山东省大地构造格局和地质构造演化
|
摘要
山东省位于中国大陆的东部,地质构造复杂,其大地构造演化过程可划分为早前寒武纪阶段、中新元古代阶段、古生代阶段和中新生代阶段等4个阶段。
山东省早前寒武纪基底由胶辽微陆块(鲁东地块)、渤鲁微陆块(鲁西地块)和迁怀微陆块(德州地块)组成。山东于2.8Ga以前形成具岛弧性质的沂水和唐家庄古陆核。2.8～2.7Ga,鲁西地区拉张出现初始洋壳,形成具大洋高原环境特点科马提岩、枕状玄武岩组合。2.7～2.56Ga,洋盆消减,俯冲作用造成早期TTG质花岗岩侵位,形成鲁西和鲁东岛弧,为初始不成熟陆壳。2.56～2.4Ga,弧陆碰撞,大量碰撞型花岗岩侵位,第二期TTG质花岗岩系和二长花岗岩系大规模出现,地壳由不成熟陆壳向半成熟陆壳转化;至古元古代岩浆活动完全由代表成熟陆壳的重熔型二长花岗岩构成。2.4～2.1Ga,四海山A型花岗岩的出现标志着刚性陆壳发生拉张减薄,山东陆块基底大规模克拉通化完成:同时,鲁东地区强烈裂陷,形成裂陷盆地。2.1～1.9Ga,鲁东裂陷盆地闭合,古元古代地层发生强烈褶皱。
中新元古代山东陆块归属华北克拉通和大别-苏鲁造山带。中元古代初期(1.84～1.72Ga),地壳发生裂解,济宁裂谷型沉积和鲁西第一期基性岩墙群形成。中元古代晚期(1.20～1.05Ga),地壳再次裂解,海阳所幔源岩浆杂岩和鲁西第二期基性岩墙群形成。新元古代早中期(0.9～0.73Ga),出现同碰撞的S型和I型花岗岩,伴随有强烈的挤压变形作用,形成雄伟的苏鲁碰撞造山带,在造山带北西侧产生具前陆盆地性质的沂沭盆地。新元古代晚期,岚山头A型花岗岩和具后继盆地性质的蓬莱盆地及具上叠盆地性质的石桥盆地的出现,指示强烈造山作用结束,地壳演化开始了另一个新的阶段。
古生代构造单元划分为华北板块陆表海盆地、鲁东被动大陆边缘和大别-苏鲁裂谷盆地。早古生代特征是全域同步缓慢沉降,鲁西以台地相及潮坪、泻湖相碳酸盐岩沉积为主。中、晚奥陶世之后,受板块汇聚俯冲影响,鲁西地区整体抬升剥蚀,缺失晚奥陶世—泥盆纪沉积。晚古生代特征是结束了的单一海相沉积史,完成了海陆交互相向纯陆相沉积的重大古地理转变,晚石炭世至早二叠世沉积了一套准碳酸盐台地和三角洲—潮坪泻湖相的暗色砂泥岩、灰岩和煤层;从中二叠世开始,出现典型的河湖相沉积建造。鲁东被动大陆边缘和大别-苏鲁裂谷盆地的古生代沉积被后期剥蚀殆尽。
中新生代属滨太平洋前陆坳陷带和滨太平洋构造岩浆活动带,包括渤海湾盆地、鲁中隆起、蒙阴盆地群、济宁坳陷、沂沭裂谷、胶北隆起、胶莱盆地、鲁东折返带(超高压带)和苏北折返带(高压带)等次级构造单元。早中三叠世板块作用产生苏鲁碰撞造山带;晚三叠世,形成高钾钙碱性花岗岩类侵入岩,来源于富集岩石圈地幔源区的碱质花岗岩浆的侵位,则标志着后造山拉张作用的开始。侏罗纪时,鲁东地区形成了类似于埃达克岩的高锶花岗岩;鲁西地区局部发生沉降,产生盆地,同时形成了一套与大陆的造陆抬升有关的高镁中基性侵入岩;早侏罗世末,沂沭断裂开始产生并发生左行平移运动。白垩纪构造岩浆活动非常活跃,形成大规模具有弧后拉张性质活动大陆边缘特点的火成岩组合,崂山A型花岗岩的出现标志着强烈岩浆活动趋于尾声;由侏罗纪—白垩纪晚期地幔具有由EMⅠ富集地幔向EMⅡ富集地幔演变和由富集向亏损或由岩石圈向软流圈演变的趋势:受太平洋板块俯冲影响,郯庐断裂发生大幅度左行平移,沂沭断裂二侧伴生形成羽状断裂系统、棋盘格状断裂系统和多层次拆离滑脱构造系统;同时,产生大量断陷盆地,构成隆起与凹陷相间分布的盆山耦合格局。新生代构造格局具有明显的继承性和新生性双重特点,主要地质事件是受断裂控制的新生代盆地和玄武岩喷发。
The position of Shandong province locate in east of China continente.Its geological structure is complicated.Its tectonic evolution can be divided into the early Precambrian stage,Meso- to Neoproterozoic stage,Paleozoic stage and Meso- to Cenozoic stage.
There are three Early Pre-Cambrian micro-continental blocks consisting the basement of Shandong Province.they are Jiaoliao(Ludong),Bolu(Luxi),and Qianhuai(Dezhou).All of them have a complicated evolution history.In ca.2.8 Ga,Yishui Paleo-continental core of the Qianhuai and Tangjiazhuang Paleo-continental core of the Bolu formed,likely resulting from island-arc-like activation.During ca.2.8～2.7Ga,infantile oceanic crust appeared in Luxi area due to lithosphere extension,evidenced by occurrence of komatiite and pillow basalt.During ca.2.7～2.56Ga,the infantile ocean crust subducted under the continental core,giving rise to the Ludong and Luxi continental arcs respectively,which are indicated by the intrusion of the earlier stage TTG granite.By this process,the Luxi and Ludong infantile ensialic continental crust formed.The subsequent arc-continent collision at ca.2.56～2.4Ga has led to a large amount of collision-type plutons including later stage TTG granite and monzonitic granites.At this time, the Shandong crust evolved into semi-mature ones.The Paleoproterozoic anatectic magmatic activity completely matured the Shandong continental crust.During ca.2.4～2.1Ga,the matured Shandong continental crust experienced strongly extension,resulting in Sihaishan A-type grannite in the Luxi area and rift-related magma activity and sediments in the Ludong area.At ca.2.1～1.9Ga,the Ludong rift closed suggesting the completion of the cratonization in Shandong Province.
Above mentioned cratonization resulted in two different cratons with different evolutional history: the Luxi belongs to the North China Craton and Ludong to the Dabie-Sulu orogenic belt at Mesoproterozoic and Neoproterozoic era.At Early Mesoproterozoic(1.84～1.72 Ma),crustal extension of the Luxi craton resulted in the Jining rift-type sedimentation and the first stage marie dike Swarm.Another crust extension occurred at Late Mesoproterozoic(1.2～1.05 Ma),the Haiyangsuo mantle-sourced magmatic rocks developed in the Ludong area,and the second stage mafic dyke swarm occurred in the Luxi area.During the early and middle period of Neoproterozoic(0.9～0.73 Ma),syncollision S-type and I-type granites and widespread compressional structures suggest a strong collision occurring in the Ludong area,resulting in the great Sulu collision orogenic belt.The Yishui basin as the foreland one,developed in the northwest of the Sulu orogenic belt.The collision might end at Late Neoproterozoic,being suggested by the emergence of Lanshantou A-type granite,and Penglai and Shiqiao basins which were superposed upon the orogenic belt.
During the Paleozoic period,the Shandong Province might consisted of three tectonic units:the North China shallow marine basin(west Shandong),a passive continental margin basin(east Shandong) and the Dabie-Sulu rift basin(southeast Shandong).Whole-area scale outcropping of the early Paleozoic strata suggests a whole-area-scale subsidence synchronously in the Luxi area at the early Paleozoic.The most significant sedimentary facies includes platform,tidal flat,and lagoon facies,implying the earlier Paleozoic subsidence was quite slow.The absence of the Upper Ordovician to Devonian strata in the Luxi area suggests regional scale uplift during this period.Since the Late Carboniferous,a new continental basin developed overlapping the earlier Paleozoic strata,where deposited meta-platform,deltaic,tidal flat,and lagoon facies limestone,dark arenited mudstone,and coal bed.The development of the Late Paleozoic basin indicates a complete transformation of the paleogeography from the marine to terrestrial ones.The Palaeozoic sediments in the Ludong area were completely eroded during the Mesozoic uplifting;sparse information comes from provenance analyses on the strata of the Mesozoic basin.
In the Mesozoic and Cenozoic period,Shandong Province totally belongs to the circum-Pacific foreland depression belt and the circum-Pacific magmatic province,which is consisted of sub-units as bellow:Bohaiwan basin,Luzhong Rise,Mengyin basin groups,Jining depression,Yishu rift,Jiaobei Rise, Jiaolai basin,Ludong exhumed UHP(ultrahigh pressure metamorphic) belt,and Subei exhumed HP belt (high pressure metamorphic belt).The Early Triassic collision between the south China and North China plates given raise the Sulu collision orogenic belt.During the Late Triassic,high potassium calc-alkaline granites intruded into the orogenic belt,which sourced from enriched lithosphere mantle,and indicated the beginning of post-orogen extensional collapse.In the Jurassic,Adakite-like high Sr granite developed in the Ludong area.Meanwhile,a series of extensional basins developed in the Luxi area,indicating locally crustal subsidence alternative with adjacent rising.The rising was accompanied by a suit of high Mg basic to andesitic intrusions.In the last stage of the Late Jurassic,the Yishu fault system began to sliding in sinistral manner.Intensive Cretaceous magmatic activity suggests the beginning of another thermo-tectonic event in the Shandong Province.The widespread Cretaceous igneous rock have the same geochemical features as those formed under back-arc spreading setting.The spreading-related magmatic activation ended in the appearing of the Laoshan A-type granite.From the Triassic to Cretaceous,the mantle of the Shandong province changed from the EMⅠ- to EMⅡ- type although it remained enriched.Also due to the westward subduction of the Pacific Ocean plate,significant sinistral movement occurred along the Tanlu fault system.Besides the sinistral displacement,large amount of plume-like,chess-board-like fault systems,and multi-level detachment developed within the two displaced fault-wall blocks.Meanwhile, several sag basins formed due to the detachments,resulting in ridge-basin structures.During the Cenozoic, the major tectonic grains of Shandong Province are basins that were controlled by boundary faults.Part of the boundary faults are re-active ones,while the other are newly formed.The formation of the Cenozoic basins is accompanied by basaltic volcano eruption.
