheric mantle wedge and finally account for the formation of the highly enriched Mesozoic lithospheric mantle beneath the North China Craton.During the middle-late Jurassic,the pre-metasomatized enriched lithospheric mantle would begin to melt due to the upwelling of the hot asthenosphere,these mantle-derived magmas would underplate at the base of the lower crust or crust-mantle transition zone,causing the partial melting of the subducted Yangtze crust and giving the formation of the granitic rocks.The left-laeral strike-slip fault of the Tanlu fault in the Early Cretaceous triggered the strong upwelling of the asthenosphere,and simultaneously caused the intensive extension of the lithospheric mantle and crust,accompanied by splited apart of the lithosphere;the majority of the enriched lithospheric mantle was then considerably thinned by partial melting,these mantle-derived magmas may mixed with the crustal acid magmas and formed granitic rocks and certain environments.From late Cretaceous to Cenozoic,the oblique subduction of the pacific plate caused the oceanic crustal materials adequately mingled with the asthenosphere,and then the progresive asthenospheric cooling lowered the boundary between the lithosphere and the asthenosphere and created new oceanic-type lithospheric mantle.
引文
[1]Liu D Y,Nutman A P,Compston W,et al.Remnants of 3800Ma crust in Chinese part of the Sino-Korean craton.Geology,1992,20:339-342
[2]Zheng J P,Griffin W L,O'Reilly S Y,et al.3.6Ga lower crust in central China:new evidence on the assembly of the North China Craton.Geology,2004,32:229-232
[3]Menzies M A,Fan W M & Zhang M.Paleozoic and Cenozoic lithoprobes and loss of＞120 km of Archaean lithosphere,Sino-Korean Craton,China.In:Prichard H M,Alabaster T,Harris N B W,et al(eds).Magmatic processes and plate tectonics.Geological Society of London,Special Publication no.76.1993,71-78
[4]Griffin W L,Zhang A,O'Reilly S Y,et al.Phanerozoic evolution of the lithosphere beneath the Sino-Korean Craton.In:Flower M,Chung S L,Lo C H,et al(eds).Mantle dynamics and plate interactions in East Asia.American Geophysical Union Geodynamics Series no.27.Washington D C,1998,107-126
[5]Menzies M A & Xu Y G.Geodynamics of the North China Craton.In:Flower M,Chung S L,Lo C H,et al(eds).Mantle dynamics and plate interactions in East Asia.American Geophysical Union Geodynamics Series no.27.Washington D C,1998,155-165
[6]Xu Y G,Menzies M A,Mattey D P,et al.The nature of lithospheric mantle near the Tancheng-Lujiang fault,China:an integration of texture,chemistry and O-isotopes.Chemical Geology,1996,134:67-81
[7]Fan W M,Zhang H F,Baker J,et al.On and offthe North China Craton:where is the Archean keel? Journal of Petrology,2000,41:933-950
[8]郑建平.中国东部地幔置换作用与中新生代岩石圈减薄.武汉:中国地质大学出版社,1999
[9]Gao S.Rudnick R L,Yuan H L,et al.Recycling lower continental crust in the North China Craton.Nature,2004,432:892-897
[10]Deng J F,Mo X X,Zhao H L,et al.2004.A new model for the dynamic evolution of Chinese lithosphere:'continental roots-plume tectonics'.Earth-Science Reviews,2004,65:223-275
[11]Deng J F,Su S G,Niu Y L,et al.A possible model for the lithospheric thinning of North China Craton:evidence form the Yanshanian(Jura-Cretaceous)magmatism and tectonism.Lithos,2007,96:22-35
[12]邓晋福,莫宣学,赵海玲,等.中国东部岩石圈根/去根作用与大陆“活化”-东亚型大陆动力学模式研究计划.现代地质,1994,8(3):349-356
[13]邓晋福,赵海玲,莫宣学,等.中国大陆根柱构造-大陆动力学的钥匙.北京:地质出版社,1996,33-34
[14]吴福元,葛文春,孙德有,等.中国东部岩石圈减薄研究中的几个问题.地学前缘,2003,10(3):51-60
[15]吴福元,孙德有.中国东部中生代岩浆作用与岩石圈减薄.长春科技大学学报,1999,29(4):313-318
[16]Xu Y G.Thermo-tectonic destruction of the Archean lithospheric keel beneath the Sino-Korean Craton in China:evidence,timing and mechanism.Physics and Chemistry of the Earth(A),2001,26(9-10):747-757
[17]Zheng J p,O'Reilly S Y,Griffin W L,et al.Nature and evolution of Cenozoic lithospheric mantle beneath Shandong peninsula,Sino-Korean craton.International Geology Review,1998,40:471-499
[18]Zheng J P,Griffin W L,O'Reilly S Y,et al.Late Mesozoic-Eocene mantle replacement beneath the eastern North China Craton:evidences from the Paleozoic and Cenozoic peridotite xenoliths.International Geology Review,2005,47:457-472
[19]Zheng J P,Griffin,W L,O'Reilly,S Y,et al.Mineral chemistry of peridotites from Paleozoic,Mesozoic and Cenozoic lithosphere:constraints on mantle evolution beneath eastern China.Journal of Petrology,2006,47(11):2233-2256
[20]Gao S,Rudnick R L,Carlson R W,et al.Re-Os evidence for replacement of ancient mantle lithosphere beneath the North China craton.Earth and Planetary Science Letters,2002,198:307-322
[21]张宏福,英基丰,徐平,等.华北中生代玄武岩中地幔橄榄石捕虏晶:对岩石圈地幔置换过程的启示.科学通报,2004,49(8):784-789
[22]Xu Y G,Huang X L,Ma J L,et al.Crust-mantle interaction during the tectono-thermal reactivation of the North China Craton:constraints from SHRIMP zircon U-Pb chronology and geochemistry of Mesozoic plutons from western Shandong.Contribution to Mineralogy and Petrology,2004,147:750-767
[23]翟明国,朱日祥,刘建明,等.华北东部构造体制转折的关键时限.中国科学(D辑),2003,33(10):913-920
[24]Zhang H F,Sun M,Zhou X H,et al.Mesozoic lithosphere destruction beneath the North China Craton:evidence from major-,trace-element and Sr-Nd-Pb isotope studies of Fangcheng basalts.Contribution to Mineralogy and Petrology,2002,144:241-253
[25]Zhang H F,Sun M,Zhou X H,et al.Secular evolution of the lithosphere beneath the eastern North China Craton:Evidence from Mesozoic basalts and high-Mg andesites.Geochimica et Cosmochimica Acta,2003,67(22):4373-4387
[26]许文良,王冬艳,高山,等.鲁西中生代金岭闪长岩中纯橄岩和辉石岩包体的发现及其意义.科学通报,2003,48(8):863-868
[27]许文良,王冬艳,王清海,等.鲁西中生代闪长岩中两类幔源捕虏体的岩石学和地球化学.岩石学报,2003,19(4):623-636
[28]Zheng J P,Griffin,W L,O'Reilly,S Y,et al.Mechanism and timing of lithospheric modification and replacement beneath the eastern North China Craton:Peridotitic xenoliths from the 100 Ma Fuxin basalts and a regional synthesis.Geochimica et Cosmochimica Acta,2007,71(21):5203-5225
[29]张宏福,郑建平.华北中生代玄武岩的地球化学特征与岩石成因:以辽宁阜新为例.科学通 报,2003,48(6):603-609
[30]裴福萍,许文良,王清海,等.鲁西费县中生代玄武岩及幔源捕虏晶的矿物化学:对岩石圈地幔性质的制约.高校地质学报,2004,10(1):88-97
[31]闫峻,陈江峰,谢智,等.鲁东晚白垩世玄武岩中的幔源捕虏体:对中国东部岩石圈减薄时间制约的新证据.科学通报,2003,48(14):1570-1574
[32]Ying J F,Zhang H F,Noriko K,et al.Nature and evolution of Late Cretaceous lithospheric mantle beneath the eastern North China Craton:Constraints from petrology and geochemistry of peridotitic xenoliths from Jünan,Shandong province,China.Earth and Planetary Science Letters,2006,244:622-638
[33]Zheng J P,Sun M,Zhou M F,et al.Trace elemental and PGE geochemical constraints of Mesozoic and Cenozoic peridotitic xenoliths on lithospheric evolution of the North China Craton.Geochimica et Cosmochimica Acta,2005,69(13):3401-3418
[34]黄福生,薛绥洲.邢邯侵入体中幔源超镁铁质岩包体的发现及其矿物地球化学特征.岩石学报,1990,4:40-45
[35]许文良,林景仟.河北邢邯地区角闪闪长岩中地幔纯橄岩包体的发现与研究.地质学报,1991,1:33-41
[36]Chen L H,Zhou X H.Subduction-related metasomatism in the thinning lithosphere:evidence from a composite dunite-orthopyroxenite xenoliths entrained in Mesozoic Laiwu high-Mg diorite,North China.Geochemistry,Geophysics,Geosystems,2005,6(6),doi:10.1029/2005GC000938
[37]陈立辉,周新华,2003.鲁西中生代闪长岩中的深源超镁铁质岩捕虏体及其富硅交代特征.中国科学(D辑),33(8):735-744
[38]许文良,王冬艳,王清海,等.鲁西纯橄岩捕虏体中富硅质熔(流)体的交代作用:对中生代岩石圈地幔减薄的意义.地质学报,2004,78(1):72-80
[39]张瑾,张宏福,英基丰,等.华北晚中生代中基性侵入岩中橄榄岩捕虏体是岩石圈地幔直接样品?岩石学报,2005,21(6):1559-1568
[40]支霞臣,孟庆,许文良,等.鲁西铁铜沟中生代闪长岩中橄榄岩包体代表SCLM吗?-Re-Os同位素体系启示.2004年全国岩石学与地球动力学研讨会摘要(海口),407-409
[41]Xu Y G,Ma J L,Huang X L,et al.Early Cretaceous gabbroic complex from Yinan,Shandong Province:petrogenesis and mantle domains beneath the North China Craton.International Journal of Earth Science,2004,93:1025-1041
[42]徐义刚.华北岩石圈减薄的时空不均一特征.高校地质学报,2004,10(3):324-331
[43]Wu F Y,Lin J Q,Wilde S A,et al.Nature and significance of the Early Cretaceous giant igneous event in eastern China.Earth and Planetary Science Letters,2005,233:103-119
[44]许文良,王清海,王冬艳,等.华北克拉通东部岩石圈减薄的过程与机制:中生代火成岩和深源捕虏体证据.地学前缘,2004,11(3):309-317
[45]许文良,王冬艳,王清海,等.华北地块中东部中生代侵入杂岩中角闪石和黑云母的~(40)Ar/~(39)Ar 定年:对岩石圈减薄时间的制约.地球化学,2004,33(3):221-231
[46]王晓蕊,高山,柳小明,等.辽西四合屯早白垩世义县组高镁安山岩的地球化学:对下地壳拆沉作用和Sr/Y变化的指示.中国科学(D辑),2005,35(8):700-709
[47]Zhang H F,Sun M,Zhou X H,et al.Geochemical constraints on the origin of Mesozoic alkaline intrusive complexes from the North China Craton and tectonic implications.Lithos,2005,81:297-317
[48]Fan W M,Guo F,Wang Y J,et al.Post-Orogenic bimodal volcanism along the Sulu orogenic belt in eastern China.Physics and Chemistry of the Earth(A),2001,26(9-10):733-746