山东省早前寒武纪基底由胶辽微陆块(鲁东地块)、渤鲁微陆块(鲁西地块)和迁怀微陆块(德州地块)组成。山东于2.8Ga以前形成具岛弧性质的沂水和唐家庄古陆核。2.8～2.7Ga,鲁西地区拉张出现初始洋壳,形成具大洋高原环境特点科马提岩、枕状玄武岩组合。2.7～2.56Ga,洋盆消减,俯冲作用造成早期TTG质花岗岩侵位,形成鲁西和鲁东岛弧,为初始不成熟陆壳。2.56～2.4Ga,弧陆碰撞,大量碰撞型花岗岩侵位,第二期TTG质花岗岩系和二长花岗岩系大规模出现,地壳由不成熟陆壳向半成熟陆壳转化;至古元古代岩浆活动完全由代表成熟陆壳的重熔型二长花岗岩构成。2.4～2.1Ga,四海山A型花岗岩的出现标志着刚性陆壳发生拉张减薄,山东陆块基底大规模克拉通化完成:同时,鲁东地区强烈裂陷,形成裂陷盆地。2.1～1.9Ga,鲁东裂陷盆地闭合,古元古代地层发生强烈褶皱。
中新元古代山东陆块归属华北克拉通和大别-苏鲁造山带。中元古代初期(1.84～1.72Ga),地壳发生裂解,济宁裂谷型沉积和鲁西第一期基性岩墙群形成。中元古代晚期(1.20～1.05Ga),地壳再次裂解,海阳所幔源岩浆杂岩和鲁西第二期基性岩墙群形成。新元古代早中期(0.9～0.73Ga),出现同碰撞的S型和I型花岗岩,伴随有强烈的挤压变形作用,形成雄伟的苏鲁碰撞造山带,在造山带北西侧产生具前陆盆地性质的沂沭盆地。新元古代晚期,岚山头A型花岗岩和具后继盆地性质的蓬莱盆地及具上叠盆地性质的石桥盆地的出现,指示强烈造山作用结束,地壳演化开始了另一个新的阶段。
古生代构造单元划分为华北板块陆表海盆地、鲁东被动大陆边缘和大别-苏鲁裂谷盆地。早古生代特征是全域同步缓慢沉降,鲁西以台地相及潮坪、泻湖相碳酸盐岩沉积为主。中、晚奥陶世之后,受板块汇聚俯冲影响,鲁西地区整体抬升剥蚀,缺失晚奥陶世—泥盆纪沉积。晚古生代特征是结束了的单一海相沉积史,完成了海陆交互相向纯陆相沉积的重大古地理转变,晚石炭世至早二叠世沉积了一套准碳酸盐台地和三角洲—潮坪泻湖相的暗色砂泥岩、灰岩和煤层;从中二叠世开始,出现典型的河湖相沉积建造。鲁东被动大陆边缘和大别-苏鲁裂谷盆地的古生代沉积被后期剥蚀殆尽。
中新生代属滨太平洋前陆坳陷带和滨太平洋构造岩浆活动带,包括渤海湾盆地、鲁中隆起、蒙阴盆地群、济宁坳陷、沂沭裂谷、胶北隆起、胶莱盆地、鲁东折返带(超高压带)和苏北折返带(高压带)等次级构造单元。早中三叠世板块作用产生苏鲁碰撞造山带;晚三叠世,形成高钾钙碱性花岗岩类侵入岩,来源于富集岩石圈地幔源区的碱质花岗岩浆的侵位,则标志着后造山拉张作用的开始。侏罗纪时,鲁东地区形成了类似于埃达克岩的高锶花岗岩;鲁西地区局部发生沉降,产生盆地,同时形成了一套与大陆的造陆抬升有关的高镁中基性侵入岩;早侏罗世末,沂沭断裂开始产生并发生左行平移运动。白垩纪构造岩浆活动非常活跃,形成大规模具有弧后拉张性质活动大陆边缘特点的火成岩组合,崂山A型花岗岩的出现标志着强烈岩浆活动趋于尾声;由侏罗纪—白垩纪晚期地幔具有由EMⅠ富集地幔向EMⅡ富集地幔演变和由富集向亏损或由岩石圈向软流圈演变的趋势:受太平洋板块俯冲影响,郯庐断裂发生大幅度左行平移,沂沭断裂二侧伴生形成羽状断裂系统、棋盘格状断裂系统和多层次拆离滑脱构造系统;同时,产生大量断陷盆地,构成隆起与凹陷相间分布的盆山耦合格局。新生代构造格局具有明显的继承性和新生性双重特点,主要地质事件是受断裂控制的新生代盆地和玄武岩喷发。
The position of Shandong province locate in east of China continente.Its geological structure is complicated.Its tectonic evolution can be divided into the early Precambrian stage,Meso- to Neoproterozoic stage,Paleozoic stage and Meso- to Cenozoic stage.
There are three Early Pre-Cambrian micro-continental blocks consisting the basement of Shandong Province.they are Jiaoliao(Ludong),Bolu(Luxi),and Qianhuai(Dezhou).All of them have a complicated evolution history.In ca.2.8 Ga,Yishui Paleo-continental core of the Qianhuai and Tangjiazhuang Paleo-continental core of the Bolu formed,likely resulting from island-arc-like activation.During ca.2.8～2.7Ga,infantile oceanic crust appeared in Luxi area due to lithosphere extension,evidenced by occurrence of komatiite and pillow basalt.During ca.2.7～2.56Ga,the infantile ocean crust subducted under the continental core,giving rise to the Ludong and Luxi continental arcs respectively,which are indicated by the intrusion of the earlier stage TTG granite.By this process,the Luxi and Ludong infantile ensialic continental crust formed.The subsequent arc-continent collision at ca.2.56～2.4Ga has led to a large amount of collision-type plutons including later stage TTG granite and monzonitic granites.At this time, the Shandong crust evolved into semi-mature ones.The Paleoproterozoic anatectic magmatic activity completely matured the Shandong continental crust.During ca.2.4～2.1Ga,the matured Shandong continental crust experienced strongly extension,resulting in Sihaishan A-type grannite in the Luxi area and rift-related magma activity and sediments in the Ludong area.At ca.2.1～1.9Ga,the Ludong rift closed suggesting the completion of the cratonization in Shandong Province.
Above mentioned cratonization resulted in two different cratons with different evolutional history: the Luxi belongs to the North China Craton and Ludong to the Dabie-Sulu orogenic belt at Mesoproterozoic and Neoproterozoic era.At Early Mesoproterozoic(1.84～1.72 Ma),crustal extension of the Luxi craton resulted in the Jining rift-type sedimentation and the first stage marie dike Swarm.Another crust extension occurred at Late Mesoproterozoic(1.2～1.05 Ma),the Haiyangsuo mantle-sourced magmatic rocks developed in the Ludong area,and the second stage mafic dyke swarm occurred in the Luxi area.During the early and middle period of Neoproterozoic(0.9～0.73 Ma),syncollision S-type and I-type granites and widespread compressional structures suggest a strong collision occurring in the Ludong area,resulting in the great Sulu collision orogenic belt.The Yishui basin as the foreland one,developed in the northwest of the Sulu orogenic belt.The collision might end at Late Neoproterozoic,being suggested by the emergence of Lanshantou A-type granite,and Penglai and Shiqiao basins which were superposed upon the orogenic belt.
During the Paleozoic period,the Shandong Province might consisted of three tectonic units:the North China shallow marine basin(west Shandong),a passive continental margin basin(east Shandong) and the Dabie-Sulu rift basin(southeast Shandong).Whole-area scale outcropping of the early Paleozoic strata suggests a whole-area-scale subsidence synchronously in the Luxi area at the early Paleozoic.The most significant sedimentary facies includes platform,tidal flat,and lagoon facies,implying the earlier Paleozoic subsidence was quite slow.The absence of the Upper Ordovician to Devonian strata in the Luxi area suggests regional scale uplift during this period.Since the Late Carboniferous,a new continental basin developed overlapping the earlier Paleozoic strata,where deposited meta-platform,deltaic,tidal flat,and lagoon facies limestone,dark arenited mudstone,and coal bed.The development of the Late Paleozoic basin indicates a complete transformation of the paleogeography from the marine to terrestrial ones.The Palaeozoic sediments in the Ludong area were completely eroded during the Mesozoic uplifting;sparse information comes from provenance analyses on the strata of the Mesozoic basin.
In the Mesozoic and Cenozoic period,Shandong Province totally belongs to the circum-Pacific foreland depression belt and the circum-Pacific magmatic province,which is consisted of sub-units as bellow:Bohaiwan basin,Luzhong Rise,Mengyin basin groups,Jining depression,Yishu rift,Jiaobei Rise, Jiaolai basin,Ludong exhumed UHP(ultrahigh pressure metamorphic) belt,and Subei exhumed HP belt (high pressure metamorphic belt).The Early Triassic collision between the south China and North China plates given raise the Sulu collision orogenic belt.During the Late Triassic,high potassium calc-alkaline granites intruded into the orogenic belt,which sourced from enriched lithosphere mantle,and indicated the beginning of post-orogen extensional collapse.In the Jurassic,Adakite-like high Sr granite developed in the Ludong area.Meanwhile,a series of extensional basins developed in the Luxi area,indicating locally crustal subsidence alternative with adjacent rising.The rising was accompanied by a suit of high Mg basic to andesitic intrusions.In the last stage of the Late Jurassic,the Yishu fault system began to sliding in sinistral manner.Intensive Cretaceous magmatic activity suggests the beginning of another thermo-tectonic event in the Shandong Province.The widespread Cretaceous igneous rock have the same geochemical features as those formed under back-arc spreading setting.The spreading-related magmatic activation ended in the appearing of the Laoshan A-type granite.From the Triassic to Cretaceous,the mantle of the Shandong province changed from the EMⅠ- to EMⅡ- type although it remained enriched.Also due to the westward subduction of the Pacific Ocean plate,significant sinistral movement occurred along the Tanlu fault system.Besides the sinistral displacement,large amount of plume-like,chess-board-like fault systems,and multi-level detachment developed within the two displaced fault-wall blocks.Meanwhile, several sag basins formed due to the detachments,resulting in ridge-basin structures.During the Cenozoic, the major tectonic grains of Shandong Province are basins that were controlled by boundary faults.Part of the boundary faults are re-active ones,while the other are newly formed.The formation of the Cenozoic basins is accompanied by basaltic volcano eruption.
引文
[1]任纪舜,郝杰,肖藜薇.回顾与展望:中国大地构造学.地质论评,2002,18(2):113-124.
[2]杨巍然.地球表层系统与中国区域大地构造的研究发展.地学前缘(中国地质大学(北京):北京大学),2006,13(6):102-110.
[3]Meyerhoff A A,Taner I,Morris AMS,等(白星碧,关玉华,陈华译).全球构造的新概念--颤动构造简介.北京:中国地质矿产信息研究院.
[4]Maruyama.plume tectonics.J.Geol.Soc.Japan,1994,100(1):24-49.
[5]李晓波.造山模式的新框架--大陆动力学演化过程.中国地质,2002,29(2):25-28.
[6]李锦轶,肖序常.1998.板块构造学说与大陆动力学--纪念李春昱教授逝世十周年(代前言).地质论评,44(4):337-338.
[7]丁国瑜.1999.大陆动力学地学研究的新动向.内陆地震,13(4):289-290.
[8]曹国权.1990.试论“胶南地体”.山东地质,6(2):1-10
[9]牛树银,胡华斌,毛景文,等.鲁西地区地质构造特征及其形成机制.中国地质,2004,31(1):34-39.
[10]宋明春,王沛成,梁帮启,等.山东省区域地质.济南:山东省地图出版社,2003,25-720.
[11]黄汲清,任纪舜,姜春发,等.中国大地构造基本轮廓.地质学报,1977,51(2):117-135.
[12]任纪舜,王作勋,陈炳蔚,等.从全球看中国的大地构造--中国及邻区大地构造图的简要说明.北京:地质出版社,1999.
[13]李春昱.中国板块构造的轮廓.中国地质科学院院报,1980,2(1),11-22.
[14]李春昱,王荃,刘雪亚,等.亚洲大地构造图(1:800万)及说明书.北京:地图出版社,1982.
[15]李春昱.在经济体制改革时期,地质工作如何面向经济建设.大自然探索,1985,4(13):9-10.
[16]李锦轶.中国大陆地壳“镶嵌与叠覆”的结构特征及其演化.地质通报,2004,23(9-10):986-1004.
[17]程裕淇主编.中国区域地质概论.北京:地质出版社,1994,16-17.
[18]任纪舜,陈廷愚,牛宝贵,等.中国东部及邻区大陆岩石圈的构造演化与成矿.北京:科学出版社,1992,26-27.
[19]伍家善,耿元生,沈其韩,等.中朝古大陆地质特征及构造演化.北京:地质出版社,1998,1-212.
[20]邓晋福,吴宗絮,赵国春,等.华北地台前寒武花岗岩类陆壳演化与克拉通形成.岩石学报,1999,15(2):190-198.
[21]Bai J,Dai F Y.Archean crust of China.In:Ma X Y,Bai J,eds.Precambrian Crust Evolution of China.Beijing:Geological Publishing House,1998.15-86.
[22]李继亮,王凯怡,王清晨,等.五台山早元古代碰撞带初步认识.地质科学,1990,25(1):1-11.
[23]李继亮,王凯怡,郝杰,等.山西五台山晚太古代镁铁质-超镁铁质岩:一种可能的古蛇绿岩.岩石学报,1997,13(2):139-151.
[24]白瑾,王汝铮,郭进京,等.五台山早前寒武纪重大地质事件及其年代.北京:地质出版社,1992,1-55.
[25]翟明国,郭敬辉,闫月华,等.中国华北太古宙高压麻粒岩的发现及初步研究.中国科学,B辑, 1992.(12):1325-1330.