[49]Guo F,Fan W M,Wang Y J,et al.Origin of early Cretaceous talc-alkaline lamprophyres from the Sulu orogen in eastern China:implications for enrichment processes beneath continental collisional belt.Lithos,2004,78:291-305
[50]Guo F,Fan W M,Wang Y J,et al.Late Mesozoic mafic intrusive complexes in North China Block:constraints on the nature of subcontinental lithospheric mantle.Physics and Chemistry of the Earth(A),2001,26(9-10):759-771
[51]Ying J F,Zhou X H,Zhang H F.Geochemical and isotopic investigation of the Lalwu-Zibo carbonatites from western Shandong province,China and implications for their petrogenesis and enriched mantle source.Lithos,2004,75:413-426
[52]Ying,J F,Zhou,X H,Zhang H F.The geochemical variations of mid-Cretaceous lavas across western Shandong province,China and their tectonic implications.International Journal of Earth Science,2006,95:68-79
[53]Yang J H,Chung S L,Zhai M G,et al.Geochemical and Sr-Nd-Pb isotopic compositions of mafic dikes from the Jiaodong peninsula,China:evidence for vein-plus-peridotite melting in the lithospheric mantle.Lithos,2004,73:145-160
[54]邱检生,徐夕生,罗清华.鲁西富钾火山岩和煌斑岩的~(40)Ar-~(39)Ar定年及源区示踪.科学通报,2001,46(18):1500-1508
[55]杨进辉,朱美妃,刘伟,等.胶东地区郭家岭花岗闪长岩的地球化学特征及成因.岩石学报,2003,19(4):692-700
[56]袁洪林,柳小明,刘勇胜,等.北京西山晚中生代火山岩U-Pb锆石年代学及地球化学研究.中国科学(D辑),2005,35(9):821-836
[57]杨承海,许文良,杨德彬,等.鲁西中生代高Mg闪长岩的成因:年代学与岩石地球化学证据.地球科学-中国地质大学学报,2006,31(1):81-92
[58]Chen B,Jahn B M,Arakawa Y,et al.Petrogenesis of the Mesozoic intrusive complexes from the southern Taihang orogen,North China Craton:elemental and Sr-Nd-Pb isotopic constraints.Contribution to Mineralogy and Petrology,2004,148:489-501
[59]Chen B,Zhai M G.Geochemistry of late Mesozoic lamprophyre dykes from the Taihang Mountains,North China,and implications for the sub-continental lithospheric mantle.Geological Magazine,2003,140:87-93
[60]Wang Y J,Fan W M,Zhang H F,et al.Early Cretaceous gabbroic rocks from the Taihang Mountains:implications for a paleosubduction-related lithospheric mantle beneath the central North China Craton.Lithos,2006,86:281-302
[61]陈斌,田伟,翟明国,等.太行山和华北其它地区中生代岩浆作用的锆石U-Pb年代学和地球化学特征及其岩浆成因和地球动力学意义.岩石学报,2005,21(1):13-24
[62]陈斌,翟明国,邵济安.太行山北段中生代岩基的成因和意义:主要和微量元素地球化学证 据.中国科学(D辑),2002,32(11):896-907
[63]蔡剑辉,阎国翰,肖成东,等.太行山大兴安岭构造岩浆带中生代侵入岩Nd、Sr、Pb同位素特征及物质来源探讨.岩石学报,2004,20(5):1225-1242
[64]彭头平,王岳军,范蔚茗,等.南太行山闪长岩的SHRIMP锆石U-Pb年龄及岩石成因研究.岩石学报,2004,20(5):1253-1262
[65]张旗,钱七,王二七,等.燕山中晚期的“中国东部高原”:埃达克岩的启示.地质科学,2001,36(2):248-255
[66]张旗,王焰,钱青,等.中国东部晚中生代埃达克岩的特征及其构造-成矿意义.岩石学报,2001,17(2):236-244
[67]张旗,王焰,王云龙,等.燕山期中国东部高原下地壳组成初探:埃达克质岩Sr、Nd同位素制约.岩石学报,2001,17(4):505-513
[68]葛晓月,李献华,陈志刚,等.中国东部燕山期高Sr低Y型中酸性火成岩的地球化学特征及成因:对中国东部地壳厚度的制约.科学通报,2002,47(6):474-480
[69]Chen B,Jahn B M,Wei C J.Petrogenesis of Mesozoic granitoids in the Dabie UHP complex,central China:trace element and Nd-Sr isotope evidence.Lithos,2002,60:67-68
[70]张华锋,翟明国,何中甫,等.胶东昆嵛山杂岩中高锶花岗岩地球化学成因及其意义.岩石学报,2004,20(3):369-380
[71]Bird P.Initiation of intracontinental subduction in the Himalayas.Journal of Geophysics Research.1978.83(B10):4975-4987
[72]郑建平,孙敏,路凤香,等.信阳基性麻粒岩捕掳体及其华北南缘早中生代下地壳性质.岩石学报,2005,21(1):91-98
[73]Zhai M G,Fan Q C,Zhang H F,et al.Lower crustal processes leading to Mesozoic lithospheric thinning beneath eastern North China:underplating,replacement and delamination.Lithos,2007,96:36-54
[74]Wang K L,O'Reilly S Y,Griffin W L,et al.Proterozoic mantle lithosphere beneath the extended margin of the south China Block:In situ Re-Os evidence.Geology,2003,31(8):709-712
[75]Wu F Y,Walker R J,Ren X W,et al.Osmium isotopic constraints on the age of lithospheric mantle beneath Northeastern China.Chemical Geology,2003,196:107-129
[76]高山,Rudnick R L,Carlson R W,et al.华北克拉通岩石圈地幔置换作用和壳幔生长耦合的Re-Os同位素证据.地学前缘,2003,10(3):61-67
[77]支霞臣,彭子成,陈道公,等.苏皖地区大陆岩石圈地幔的长时性-地幔橄榄岩捕虏体的锇同位素模式年龄.中国科学(D辑),2001,31(6):464-470
[78]支霞臣,彭子成,陈道公,等.苏皖地区幔源橄榄岩捕虏体的锇同位素组成、模式年龄及其意义.岩石学报,2001,17(1):11-18
[79]支霞臣,秦协.中国东部地幔橄榄岩捕虏体的Re-Os同位素地球化学:岩石圈地幔的形成年龄和减薄作用的制约.岩石学报,2004,20(5):989-998
[80]余淳梅,郑建平,Griffin W L.汉诺坝橄榄岩捕掳体原位Re-Os同位素年龄与多发地幔事件.科学通报,2007,31(1):93-100
[81]Robinson P T,Zhou M F,Hu X F,et al.Geochemical constraints on the origin of the Hegenshan ophiolite,Inner Mongolia,China.Journal of Asian Earth Sciences,1999,17:423-442
[82]Zhang H F,Ying J F,Shimoda G,et al.Importance of melt circulation and crust-mantle interaction in the lithospheric evolution beneath the North China Craton:evidence from Mesozoic basalts-borne clinopyroxene xenocrysts and pyroxenite xenoliths.Lithos,2007,96:67-89
[83]邱检生,胡建,蒋少涌,等.鲁西中新生代镁铁质岩浆作用与地幔化学演化.地球科学-中国地质大学学报,2005,30(6):646-658
[84]姜耀辉,蒋少涌,赵葵东,等.辽东半岛煌斑岩SHRIMP锆石U-Pb年龄及其对中国东部岩石圈减薄开始时间的制约.科学通报,2005,50(19):2161-2168
[85]邓晋福,苏尚国,赵海玲,等.华北地区燕山期岩石圈减薄的深部过程.地学前缘,2003,10(3):41-50
[86]邓晋福,苏尚国,刘翠,等.关于华北克拉通燕山期岩石圈减薄的机制与过程的讨论:是拆沉,还是热侵蚀和化学交代?地学前缘,2006,13(2):105-119
[87]张宏福,周新华,范蔚茗,等.华北东南部中生代岩石圈地幔性质、组成、富集过程及其形成机理.岩石学报,2005,21(4):1271-1280
[88]Zhang H F,Sun M,Zhou M F,et al.Highly heterogeneous late Mesozoic lithospheric mantle beneath the North China Craton:evidence from Sr-Nd-Pb isotopic systematics of mafic igneous rocks.Geological Magazine,2004,141:55-62
[89]Zhang H F.Transformation of lithospheric mantle through peridotite-melt reaction:a case of Sino-Korean craton.Earth and Planetary Science Letters,2005,237:768-780
[90]Wang X M,Liou J G,Mao H K.Coesite-bearing eclogites from the Dabie Mountains in central China.Geology,1989,17:1085-1088
[91]Okay A I,Xu S T,Sengor A M C.Coesite from the Dabie Shan eclogites,central China.European Journal of Mineralogy,1989,1:595-598
[92]Hirajima T,Ishiwatari A,Cong B L,et al.Coesite from Mengzhong eclogite at Donghai County,northeastern Jiangsu Province,China.Mineralogy Magazine,1990,54:579-583
[93]Xu S T,Okay A I,Ji S Y,et al.Diamond from the Dabie Shan metamorphic rocks and its implication for tectonic setting.Science,1992,256:80-92
[94]Brueckner H K & Medaris L G.A general model for the intrusion and evolution of "mantle"garnet peridotites in high-pressure and ultra-high-pressure metamorphic terranes.Journal of Metamorphic Geology,2000,18(2):123-133
[95]Yang J J.Titanian clinohumite-gamet-pyroxene rock from the Sulu UHP metamorphic terran,China:chemical evolution and tectonic implications.Lithos,2003,70:359-379
[96]Yang J J & Jahn B M.Deep subduction of mantle-derived garnet peridotites from the Sulu UHP metamorphic terran in China.Journal of Metamorphic Geology,2000,18:167-180
[97]Zhang R Y,Liou J G,Zheng J P,et al.Petrogenesis of the Yangkou layered gamet-peridotite complex,Sulu UHP terrane,China.American Mineralogist,2005,90:801-813
[98]Zhang R Y,Liou J G,Yang J S,et al.Petrochemical constraints for dual origin of garnet peridotites from the Dabie-Sulu UHP terrane,eastern-central China.Journal of Metamorphic Geology,2000,18(2):149-166
[99]Zhang R Y,Liou J G,Yang J S,et al.Ultrahigh-pressure metamorphism in the forbidden zone:the Xugou garnet peridotite,Sulu terrane,eastern China.Journal of Metamorphic Geology,2003,21(6):1-12
[100]Fan W M,Guo F,Wang Y J,et al.Late Mesozoic volcanism in the northern Huaiyang tectono-magmatic belt,central China:partial melts from a lithospheric mantle with subducted continental crust relicts beneath the Dabie orogen? Chemical Geology,2004,209:27-48
[101]Wang Y J,Fan W M,Peng T P,et al.Natrue of the Mesozoic lithospheric mantle and tectonic decoupling beneath the Dabie orogen,central China:evidence from ~(40)Ar/~(39)Ar geochronology,elemental and Sr-Nd-Pb isotopic compositions of early Cretaceous mafic igneous rocks.Chemical Geology,2005,220:165-189
[102]Zheng J P,Griffin W L,O'Reilly S Y,et al.A refractory mantle protolith in younger continental crust,eastern China:Age and composition of zircon in the Sulu ultrahigh-pressure peridotite.Geology,2006,34(9):705-708
[103]Zheng J P,Zhang R Y,Griffin W L,et al.Heterogeneous and metasomatised mantle recorded by trace elements in minerals of the Donghai garnet peridotites,Sulu UHP terrane,China.Chemical Geology,2005,221:243-259
[104]Huang F,Li S G,Dong F,et al.Recycling of deeply subducted continental crust in the Dabie Mountains,central China.Lithos,2007,96:151-169
[105]Jahn B M,Wu F Y,Ching H L,et al.Crust-mantle interaction induced by deep subduction of the continental crust:geochemical and Sr-Nd isotopic evidence from post-collisional mafic-ultramafic intrusions of the north Dabie complex,central China.Chemical Geology,1999,157:119-146