[26]翟明国,郭敬辉,李江海等,等.太古宙退化榴辉岩的发现及其地质意义.科学通报,1995,40(17):1590-1594.
[27]李江海,钱祥麟.太行山北段龙泉关剪切带研究.山西地质,1991,6(1):17-29.
[28]吴昌华,钟长汀.华北陆台中段吕梁期的SW-NE向碰撞.前寒武纪研究进展,1998,21(3):28-50
[29]Liu D Y,Nutman A P,Compston W,et al.Remnants of 3800 Ma crust in the Chinese Part of the Sino-Korean craton.Geology,1992,(20):339-342.
[30]沈其韩,钱祥麟.中国太古宙地质体组成、阶段划分和演化.地球学报,1995,(2):113-120.
[31]李江海,钱祥麟,翟明国.华北北部麻粒岩相构造区划及其早前寒武纪构造演化.地质科学,1997,32(3):254-265.
[32]翟明国,卞爱国.华北克拉通新太古代末超大陆拼合及古元古代末-中元古代裂解.中国科学D 辑,2000,30(增刊):129-137.
[33]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):539-549.
[34]李江海,牛向龙,程素花,钱祥麟.大陆克拉通早期演化历史探讨:以华北为例.地球科学--中国地质大学学报,2006,31(3):285-293.
[35]翟明国.华北克拉通2.1-1.7Ga地质事件群的分解和构造意义探讨.岩石学报,2004,20(6):1343-1354.
[36]白瑾,黄学光,王惠初,等.中国前寒武纪地壳演化(第二版).北京:地质出版社,1996,20-60.
[37]耿元生,万渝生,沈其韩.华北克拉通早前寒武纪基性火山作用与地壳增生.地质学报,2002,76(2):199-208.
[38]李江海,刘守偈,侯贵廷.华北中部古元古代末期构造-热事件性质及其构造成因模式.中国地质.2006,33(6):1256-1266.
[39]Kusky T.,Li J.Paleoproterozoic tectonic evolution of the North China craton.Journal of Asian Earth Sciences,2003,22(4):383-397.
[40]赵宗溥.中朝准地台前寒武纪地质演化.北京:科学出版社,1993,1-83.
[41]沈其韩,沈比,耿元生,等.山东沂水杂岩的岩石组成与地质演化.北京:地质出版社,2000,5-73.130-142.
[42]程裕淇,沈其韩,等.山东新泰一带泰山群变质岩和岩浆岩类岩石的地质地球化学研究.地质论评,1964,22(3):198-209.
[43]程裕洪,沈其韩,王泽九.山东太古代雁翎关变质火山-沉积岩.北京:地质出版社,1982.
[44]程裕淇,沈其韩,王泽九.山东新泰雁翎关一带泰山群变质岩系的初步研究.地质矿产研究,1987,(3).
[45]程裕淇,徐惠芬.对山东新泰晚太古代雁翎关组中科马提岩类的一些认识.中国地质,1991,(4):31-32.
[46]徐惠芬.鲁西花岗绿岩带和变质作用.山东地质,1990,6(1):50-57.
[47]徐惠芬,董一杰,施允亨,等.鲁两花岗绿岩带.北京:地质出版社,1992.
[48]程素华,李江海,陈征,等.山东科马提岩地球化学特征及其意义.岩石矿物学杂志,2006,25(2):119-126.
[49]曹国权,等著.鲁西早前寒武纪地质.北京:地质出版社,1996,48-93,112-123.
[50]Kusky T M and Polat A.Growth of granit-greenstone terranes at convergent margins and stabilizaton of Archean craton.tectoniphysics,1999,305:45-73.
[51]Myers J S.The generation and assembly of an Archean supercontinent:Evidence from the Yilgarn craton western Australia.In:Coward M P,Ries A C.Geological society' s Special Publication,1995,95:143-154.
[52]Moores E M.Pre-1 Ga(pre-Rodinia) ophiolites:their tectonic and environmental implications.GSA Bulletin 2002,114(1):80-90.
[53]Foley F S,Buhre S,Jacob D E.Evolution of the Archaean crust by delamination an shallow subduction.Nature,2003,421:249-252.
[54]Baker F.Trondhjemites,dacites and related rocks.New York.Elsew.Sci.Pub.Comp pp.1979,321.
[55]苏尚国,邓晋福,梁风华,等.山东沂水紫苏花岗岩中残品相矿物的发现及紫苏花岗岩的形成过程.地学前缘,2003,10(3):257-267.
[56]Eby G N.Chemical subdivision ofthe A-Type granitoids:petrogenesis and implications.Geology,1992,20:641-644.
[57]魏春生.A型花岗岩成因模式及其地球动力学意义.地学前缘,2000,7(1):238.
[58]卢良兆,徐学纯,刘福来,著.中国北方前早寒武纪孔兹岩系.长春:长春山版社,1996.
[59]张本仁,高山,韩吟文.秦巴区域地球化学文集.武汉:中国地质大学山版社,1990.
[60]李江海,穆剑.我国境内格林威尔期造山带的存在及其对中元古代末期超大陆再造的制约.地球科学,1999,34(3):259-272.
[61]吴根耀.白垩纪:中国及邻区板块构造演化的一个重要变换期.中国地质,2006,33(1):64-77.
[62]王鸿祯,张世红.全球前寒武纪基底构造格局与古大陆再造问题.地球科学--中国地质大学学报,2002,27(5):467-481.
[63]邵济安,张履桥,李大明.华北克拉通元古代的三次伸展事什.岩石学报,2002,16(2):152-160.
[64]亓润章.鲁西前寒武纪地层划分及含铁建造地质特征.南京地质矿产研究所所刊,1984,5(3).
[65]张增奇,刘明渭主编.山东省岩石地层.武汉:中国地质大学出版社,1996,81-83.
[66]Hugh R.Rollinson.Using geochemical data:evaluation,presentation,interpretation.Langman Singapore Publishers Ltd,1993.
[67]王岳军,彭头平,范蔚茗,等.华北陆块基性岩墙群及其构造意义.矿物岩石地球化学通报,2007,26(1):1-9.
[68]王世进.鲁西前寒武纪侵入岩期次划分及基本特征.中国区域地质,1991,4:298-307.
[69]侯贵廷,刘玉琳,李江海,等.关于基性岩墙群的U-Pb SHRIMP地质年代学的探讨.岩石矿物学杂志,2005,14(3):179-185.
[70]侯贵廷,李江海,刘玉琳,等.华北克拉通古元古代末的伸展事件:拗拉谷与岩墙群.自然科学进展,2005,15(11):1366-1373.
[71]李曙光,孙卫东,葛宁洁,等.青岛榴辉岩相蛇绿混杂岩的岩石学证据及退变质P-T轨迹.岩石学报,1992,(4):351-361.
[72]王仁民,安家桐,赖兴运.胶东蛇绿岩套的发现及其地质意义.岩石学报,1995,11(增刊):211-227.
[73]倪志耀,王仁民.胶东元古宙变质硅质岩的地球化学及成因.矿物岩石,2001,21(1):59-66.
[74]赵大升,张旗,刘若新,等.山东梭罗树岩体橄榄岩中的尖品石-石榴石相转变的初步研究.科学通报,1993,38(17):1582-1584.
[75]Jahn B M,Cornichet J,Cong B.Crustal Evalution of The Qinling-Dabie orogen:Isotopic and Geochemical Constraints From Coesite-bearing Eclogites of The Su-Lu and Dabie Terranes,China.Chinese Science Bulletin,1995,40:116-119.
[76]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):1-9.
[77]宋明春,张景信,张希道.山东省胶南地区斜长花岗岩的发现.中国区域地质,1998,17(3):273-277.
[78]刘福来,许志琴,杨经绥,等.中国大陆科学钻探工程主孔及周边地区花岗质片麻岩的地球化学性质和超高压变质作用标志的识别.岩石学报,2004,20(1):9-26.
[79]Barbarin B.Granitoids main petrogenetic classifications in relation to origin and tectonic setting.Geol.J,1990,25:227-238.
[80]Leech M L.Arrested orogenic development:eclogitization,delamination,and tectonic collapse.Earth Planet Sci Lett,2001,185(1-2):149-159.
[81]马吕前,杨坤光,明厚利,等.大别山中生代地壳从挤压转向伸展的时间:花岗岩的证据.中国科学,2003,33(9):817-827.
[82]Whalen J A,Currie K L,Chappell B W.A-type granites:Geochemical characteristics,discrimination and petrogenesis.Contributions to Mineralogy and Petrology,1987,95:407-419.
[83]胡健,邱检生,王汝成,等.江苏东海片麻状碱性花岗岩的地球化学及其构造指示意义.地质学报,2006,80(12):1877-1891.
[84]薛怀民,刘福来,孟繁聪.苏鲁造山带胶东区段花岗片麻岩类的常量与微量元素地球化学:扬子克拉通北缘新元古代活动大陆边缘的证据.岩石学报,2006,22(7):1779-1790.
[85]苏玉平,唐红峰.A型花岗岩的微量元素地球化学.矿物岩石地球化学通报,2005,24(3):245-251.
[86]董树文,张勇,黄德志.苏北超高压变质带石桥构造窗地质特征.安徽地质,1996,6(1):9-13.
[87]钱存超,汤加富,常丹岩.安徽大别造山带南部浅变质岩层分布、层序与时代研究.地层学杂志,2001,25(3):222-227.
[88]乔秀夫,高林志.华北中新元古代及早古生代地震灾变事件及与Rodinia的关系.科学通报,1999,44(16):1753-1758.
[89]宋明春,吕法堂.山东胶南地区榴辉岩围岩中白云母的初步研究.矿物岩石,1997,17(2):17-21
[90]张儒媛,从柏林,刘忠光.苏鲁超高压变质地体及其成冈解释.岩石学报,1993,9(3):211-222
[91]李锦轶,杨天南,陈文,等.中国东部东海地区超高压变质岩构造变形事件的~(40)Ar/~(39)Ar定年与超高压变质岩折返过程的重建.地质学报,2004,78(1):97-108.
[92]宋明春,宋志勇,安丰琴.苏鲁超高压变质带南部浅变质岩的全岩Rb-Sr同位素年龄.江苏地质.2004,28(3):140-144.
[93]朱光,徐嘉炜,Futches W R,等.胶北蓬莱群的同位素年龄及其区域大地构造意义.地质学报,1994,68:158-172.
[94]王来明,宋明春,王沛成,等.苏鲁超高压变质带的结构与演化.北京:地质出版社,2005.
[95]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):229-237.
[96]Lindsay J F,Korsch R J,Wilford J R.Timing the breakup of a Neoproterozoic supercontinent:Evidence from Australian intrac-ratonic basins.Geology,1987,15:1061-1064.
[97]McLelland J,Daly J S,McCulloch J M.The Grenville orogenic cycle(ca.1350-1000Ma):an Adirondack perspective.Tectonophysics,1996,256:1-28.
[98]Meert J G,Torsvik T H.The making and unmaking of a supercontinent:Rodinia revisited. Tectonophysics,2003,375(1-4):261-288.
[99]McMenamin M A S,McMenamin D L S.The emergence of animals,The Cambrian breakthrough.New York:Columbia University Press,1990:1-217.
[100]Li X H,Li Z X,Ge WC,Zhou H W,Li WX,Liu Y,Wingate M T D.Neoproterozoic granitoids in south China:crustal melting above a mantle plume at ca 825Ma?Precambrian research 2003,122:45-83.
[101]任纪舜,肖藜薇.中国大地构造与地层区划.地层学杂志,2001,25(增刊):361-369.
[102]李锦轶,何国琦,徐新.新疆北部及邻区地壳构造格架及其形成过程的初步探讨,地质学报,2006,8(1):148-168.
[103]邵济安,唐克东.蛇绿岩与古蒙古洋的演化.见:张旗主编,蛇绿岩与地球动力学研究.北京:地质出版社,1996,117-120.
[104]段吉业,刘鹏举,夏德馨.浅析华北板块中元古代-古生代构造格局及其演化.现代地质,2002,(4):331-228.
[105]杨志坚.胶东地块研究取得新进展.中国区域地质,1992,11(1):43-50.