[106]Ma C Q,Ehlers C,Xu C H,et al.The roots of the Dabieshan ultrahigh-pressure metamorphic terrane:constraints from geochemistry and Nd-Sr isotope systematics.Precambrian Research,2000,102:279-301
[107]Zhang H F,Gao S,Zhong Z Q,et al.Geochemical and Sr-Nd-Pb isotopic compositions of Cretaceous granitoids:constraints on tectonic framework and crustal structure of the Dabieshan ultrahigh-pressure metamorphic belt,China.Chemical Geology,2002,186:281-299
[108]Yang J H,Chung S L,Wilde S A.Petrogenesis of post-orogenic syenites in the Sulu orogenic belt,eastern China:geochronological,geochemical and Nd-Sr isotopic evidence.Chemical Geology,2005,214:99-125
[109]Yang J H,Wu F Y,Chung S L,et al.Petrogenesis of early Cretaceous intrusions in the Sulu ultrahigh-pressure orogenic belt,eastern China and their relationship to lithospheric thinning.Chemical Geology,2005,222:200-231
[110]黄洁,郑永飞,吴元保,等.苏鲁造山带五莲地区岩浆岩元素和同位素地球化学研究.岩石学报,2005,21(3):545-568
[111]高天山,陈江峰,谢智,等.苏鲁超高压变质带中三叠纪石岛杂岩体的地球化学研究.岩石学报,2004,20(5):1025-1038
[112]周建波,郑永飞,吴元保.苏鲁造山带西北缘五莲花岗岩中锆石U-Pb年龄及其地质意义.科学通报,2002,47(22):1745-1750
[113]胡芳芳,范宏瑞,杨进辉,等.胶东文登长山南花岗闪长岩体的岩浆混合成因:闪长质包体及寄主岩石的地球化学、Sr-Nd同位素和锆石Hf同位素证据.岩石学报,2005,21(3):569-586
[114]张华锋,翟明国,童英,等.胶东半岛三佛山高Ba-Sr花岗岩成因.地质论评,2006,52(1):43-53
[115]魏春景,张立飞,王式洗.安徽省大别山东段中生代高钾花岗质岩石及其地质意义.中国科学(D辑),2000,30(4):355-363
[116]王德滋,王赐银,于津海.昆嵛山混合杂岩体的地质特征及成因.南京大学学报,1989,25(4):679-688
[117]徐金芳,沈步云,牛良柱,等.胶北地块与金矿有关的花岗岩类研究.山东地质,1989,5(2):1-25
[118]于津海.胶东东部昆嵛山混合杂岩体的形成时代及成因.地质论评,1989,35(4):285-296
[119]徐景奎,杨忠芳,赵伦山,等.胶东昆嵛山复式花岗岩体的地质地球化学研究.长春地质学院学报,1991,21(2):167-174
[120]张德全,徐洪林,孙桂英.山东邓格庄金矿与昆嵛山花岗岩的定位时代及其地质意义.地质论评,1995,41(5):415-425
[121]徐洪林,张德全,孙桂英.胶东昆嵛山花岗岩的特征、成因及其与金矿的关系.岩石矿物杂志,1997,16(2):131-143
[122]杨进辉.胶东地区金矿成矿时代及其成矿地球动力学背景.兼论壳幔相互作用与成岩成矿.[博士学位论文],北京:中国科学院地质与地球物理研究所,2000,1-133
[123]陈光远,孙岱生,邵岳.胶东昆嵛山二长花岗岩副矿物成因矿物学研究.现代地质,1996,10(2):175-186
[124]郭敬辉,陈福坤,张晓曼,等.苏鲁超高压带花岗岩类成因与碰撞后构造过程:锆石U-Pb年代学和地球化学研究.见:从柏林,翟明国,郭敬辉,等编.大陆的俯冲、拆离和减薄作用学术研讨会论文摘要集.西安:西北大学,2001,99-102
[125]郭敬辉,陈福坤,张晓曼,等.苏鲁超高压带北部中生代岩浆侵入活动与同碰撞.碰撞后构造过程:锆石U-Pb年代学.岩石学报,2005,21(4):1281-1301
[126]孟繁聪,薛怀民,李天福,等.苏鲁造山带晚中生代地幔的富集特征-来自辉长岩的地球化学证据.岩石学报,2005,21(6):1583-1592
[127]胡芳芳,范宏瑞,杨进辉,等.鲁东昆嵛山地区宫家辉长.闪长岩成因:岩石地球化学、锆石U-Pb年代学与Hf同位素制约.岩石学报,2007,23(2):369-380
[128]Zhao G C,Cawood P A,Wilde S A,et al.Metamorphism of basement rocks in the Central Zone of the North China Craton:implications for Paleoproterozoic tectonic evolution.Precambrian Research,2000,103:55-88
[129]Zhao G C,Wilde S A,Cawood P A,et al.Archean blocks and their boundaries in the North China Craton:lithological,geochemical,structural and P-T path constraints and tectonic evolution.Precambrian Research,2001,107:45-73
[130]Zhao G C,Wilde S A,Cawood P A,et al.Thermal evolution of two texrural types of mafic granulites in the North China Craton:evidence for both mantle plume and collisional tectonics.Geological Mmagazine,1999,136:223-240
[131]赵国春,孙敏.华北克拉通基底构造单元特征及早元古代拼合.中国科学(D辑),2002,32(7):538-549
[132]Sun M,Armstrong R L,Lambert R S J.Petrochemistry and Sr,Pb and Nd isotopic geochemistry of Early Precambrian rocks,Wutaishan and Taihangshan areas,China.Precambrian Research,1992,56:1-31
[133]陈国英,宋仲和,安昌强,等.华北地区三维地壳上地幔地幔结构.地球物理学报,1991,34(2):172-181
[134]Zheng J P,O'Reilly S Y,Griffin W L,et al.Relict refractory mantle beneath the eastern North China block:significance for lithosphere evolution.Lithos,2001:57:43-66
[135]林景迁,谭冬娟,迟效国,等.胶辽半岛中生代花岗岩.北京:科学出版社,1992,17-23,72-88
[136]路孝平,吴福元,赵成弼,等.通化地区印支期花岗岩锆石U-Pb年龄及其与大别-苏鲁超高压带碰撞造山作用之间的关系.科学通报,2003,48(8):843-849
[137]许文良,王清海,杨德彬,等.蚌埠荆山“混合花岗岩"SHRIMP锆石U-Pb定年及其地质意义.中国科学(D辑),2004,34(5):423-428
[138]许文良,王冬艳,刘晓春,等.徐淮地区早侏罗世侵入杂岩体中榴辉岩类包体的发现及其地质意义.科学通报,2002,47(8):618-622
[139]杨进辉,朱美妃,刘伟,等.胶东地区郭家岭花岗闪长岩的地球化学特征及成因.岩石学报,2003,19(4):692-700
[140]陈立辉.山东莱芜中生代高镁侵入岩及其超镁铁质岩捕掳体的成因研究.[博士学位论文],北京:中国科学院地质与地球物理研究所,2001,9-12
[141]刘若新,陈文寄,孙建中,等.中国新生代火山岩的K-Ar年代学与构造环境.见:刘若新主编.中国新生代火山岩年代学与地球化学.北京:地震出版社,1992,1-43
[142]曹国权.试论“胶南地体”.山东地质,1990,5(2):1-10
[143]丛源.胶东西北部北截-大河一带造山型金矿的地质特征及狂化富集规律.[硕士学位论文],长春:吉林大学,2005,6-18
[144]Ishizaka K,Hirazima T & Zheng X S.Rb-Sr dating for the Jiaodong gneiss of the Su-lu ultrahigh-high pressure province,eastern China.The Island Arc,1994,3:232-241
[145]王仁民,安家桐,赖兴远.胶东蛇绿岩套的发现及其地质意义.岩石学报,1995,11:221-240
[146]张希道,王来明.胶东威海-乳山麻粒岩相岩石的发现及初步研究.中国区域地质,1996,58(3):213-221
[147]王清晨,从柏林.大别山超高压变质岩的地球动力学意义.中国科学(D辑),1996,26(3):271-276
[148]Yin A,Nie S.An indentation model for the North and South China collision and the development of the Tan-Lu and Honam fault systems,eastern Asian.Tectonics,1993,12(4):801-813
[149]Zhai M G,Liu W J.The boundary between Sino-Korea craton and Yangtze craton and its extension to the Korea peninsula.In:Jang B A,Cheong D K.(eds),Crustal evolution in Northeast Asia.Kangweon National University,Chuncheon,1997,18-27
[150]Zhai M G,Cong B L,Guo J H,et al.Sm-Nd geochronology and petrography of garnet pyroxene granulites in the northern Sulu region of China and their geotectonic implication.Lithos,2000,52:23-33
[151]宋明春,王来明.对胶南造山带基础地质问题的新认识.中国区域地质,2000,19(1):1-6
[152]王来明,王世进,张富中.2001年山东省地质调查工作进展和主要成果.山东地质,2001,17(6):1-6
[153]Wallis S,Enami M & Banno S.The Sulu UHP terrane:A review of the petrology and structural geology.International Geology Review,1999,41:906-920
[154]李永刚,郭敬辉,翟明国,等.胶东地区基底长英质片麻岩的地球化学特征及其构造归属.岩石学报,1999,15(4):557-563
[155]许志琴,戚学详,杨经绥,等.苏鲁高压-超高压变质地体的陆-陆碰撞深俯冲剥蚀模式.地球科学-中国地质大学学报,2006,31(4):427-436
[156]杨敏之,吕古贤.胶东绿岩带金矿地质地球化学.北京:地质出版社,1996
[157]王来明,鄢毅民.山东栖霞地区太古宙英云闪长岩的地球动力学意义,山东地质,1992,1:80-87
[158]李兆龙,杨敏之,胶东金矿床地质地球化学.天津,天津科学技术出版社,1993
[159]张田,张岳桥.胶东半岛中生代侵入岩浆活动序列及其构造制约.高校地质学报,2007,13(2):323-336
[160]Chen J F,Xie Z,Li H M,et al.U-Pb zircon ages for a collision-related K-rich complex at Shidao in the Sulu ultrahigh pressure terrane,China.Geochemical Journal,2003,37:35-46
[161]罗振宽,关康,苗来成,等.胶东招掖地区与金矿化有关花岗岩继承锆石年龄及其意义.地球学报,1997,18:138-141
[162]关康,罗振宽,苗来成,等.胶东招掖郭家岭型花岗岩锆石SHRIMP年代学研究.地质科学,1998,33(3):318-328
[163]王德滋,赵广涛,邱检生.中国东部晚中生代A型花岗岩的构造制约.高校地质学报,1995,1(2):13-20
[164]孙景贵,胡受奚,凌洪飞.胶东金矿区高钾-钾质脉岩地球化学与俯冲-壳幔作用研究.岩石学报,2000,16(3):401-412
[165]Li S G,Xiao T L,Liou D L,et al.Collision of the North China and Yangtze Blocks and formation of coesite-bearing eclogite:Timing and processes.Chemical Geology,1993,109:89-111
[166]Li S G,Jagoutz E,Chen Y,et al.Sm-Nd and Rb-Sr isotopic chronology and cooling history of ultrahigh pressure mtamorphic rocks and their country rocks at Shuanghe in the Dabie Mountains,Central China.Geochimica et Cosmochimica Acta,1999,64(6):1077-1093
[167]Hacker B R,Wang Q C.Ar/Ar geochronology of ultrahigh-pressure metamorphism in central China.Tectonics,1995,14:994-1006
[168]Zhang R Y,Hirajima T,Banno S,et al.Petrology of ultrahigh-pressure metamorphic rocks in southern Sulu region,eastern China.Journal of Metamorphic Geology,1995,13:659-75
[169]Hirajima T,Zhang R Y,Li J J.Nyboite from the Donghai area,Jiangsu province,eastern China.Mineralogy Magazine,1992,56:37-46
[170]Chavagnac V & Jahn B M.Coesite-bearing eclogites from the Bixiling complex,Dabie mountains,China:Sm-Nd ages,geochemical characteristics and tectonic implications.Chemical Geology,1996,133:29-51
[171]Li S G,Huang F,Nie Y H,et al.Geochemical and geochronological constraints on the structure location between the North and and South China blocks in the Dabie orogen,central China.Physics and Chemistry of the Earth(A),2001,26(9-10):655-672
[172]Hacker B,Ratschbacher L,Webb L,et al.U/Pb zircon ages constrain the architecture of the ultrahigh-pressure Qinling-Dabie orogen,China.Earth and Planetary Science Letters,1998,161:215-30
[173]Liu F L,Xu Z Q & Xue H M.Tracing the protolith,UHP metamorphism,and exhumation ages of orthogneiss from the SW Sulu terrane(eastern China):SHRIMP U-Pb dating of mineral inclusion-bearing zircons.Lithos,2004,78:411-29
[174]Ye K,Cong B L & Ye D N.The possible subduction of continental material to depths greater than 200 km.Nature,2000,407:734-36
[175]金振民,金淑燕,高山,等.大别山超高压岩石形成深度局限于100-150km吗?科学通报,1998,43:767-771
[176]叶凯,平岛崇男,石渡明,等.青岛仰口榴辉岩中粒间柯石英的发现及其意义.科学通报,1996,41(15):1407-1408
[177]Cong B L.Ultrahigh-pressure metamorphic rocks in the Dabieshan-Sulu region of China.Science Press,Beijing,1996,224
[178]Wang Q C,Ishiwateri A,Zhao Z U,et al.Coesite-bearing granulite retrograded from eclogite in Weihai,eastern China.Journal of Mineralogy,1993,5:141-152
[179]Zheng Y F,Fu B,Gong B L,et al.Stable isotope geochemistry of ultrahigh pressure metamorphic rocks from the Dabie-Sulu orogen in China:Implications for geodynamics and fliud regime.Earth Science Review,2003,62:105-161