[106]牛保祥,刘书才,刘怀书.栖霞地区蓬莱群的时代属震旦纪.山东地质,1996,12(1):63-68.
[107]郭振一,孙秀珠.胶莱拗陷南缘晚侏罗世鲕状灰岩砾石中有孔虫、蜒化石的发现及其大地构造意义.地质论评,1985,31(2):179-181.
[108]牛保祥,陆荣莉,杨斌,等.鲁东地块的大地构造位置.山东国土资源,2004,20(4):41-45.
[109]刘占声主编.郯庐断裂带中段地质.长春:吉林科学技术出版社,1995,65-69.
[110]赵达,程立人,刘茂修.胶南地区五莲群中管孔藻类的发现及其意义.中国区域地质,1995,14(4):379-384.
[111]周春平.苏北.胶南地体构造初探.地震地质,1989,11(1):60-64.
[112]马杏垣.江苏响水至内蒙满都拉地学断面南北两段的地质观察.地球科学,1989,14(1):1-7.
[113]余和中,韩守华,谢锦龙,等.华北板块东南缘原型沉积盆地类型与构造演化.石油与天然气地质,2005,27(2):244-252.
[114]许志琴,杨经绥,李海兵,等.中央造山带早古生代地体构架与高乐/超高压变质带的形成.地质学报,2006,80(12):1793-1806.
[115]张宏福,杨岳衡.华北克拉通东部含金刚石金伯利岩的同位素年龄和Sr-Nd-Hf同位素地球化学特征.岩石学报,2007,23(2):285-294.
[116]Dobbs P N,Duncan D J,Hu S,et al.The geology of the Mengyin kimberlites,Shandong,China.In:Meyer H O A,Leonardos O H(ed).Proc 5th Int Kimb Conf 1.Diamonds:characterisation,genesis and exploration,CPRM Brasilia,1994,106-115.
[117]路风香,郑建平.华北地台古生代岩石圈地幔特征及深部过程.见:池际尚,路风香.华北地台金伯利岩及古生代岩石圈地幔特征.北京:科学技术出版社,1996,215-274.
[118]Meyer H O A,Zhang A,Milledge H j,et al.Diamonds and inclusions from Chinese kimberlites.In:Meyer H O A,Leonardos O H(ed).Proc 5th Int Kimb Conf 1.Diamonds:characterisation,genesis and exploration,1994,98-105.
[119]Harris J W,Duncan D J,Zhang F,et al.The physical characteristics and syngenetic inclusion geochemistry of diamonds from Pipe 50,Liaoning province,People' s Republic of China.In:Meyer H O A,Leonardos O H(ed).Proc 5th Int Kimb Conf 1.Diamonds:characterisation,genesis and exploration,1994,106-115.
[120]张开均.华北板块东缘晚古生代火山活动及其大地构造意义.中国煤田地质,1998,10(3):10-20.
[121]王永平.济宁、巨野、滕县煤田石炭-二叠纪的火山碎屑岩.煤田地质与勘探,1990,20(4):9-11.
[122]钟蓉,孙善平,傅泽明.山东及邻区晚石炭世-早二叠世火山事件沉积及地层对比.地质学报,1996,70(2):142-152.
[123]杨巍然,王国灿,简平.大别造山带构造年代学.武汉:中国地质大学出版社,2000:141.
[124]杨巍然,简平,韩郁菁.大别造山带加里东期高压、超高压变质作用的确定及其意义.地学前缘,2002,9(4):273-283.
[125]车自成,刘良,罗金海.中国及其邻区区域大地构造学.北京:科学出版社,2002,519.
[126]李廷栋,莫杰.中国滨太平洋构造域构造格架和东海地质演化.海洋地质与第四纪地质,2002,22(4):1-6.
[127]邵济安,牟堡磊,张履桥.华北东部构造格局转换过程中的深部作用与浅部响应.地质论评,2000,46(1):32-40.
[128]徐贵忠,周瑞,闫臻,等.论胶东地区中生代岩石圈减薄的证据及其动力学机制.大地构造与成矿学,2001,25(1):368-380.
[129]翟明国,樊祺诚,张宏福,隋建立.华北东部岩石圈减薄中的下地壳过程:岩浆底侵、置换与拆沉作用.岩石学报,2005,21(6):1509-1526.
[130]苗来成,罗镇宽,关康,黄佳展.玲珑花岗岩中锆石的离子质谱U-Pb年龄及其岩石学意义.岩石学报,1998,14(2):
[131]闫峻,陈江峰,谢智,等.鲁东晚白垩世玄武岩及其中幔源包体的岩石学和地球化学研究.岩石学报,2005,21(1):99-112.
[132]周立宏,李三忠,赵国春,等.华北克拉通中东部基底构造单元的重磁特征.地球物理学进展,2004,19(1):91-100.
[133]万天丰,朱鸿.中国大陆及邻区中生代-新生代大地构造与环境变迁.现代地质,2002,(2):107-120.
[134]Jin-Hui Yang,Sun-Lin Chung,Simon A.Wilde,et al.Petrogenesis of post-orogenic syenites in the Sulu Orogenic Belt,East China:geochronological,geochemical and Nd-Sr isotopic evidence.Chemical Geology,214(2005):99-125.
[135]Chen J F,Xie Z,Li HM,et al.U-Pb zircon for a collision-related K-rich complex at Shidao in the Sulu ultrahigh pressure terrane,China.Chemical Journal,2003,37(1):35-46.
[136]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,2004,1025-1038.
[137]穆克敏,林景仟,邹祖荣,等.华北地台区花岗质岩石的成因.长春:吉林科学技术出版社,1989,172-225.
[138]谢智.大别-苏鲁造山带岩石的锆石U-Pb年龄:[博士研究生学位论文].合肥:中国科学技术大学,1998,8-14.
[139]林景仟,谭东娟,迟效国.胶东半岛中生代花岗岩.北京:科学出版社,1992,208.
[140]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,2005,2l(4)1281-1301.
[141]宋明春,韩景敏.苏鲁超高压变质带北段夏河城岩体的形成时代及其意义.地质论评,2006, 52(5):601-608.
[142]宋明春,赵庆龄.山东日照官山闪长玢岩锆石SHRIMP年龄:印支期岩浆热事件及其对超高压变质岩折返历史的限定.地质通报,2004,23(12):1254-1258.
[143]Sun WD,Li S G,Chen Y D and Li Y J.Time of synorogenic granitoids in the South Qinling,Central China:constraints on the evolution of the Qinling-Dabie orogenic belt.Journal of Petrology,2002,110:457-468.
[144]肖庆辉,邓晋福,马大铨,等著.花岗岩研究思维与方法.北京:地质出版社,2002,247-254。
[145]陆孝平,吴福元,赵成弼,张艳斌.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.
[146]崔盛芹,李锦蓉.试论中国滨太平洋的印支运动.地质学报,1983,57(1):51-62.
[147]李之彤,赵春荆.东北地区的印支运动.地质科学,1985,20(3):211-223.
[148]宋明春,宋志勇,安丰琴.苏鲁超高压变质带南部浅变质岩的全岩Rb-Sr同位素年龄.江苏地质.2004,28(3):140-144.
[149]张旗,王阎,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.
[150]葛小月,李献华,陈志刚,等.中国东部高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.
[151]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.
[152]Guo Jinghui,Chen Fukun,Wolfgang Siebel,Cong Boling.Melting of the once deeply subducted continental slab:revealed by SHRIMP zircon ages of post-collisional granites from SuLu UHP zone,eastern China.Terra Nova,2003.
[153]杨进辉,朱美妃,刘伟,等.胶东地区郭家岭花岗岩的地球化学特征及成冈.岩石学报,2003,19(4):692-700.
[154]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.
[155]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.
[156]Zen E-an and Hammarstrom J M.Magmatic epidote and its petrologic significance.Geology,1984,12:515-518.
[157]张旗,李承东,王阎,等.中国东部中生代高Sr低Yb和低Sr高Yb型花岗岩:对比及其地质意义.岩石学报,2005,21(6):1527-1537.
[158]闫峻,张巽,陈江峰,等.济南辉长岩的锶、钕同位素特征.矿物岩石地球化学通报,2001,20(4):302-305.
[159]杨承海,许文良,杨德彬,等.鲁西济南辉长岩的形成时代:锆石LA-ICP-MS U-Pb定年证据.地球学报,2005,26(4):321-325.
[160]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.
[161]陈道公.郯庐断裂带中南段新生代玄武岩地球化学.见:刘若新,中国新生代火山岩年代学与地球化学.北京:地出版社,1992,1-43.
[162]支霞臣,陈道公,张宗清,等.山东蓬莱、临胸新生代碱性玄武岩的钕、锶同位素组成.地质论评,1994,40(6):526-533.
[163]黄朋,付永涛,李安春,等.山东蓬莱大黑山岛碱性玄武岩地球化学特征.海洋与湖沼,2007, 38(1):91-96.
[164]赵国连.济阳凹陷火山岩的岩石学与地球化学.矿物学报,2006,26(3):335-345.
[165]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.Phys.Chem.Earth,2001,26:759-771.
[166]Qiu J.S.,Xu X.S.,Lo Q.H..Potash-rich volcanic rocks and lamprophyres in western Shandong Province:~(40)Ar-~(39)Ar dating and source tracing.Chinese Science Bulletin,2002,47(2):91-99.
[167]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.Contrib.Min.Petrol.,2002,144:241-253.
[168]Guo F.,Fan W.M,Wang Y.J.,et al..Geochemistry of Late Mesozoic mafic magmatism in west Shandong Province,eastern China:C haracterizing the lost lithospheric mantle beneath the North China block.Geochem.J.,2003,37:63-77.
[169]邱检生,王德滋.山东五莲七宝山辉石二长岩的地球化学及岩浆源区性质.地质论评,45(增刊):1999,612-617.
[170]Fan W.M,Guo F.,Wang Y.J.,et al..Post-orogenis bimodal volcanism along the Sulu orogenic belt in eastern China.Phys Chem.Earth(A),2001,26:733-746.
[171]Xu Y G,Huang XL,Ma JL,et al.Crustal-mantle interaction during the thermo-tectonic reactivation of the North China craton:SHRIMP zircon U-Pb age,petrology and geochemistry of Mesozoic plutons western Shandong.Contrib.Mineral.Petrol..2004,147:750-767.
[172]徐义刚,巫祥阳,罗震宇,等.山东中侏罗世-早白垩世侵入岩的Hf同位素组成及其意义.岩石学报,2007,23(2):307-316.
[173]Wang L,Qiu Y,McNaughton N J,et al.Constraints on crustal evolution and gold metallogeny in the Northeastern Jiaodong peninsula,China,from SHRIMP U-Pb zircon studies of granitoids.Ore Geology geviews,1998,13:275-291.
[174]罗镇宽,苗来成.胶东招莱地区花岗岩与金矿.北京:冶金工业出版社,2002.
[175]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):1-125.
[176]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.
[177]张华锋,翟明国,童英,等.胶东半岛二佛山高Ba-Sr花岗岩成因.地质论评,2006,52(1):43-53.
[178]赵广涛,王德滋.崂山花岗岩岩石地球化学与成因.高校地质学报,1997,3(1):1-15.
[179]吴锁平,王梅英,戚开静.A型花岗岩研究现状及评述.矿物岩石学杂志,2007,26(1):57-66.
[180]杨进辉,周新华,陈立辉.胶东地区破碎带蚀变岩型金矿时代的测定及其地质意义.岩石学报,2000,16(3):454-458.
[181]谭俊,魏俊浩,杨春福,等.胶东郭城地区脉岩类岩石地球化学特征及成岩构造背景.地质学报,2006,80(8):1177-1188.
[182]孙景贵,胡受奚,凌洪飞,等.胶西北两类金矿田的高钾-钾质脉岩元素地球化学与成岩作用研究.地球化学,2000,29(2):143-152.
[183]刘洪文,邢树文,孙景贵.胶西北两类金矿床暗色脉岩的碳、氧同位素地球化学.吉林大学学 报(地球科学版),2002,32(1):11-15.
[184]刘建明,张宏福,孙景贵,等.山东幔源岩浆岩的碳-氧和锶-钕同位素地球化学研究.中国科学(D辑),2003,33(10):921-930.
[185]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岩石化学.岩石学报,2003,19(4):623-636.
[186]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.
[187]Xu Y G,Ma JL,Huang XL,et al.Early Cretaceous gabbroic complex from Yinan,Shandong Provincel Petrogenesis and mantle domains beneath the North China Craton.International J.Sci.,2004,93:1025-1041.
[188]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.2006,31(1):81-92.
[189]Chen I H,Zou X H.Subduction-related metasomatism in the thinning lithosphere:Evidence from a compositedunite orthopyroxenite xenolith entrained in Mesozoic Laiwu high Mg diorite,North China craton.Geochemistry,Geophysics,Geosystems(G3).2005,6(6):1-20.
[190]许文良,王冬艳,王清海,等.华北克拉通东部中生代岩石圈减薄的过程与机制:中生代火成岩与深源捕虏体证据.地学前缘(中国地质大学,北京),2004,11(3):309-317.
[191]英基丰,周新华.鲁西地区中生代碳酸盐类的微量元素和锶、钕同位素组成特征.矿物岩石地球化学通报,2001,20(4):309-311.
[192]邱检生,徐夕生,罗清华.鲁西富钾火山岩和煌斑岩的~(39)Ar-~(40)Ar定年及源区示踪.科学通报,2001,46(18):1500-1508.
[193]邱检生,王德滋,周金城,等.山东中生代橄榄安粗岩系火山岩的地质、地球化学特征及演石成因.地球科学,1996,21(5):546-552.
[194]邱检生,王德滋,罗清华,等.鲁东胶莱盆地青山组火山岩的~(39)Ar-~(40)Ar定年--以分岭山火山机构为例.高效地质学报,2001,7(3):351-355.
[195]凌文黎,谢先军,柳小明,等.鲁东中生代标准剖面青山群火山岩锆石U-Pb年龄及其构造意义.中国科学(D辑,地球科学),2006,36(5):401-411.
[196]闫峻,陈江峰,谢智,等.鲁东晚白垩世玄武岩中的幔源捕虏体:对中国东部岩石罔减薄时间制约的新证据.科学通报,2003,48(14):1570-1574.
[197]王德滋,邱检生,任启江,等.中国东部橄榄安粗岩省的火山岩特征及其成矿作用.地质学报,1996.70(1):23-34
[198]Fan W M,Zhang H F,Baker J.et al..On-craton and off-craton Cenozoic spinel peridotites in eastern China:similarity and difference.J.Petrology,2000,41:933-950.
[199]Zhou X H,Yang J H,Zhang L C.Metallogenesis of superlarge gold deposits in Jiaodong region and deep processes of subcontinental lithosphere beneath North China craton in Mesozoic.Science in China(Series),2002,32(Suppl.):14-25.
[200]洪大卫,王涛,童英,等.华北地台和苏鲁-大别-秦岭造山带的中生代花岗岩与深部地球动力学过程.地学前缘,2003,10(3):231-256.
[201]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.
[202]Boyd F R.Compositional distinction between oceanic and cratonic lithosphere.Earth Planet Sci Leer,1989,96:15-26.
[203]许志琴.郯庐裂谷系.构造地质论丛,1984,3:39-46.
[204]廖远涛.胶莱盆地盆地样式及构造演化.新疆石油地质,2002,23(4):345-347.
[205]唐华风,程日辉,白云风,等.胶莱盆地构造演化规律.世界地质,2003,22(3):246-251.
[206]王世称,刘玉强,伊丕厚,等.山东省金矿床及金矿床密集区综合信息成矿预测.北京:地质出版社,2003,123-125.
[207]李桂群,范德江.胶莱盆地单元划分及特征.青岛海洋大学学报,1994,24(2):239-246.
[208]陆克政,戴俊生.胶莱盆地的形成和演化.东营:石油大学出版社,1994,47-48.
[209]吴智平,李凌,李伟,等.胶莱盆地莱阳期原型盆地的沉积格局及有利油气勘探区选择.大地构造与成矿学,2004,28(3):330-337.
[210]李金良,张岳桥,柳宗泉,等.胶莱盆地沉积-沉降史分析与构造演化.中国地质,2007,34(2):240-250.
[211]Li SG,Xiao Y,Liu D,et al..Collision of the North China and Yangtze blocks and formation of coesite-bearing eclogites:Timing and processes.Chemical Geology,1993,109:89-111.
[212]Li SG,Wang W,Chen Y,et al..Excess argon in phengite from eclogite:Evidence from dating of eclogite minerals by Sm-Nd,Rb-Sr and ~(39)Ar-~(40)Ar methods.Chemical Geology,1994,112:343-350.
[213]Ames L,Zhou G,Xiong B.Geochronology and geochemistry of ultrahigh-pressure metamorphism with implications for collision of the Sino-Korean and Yangtze cratons,central China.Tectonics,1996,15:422-489.
[214]杨经绥,许志琴,吴才来,刘福来,史仁灯,J Wooden,S Maruyama.含柯石英锆石的SHRIMP U-Pb定年:胶东印支期超高压变质作用的证据.地质学报,2002,76(3):354-372.
[215]李理,张进江,钟大赉,等.鲁西地区沿寒武系/太古宇不整合面滑脱构造的主要特征及形成机制.地质科学,2007,42(2):335-352.
[216]段秋梁,杨长春,闫臻,等.鲁西地区煤田滑动构造特征.煤田地质与勘探,2006,34(3):10-12.
[217]胡绍祥,施龙青,杨增夫,等.新汶煤田汶南井田滑动构造发育规律.煤田地质与勘探,2003,31(2):16-19.
[218]吕朋菊,张永双,张明利,等.鲁西煤田多级滑动构造系.地质论评,1995,41(6):503-508.
[219]吕朋菊,魏传久,张明利.肥城煤田滑动构造的发现及其意义.山东矿业学院学报,1992,11(2):120-126.
[220]张永双,吕朋菊,张明利.鲁西煤田滑动构造与矿井灾害.中国煤田地质,1995,7(2):11-17.
[221]沈远超,杨金中,刘铁兵等.胶东新型金矿——层间滑动角砾岩型金矿床.地质与勘探,2002,38(2):11-14.
[222]杨金中,沈远超,赵玉灵.层间滑动角砾岩型金矿床的地质特征及形成机制——以山东乳山蓬家夼金矿为例.黄金科学技术,1999,7(3):15-20.
[223]杨金中,沈远超,赵玉灵,等.胶莱盆地东北缘与低角度拆离有关的金成矿作用——以山东海阳郭城金矿为例.黄金科学技术,2000,8(4):13-20.
[224]邹为雷,沈远超,杨金中,等.浅析胶莱盆地边缘层间滑动断层构造及其控矿机制.地质地球化学,2001,29(2):58-65
[225]张连吕,沈远超,刘铁兵,等.胶东蓬家夼金矿床地质地球化学特征——一个与低角度层间滑动断层有关的金矿床.矿物岩石地球化学通报,2000,19(4):268-270.
[226]张岳桥,李金良,柳宗泉,等.胶莱盆地深部拆离系统及其区域构造意义.石油与天然气地质, 2006,27(4):505-511.
[227]刘建中,李三忠,周立宏,等.华北板块东部中生代构造变形与盆地格局.海洋地质与第四纪地质,2004,24(4):45-54.
[228]金振奎,刘泽荣,石占中.鲁西地区断裂构造类型及其形成机制.石油大学学报(自然科学版),1999,23(5):1-5.
[229]李三忠,王金铎,刘建中,等.鲁两地块中生代构造格局及其形成背景.地质学报,2005,79(4):487-497.
[230]单松炜,王淑霞,黄春慧.鲁西控煤构造特征及其演化分析.煤田地质与勘探,2000.28(1):6-8.
[231]翟明国,范洪瑞,杨进辉,等.非造山带型金矿--胶东型金矿的陆内成矿作用.地学前缘(中国地质大学,北京),2004,11(1):85-98.
[232]李厚民,毛景文,沈远超,等.胶西北东季金矿床钾长石和石英的Ar-Ar年龄及其意义.矿床地质,2003,22(1):72-77.
[233]杨金中,李光明.胶东中生代两期金矿化作用的对比研究及其意义.地质与勘探,2001,37(1):33-37
[234]Xiao'ou Zhang,PeterA.Cawood,Simon A.Wild,et al..Geology and timing of mineralization at the Cangshang gold deposit,north-western Jiaodong peninsula China.Mineralium deposita,2003,38:141-153.
[235]汪劲草,夏斌,汤静如.对玲珑-焦家矿集区几个关键地质问题的认识.大地构造与成矿学,2003,27(2):147-151.
[236]苗来成,罗镇宽,关康,等.胶东招掖金矿带控矿断裂演化规律.地质找矿论丛,1997,12(1):26-35.
[237]李厚民,沈远超,刘铁兵.胶东西北部焦家式与玲珑式金矿的成因联系.矿床地质,2002,21(增刊):621-624.
[238]李俊建,罗镇宽,刘晓阳,等.胶东中生代花岗岩及大型-超大型金矿床形成的地球动力学背景.矿床地质,2005,24(4):361-372.
[239]徐刚,郑达兴,温长顺.胶东焦家断裂带与金矿的成生关系.地质力学学报,1998,4(2):53-58.
[240]徐刚.焦家金矿田断裂构造与矿化特征的关系研究.矿床地质,2002,21(增刊):731-734.
[241]卢焕章,Guy Acambault,李院生,等.山东玲珑-焦家地区形变类型与金矿的关系.地质学报,1999,73(2):174-188.
[242]朱志澄,宋鸿林主编.构造地质学.武汉:中国地质大学出版社,1990,183-190.
[243]胡受奚,孙景贵,凌洪飞,等.中生代苏.鲁活动大陆边缘榴辉岩、煌斑岩、金矿及富集地幔间的成因联系.岩石学报,2001,17(3):425-435.
[244]李宏骥.胶北地区内生金矿成矿规律.山东地质,2002,18(3-4):72-77.
[245]沈远超.李厚民,刘铁兵,等.胶西北焦家式金矿化类型及其研究意义.地质与勘探,2001,37(1):48-51.
[246]王燕,卢作祥.山东焦掖金矿带焦家式金矿的矿床分带.地球科学--中国地质大学学报,1988,13(2):137-146.
[247]姚凤良,刘连登,孔庆存,等.胶东西北部脉状金矿.长春:吉林科学技术山版社,1990,234.
[248]吕古贤.山东玲珑金矿田和焦家金矿田成矿深度的测算与研究方法.中国科学,D辑,1997,27(4):338-342.
[249]李金祥,郭涛,吕古贤.试论胶东西北部金矿化类型及其与构造关系.贵金属地质,1999,8(2):87-91.
[250]邓军.山东招掖金矿带断裂构造分带与蚀变矿化分带关系研究.矿床地质,1994,13(增刊):17-19.
[251]张连昌,曾庆栋,沈远超,等.胶西北红布金矿地质特征及构造解析[J].地质与勘探,2002,38(3):18-22.
[252]张锐,曾庆栋.焦家金矿3~#脉成矿规律探讨.黄金科学技术,2004,12(2):16-21.
[253]李三忠,周立宏,刘建中,等.华北板块东部新生代断裂构造特征与盆地成因.海洋地质与第四纪地质,2004,24(3):57-66.
[254]王颖,赵锡奎,高博禹.济阳坳陷构造演化特征.成都理工学院院报,2002,29(2):181-187.
[255]杨超,陈清华.济阳坳陷构造演化及其构造层的划分.油气地质与采收率,2005,12(2):9-22.
[256]李理,戴俊生.埕岛地区中生界和古生界构造应力场数值模拟及裂缝分析.石油大学学报(自然科学版),2000,24(1):6-11.
[257]戴俊生.埕岛油田古生界构造特征及演化.中国海上油气(地质),2000,14(3):174-175.
[258]宗国洪,肖焕钦,李常宝,等.济阳坳陷构造演化及其大地构造意义.高效地质学报,1999,5(3):275-282.
[259]王毅,陆克政,任安身.济阳坳陷东北部中生构造运动和代火山活动及盆地演化.石油大学学报(自然科学版),1994,18(2):1-7.
[260]侯方辉,李三忠,张志珣,等.济阳坳陷陡坡带构造特征--以东营凹陷北坡为例.海洋地质动态,2006,22(2),6-8.