[180]Xu J W,Zhu G,Tong W X,et al.Formation and evolution of the Tancheng-Lujiang wrench fault system:A major shear system to the northwest of the Pacific Ocean.Tectonophysics,1987,134:273-310
[181]刘福来,许志琴,宋彪.苏鲁超高压变质带中非超高压花岗质片麻岩的准确识别:来自锆石微区矿物包体及SHRIMP U-Pb定年的证据.地质学报,2003,77(4):534-540
[182]刘福来,许志琴,宋彪.苏鲁地体超高压和退变质时代的厘定:来自片麻岩锆石微区SHRIMP U-Pb定年的证据.地质学报,2003,77(2):229-239
[183]杨经绥,许志琴,刘福来,等.含柯石英锆石的SHRIMP U-Pb定年:胶东印支超高压变质作用的证据.地质学报,2002,76(3):354-371
[184]Zhang R Y,Liou J G,Ernst W C.Ultrahigh-pressure metamorphism and decompressional P-T paths of eclogites and country rocks from Weihai,eastern China.The Island Arc,1995,4:293-309
[185]山东地质矿产局.山东省区域地质志.北京:地质出版社,1991,1-274
[186]Ludwig K R.ISOPLOT 3.00:A Geochronological Toolkit for Mi-crosoft Excel.Berkeley Geochronology Center Special Publication no.4,2003,1-70
[187]王岳军,范蔚茗,郭锋,等.北大别晚中生代火山岩的地球化学特征及对北大别构造属性的 启示.地学前缘,2003,10(4):529-538
[188]Rickwood P C.Boundary lines within petrological diagrams which use oxides of major and minor elements.Lithos,1989,22:247-263
[189]Le Maitre R W.Bateman P,Dudek A,et al.A classification of igneous rocks and glossary terms.Blackwell,Oxford,1989
[190]刘桑,胡瑞忠,赵军红,等.山东中生代基性脉岩的元素地球化学及其成因.地球化学,2005,34(4):339-350
[191]Sun S S & Mcdonough W F.Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and processes.In:Saunders A D & Norry M J(eds).Magmatism in the Ocean Basins.Geological Society of London,Special Publication no.42,1989,314-345
[192]Yan M C & Chi Q H.Chemical composition of eastern China crest and crustal rocks.Scientific Press,Beijing,1997
[193]Wang Y J,Fan W M,Guo F,et al.Geochemistry of Mesozoic marie rocks around the Chenzhou-Linwu fault in South China:implication for the lithospheric boundary between the Yangtze and the Cathaysia blocks.International Geology Review,2003,45:267-88
[194]Chen J F,Yan J,Xie Z,et al.Nd and Sr isotopic compositions of igneous rocks from the lower Yangtze region in eastern China:constraints on sources.Physics and Chemistry of the Earth(A),2001,26:719-31
[195]闫峻,陈江峰,谢智,等.长江中下游地区蝌蚪山晚中生代玄武岩的地球化学研究:岩石圈地幔性质与演化的制约.地球化学,2005,34(5):455-469
[196]郑建平,路凤香.胶辽半岛金伯利岩中地幔捕掳体岩石学特征:古生代岩石圈地幔及其不均一性.岩石学报,1999,15(1):65-74
[197]Gao S,Ling W L,Qiu Y M,et al.Contrasting geochemical and Sm-Nd isotopic compositions of Archean metasediments from the Kongling high-grade terrain of the Yangtze craton:evidence for cratonic evolution and redistribution of REE during crustal anatexis.Geochimica et Cosmochimica Acta,1999,63:2071-88
[198]Peucat J J,Vidal P,Bernard-Griffiths J,et al.Sr,Nd,Pb isotopic systematics in the Archean low-to high-grade transition zone of southern India:syn-accretion vs.post-accretion granulites.Journal of Geology,1988,97:537-550
[199]Steiger R H & Jager E.Subcommission on geochronology:convention on the use of decay constants in geochronology and cosmochronology.Earth and Planetary Science Letters,1977,36:359-62
[200]Lugmair G W & Marti K.Lunar initial ~(134)Nd/~(144)Nd:differential evolution of the lunar crust and mantle.Earth and Planetary Science Letters,1978,39:349-57
[201]Rudnick R L & Fountain D M.Nature and compositions of the continental crust:a lower crustal perspective.Review Geophysics,1995,33:267-309
[202]Defant M J & Drummond M S.Derivation of some modern arc magmas by melting of young subducted lithosphere.Nature,1990,347:662-65
[203]Xu J F,Shinjo R,Defant M J,et al.Origin of Mesozoic adakitic intrusive rocks in the Ningzhen area of eastern China:partial melting of delaminated lower crust continental crust.Geology,2002,30(12):1111-1114
[204]Huang X L,Xu Y G & Liu D Y.Geochronology,petrology and geochemistry of the granulite xenoliths from Nushan,east China:implication for a heterogeneous lower crust beneath the Sino-Korean craton.Geochimica et Cosmochimica Acta,2004,68:127-149
[205]Zhou X H,Sun M,Zhang G H,et al.Continental crust and lithospheric mantle interaction beneath North China:isotopic evidence from granulite xenoliths in Hannuoba,Sino-Korean craton.Lithos,2002,62:111-124
[206]Wang Q,Wyman D A,Zhao Z H,et al.Petrogenesis of Carboniferous adakites and Nb-enriched arc basalts in the Alataw area,northern Tianshan Range(western China):implications for Phanerozoic crustal growth in the central Asia orogenic belt.Chemical Geology,2007,236:42-64
[207]La Flèche M R,Camiré G & Jenner G A.Geochemistry of post-Acadian,Carboniferous continental intraplate basalts from the Maritimes Basins,Magdalen Islands,Quebec,Canada.Chemical Geology,1998,148:115-136
[208]Furman T & Graham D.Erosion of lithospheric mantle beneath the East African Rift system:geochemical evidence from the Kivu volcanic province.Lithos,1999,48:237-262
[209]Mckenzie D P & O'Nions R K.Partial melt distribution from inversion of rare element concentrations.Journal of Petrology,1991,32:625-679
[210]方长青.乳山海阳所地区超镁铁岩的主要特征.山东地质,1997,13(2):1-5
[211]邵济安,韩庆军,张履桥,等.内蒙古东部早中生代堆积杂岩捕掳体的发现.科学通报,1999,44(5):478-485
[212]许文良,迟效国,袁朝,等.华北地台中部中生代闪长质岩石及深源岩石包体.北京:地质出版社,1993
[213]Rudnick R L.Xenoliths-samples of the lower continental crust.In:Fountain D M(eds).The continental lower crust.Elsevier,1992,269-316
[214]邓万明,钟大赉.壳幔过渡带及其在岩石圈构造演化中的地质意义.科学通报,1998,42:2474-2482
[215]谢宏远,王岳军,沈远超,等.山东铜岭金矿的矿体定位构造.地质与勘探,1998,34(2):5-8
[216]Tarney J & Jones C E.Trace element geochemistry of orogenic igneous rocks and crustal growth.Journal of Geological Society,London,1994,151:855-868
[217]Fowler M B & Henney P J.Mixed Caledonian appinite magmas:implications for lamprophyre fractionation and high Ba-Sr granite genesis.Contribution to Minerology and Petrology,1996,126:199-215
[218]钱青,钟孙霖,李通艺,等.八达岭基性岩和高Ba-Sr花岗岩地球化学特征及成因探讨:华北和大别-苏鲁造山带中生代岩浆岩的对比.岩石学报,2002,18(3):275-292
[219]Rutter J M & Wyllie P.Melting of vapour-absent tonalite at 10kbar to simulate dehydration-melting in the deep crust.Nature,1988,331:159-160
[220]Rapp R P,Watson E B,Miller C F.Partial melting of amphibolite/eclogite and the origin of Archean trondhjemites and tonalities.Precambrian Research,1991,51:1-25
[221]Rapp R P,Watson E B.Dehydration melting of metabasalt mantle recycling.Journal of Petrology,1995,36:891-931
[222]Panino D A E.What do experiments tell us about the relative contributions of crust and mantle to the origin of granitic magmas.In:Catro A F C,Vigneresse J L(eds).Understanding granites:intergrating new and classical techiniques.Geological Society,London,Special publications,1999,168:55-75
[223]Roberts M P & Clemens J D.Origin of high-potassium,calcalkaline,Ⅰ-type granitiods.Geology,1993,21:825-828
[224]Pefford N & Atherton M.Na-rich partial melts from newly underplated basaltic crust:the Cordillera Blanca Batholith,Peru.Journal of Petrology,1996,37:1497-1521
[225]伍家善,耿元生,沈其韩,等.华北陆台早前寒武纪重大地质事件.北京:地质出版社,1991
[226]李继亮.五台山早元古代碰撞造山带的初步认识.地质科学,1990,1:1-11
[227]Zhao G C,Wilde S A,Cawood P A,et al.Thermal evolution of Archean basement rocks from the eastern part of the Noryh Chian craton and its bearing on tectonic setting.International Geology Review,1998,40:706-721
[228]Wang W.Formation of diamond with mineral inclusions of "mixed" eclogite and peridotite paragenesis.Earth and Planetary Science Letters,1998,160:831-843
[229]高山,金振民.拆沉作用(Delamination)及其壳-幔演化动力学意义.地质科技情报,1997,16(1):1-9
[230]Gao S,Zhang B R,Jin Z M.et al.How mafic is the lower continental crust? Earth planetary Science Letter,1998,161:101-117
[231]高山,张本仁,金振民.秦岭-大别造山带下地壳拆沉作用.中国科学(D辑),1999,29(6):532-541
[232]袁学诚.秦岭岩石圈速度结构与蘑菇云构造模型.中国科学(D辑),1996,26(3):209-215
[233]路凤香,郑建平,李伍平,等.中国东部显生宙地幔演化的主要样式:“蘑菇云”模型.地学前缘,2000,7(1):97-107
[234]郑建平,路凤香,余淳梅,等.地幔置换作用:华北两类橄榄岩及其透辉石微量元素对比.地球科学,2003,28:235-240
[235]徐义刚.岩石圈的热-机械侵蚀和化学侵蚀与岩石圈减薄.矿物岩石地球化学通报,1999,18(1):1-5
[236]余淳梅,郑建平,Griffin WL.汉诺坝橄榄岩捕掳体的单斜辉石LAM-ICPMS分析及其地幔演化意义.地球科学,2006,31(1):93-100
[237]陈丕基.郯庐断裂巨大平移的时代与格局.科学通报,1989,(4):289-293
[238]徐嘉炜,马国锋.郯庐断裂带研究的十年回顾.地质论评,1992,38(4):316-324
[239]Engebretson D C,Cox A,Gordon R G.Relative motions between oceanic and continental plates in the Pacific basins.Geological Society of American Special Publication,1985,206:1-59
[240]Yang J H,Wu F Y,Chung S L,et al.Rapid exhumation and cooling of the Liaonan metamorphic core complex:inferences from ~(40)Ar/~(39)Ar thermochronology and implications for Late Mesozoic extension in the eastern North China Craton.GSA Bulletin,2007,119: 1405-1414
[241]张宏福,Menzies MA,路凤香,等.华北古生代地幔岩捕虏体中石榴石和巨晶石榴石的主、微量元素.中国科学(D辑),2000,30(2):128-134
[242]张宏福,杨岳衡.华北克拉通东部含金刚石金伯利岩的侵位年龄和Sr-Nd-Hf同位素地球化学特征,岩石学报,2007,23(2):285-294
[243]汤华云,郑建平,余淳梅.华北东部新生代玄武岩中橄榄岩捕虏体的流体和稀有气体组成研究.岩石学报,2007,23(6):1531-1542