[261]张宇.济阳缓坡带构造特征及分类.断块油气田,2005,12(3):22-24.
[262]付谨平,郑和荣,孙红蕾.东营坳陷断裂构造特征及其与油气成藏的关系.复式油气田,1995,6(2):5-11.
[263]刘朝露,夏斌.济阳坳陷中生代原型盆地初步恢复及主控因素.天然气地球科学,2006,17(1):60-63.
[264]郑德顺,吴智平,李伟,等.济阳坳陷中、新生代盆地转型期断裂特征及其对盆地的控制作用.地质学报,2005,79(3):386-394.
[265]王世虎,夏斌,陈根文,等.济阳凹陷构造特征及形成机制讨论.大地构造与成矿学,2004,28(4):428-434.
[266]郝雪峰,宗国洪,李传华,等.济阳坳陷正反转构造初步分析.油气地质与采收率,2001,8(3):8-10.
[267]夏斌,刘朝露,陈根文.渤海湾盆地中新生代构造演化.天然气工业,2006,26(12):57-60.
[268]吴智平,李伟,任拥军,等.济阳坳陷中生代盆地演化及其与新生代盆地的叠合关系探讨.地质学报,2003,77(2):280-286.
[269]田在艺,张庆春.中国含油气盆地岩相古地理与油气.北京:地质出版社,1997.
[270]王同和,李洪革,张功成.渤海湾盆地构造演化与油气分布规律,中国含油气盆地构造.北京:石油工业出版社,1999,187-200.
[271]朱炎铭,秦勇,范炳恒,等.渤海湾盆地三叠系沉积厚度分布及其意义.中国矿业大学学报,2001,30(2):195-200.
[272]陈杰,董冬.邱明文.济阳坳陷内的负反转构造及其石油地质意义.石油试验地质,1999,21(3):201-206.
[273]陈广军.胜利油区长堤潜山区域构造关系探讨.新疆石油学院学报,2001,13(3):15-18.
[274]黄朋,付永涛,李安春,等.山东蓬莱大黑山岛碱性玄武岩地球化学特征.海洋与湖沼,2007, 38(1):91-96.
[275]郭华,夏斌,陈根文,等.惠民凹陷渐新世玄武岩地球化学特征及大地构造意义.大地构造与成矿学,2005,29(3):303-315.
[276]余晓露,郑建平.复杂的山东昌乐新生代玄武岩辉石岩捕虏体及其岩石圈演化意义.现代地质,2007,21(2):318-326.
[277]王志才,石荣会,晁洪太,等.鲁中南隆起区第四纪晚期断裂活动特征.海洋地质与第四纪地质,2001,21(4):100-108.
[278]周本刚,冉勇康,环文林,等.山东海阳断裂东石兰沟断晚更新世以来地表错断特征与最大潜在地震估计,地震地质,2002,24(2):159-166.
[279]马保起,舒赛兵,刘光勋.山东半岛东北部发现近东西向活断层.地震地质,2004,26(4):638-644.
[2]杨巍然.地球表层系统与中国区域大地构造的研究发展.地学前缘(中国地质大学(北京):北京大学),2006,13(6):102-110.
[3]Meyerhoff A A,Taner I,Morris AMS,等(白星碧,关玉华,陈华译).全球构造的新概念--颤动构造简介.北京:中国地质矿产信息研究院.
[4]Maruyama.plume tectonics.J.Geol.Soc.Japan,1994,100(1):24-49.
[5]李晓波.造山模式的新框架--大陆动力学演化过程.中国地质,2002,29(2):25-28.
[6]李锦轶,肖序常.1998.板块构造学说与大陆动力学--纪念李春昱教授逝世十周年(代前言).地质论评,44(4):337-338.
[7]丁国瑜.1999.大陆动力学地学研究的新动向.内陆地震,13(4):289-290.
[8]曹国权.1990.试论“胶南地体”.山东地质,6(2):1-10
[9]牛树银,胡华斌,毛景文,等.鲁西地区地质构造特征及其形成机制.中国地质,2004,31(1):34-39.
[10]宋明春,王沛成,梁帮启,等.山东省区域地质.济南:山东省地图出版社,2003,25-720.
[11]黄汲清,任纪舜,姜春发,等.中国大地构造基本轮廓.地质学报,1977,51(2):117-135.
[12]任纪舜,王作勋,陈炳蔚,等.从全球看中国的大地构造--中国及邻区大地构造图的简要说明.北京:地质出版社,1999.
[13]李春昱.中国板块构造的轮廓.中国地质科学院院报,1980,2(1),11-22.
[14]李春昱,王荃,刘雪亚,等.亚洲大地构造图(1:800万)及说明书.北京:地图出版社,1982.
[15]李春昱.在经济体制改革时期,地质工作如何面向经济建设.大自然探索,1985,4(13):9-10.
[16]李锦轶.中国大陆地壳“镶嵌与叠覆”的结构特征及其演化.地质通报,2004,23(9-10):986-1004.
[17]程裕淇主编.中国区域地质概论.北京:地质出版社,1994,16-17.
[18]任纪舜,陈廷愚,牛宝贵,等.中国东部及邻区大陆岩石圈的构造演化与成矿.北京:科学出版社,1992,26-27.
[19]伍家善,耿元生,沈其韩,等.中朝古大陆地质特征及构造演化.北京:地质出版社,1998,1-212.
[20]邓晋福,吴宗絮,赵国春,等.华北地台前寒武花岗岩类陆壳演化与克拉通形成.岩石学报,1999,15(2):190-198.
[21]Bai J,Dai F Y.Archean crust of China.In:Ma X Y,Bai J,eds.Precambrian Crust Evolution of China.Beijing:Geological Publishing House,1998.15-86.
[22]李继亮,王凯怡,王清晨,等.五台山早元古代碰撞带初步认识.地质科学,1990,25(1):1-11.
[23]李继亮,王凯怡,郝杰,等.山西五台山晚太古代镁铁质-超镁铁质岩:一种可能的古蛇绿岩.岩石学报,1997,13(2):139-151.
[24]白瑾,王汝铮,郭进京,等.五台山早前寒武纪重大地质事件及其年代.北京:地质出版社,1992,1-55.
[25]翟明国,郭敬辉,闫月华,等.中国华北太古宙高压麻粒岩的发现及初步研究.中国科学,B辑, 1992.(12):1325-1330.
[26]翟明国,郭敬辉,李江海等,等.太古宙退化榴辉岩的发现及其地质意义.科学通报,1995,40(17):1590-1594.
[27]李江海,钱祥麟.太行山北段龙泉关剪切带研究.山西地质,1991,6(1):17-29.
[28]吴昌华,钟长汀.华北陆台中段吕梁期的SW-NE向碰撞.前寒武纪研究进展,1998,21(3):28-50
[29]Liu D Y,Nutman A P,Compston W,et al.Remnants of 3800 Ma crust in the Chinese Part of the Sino-Korean craton.Geology,1992,(20):339-342.
[30]沈其韩,钱祥麟.中国太古宙地质体组成、阶段划分和演化.地球学报,1995,(2):113-120.
[31]李江海,钱祥麟,翟明国.华北北部麻粒岩相构造区划及其早前寒武纪构造演化.地质科学,1997,32(3):254-265.
[32]翟明国,卞爱国.华北克拉通新太古代末超大陆拼合及古元古代末-中元古代裂解.中国科学D 辑,2000,30(增刊):129-137.
[33]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):539-549.
[34]李江海,牛向龙,程素花,钱祥麟.大陆克拉通早期演化历史探讨:以华北为例.地球科学--中国地质大学学报,2006,31(3):285-293.
[35]翟明国.华北克拉通2.1-1.7Ga地质事件群的分解和构造意义探讨.岩石学报,2004,20(6):1343-1354.
[36]白瑾,黄学光,王惠初,等.中国前寒武纪地壳演化(第二版).北京:地质出版社,1996,20-60.
[37]耿元生,万渝生,沈其韩.华北克拉通早前寒武纪基性火山作用与地壳增生.地质学报,2002,76(2):199-208.
[38]李江海,刘守偈,侯贵廷.华北中部古元古代末期构造-热事件性质及其构造成因模式.中国地质.2006,33(6):1256-1266.
[39]Kusky T.,Li J.Paleoproterozoic tectonic evolution of the North China craton.Journal of Asian Earth Sciences,2003,22(4):383-397.
[40]赵宗溥.中朝准地台前寒武纪地质演化.北京:科学出版社,1993,1-83.
[41]沈其韩,沈比,耿元生,等.山东沂水杂岩的岩石组成与地质演化.北京:地质出版社,2000,5-73.130-142.
[42]程裕淇,沈其韩,等.山东新泰一带泰山群变质岩和岩浆岩类岩石的地质地球化学研究.地质论评,1964,22(3):198-209.
[43]程裕洪,沈其韩,王泽九.山东太古代雁翎关变质火山-沉积岩.北京:地质出版社,1982.
[44]程裕淇,沈其韩,王泽九.山东新泰雁翎关一带泰山群变质岩系的初步研究.地质矿产研究,1987,(3).
[45]程裕淇,徐惠芬.对山东新泰晚太古代雁翎关组中科马提岩类的一些认识.中国地质,1991,(4):31-32.
[46]徐惠芬.鲁西花岗绿岩带和变质作用.山东地质,1990,6(1):50-57.
[47]徐惠芬,董一杰,施允亨,等.鲁两花岗绿岩带.北京:地质出版社,1992.
[48]程素华,李江海,陈征,等.山东科马提岩地球化学特征及其意义.岩石矿物学杂志,2006,25(2):119-126.
[49]曹国权,等著.鲁西早前寒武纪地质.北京:地质出版社,1996,48-93,112-123.
[50]Kusky T M and Polat A.Growth of granit-greenstone terranes at convergent margins and stabilizaton of Archean craton.tectoniphysics,1999,305:45-73.
[51]Myers J S.The generation and assembly of an Archean supercontinent:Evidence from the Yilgarn craton western Australia.In:Coward M P,Ries A C.Geological society' s Special Publication,1995,95:143-154.
[52]Moores E M.Pre-1 Ga(pre-Rodinia) ophiolites:their tectonic and environmental implications.GSA Bulletin 2002,114(1):80-90.
[53]Foley F S,Buhre S,Jacob D E.Evolution of the Archaean crust by delamination an shallow subduction.Nature,2003,421:249-252.
[54]Baker F.Trondhjemites,dacites and related rocks.New York.Elsew.Sci.Pub.Comp pp.1979,321.
[55]苏尚国,邓晋福,梁风华,等.山东沂水紫苏花岗岩中残品相矿物的发现及紫苏花岗岩的形成过程.地学前缘,2003,10(3):257-267.
[56]Eby G N.Chemical subdivision ofthe A-Type granitoids:petrogenesis and implications.Geology,1992,20:641-644.
[57]魏春生.A型花岗岩成因模式及其地球动力学意义.地学前缘,2000,7(1):238.
[58]卢良兆,徐学纯,刘福来,著.中国北方前早寒武纪孔兹岩系.长春:长春山版社,1996.
[59]张本仁,高山,韩吟文.秦巴区域地球化学文集.武汉:中国地质大学山版社,1990.
[60]李江海,穆剑.我国境内格林威尔期造山带的存在及其对中元古代末期超大陆再造的制约.地球科学,1999,34(3):259-272.
[61]吴根耀.白垩纪:中国及邻区板块构造演化的一个重要变换期.中国地质,2006,33(1):64-77.
[62]王鸿祯,张世红.全球前寒武纪基底构造格局与古大陆再造问题.地球科学--中国地质大学学报,2002,27(5):467-481.
[63]邵济安,张履桥,李大明.华北克拉通元古代的三次伸展事什.岩石学报,2002,16(2):152-160.
[64]亓润章.鲁西前寒武纪地层划分及含铁建造地质特征.南京地质矿产研究所所刊,1984,5(3).
[65]张增奇,刘明渭主编.山东省岩石地层.武汉:中国地质大学出版社,1996,81-83.
[66]Hugh R.Rollinson.Using geochemical data:evaluation,presentation,interpretation.Langman Singapore Publishers Ltd,1993.
[67]王岳军,彭头平,范蔚茗,等.华北陆块基性岩墙群及其构造意义.矿物岩石地球化学通报,2007,26(1):1-9.
[68]王世进.鲁西前寒武纪侵入岩期次划分及基本特征.中国区域地质,1991,4:298-307.
[69]侯贵廷,刘玉琳,李江海,等.关于基性岩墙群的U-Pb SHRIMP地质年代学的探讨.岩石矿物学杂志,2005,14(3):179-185.
[70]侯贵廷,李江海,刘玉琳,等.华北克拉通古元古代末的伸展事件:拗拉谷与岩墙群.自然科学进展,2005,15(11):1366-1373.
[71]李曙光,孙卫东,葛宁洁,等.青岛榴辉岩相蛇绿混杂岩的岩石学证据及退变质P-T轨迹.岩石学报,1992,(4):351-361.
[72]王仁民,安家桐,赖兴运.胶东蛇绿岩套的发现及其地质意义.岩石学报,1995,11(增刊):211-227.
[73]倪志耀,王仁民.胶东元古宙变质硅质岩的地球化学及成因.矿物岩石,2001,21(1):59-66.
[74]赵大升,张旗,刘若新,等.山东梭罗树岩体橄榄岩中的尖品石-石榴石相转变的初步研究.科学通报,1993,38(17):1582-1584.
[75]Jahn B M,Cornichet J,Cong B.Crustal Evalution of The Qinling-Dabie orogen:Isotopic and Geochemical Constraints From Coesite-bearing Eclogites of The Su-Lu and Dabie Terranes,China.Chinese Science Bulletin,1995,40:116-119.
[76]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):1-9.
[77]宋明春,张景信,张希道.山东省胶南地区斜长花岗岩的发现.中国区域地质,1998,17(3):273-277.
[78]刘福来,许志琴,杨经绥,等.中国大陆科学钻探工程主孔及周边地区花岗质片麻岩的地球化学性质和超高压变质作用标志的识别.岩石学报,2004,20(1):9-26.
[79]Barbarin B.Granitoids main petrogenetic classifications in relation to origin and tectonic setting.Geol.J,1990,25:227-238.
[80]Leech M L.Arrested orogenic development:eclogitization,delamination,and tectonic collapse.Earth Planet Sci Lett,2001,185(1-2):149-159.
[81]马吕前,杨坤光,明厚利,等.大别山中生代地壳从挤压转向伸展的时间:花岗岩的证据.中国科学,2003,33(9):817-827.
[82]Whalen J A,Currie K L,Chappell B W.A-type granites:Geochemical characteristics,discrimination and petrogenesis.Contributions to Mineralogy and Petrology,1987,95:407-419.
[83]胡健,邱检生,王汝成,等.江苏东海片麻状碱性花岗岩的地球化学及其构造指示意义.地质学报,2006,80(12):1877-1891.
[84]薛怀民,刘福来,孟繁聪.苏鲁造山带胶东区段花岗片麻岩类的常量与微量元素地球化学:扬子克拉通北缘新元古代活动大陆边缘的证据.岩石学报,2006,22(7):1779-1790.
[85]苏玉平,唐红峰.A型花岗岩的微量元素地球化学.矿物岩石地球化学通报,2005,24(3):245-251.
[86]董树文,张勇,黄德志.苏北超高压变质带石桥构造窗地质特征.安徽地质,1996,6(1):9-13.
[87]钱存超,汤加富,常丹岩.安徽大别造山带南部浅变质岩层分布、层序与时代研究.地层学杂志,2001,25(3):222-227.
[88]乔秀夫,高林志.华北中新元古代及早古生代地震灾变事件及与Rodinia的关系.科学通报,1999,44(16):1753-1758.
[89]宋明春,吕法堂.山东胶南地区榴辉岩围岩中白云母的初步研究.矿物岩石,1997,17(2):17-21
[90]张儒媛,从柏林,刘忠光.苏鲁超高压变质地体及其成冈解释.岩石学报,1993,9(3):211-222
[91]李锦轶,杨天南,陈文,等.中国东部东海地区超高压变质岩构造变形事件的~(40)Ar/~(39)Ar定年与超高压变质岩折返过程的重建.地质学报,2004,78(1):97-108.
[92]宋明春,宋志勇,安丰琴.苏鲁超高压变质带南部浅变质岩的全岩Rb-Sr同位素年龄.江苏地质.2004,28(3):140-144.
[93]朱光,徐嘉炜,Futches W R,等.胶北蓬莱群的同位素年龄及其区域大地构造意义.地质学报,1994,68:158-172.
[94]王来明,宋明春,王沛成,等.苏鲁超高压变质带的结构与演化.北京:地质出版社,2005.
[95]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):229-237.
[96]Lindsay J F,Korsch R J,Wilford J R.Timing the breakup of a Neoproterozoic supercontinent:Evidence from Australian intrac-ratonic basins.Geology,1987,15:1061-1064.
[97]McLelland J,Daly J S,McCulloch J M.The Grenville orogenic cycle(ca.1350-1000Ma):an Adirondack perspective.Tectonophysics,1996,256:1-28.
[98]Meert J G,Torsvik T H.The making and unmaking of a supercontinent:Rodinia revisited. Tectonophysics,2003,375(1-4):261-288.
[99]McMenamin M A S,McMenamin D L S.The emergence of animals,The Cambrian breakthrough.New York:Columbia University Press,1990:1-217.
[100]Li X H,Li Z X,Ge WC,Zhou H W,Li WX,Liu Y,Wingate M T D.Neoproterozoic granitoids in south China:crustal melting above a mantle plume at ca 825Ma?Precambrian research 2003,122:45-83.
[101]任纪舜,肖藜薇.中国大地构造与地层区划.地层学杂志,2001,25(增刊):361-369.
[102]李锦轶,何国琦,徐新.新疆北部及邻区地壳构造格架及其形成过程的初步探讨,地质学报,2006,8(1):148-168.
[103]邵济安,唐克东.蛇绿岩与古蒙古洋的演化.见:张旗主编,蛇绿岩与地球动力学研究.北京:地质出版社,1996,117-120.
[104]段吉业,刘鹏举,夏德馨.浅析华北板块中元古代-古生代构造格局及其演化.现代地质,2002,(4):331-228.
[105]杨志坚.胶东地块研究取得新进展.中国区域地质,1992,11(1):43-50.
[106]牛保祥,刘书才,刘怀书.栖霞地区蓬莱群的时代属震旦纪.山东地质,1996,12(1):63-68.
[107]郭振一,孙秀珠.胶莱拗陷南缘晚侏罗世鲕状灰岩砾石中有孔虫、蜒化石的发现及其大地构造意义.地质论评,1985,31(2):179-181.
[108]牛保祥,陆荣莉,杨斌,等.鲁东地块的大地构造位置.山东国土资源,2004,20(4):41-45.
[109]刘占声主编.郯庐断裂带中段地质.长春:吉林科学技术出版社,1995,65-69.
[110]赵达,程立人,刘茂修.胶南地区五莲群中管孔藻类的发现及其意义.中国区域地质,1995,14(4):379-384.
[111]周春平.苏北.胶南地体构造初探.地震地质,1989,11(1):60-64.
[112]马杏垣.江苏响水至内蒙满都拉地学断面南北两段的地质观察.地球科学,1989,14(1):1-7.
[113]余和中,韩守华,谢锦龙,等.华北板块东南缘原型沉积盆地类型与构造演化.石油与天然气地质,2005,27(2):244-252.
[114]许志琴,杨经绥,李海兵,等.中央造山带早古生代地体构架与高乐/超高压变质带的形成.地质学报,2006,80(12):1793-1806.
[115]张宏福,杨岳衡.华北克拉通东部含金刚石金伯利岩的同位素年龄和Sr-Nd-Hf同位素地球化学特征.岩石学报,2007,23(2):285-294.
[116]Dobbs P N,Duncan D J,Hu S,et al.The geology of the Mengyin kimberlites,Shandong,China.In:Meyer H O A,Leonardos O H(ed).Proc 5th Int Kimb Conf 1.Diamonds:characterisation,genesis and exploration,CPRM Brasilia,1994,106-115.
[117]路风香,郑建平.华北地台古生代岩石圈地幔特征及深部过程.见:池际尚,路风香.华北地台金伯利岩及古生代岩石圈地幔特征.北京:科学技术出版社,1996,215-274.
[118]Meyer H O A,Zhang A,Milledge H j,et al.Diamonds and inclusions from Chinese kimberlites.In:Meyer H O A,Leonardos O H(ed).Proc 5th Int Kimb Conf 1.Diamonds:characterisation,genesis and exploration,1994,98-105.
[119]Harris J W,Duncan D J,Zhang F,et al.The physical characteristics and syngenetic inclusion geochemistry of diamonds from Pipe 50,Liaoning province,People' s Republic of China.In:Meyer H O A,Leonardos O H(ed).Proc 5th Int Kimb Conf 1.Diamonds:characterisation,genesis and exploration,1994,106-115.
[120]张开均.华北板块东缘晚古生代火山活动及其大地构造意义.中国煤田地质,1998,10(3):10-20.
[121]王永平.济宁、巨野、滕县煤田石炭-二叠纪的火山碎屑岩.煤田地质与勘探,1990,20(4):9-11.
[122]钟蓉,孙善平,傅泽明.山东及邻区晚石炭世-早二叠世火山事件沉积及地层对比.地质学报,1996,70(2):142-152.
[123]杨巍然,王国灿,简平.大别造山带构造年代学.武汉:中国地质大学出版社,2000:141.
[124]杨巍然,简平,韩郁菁.大别造山带加里东期高压、超高压变质作用的确定及其意义.地学前缘,2002,9(4):273-283.
[125]车自成,刘良,罗金海.中国及其邻区区域大地构造学.北京:科学出版社,2002,519.
[126]李廷栋,莫杰.中国滨太平洋构造域构造格架和东海地质演化.海洋地质与第四纪地质,2002,22(4):1-6.
[127]邵济安,牟堡磊,张履桥.华北东部构造格局转换过程中的深部作用与浅部响应.地质论评,2000,46(1):32-40.
[128]徐贵忠,周瑞,闫臻,等.论胶东地区中生代岩石圈减薄的证据及其动力学机制.大地构造与成矿学,2001,25(1):368-380.
[129]翟明国,樊祺诚,张宏福,隋建立.华北东部岩石圈减薄中的下地壳过程:岩浆底侵、置换与拆沉作用.岩石学报,2005,21(6):1509-1526.
[130]苗来成,罗镇宽,关康,黄佳展.玲珑花岗岩中锆石的离子质谱U-Pb年龄及其岩石学意义.岩石学报,1998,14(2):
[131]闫峻,陈江峰,谢智,等.鲁东晚白垩世玄武岩及其中幔源包体的岩石学和地球化学研究.岩石学报,2005,21(1):99-112.
[132]周立宏,李三忠,赵国春,等.华北克拉通中东部基底构造单元的重磁特征.地球物理学进展,2004,19(1):91-100.
[133]万天丰,朱鸿.中国大陆及邻区中生代-新生代大地构造与环境变迁.现代地质,2002,(2):107-120.
[134]Jin-Hui Yang,Sun-Lin Chung,Simon A.Wilde,et al.Petrogenesis of post-orogenic syenites in the Sulu Orogenic Belt,East China:geochronological,geochemical and Nd-Sr isotopic evidence.Chemical Geology,214(2005):99-125.
[135]Chen J F,Xie Z,Li HM,et al.U-Pb zircon for a collision-related K-rich complex at Shidao in the Sulu ultrahigh pressure terrane,China.Chemical Journal,2003,37(1):35-46.
[136]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,2004,1025-1038.
[137]穆克敏,林景仟,邹祖荣,等.华北地台区花岗质岩石的成因.长春:吉林科学技术出版社,1989,172-225.
[138]谢智.大别-苏鲁造山带岩石的锆石U-Pb年龄:[博士研究生学位论文].合肥:中国科学技术大学,1998,8-14.
[139]林景仟,谭东娟,迟效国.胶东半岛中生代花岗岩.北京:科学出版社,1992,208.
[140]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,2005,2l(4)1281-1301.
[141]宋明春,韩景敏.苏鲁超高压变质带北段夏河城岩体的形成时代及其意义.地质论评,2006, 52(5):601-608.