[244]李延河,李金城,宋鹤彬,等.中国东部新生代玄武岩中幔源包体和高压巨晶的氦同位素研究.中国科学(D),2001,31(8):641-647
[245]马锦龙,陶明信,叶先仁.山东沂沭地区幔源矿物中的流体和稀有气体地球化学研究.中国科学(D),2005,35(11):1019-1027
[246]马锦龙.沂沭断裂带新生代玄武岩及其地幔岩包体中的流体和稀有气体研究.[博士学位论文].兰州:中国科学院兰州地质研究,2003,31-40
[247]徐胜,刘丛强.我国东北部幔源包体中稀有气体丰度和同位素组成.科学通报,2002,47(2):141-146
[248]Tang Huayun,Zheng Jianping,Yu Chunmei.Age and composition of the Rushan intrusive complex in the northern Sulu orogen,eastern China:petrogenesis and lithospheric mantle evolution.Geological Magazine,2008,in press
[249]汤华云,郑建平,陈红汉,等.山东半岛第三纪基性火成岩He-Ar同位素与岩浆起源.中国科学(D辑),2007,37(4):451-459
[250]樊祺诚,隋建立,刘若新,等.汉诺坝榴辉岩相石榴辉石岩-岩浆底侵作用新证据.岩石学报,2001,17(1):1-6
[251]刘勇胜,袁洪林,高山,等.汉诺坝橄榄辉石岩包体锆石U-Pb年龄:97-158Ma岩浆底侵作用和麻粒岩相变质作用之间的成因联系.科学通报,2004,49(8):790-797
[2]Zheng J P,Griffin W L,O'Reilly S Y,et al.3.6Ga lower crust in central China:new evidence on the assembly of the North China Craton.Geology,2004,32:229-232
[3]Menzies M A,Fan W M & Zhang M.Paleozoic and Cenozoic lithoprobes and loss of＞120 km of Archaean lithosphere,Sino-Korean Craton,China.In:Prichard H M,Alabaster T,Harris N B W,et al(eds).Magmatic processes and plate tectonics.Geological Society of London,Special Publication no.76.1993,71-78
[4]Griffin W L,Zhang A,O'Reilly S Y,et al.Phanerozoic evolution of the lithosphere beneath the Sino-Korean Craton.In:Flower M,Chung S L,Lo C H,et al(eds).Mantle dynamics and plate interactions in East Asia.American Geophysical Union Geodynamics Series no.27.Washington D C,1998,107-126
[5]Menzies M A & Xu Y G.Geodynamics of the North China Craton.In:Flower M,Chung S L,Lo C H,et al(eds).Mantle dynamics and plate interactions in East Asia.American Geophysical Union Geodynamics Series no.27.Washington D C,1998,155-165
[6]Xu Y G,Menzies M A,Mattey D P,et al.The nature of lithospheric mantle near the Tancheng-Lujiang fault,China:an integration of texture,chemistry and O-isotopes.Chemical Geology,1996,134:67-81
[7]Fan W M,Zhang H F,Baker J,et al.On and offthe North China Craton:where is the Archean keel? Journal of Petrology,2000,41:933-950
[8]郑建平.中国东部地幔置换作用与中新生代岩石圈减薄.武汉:中国地质大学出版社,1999
[9]Gao S.Rudnick R L,Yuan H L,et al.Recycling lower continental crust in the North China Craton.Nature,2004,432:892-897
[10]Deng J F,Mo X X,Zhao H L,et al.2004.A new model for the dynamic evolution of Chinese lithosphere:'continental roots-plume tectonics'.Earth-Science Reviews,2004,65:223-275
[11]Deng J F,Su S G,Niu Y L,et al.A possible model for the lithospheric thinning of North China Craton:evidence form the Yanshanian(Jura-Cretaceous)magmatism and tectonism.Lithos,2007,96:22-35
[12]邓晋福,莫宣学,赵海玲,等.中国东部岩石圈根/去根作用与大陆“活化”-东亚型大陆动力学模式研究计划.现代地质,1994,8(3):349-356
[13]邓晋福,赵海玲,莫宣学,等.中国大陆根柱构造-大陆动力学的钥匙.北京:地质出版社,1996,33-34
[14]吴福元,葛文春,孙德有,等.中国东部岩石圈减薄研究中的几个问题.地学前缘,2003,10(3):51-60
[15]吴福元,孙德有.中国东部中生代岩浆作用与岩石圈减薄.长春科技大学学报,1999,29(4):313-318
[16]Xu Y G.Thermo-tectonic destruction of the Archean lithospheric keel beneath the Sino-Korean Craton in China:evidence,timing and mechanism.Physics and Chemistry of the Earth(A),2001,26(9-10):747-757
[17]Zheng J p,O'Reilly S Y,Griffin W L,et al.Nature and evolution of Cenozoic lithospheric mantle beneath Shandong peninsula,Sino-Korean craton.International Geology Review,1998,40:471-499
[18]Zheng J P,Griffin W L,O'Reilly S Y,et al.Late Mesozoic-Eocene mantle replacement beneath the eastern North China Craton:evidences from the Paleozoic and Cenozoic peridotite xenoliths.International Geology Review,2005,47:457-472
[19]Zheng J P,Griffin,W L,O'Reilly,S Y,et al.Mineral chemistry of peridotites from Paleozoic,Mesozoic and Cenozoic lithosphere:constraints on mantle evolution beneath eastern China.Journal of Petrology,2006,47(11):2233-2256
[20]Gao S,Rudnick R L,Carlson R W,et al.Re-Os evidence for replacement of ancient mantle lithosphere beneath the North China craton.Earth and Planetary Science Letters,2002,198:307-322
[21]张宏福,英基丰,徐平,等.华北中生代玄武岩中地幔橄榄石捕虏晶:对岩石圈地幔置换过程的启示.科学通报,2004,49(8):784-789
[22]Xu Y G,Huang X L,Ma J L,et al.Crust-mantle interaction during the tectono-thermal reactivation of the North China Craton:constraints from SHRIMP zircon U-Pb chronology and geochemistry of Mesozoic plutons from western Shandong.Contribution to Mineralogy and Petrology,2004,147:750-767
[23]翟明国,朱日祥,刘建明,等.华北东部构造体制转折的关键时限.中国科学(D辑),2003,33(10):913-920
[24]Zhang H F,Sun M,Zhou X H,et al.Mesozoic lithosphere destruction beneath the North China Craton:evidence from major-,trace-element and Sr-Nd-Pb isotope studies of Fangcheng basalts.Contribution to Mineralogy and Petrology,2002,144:241-253
[25]Zhang H F,Sun M,Zhou X H,et al.Secular evolution of the lithosphere beneath the eastern North China Craton:Evidence from Mesozoic basalts and high-Mg andesites.Geochimica et Cosmochimica Acta,2003,67(22):4373-4387
[26]许文良,王冬艳,高山,等.鲁西中生代金岭闪长岩中纯橄岩和辉石岩包体的发现及其意义.科学通报,2003,48(8):863-868
[27]许文良,王冬艳,王清海,等.鲁西中生代闪长岩中两类幔源捕虏体的岩石学和地球化学.岩石学报,2003,19(4):623-636
[28]Zheng J P,Griffin,W L,O'Reilly,S Y,et al.Mechanism and timing of lithospheric modification and replacement beneath the eastern North China Craton:Peridotitic xenoliths from the 100 Ma Fuxin basalts and a regional synthesis.Geochimica et Cosmochimica Acta,2007,71(21):5203-5225
[29]张宏福,郑建平.华北中生代玄武岩的地球化学特征与岩石成因:以辽宁阜新为例.科学通 报,2003,48(6):603-609
[30]裴福萍,许文良,王清海,等.鲁西费县中生代玄武岩及幔源捕虏晶的矿物化学:对岩石圈地幔性质的制约.高校地质学报,2004,10(1):88-97
[31]闫峻,陈江峰,谢智,等.鲁东晚白垩世玄武岩中的幔源捕虏体:对中国东部岩石圈减薄时间制约的新证据.科学通报,2003,48(14):1570-1574
[32]Ying J F,Zhang H F,Noriko K,et al.Nature and evolution of Late Cretaceous lithospheric mantle beneath the eastern North China Craton:Constraints from petrology and geochemistry of peridotitic xenoliths from Jünan,Shandong province,China.Earth and Planetary Science Letters,2006,244:622-638
[33]Zheng J P,Sun M,Zhou M F,et al.Trace elemental and PGE geochemical constraints of Mesozoic and Cenozoic peridotitic xenoliths on lithospheric evolution of the North China Craton.Geochimica et Cosmochimica Acta,2005,69(13):3401-3418
[34]黄福生,薛绥洲.邢邯侵入体中幔源超镁铁质岩包体的发现及其矿物地球化学特征.岩石学报,1990,4:40-45
[35]许文良,林景仟.河北邢邯地区角闪闪长岩中地幔纯橄岩包体的发现与研究.地质学报,1991,1:33-41
[36]Chen L H,Zhou X H.Subduction-related metasomatism in the thinning lithosphere:evidence from a composite dunite-orthopyroxenite xenoliths entrained in Mesozoic Laiwu high-Mg diorite,North China.Geochemistry,Geophysics,Geosystems,2005,6(6),doi:10.1029/2005GC000938
[37]陈立辉,周新华,2003.鲁西中生代闪长岩中的深源超镁铁质岩捕虏体及其富硅交代特征.中国科学(D辑),33(8):735-744
[38]许文良,王冬艳,王清海,等.鲁西纯橄岩捕虏体中富硅质熔(流)体的交代作用:对中生代岩石圈地幔减薄的意义.地质学报,2004,78(1):72-80
[39]张瑾,张宏福,英基丰,等.华北晚中生代中基性侵入岩中橄榄岩捕虏体是岩石圈地幔直接样品?岩石学报,2005,21(6):1559-1568
[40]支霞臣,孟庆,许文良,等.鲁西铁铜沟中生代闪长岩中橄榄岩包体代表SCLM吗?-Re-Os同位素体系启示.2004年全国岩石学与地球动力学研讨会摘要(海口),407-409
[41]Xu Y G,Ma J L,Huang X L,et al.Early Cretaceous gabbroic complex from Yinan,Shandong Province:petrogenesis and mantle domains beneath the North China Craton.International Journal of Earth Science,2004,93:1025-1041
[42]徐义刚.华北岩石圈减薄的时空不均一特征.高校地质学报,2004,10(3):324-331
[43]Wu F Y,Lin J Q,Wilde S A,et al.Nature and significance of the Early Cretaceous giant igneous event in eastern China.Earth and Planetary Science Letters,2005,233:103-119
[44]许文良,王清海,王冬艳,等.华北克拉通东部岩石圈减薄的过程与机制:中生代火成岩和深源捕虏体证据.地学前缘,2004,11(3):309-317
[45]许文良,王冬艳,王清海,等.华北地块中东部中生代侵入杂岩中角闪石和黑云母的~(40)Ar/~(39)Ar 定年:对岩石圈减薄时间的制约.地球化学,2004,33(3):221-231
[46]王晓蕊,高山,柳小明,等.辽西四合屯早白垩世义县组高镁安山岩的地球化学:对下地壳拆沉作用和Sr/Y变化的指示.中国科学(D辑),2005,35(8):700-709
[47]Zhang H F,Sun M,Zhou X H,et al.Geochemical constraints on the origin of Mesozoic alkaline intrusive complexes from the North China Craton and tectonic implications.Lithos,2005,81:297-317
[48]Fan W M,Guo F,Wang Y J,et al.Post-Orogenic bimodal volcanism along the Sulu orogenic belt in eastern China.Physics and Chemistry of the Earth(A),2001,26(9-10):733-746
[49]Guo F,Fan W M,Wang Y J,et al.Origin of early Cretaceous talc-alkaline lamprophyres from the Sulu orogen in eastern China:implications for enrichment processes beneath continental collisional belt.Lithos,2004,78:291-305
[50]Guo F,Fan W M,Wang Y J,et al.Late Mesozoic mafic intrusive complexes in North China Block:constraints on the nature of subcontinental lithospheric mantle.Physics and Chemistry of the Earth(A),2001,26(9-10):759-771
[51]Ying J F,Zhou X H,Zhang H F.Geochemical and isotopic investigation of the Lalwu-Zibo carbonatites from western Shandong province,China and implications for their petrogenesis and enriched mantle source.Lithos,2004,75:413-426
[52]Ying,J F,Zhou,X H,Zhang H F.The geochemical variations of mid-Cretaceous lavas across western Shandong province,China and their tectonic implications.International Journal of Earth Science,2006,95:68-79
[53]Yang J H,Chung S L,Zhai M G,et al.Geochemical and Sr-Nd-Pb isotopic compositions of mafic dikes from the Jiaodong peninsula,China:evidence for vein-plus-peridotite melting in the lithospheric mantle.Lithos,2004,73:145-160
[54]邱检生,徐夕生,罗清华.鲁西富钾火山岩和煌斑岩的~(40)Ar-~(39)Ar定年及源区示踪.科学通报,2001,46(18):1500-1508
[55]杨进辉,朱美妃,刘伟,等.胶东地区郭家岭花岗闪长岩的地球化学特征及成因.岩石学报,2003,19(4):692-700
[56]袁洪林,柳小明,刘勇胜,等.北京西山晚中生代火山岩U-Pb锆石年代学及地球化学研究.中国科学(D辑),2005,35(9):821-836
[57]杨承海,许文良,杨德彬,等.鲁西中生代高Mg闪长岩的成因:年代学与岩石地球化学证据.地球科学-中国地质大学学报,2006,31(1):81-92
[58]Chen B,Jahn B M,Arakawa Y,et al.Petrogenesis of the Mesozoic intrusive complexes from the southern Taihang orogen,North China Craton:elemental and Sr-Nd-Pb isotopic constraints.Contribution to Mineralogy and Petrology,2004,148:489-501
[59]Chen B,Zhai M G.Geochemistry of late Mesozoic lamprophyre dykes from the Taihang Mountains,North China,and implications for the sub-continental lithospheric mantle.Geological Magazine,2003,140:87-93
[60]Wang Y J,Fan W M,Zhang H F,et al.Early Cretaceous gabbroic rocks from the Taihang Mountains:implications for a paleosubduction-related lithospheric mantle beneath the central North China Craton.Lithos,2006,86:281-302
[61]陈斌,田伟,翟明国,等.太行山和华北其它地区中生代岩浆作用的锆石U-Pb年代学和地球化学特征及其岩浆成因和地球动力学意义.岩石学报,2005,21(1):13-24
[62]陈斌,翟明国,邵济安.太行山北段中生代岩基的成因和意义:主要和微量元素地球化学证 据.中国科学(D辑),2002,32(11):896-907
[63]蔡剑辉,阎国翰,肖成东,等.太行山大兴安岭构造岩浆带中生代侵入岩Nd、Sr、Pb同位素特征及物质来源探讨.岩石学报,2004,20(5):1225-1242
[64]彭头平,王岳军,范蔚茗,等.南太行山闪长岩的SHRIMP锆石U-Pb年龄及岩石成因研究.岩石学报,2004,20(5):1253-1262
[65]张旗,钱七,王二七,等.燕山中晚期的“中国东部高原”:埃达克岩的启示.地质科学,2001,36(2):248-255
[66]张旗,王焰,钱青,等.中国东部晚中生代埃达克岩的特征及其构造-成矿意义.岩石学报,2001,17(2):236-244
[67]张旗,王焰,王云龙,等.燕山期中国东部高原下地壳组成初探:埃达克质岩Sr、Nd同位素制约.岩石学报,2001,17(4):505-513
[68]葛晓月,李献华,陈志刚,等.中国东部燕山期高Sr低Y型中酸性火成岩的地球化学特征及成因:对中国东部地壳厚度的制约.科学通报,2002,47(6):474-480
[69]Chen B,Jahn B M,Wei C J.Petrogenesis of Mesozoic granitoids in the Dabie UHP complex,central China:trace element and Nd-Sr isotope evidence.Lithos,2002,60:67-68
[70]张华锋,翟明国,何中甫,等.胶东昆嵛山杂岩中高锶花岗岩地球化学成因及其意义.岩石学报,2004,20(3):369-380
[71]Bird P.Initiation of intracontinental subduction in the Himalayas.Journal of Geophysics Research.1978.83(B10):4975-4987
[72]郑建平,孙敏,路凤香,等.信阳基性麻粒岩捕掳体及其华北南缘早中生代下地壳性质.岩石学报,2005,21(1):91-98
[73]Zhai M G,Fan Q C,Zhang H F,et al.Lower crustal processes leading to Mesozoic lithospheric thinning beneath eastern North China:underplating,replacement and delamination.Lithos,2007,96:36-54
[74]Wang K L,O'Reilly S Y,Griffin W L,et al.Proterozoic mantle lithosphere beneath the extended margin of the south China Block:In situ Re-Os evidence.Geology,2003,31(8):709-712
[75]Wu F Y,Walker R J,Ren X W,et al.Osmium isotopic constraints on the age of lithospheric mantle beneath Northeastern China.Chemical Geology,2003,196:107-129
[76]高山,Rudnick R L,Carlson R W,et al.华北克拉通岩石圈地幔置换作用和壳幔生长耦合的Re-Os同位素证据.地学前缘,2003,10(3):61-67
[77]支霞臣,彭子成,陈道公,等.苏皖地区大陆岩石圈地幔的长时性-地幔橄榄岩捕虏体的锇同位素模式年龄.中国科学(D辑),2001,31(6):464-470
[78]支霞臣,彭子成,陈道公,等.苏皖地区幔源橄榄岩捕虏体的锇同位素组成、模式年龄及其意义.岩石学报,2001,17(1):11-18
[79]支霞臣,秦协.中国东部地幔橄榄岩捕虏体的Re-Os同位素地球化学:岩石圈地幔的形成年龄和减薄作用的制约.岩石学报,2004,20(5):989-998
[80]余淳梅,郑建平,Griffin W L.汉诺坝橄榄岩捕掳体原位Re-Os同位素年龄与多发地幔事件.科学通报,2007,31(1):93-100
[81]Robinson P T,Zhou M F,Hu X F,et al.Geochemical constraints on the origin of the Hegenshan ophiolite,Inner Mongolia,China.Journal of Asian Earth Sciences,1999,17:423-442
[82]Zhang H F,Ying J F,Shimoda G,et al.Importance of melt circulation and crust-mantle interaction in the lithospheric evolution beneath the North China Craton:evidence from Mesozoic basalts-borne clinopyroxene xenocrysts and pyroxenite xenoliths.Lithos,2007,96:67-89
[83]邱检生,胡建,蒋少涌,等.鲁西中新生代镁铁质岩浆作用与地幔化学演化.地球科学-中国地质大学学报,2005,30(6):646-658
[84]姜耀辉,蒋少涌,赵葵东,等.辽东半岛煌斑岩SHRIMP锆石U-Pb年龄及其对中国东部岩石圈减薄开始时间的制约.科学通报,2005,50(19):2161-2168
[85]邓晋福,苏尚国,赵海玲,等.华北地区燕山期岩石圈减薄的深部过程.地学前缘,2003,10(3):41-50
[86]邓晋福,苏尚国,刘翠,等.关于华北克拉通燕山期岩石圈减薄的机制与过程的讨论:是拆沉,还是热侵蚀和化学交代?地学前缘,2006,13(2):105-119
[87]张宏福,周新华,范蔚茗,等.华北东南部中生代岩石圈地幔性质、组成、富集过程及其形成机理.岩石学报,2005,21(4):1271-1280
[88]Zhang H F,Sun M,Zhou M F,et al.Highly heterogeneous late Mesozoic lithospheric mantle beneath the North China Craton:evidence from Sr-Nd-Pb isotopic systematics of mafic igneous rocks.Geological Magazine,2004,141:55-62
[89]Zhang H F.Transformation of lithospheric mantle through peridotite-melt reaction:a case of Sino-Korean craton.Earth and Planetary Science Letters,2005,237:768-780
[90]Wang X M,Liou J G,Mao H K.Coesite-bearing eclogites from the Dabie Mountains in central China.Geology,1989,17:1085-1088
[91]Okay A I,Xu S T,Sengor A M C.Coesite from the Dabie Shan eclogites,central China.European Journal of Mineralogy,1989,1:595-598
[92]Hirajima T,Ishiwatari A,Cong B L,et al.Coesite from Mengzhong eclogite at Donghai County,northeastern Jiangsu Province,China.Mineralogy Magazine,1990,54:579-583
[93]Xu S T,Okay A I,Ji S Y,et al.Diamond from the Dabie Shan metamorphic rocks and its implication for tectonic setting.Science,1992,256:80-92
[94]Brueckner H K & Medaris L G.A general model for the intrusion and evolution of "mantle"garnet peridotites in high-pressure and ultra-high-pressure metamorphic terranes.Journal of Metamorphic Geology,2000,18(2):123-133
[95]Yang J J.Titanian clinohumite-gamet-pyroxene rock from the Sulu UHP metamorphic terran,China:chemical evolution and tectonic implications.Lithos,2003,70:359-379
[96]Yang J J & Jahn B M.Deep subduction of mantle-derived garnet peridotites from the Sulu UHP metamorphic terran in China.Journal of Metamorphic Geology,2000,18:167-180
[97]Zhang R Y,Liou J G,Zheng J P,et al.Petrogenesis of the Yangkou layered gamet-peridotite complex,Sulu UHP terrane,China.American Mineralogist,2005,90:801-813
[98]Zhang R Y,Liou J G,Yang J S,et al.Petrochemical constraints for dual origin of garnet peridotites from the Dabie-Sulu UHP terrane,eastern-central China.Journal of Metamorphic Geology,2000,18(2):149-166
[99]Zhang R Y,Liou J G,Yang J S,et al.Ultrahigh-pressure metamorphism in the forbidden zone:the Xugou garnet peridotite,Sulu terrane,eastern China.Journal of Metamorphic Geology,2003,21(6):1-12
[100]Fan W M,Guo F,Wang Y J,et al.Late Mesozoic volcanism in the northern Huaiyang tectono-magmatic belt,central China:partial melts from a lithospheric mantle with subducted continental crust relicts beneath the Dabie orogen? Chemical Geology,2004,209:27-48
[101]Wang Y J,Fan W M,Peng T P,et al.Natrue of the Mesozoic lithospheric mantle and tectonic decoupling beneath the Dabie orogen,central China:evidence from ~(40)Ar/~(39)Ar geochronology,elemental and Sr-Nd-Pb isotopic compositions of early Cretaceous mafic igneous rocks.Chemical Geology,2005,220:165-189
[102]Zheng J P,Griffin W L,O'Reilly S Y,et al.A refractory mantle protolith in younger continental crust,eastern China:Age and composition of zircon in the Sulu ultrahigh-pressure peridotite.Geology,2006,34(9):705-708
[103]Zheng J P,Zhang R Y,Griffin W L,et al.Heterogeneous and metasomatised mantle recorded by trace elements in minerals of the Donghai garnet peridotites,Sulu UHP terrane,China.Chemical Geology,2005,221:243-259
[104]Huang F,Li S G,Dong F,et al.Recycling of deeply subducted continental crust in the Dabie Mountains,central China.Lithos,2007,96:151-169
[105]Jahn B M,Wu F Y,Ching H L,et al.Crust-mantle interaction induced by deep subduction of the continental crust:geochemical and Sr-Nd isotopic evidence from post-collisional mafic-ultramafic intrusions of the north Dabie complex,central China.Chemical Geology,1999,157:119-146
[106]Ma C Q,Ehlers C,Xu C H,et al.The roots of the Dabieshan ultrahigh-pressure metamorphic terrane:constraints from geochemistry and Nd-Sr isotope systematics.Precambrian Research,2000,102:279-301
[107]Zhang H F,Gao S,Zhong Z Q,et al.Geochemical and Sr-Nd-Pb isotopic compositions of Cretaceous granitoids:constraints on tectonic framework and crustal structure of the Dabieshan ultrahigh-pressure metamorphic belt,China.Chemical Geology,2002,186:281-299
[108]Yang J H,Chung S L,Wilde S A.Petrogenesis of post-orogenic syenites in the Sulu orogenic belt,eastern China:geochronological,geochemical and Nd-Sr isotopic evidence.Chemical Geology,2005,214:99-125
[109]Yang J H,Wu F Y,Chung S L,et al.Petrogenesis of early Cretaceous intrusions in the Sulu ultrahigh-pressure orogenic belt,eastern China and their relationship to lithospheric thinning.Chemical Geology,2005,222:200-231
[110]黄洁,郑永飞,吴元保,等.苏鲁造山带五莲地区岩浆岩元素和同位素地球化学研究.岩石学报,2005,21(3):545-568
[111]高天山,陈江峰,谢智,等.苏鲁超高压变质带中三叠纪石岛杂岩体的地球化学研究.岩石学报,2004,20(5):1025-1038
[112]周建波,郑永飞,吴元保.苏鲁造山带西北缘五莲花岗岩中锆石U-Pb年龄及其地质意义.科学通报,2002,47(22):1745-1750
[113]胡芳芳,范宏瑞,杨进辉,等.胶东文登长山南花岗闪长岩体的岩浆混合成因:闪长质包体及寄主岩石的地球化学、Sr-Nd同位素和锆石Hf同位素证据.岩石学报,2005,21(3):569-586
[114]张华锋,翟明国,童英,等.胶东半岛三佛山高Ba-Sr花岗岩成因.地质论评,2006,52(1):43-53
[115]魏春景,张立飞,王式洗.安徽省大别山东段中生代高钾花岗质岩石及其地质意义.中国科学(D辑),2000,30(4):355-363
[116]王德滋,王赐银,于津海.昆嵛山混合杂岩体的地质特征及成因.南京大学学报,1989,25(4):679-688
[117]徐金芳,沈步云,牛良柱,等.胶北地块与金矿有关的花岗岩类研究.山东地质,1989,5(2):1-25
[118]于津海.胶东东部昆嵛山混合杂岩体的形成时代及成因.地质论评,1989,35(4):285-296
[119]徐景奎,杨忠芳,赵伦山,等.胶东昆嵛山复式花岗岩体的地质地球化学研究.长春地质学院学报,1991,21(2):167-174
[120]张德全,徐洪林,孙桂英.山东邓格庄金矿与昆嵛山花岗岩的定位时代及其地质意义.地质论评,1995,41(5):415-425
[121]徐洪林,张德全,孙桂英.胶东昆嵛山花岗岩的特征、成因及其与金矿的关系.岩石矿物杂志,1997,16(2):131-143
[122]杨进辉.胶东地区金矿成矿时代及其成矿地球动力学背景.兼论壳幔相互作用与成岩成矿.[博士学位论文],北京:中国科学院地质与地球物理研究所,2000,1-133
[123]陈光远,孙岱生,邵岳.胶东昆嵛山二长花岗岩副矿物成因矿物学研究.现代地质,1996,10(2):175-186
[124]郭敬辉,陈福坤,张晓曼,等.苏鲁超高压带花岗岩类成因与碰撞后构造过程:锆石U-Pb年代学和地球化学研究.见:从柏林,翟明国,郭敬辉,等编.大陆的俯冲、拆离和减薄作用学术研讨会论文摘要集.西安:西北大学,2001,99-102
[125]郭敬辉,陈福坤,张晓曼,等.苏鲁超高压带北部中生代岩浆侵入活动与同碰撞.碰撞后构造过程:锆石U-Pb年代学.岩石学报,2005,21(4):1281-1301
[126]孟繁聪,薛怀民,李天福,等.苏鲁造山带晚中生代地幔的富集特征-来自辉长岩的地球化学证据.岩石学报,2005,21(6):1583-1592
[127]胡芳芳,范宏瑞,杨进辉,等.鲁东昆嵛山地区宫家辉长.闪长岩成因:岩石地球化学、锆石U-Pb年代学与Hf同位素制约.岩石学报,2007,23(2):369-380
[128]Zhao G C,Cawood P A,Wilde S A,et al.Metamorphism of basement rocks in the Central Zone of the North China Craton:implications for Paleoproterozoic tectonic evolution.Precambrian Research,2000,103:55-88
[129]Zhao G C,Wilde S A,Cawood P A,et al.Archean blocks and their boundaries in the North China Craton:lithological,geochemical,structural and P-T path constraints and tectonic evolution.Precambrian Research,2001,107:45-73
[130]Zhao G C,Wilde S A,Cawood P A,et al.Thermal evolution of two texrural types of mafic granulites in the North China Craton:evidence for both mantle plume and collisional tectonics.Geological Mmagazine,1999,136:223-240
[131]赵国春,孙敏.华北克拉通基底构造单元特征及早元古代拼合.中国科学(D辑),2002,32(7):538-549
[132]Sun M,Armstrong R L,Lambert R S J.Petrochemistry and Sr,Pb and Nd isotopic geochemistry of Early Precambrian rocks,Wutaishan and Taihangshan areas,China.Precambrian Research,1992,56:1-31
[133]陈国英,宋仲和,安昌强,等.华北地区三维地壳上地幔地幔结构.地球物理学报,1991,34(2):172-181
[134]Zheng J P,O'Reilly S Y,Griffin W L,et al.Relict refractory mantle beneath the eastern North China block:significance for lithosphere evolution.Lithos,2001:57:43-66
[135]林景迁,谭冬娟,迟效国,等.胶辽半岛中生代花岗岩.北京:科学出版社,1992,17-23,72-88
[136]路孝平,吴福元,赵成弼,等.通化地区印支期花岗岩锆石U-Pb年龄及其与大别-苏鲁超高压带碰撞造山作用之间的关系.科学通报,2003,48(8):843-849
[137]许文良,王清海,杨德彬,等.蚌埠荆山“混合花岗岩"SHRIMP锆石U-Pb定年及其地质意义.中国科学(D辑),2004,34(5):423-428
[138]许文良,王冬艳,刘晓春,等.徐淮地区早侏罗世侵入杂岩体中榴辉岩类包体的发现及其地质意义.科学通报,2002,47(8):618-622
[139]杨进辉,朱美妃,刘伟,等.胶东地区郭家岭花岗闪长岩的地球化学特征及成因.岩石学报,2003,19(4):692-700
[140]陈立辉.山东莱芜中生代高镁侵入岩及其超镁铁质岩捕掳体的成因研究.[博士学位论文],北京:中国科学院地质与地球物理研究所,2001,9-12
[141]刘若新,陈文寄,孙建中,等.中国新生代火山岩的K-Ar年代学与构造环境.见:刘若新主编.中国新生代火山岩年代学与地球化学.北京:地震出版社,1992,1-43
[142]曹国权.试论“胶南地体”.山东地质,1990,5(2):1-10
[143]丛源.胶东西北部北截-大河一带造山型金矿的地质特征及狂化富集规律.[硕士学位论文],长春:吉林大学,2005,6-18
[144]Ishizaka K,Hirazima T & Zheng X S.Rb-Sr dating for the Jiaodong gneiss of the Su-lu ultrahigh-high pressure province,eastern China.The Island Arc,1994,3:232-241
[145]王仁民,安家桐,赖兴远.胶东蛇绿岩套的发现及其地质意义.岩石学报,1995,11:221-240
[146]张希道,王来明.胶东威海-乳山麻粒岩相岩石的发现及初步研究.中国区域地质,1996,58(3):213-221
[147]王清晨,从柏林.大别山超高压变质岩的地球动力学意义.中国科学(D辑),1996,26(3):271-276
[148]Yin A,Nie S.An indentation model for the North and South China collision and the development of the Tan-Lu and Honam fault systems,eastern Asian.Tectonics,1993,12(4):801-813
[149]Zhai M G,Liu W J.The boundary between Sino-Korea craton and Yangtze craton and its extension to the Korea peninsula.In:Jang B A,Cheong D K.(eds),Crustal evolution in Northeast Asia.Kangweon National University,Chuncheon,1997,18-27
[150]Zhai M G,Cong B L,Guo J H,et al.Sm-Nd geochronology and petrography of garnet pyroxene granulites in the northern Sulu region of China and their geotectonic implication.Lithos,2000,52:23-33
[151]宋明春,王来明.对胶南造山带基础地质问题的新认识.中国区域地质,2000,19(1):1-6
[152]王来明,王世进,张富中.2001年山东省地质调查工作进展和主要成果.山东地质,2001,17(6):1-6
[153]Wallis S,Enami M & Banno S.The Sulu UHP terrane:A review of the petrology and structural geology.International Geology Review,1999,41:906-920
[154]李永刚,郭敬辉,翟明国,等.胶东地区基底长英质片麻岩的地球化学特征及其构造归属.岩石学报,1999,15(4):557-563
[155]许志琴,戚学详,杨经绥,等.苏鲁高压-超高压变质地体的陆-陆碰撞深俯冲剥蚀模式.地球科学-中国地质大学学报,2006,31(4):427-436
[156]杨敏之,吕古贤.胶东绿岩带金矿地质地球化学.北京:地质出版社,1996
[157]王来明,鄢毅民.山东栖霞地区太古宙英云闪长岩的地球动力学意义,山东地质,1992,1:80-87
[158]李兆龙,杨敏之,胶东金矿床地质地球化学.天津,天津科学技术出版社,1993
[159]张田,张岳桥.胶东半岛中生代侵入岩浆活动序列及其构造制约.高校地质学报,2007,13(2):323-336
[160]Chen J F,Xie Z,Li H M,et al.U-Pb zircon ages for a collision-related K-rich complex at Shidao in the Sulu ultrahigh pressure terrane,China.Geochemical Journal,2003,37:35-46
[161]罗振宽,关康,苗来成,等.胶东招掖地区与金矿化有关花岗岩继承锆石年龄及其意义.地球学报,1997,18:138-141
[162]关康,罗振宽,苗来成,等.胶东招掖郭家岭型花岗岩锆石SHRIMP年代学研究.地质科学,1998,33(3):318-328
[163]王德滋,赵广涛,邱检生.中国东部晚中生代A型花岗岩的构造制约.高校地质学报,1995,1(2):13-20
[164]孙景贵,胡受奚,凌洪飞.胶东金矿区高钾-钾质脉岩地球化学与俯冲-壳幔作用研究.岩石学报,2000,16(3):401-412
[165]Li S G,Xiao T L,Liou D L,et al.Collision of the North China and Yangtze Blocks and formation of coesite-bearing eclogite:Timing and processes.Chemical Geology,1993,109:89-111
[166]Li S G,Jagoutz E,Chen Y,et al.Sm-Nd and Rb-Sr isotopic chronology and cooling history of ultrahigh pressure mtamorphic rocks and their country rocks at Shuanghe in the Dabie Mountains,Central China.Geochimica et Cosmochimica Acta,1999,64(6):1077-1093
[167]Hacker B R,Wang Q C.Ar/Ar geochronology of ultrahigh-pressure metamorphism in central China.Tectonics,1995,14:994-1006
[168]Zhang R Y,Hirajima T,Banno S,et al.Petrology of ultrahigh-pressure metamorphic rocks in southern Sulu region,eastern China.Journal of Metamorphic Geology,1995,13:659-75
[169]Hirajima T,Zhang R Y,Li J J.Nyboite from the Donghai area,Jiangsu province,eastern China.Mineralogy Magazine,1992,56:37-46
[170]Chavagnac V & Jahn B M.Coesite-bearing eclogites from the Bixiling complex,Dabie mountains,China:Sm-Nd ages,geochemical characteristics and tectonic implications.Chemical Geology,1996,133:29-51
[171]Li S G,Huang F,Nie Y H,et al.Geochemical and geochronological constraints on the structure location between the North and and South China blocks in the Dabie orogen,central China.Physics and Chemistry of the Earth(A),2001,26(9-10):655-672
[172]Hacker B,Ratschbacher L,Webb L,et al.U/Pb zircon ages constrain the architecture of the ultrahigh-pressure Qinling-Dabie orogen,China.Earth and Planetary Science Letters,1998,161:215-30
[173]Liu F L,Xu Z Q & Xue H M.Tracing the protolith,UHP metamorphism,and exhumation ages of orthogneiss from the SW Sulu terrane(eastern China):SHRIMP U-Pb dating of mineral inclusion-bearing zircons.Lithos,2004,78:411-29
[174]Ye K,Cong B L & Ye D N.The possible subduction of continental material to depths greater than 200 km.Nature,2000,407:734-36
[175]金振民,金淑燕,高山,等.大别山超高压岩石形成深度局限于100-150km吗?科学通报,1998,43:767-771
[176]叶凯,平岛崇男,石渡明,等.青岛仰口榴辉岩中粒间柯石英的发现及其意义.科学通报,1996,41(15):1407-1408
[177]Cong B L.Ultrahigh-pressure metamorphic rocks in the Dabieshan-Sulu region of China.Science Press,Beijing,1996,224
[178]Wang Q C,Ishiwateri A,Zhao Z U,et al.Coesite-bearing granulite retrograded from eclogite in Weihai,eastern China.Journal of Mineralogy,1993,5:141-152
[179]Zheng Y F,Fu B,Gong B L,et al.Stable isotope geochemistry of ultrahigh pressure metamorphic rocks from the Dabie-Sulu orogen in China:Implications for geodynamics and fliud regime.Earth Science Review,2003,62:105-161
[180]Xu J W,Zhu G,Tong W X,et al.Formation and evolution of the Tancheng-Lujiang wrench fault system:A major shear system to the northwest of the Pacific Ocean.Tectonophysics,1987,134:273-310
[181]刘福来,许志琴,宋彪.苏鲁超高压变质带中非超高压花岗质片麻岩的准确识别:来自锆石微区矿物包体及SHRIMP U-Pb定年的证据.地质学报,2003,77(4):534-540
[182]刘福来,许志琴,宋彪.苏鲁地体超高压和退变质时代的厘定:来自片麻岩锆石微区SHRIMP U-Pb定年的证据.地质学报,2003,77(2):229-239
[183]杨经绥,许志琴,刘福来,等.含柯石英锆石的SHRIMP U-Pb定年:胶东印支超高压变质作用的证据.地质学报,2002,76(3):354-371
[184]Zhang R Y,Liou J G,Ernst W C.Ultrahigh-pressure metamorphism and decompressional P-T paths of eclogites and country rocks from Weihai,eastern China.The Island Arc,1995,4:293-309
[185]山东地质矿产局.山东省区域地质志.北京:地质出版社,1991,1-274
[186]Ludwig K R.ISOPLOT 3.00:A Geochronological Toolkit for Mi-crosoft Excel.Berkeley Geochronology Center Special Publication no.4,2003,1-70
[187]王岳军,范蔚茗,郭锋,等.北大别晚中生代火山岩的地球化学特征及对北大别构造属性的 启示.地学前缘,2003,10(4):529-538
[188]Rickwood P C.Boundary lines within petrological diagrams which use oxides of major and minor elements.Lithos,1989,22:247-263
[189]Le Maitre R W.Bateman P,Dudek A,et al.A classification of igneous rocks and glossary terms.Blackwell,Oxford,1989
[190]刘桑,胡瑞忠,赵军红,等.山东中生代基性脉岩的元素地球化学及其成因.地球化学,2005,34(4):339-350
[191]Sun S S & Mcdonough W F.Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and processes.In:Saunders A D & Norry M J(eds).Magmatism in the Ocean Basins.Geological Society of London,Special Publication no.42,1989,314-345
[192]Yan M C & Chi Q H.Chemical composition of eastern China crest and crustal rocks.Scientific Press,Beijing,1997
[193]Wang Y J,Fan W M,Guo F,et al.Geochemistry of Mesozoic marie rocks around the Chenzhou-Linwu fault in South China:implication for the lithospheric boundary between the Yangtze and the Cathaysia blocks.International Geology Review,2003,45:267-88
[194]Chen J F,Yan J,Xie Z,et al.Nd and Sr isotopic compositions of igneous rocks from the lower Yangtze region in eastern China:constraints on sources.Physics and Chemistry of the Earth(A),2001,26:719-31
[195]闫峻,陈江峰,谢智,等.长江中下游地区蝌蚪山晚中生代玄武岩的地球化学研究:岩石圈地幔性质与演化的制约.地球化学,2005,34(5):455-469
[196]郑建平,路凤香.胶辽半岛金伯利岩中地幔捕掳体岩石学特征:古生代岩石圈地幔及其不均一性.岩石学报,1999,15(1):65-74
[197]Gao S,Ling W L,Qiu Y M,et al.Contrasting geochemical and Sm-Nd isotopic compositions of Archean metasediments from the Kongling high-grade terrain of the Yangtze craton:evidence for cratonic evolution and redistribution of REE during crustal anatexis.Geochimica et Cosmochimica Acta,1999,63:2071-88
[198]Peucat J J,Vidal P,Bernard-Griffiths J,et al.Sr,Nd,Pb isotopic systematics in the Archean low-to high-grade transition zone of southern India:syn-accretion vs.post-accretion granulites.Journal of Geology,1988,97:537-550
[199]Steiger R H & Jager E.Subcommission on geochronology:convention on the use of decay constants in geochronology and cosmochronology.Earth and Planetary Science Letters,1977,36:359-62
[200]Lugmair G W & Marti K.Lunar initial ~(134)Nd/~(144)Nd:differential evolution of the lunar crust and mantle.Earth and Planetary Science Letters,1978,39:349-57
[201]Rudnick R L & Fountain D M.Nature and compositions of the continental crust:a lower crustal perspective.Review Geophysics,1995,33:267-309
[202]Defant M J & Drummond M S.Derivation of some modern arc magmas by melting of young subducted lithosphere.Nature,1990,347:662-65
[203]Xu J F,Shinjo R,Defant M J,et al.Origin of Mesozoic adakitic intrusive rocks in the Ningzhen area of eastern China:partial melting of delaminated lower crust continental crust.Geology,2002,30(12):1111-1114
[204]Huang X L,Xu Y G & Liu D Y.Geochronology,petrology and geochemistry of the granulite xenoliths from Nushan,east China:implication for a heterogeneous lower crust beneath the Sino-Korean craton.Geochimica et Cosmochimica Acta,2004,68:127-149
[205]Zhou X H,Sun M,Zhang G H,et al.Continental crust and lithospheric mantle interaction beneath North China:isotopic evidence from granulite xenoliths in Hannuoba,Sino-Korean craton.Lithos,2002,62:111-124
[206]Wang Q,Wyman D A,Zhao Z H,et al.Petrogenesis of Carboniferous adakites and Nb-enriched arc basalts in the Alataw area,northern Tianshan Range(western China):implications for Phanerozoic crustal growth in the central Asia orogenic belt.Chemical Geology,2007,236:42-64
[207]La Flèche M R,Camiré G & Jenner G A.Geochemistry of post-Acadian,Carboniferous continental intraplate basalts from the Maritimes Basins,Magdalen Islands,Quebec,Canada.Chemical Geology,1998,148:115-136
[208]Furman T & Graham D.Erosion of lithospheric mantle beneath the East African Rift system:geochemical evidence from the Kivu volcanic province.Lithos,1999,48:237-262
[209]Mckenzie D P & O'Nions R K.Partial melt distribution from inversion of rare element concentrations.Journal of Petrology,1991,32:625-679
[210]方长青.乳山海阳所地区超镁铁岩的主要特征.山东地质,1997,13(2):1-5
[211]邵济安,韩庆军,张履桥,等.内蒙古东部早中生代堆积杂岩捕掳体的发现.科学通报,1999,44(5):478-485
[212]许文良,迟效国,袁朝,等.华北地台中部中生代闪长质岩石及深源岩石包体.北京:地质出版社,1993
[213]Rudnick R L.Xenoliths-samples of the lower continental crust.In:Fountain D M(eds).The continental lower crust.Elsevier,1992,269-316
[214]邓万明,钟大赉.壳幔过渡带及其在岩石圈构造演化中的地质意义.科学通报,1998,42:2474-2482
[215]谢宏远,王岳军,沈远超,等.山东铜岭金矿的矿体定位构造.地质与勘探,1998,34(2):5-8
[216]Tarney J & Jones C E.Trace element geochemistry of orogenic igneous rocks and crustal growth.Journal of Geological Society,London,1994,151:855-868
[217]Fowler M B & Henney P J.Mixed Caledonian appinite magmas:implications for lamprophyre fractionation and high Ba-Sr granite genesis.Contribution to Minerology and Petrology,1996,126:199-215
[218]钱青,钟孙霖,李通艺,等.八达岭基性岩和高Ba-Sr花岗岩地球化学特征及成因探讨:华北和大别-苏鲁造山带中生代岩浆岩的对比.岩石学报,2002,18(3):275-292
[219]Rutter J M & Wyllie P.Melting of vapour-absent tonalite at 10kbar to simulate dehydration-melting in the deep crust.Nature,1988,331:159-160
[220]Rapp R P,Watson E B,Miller C F.Partial melting of amphibolite/eclogite and the origin of Archean trondhjemites and tonalities.Precambrian Research,1991,51:1-25
[221]Rapp R P,Watson E B.Dehydration melting of metabasalt mantle recycling.Journal of Petrology,1995,36:891-931
[222]Panino D A E.What do experiments tell us about the relative contributions of crust and mantle to the origin of granitic magmas.In:Catro A F C,Vigneresse J L(eds).Understanding granites:intergrating new and classical techiniques.Geological Society,London,Special publications,1999,168:55-75
[223]Roberts M P & Clemens J D.Origin of high-potassium,calcalkaline,Ⅰ-type granitiods.Geology,1993,21:825-828
[224]Pefford N & Atherton M.Na-rich partial melts from newly underplated basaltic crust:the Cordillera Blanca Batholith,Peru.Journal of Petrology,1996,37:1497-1521
[225]伍家善,耿元生,沈其韩,等.华北陆台早前寒武纪重大地质事件.北京:地质出版社,1991
[226]李继亮.五台山早元古代碰撞造山带的初步认识.地质科学,1990,1:1-11
[227]Zhao G C,Wilde S A,Cawood P A,et al.Thermal evolution of Archean basement rocks from the eastern part of the Noryh Chian craton and its bearing on tectonic setting.International Geology Review,1998,40:706-721
[228]Wang W.Formation of diamond with mineral inclusions of "mixed" eclogite and peridotite paragenesis.Earth and Planetary Science Letters,1998,160:831-843
[229]高山,金振民.拆沉作用(Delamination)及其壳-幔演化动力学意义.地质科技情报,1997,16(1):1-9
[230]Gao S,Zhang B R,Jin Z M.et al.How mafic is the lower continental crust? Earth planetary Science Letter,1998,161:101-117
[231]高山,张本仁,金振民.秦岭-大别造山带下地壳拆沉作用.中国科学(D辑),1999,29(6):532-541
[232]袁学诚.秦岭岩石圈速度结构与蘑菇云构造模型.中国科学(D辑),1996,26(3):209-215
[233]路凤香,郑建平,李伍平,等.中国东部显生宙地幔演化的主要样式:“蘑菇云”模型.地学前缘,2000,7(1):97-107
[234]郑建平,路凤香,余淳梅,等.地幔置换作用:华北两类橄榄岩及其透辉石微量元素对比.地球科学,2003,28:235-240
[235]徐义刚.岩石圈的热-机械侵蚀和化学侵蚀与岩石圈减薄.矿物岩石地球化学通报,1999,18(1):1-5
[236]余淳梅,郑建平,Griffin WL.汉诺坝橄榄岩捕掳体的单斜辉石LAM-ICPMS分析及其地幔演化意义.地球科学,2006,31(1):93-100
[237]陈丕基.郯庐断裂巨大平移的时代与格局.科学通报,1989,(4):289-293
[238]徐嘉炜,马国锋.郯庐断裂带研究的十年回顾.地质论评,1992,38(4):316-324
[239]Engebretson D C,Cox A,Gordon R G.Relative motions between oceanic and continental plates in the Pacific basins.Geological Society of American Special Publication,1985,206:1-59
[240]Yang J H,Wu F Y,Chung S L,et al.Rapid exhumation and cooling of the Liaonan metamorphic core complex:inferences from ~(40)Ar/~(39)Ar thermochronology and implications for Late Mesozoic extension in the eastern North China Craton.GSA Bulletin,2007,119: 1405-1414
[241]张宏福,Menzies MA,路凤香,等.华北古生代地幔岩捕虏体中石榴石和巨晶石榴石的主、微量元素.中国科学(D辑),2000,30(2):128-134
[242]张宏福,杨岳衡.华北克拉通东部含金刚石金伯利岩的侵位年龄和Sr-Nd-Hf同位素地球化学特征,岩石学报,2007,23(2):285-294
[243]汤华云,郑建平,余淳梅.华北东部新生代玄武岩中橄榄岩捕虏体的流体和稀有气体组成研究.岩石学报,2007,23(6):1531-1542
[244]李延河,李金城,宋鹤彬,等.中国东部新生代玄武岩中幔源包体和高压巨晶的氦同位素研究.中国科学(D),2001,31(8):641-647
[245]马锦龙,陶明信,叶先仁.山东沂沭地区幔源矿物中的流体和稀有气体地球化学研究.中国科学(D),2005,35(11):1019-1027
[246]马锦龙.沂沭断裂带新生代玄武岩及其地幔岩包体中的流体和稀有气体研究.[博士学位论文].兰州:中国科学院兰州地质研究,2003,31-40
[247]徐胜,刘丛强.我国东北部幔源包体中稀有气体丰度和同位素组成.科学通报,2002,47(2):141-146
[248]Tang Huayun,Zheng Jianping,Yu Chunmei.Age and composition of the Rushan intrusive complex in the northern Sulu orogen,eastern China:petrogenesis and lithospheric mantle evolution.Geological Magazine,2008,in press
[249]汤华云,郑建平,陈红汉,等.山东半岛第三纪基性火成岩He-Ar同位素与岩浆起源.中国科学(D辑),2007,37(4):451-459
[250]樊祺诚,隋建立,刘若新,等.汉诺坝榴辉岩相石榴辉石岩-岩浆底侵作用新证据.岩石学报,2001,17(1):1-6
[251]刘勇胜,袁洪林,高山,等.汉诺坝橄榄辉石岩包体锆石U-Pb年龄:97-158Ma岩浆底侵作用和麻粒岩相变质作用之间的成因联系.科学通报,2004,49(8):790-797