[142]宋明春,赵庆龄.山东日照官山闪长玢岩锆石SHRIMP年龄:印支期岩浆热事件及其对超高压变质岩折返历史的限定.地质通报,2004,23(12):1254-1258.
[143]Sun WD,Li S G,Chen Y D and Li Y J.Time of synorogenic granitoids in the South Qinling,Central China:constraints on the evolution of the Qinling-Dabie orogenic belt.Journal of Petrology,2002,110:457-468.
[144]肖庆辉,邓晋福,马大铨,等著.花岗岩研究思维与方法.北京:地质出版社,2002,247-254。
[145]陆孝平,吴福元,赵成弼,张艳斌.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.
[146]崔盛芹,李锦蓉.试论中国滨太平洋的印支运动.地质学报,1983,57(1):51-62.
[147]李之彤,赵春荆.东北地区的印支运动.地质科学,1985,20(3):211-223.
[148]宋明春,宋志勇,安丰琴.苏鲁超高压变质带南部浅变质岩的全岩Rb-Sr同位素年龄.江苏地质.2004,28(3):140-144.
[149]张旗,王阎,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.
[150]葛小月,李献华,陈志刚,等.中国东部高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.
[151]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.
[152]Guo Jinghui,Chen Fukun,Wolfgang Siebel,Cong Boling.Melting of the once deeply subducted continental slab:revealed by SHRIMP zircon ages of post-collisional granites from SuLu UHP zone,eastern China.Terra Nova,2003.
[153]杨进辉,朱美妃,刘伟,等.胶东地区郭家岭花岗岩的地球化学特征及成冈.岩石学报,2003,19(4):692-700.
[154]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.
[155]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.
[156]Zen E-an and Hammarstrom J M.Magmatic epidote and its petrologic significance.Geology,1984,12:515-518.
[157]张旗,李承东,王阎,等.中国东部中生代高Sr低Yb和低Sr高Yb型花岗岩:对比及其地质意义.岩石学报,2005,21(6):1527-1537.
[158]闫峻,张巽,陈江峰,等.济南辉长岩的锶、钕同位素特征.矿物岩石地球化学通报,2001,20(4):302-305.
[159]杨承海,许文良,杨德彬,等.鲁西济南辉长岩的形成时代:锆石LA-ICP-MS U-Pb定年证据.地球学报,2005,26(4):321-325.
[160]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.
[161]陈道公.郯庐断裂带中南段新生代玄武岩地球化学.见:刘若新,中国新生代火山岩年代学与地球化学.北京:地出版社,1992,1-43.
[162]支霞臣,陈道公,张宗清,等.山东蓬莱、临胸新生代碱性玄武岩的钕、锶同位素组成.地质论评,1994,40(6):526-533.
[163]黄朋,付永涛,李安春,等.山东蓬莱大黑山岛碱性玄武岩地球化学特征.海洋与湖沼,2007, 38(1):91-96.
[164]赵国连.济阳凹陷火山岩的岩石学与地球化学.矿物学报,2006,26(3):335-345.
[165]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.Phys.Chem.Earth,2001,26:759-771.
[166]Qiu J.S.,Xu X.S.,Lo Q.H..Potash-rich volcanic rocks and lamprophyres in western Shandong Province:~(40)Ar-~(39)Ar dating and source tracing.Chinese Science Bulletin,2002,47(2):91-99.
[167]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.Contrib.Min.Petrol.,2002,144:241-253.
[168]Guo F.,Fan W.M,Wang Y.J.,et al..Geochemistry of Late Mesozoic mafic magmatism in west Shandong Province,eastern China:C haracterizing the lost lithospheric mantle beneath the North China block.Geochem.J.,2003,37:63-77.
[169]邱检生,王德滋.山东五莲七宝山辉石二长岩的地球化学及岩浆源区性质.地质论评,45(增刊):1999,612-617.
[170]Fan W.M,Guo F.,Wang Y.J.,et al..Post-orogenis bimodal volcanism along the Sulu orogenic belt in eastern China.Phys Chem.Earth(A),2001,26:733-746.
[171]Xu Y G,Huang XL,Ma JL,et al.Crustal-mantle interaction during the thermo-tectonic reactivation of the North China craton:SHRIMP zircon U-Pb age,petrology and geochemistry of Mesozoic plutons western Shandong.Contrib.Mineral.Petrol..2004,147:750-767.
[172]徐义刚,巫祥阳,罗震宇,等.山东中侏罗世-早白垩世侵入岩的Hf同位素组成及其意义.岩石学报,2007,23(2):307-316.
[173]Wang L,Qiu Y,McNaughton N J,et al.Constraints on crustal evolution and gold metallogeny in the Northeastern Jiaodong peninsula,China,from SHRIMP U-Pb zircon studies of granitoids.Ore Geology geviews,1998,13:275-291.
[174]罗镇宽,苗来成.胶东招莱地区花岗岩与金矿.北京:冶金工业出版社,2002.
[175]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):1-125.
[176]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.
[177]张华锋,翟明国,童英,等.胶东半岛二佛山高Ba-Sr花岗岩成因.地质论评,2006,52(1):43-53.
[178]赵广涛,王德滋.崂山花岗岩岩石地球化学与成因.高校地质学报,1997,3(1):1-15.
[179]吴锁平,王梅英,戚开静.A型花岗岩研究现状及评述.矿物岩石学杂志,2007,26(1):57-66.
[180]杨进辉,周新华,陈立辉.胶东地区破碎带蚀变岩型金矿时代的测定及其地质意义.岩石学报,2000,16(3):454-458.
[181]谭俊,魏俊浩,杨春福,等.胶东郭城地区脉岩类岩石地球化学特征及成岩构造背景.地质学报,2006,80(8):1177-1188.
[182]孙景贵,胡受奚,凌洪飞,等.胶西北两类金矿田的高钾-钾质脉岩元素地球化学与成岩作用研究.地球化学,2000,29(2):143-152.
[183]刘洪文,邢树文,孙景贵.胶西北两类金矿床暗色脉岩的碳、氧同位素地球化学.吉林大学学 报(地球科学版),2002,32(1):11-15.
[184]刘建明,张宏福,孙景贵,等.山东幔源岩浆岩的碳-氧和锶-钕同位素地球化学研究.中国科学(D辑),2003,33(10):921-930.
[185]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岩石化学.岩石学报,2003,19(4):623-636.
[186]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.
[187]Xu Y G,Ma JL,Huang XL,et al.Early Cretaceous gabbroic complex from Yinan,Shandong Provincel Petrogenesis and mantle domains beneath the North China Craton.International J.Sci.,2004,93:1025-1041.
[188]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.2006,31(1):81-92.
[189]Chen I H,Zou X H.Subduction-related metasomatism in the thinning lithosphere:Evidence from a compositedunite orthopyroxenite xenolith entrained in Mesozoic Laiwu high Mg diorite,North China craton.Geochemistry,Geophysics,Geosystems(G3).2005,6(6):1-20.
[190]许文良,王冬艳,王清海,等.华北克拉通东部中生代岩石圈减薄的过程与机制:中生代火成岩与深源捕虏体证据.地学前缘(中国地质大学,北京),2004,11(3):309-317.
[191]英基丰,周新华.鲁西地区中生代碳酸盐类的微量元素和锶、钕同位素组成特征.矿物岩石地球化学通报,2001,20(4):309-311.
[192]邱检生,徐夕生,罗清华.鲁西富钾火山岩和煌斑岩的~(39)Ar-~(40)Ar定年及源区示踪.科学通报,2001,46(18):1500-1508.
[193]邱检生,王德滋,周金城,等.山东中生代橄榄安粗岩系火山岩的地质、地球化学特征及演石成因.地球科学,1996,21(5):546-552.
[194]邱检生,王德滋,罗清华,等.鲁东胶莱盆地青山组火山岩的~(39)Ar-~(40)Ar定年--以分岭山火山机构为例.高效地质学报,2001,7(3):351-355.
[195]凌文黎,谢先军,柳小明,等.鲁东中生代标准剖面青山群火山岩锆石U-Pb年龄及其构造意义.中国科学(D辑,地球科学),2006,36(5):401-411.
[196]闫峻,陈江峰,谢智,等.鲁东晚白垩世玄武岩中的幔源捕虏体:对中国东部岩石罔减薄时间制约的新证据.科学通报,2003,48(14):1570-1574.
[197]王德滋,邱检生,任启江,等.中国东部橄榄安粗岩省的火山岩特征及其成矿作用.地质学报,1996.70(1):23-34
[198]Fan W M,Zhang H F,Baker J.et al..On-craton and off-craton Cenozoic spinel peridotites in eastern China:similarity and difference.J.Petrology,2000,41:933-950.
[199]Zhou X H,Yang J H,Zhang L C.Metallogenesis of superlarge gold deposits in Jiaodong region and deep processes of subcontinental lithosphere beneath North China craton in Mesozoic.Science in China(Series),2002,32(Suppl.):14-25.
[200]洪大卫,王涛,童英,等.华北地台和苏鲁-大别-秦岭造山带的中生代花岗岩与深部地球动力学过程.地学前缘,2003,10(3):231-256.
[201]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.
[202]Boyd F R.Compositional distinction between oceanic and cratonic lithosphere.Earth Planet Sci Leer,1989,96:15-26.
[203]许志琴.郯庐裂谷系.构造地质论丛,1984,3:39-46.
[204]廖远涛.胶莱盆地盆地样式及构造演化.新疆石油地质,2002,23(4):345-347.
[205]唐华风,程日辉,白云风,等.胶莱盆地构造演化规律.世界地质,2003,22(3):246-251.
[206]王世称,刘玉强,伊丕厚,等.山东省金矿床及金矿床密集区综合信息成矿预测.北京:地质出版社,2003,123-125.
[207]李桂群,范德江.胶莱盆地单元划分及特征.青岛海洋大学学报,1994,24(2):239-246.
[208]陆克政,戴俊生.胶莱盆地的形成和演化.东营:石油大学出版社,1994,47-48.
[209]吴智平,李凌,李伟,等.胶莱盆地莱阳期原型盆地的沉积格局及有利油气勘探区选择.大地构造与成矿学,2004,28(3):330-337.
[210]李金良,张岳桥,柳宗泉,等.胶莱盆地沉积-沉降史分析与构造演化.中国地质,2007,34(2):240-250.
[211]Li SG,Xiao Y,Liu D,et al..Collision of the North China and Yangtze blocks and formation of coesite-bearing eclogites:Timing and processes.Chemical Geology,1993,109:89-111.
[212]Li SG,Wang W,Chen Y,et al..Excess argon in phengite from eclogite:Evidence from dating of eclogite minerals by Sm-Nd,Rb-Sr and ~(39)Ar-~(40)Ar methods.Chemical Geology,1994,112:343-350.
[213]Ames L,Zhou G,Xiong B.Geochronology and geochemistry of ultrahigh-pressure metamorphism with implications for collision of the Sino-Korean and Yangtze cratons,central China.Tectonics,1996,15:422-489.
[214]杨经绥,许志琴,吴才来,刘福来,史仁灯,J Wooden,S Maruyama.含柯石英锆石的SHRIMP U-Pb定年:胶东印支期超高压变质作用的证据.地质学报,2002,76(3):354-372.
[215]李理,张进江,钟大赉,等.鲁西地区沿寒武系/太古宇不整合面滑脱构造的主要特征及形成机制.地质科学,2007,42(2):335-352.
[216]段秋梁,杨长春,闫臻,等.鲁西地区煤田滑动构造特征.煤田地质与勘探,2006,34(3):10-12.
[217]胡绍祥,施龙青,杨增夫,等.新汶煤田汶南井田滑动构造发育规律.煤田地质与勘探,2003,31(2):16-19.
[218]吕朋菊,张永双,张明利,等.鲁西煤田多级滑动构造系.地质论评,1995,41(6):503-508.
[219]吕朋菊,魏传久,张明利.肥城煤田滑动构造的发现及其意义.山东矿业学院学报,1992,11(2):120-126.
[220]张永双,吕朋菊,张明利.鲁西煤田滑动构造与矿井灾害.中国煤田地质,1995,7(2):11-17.
[221]沈远超,杨金中,刘铁兵等.胶东新型金矿——层间滑动角砾岩型金矿床.地质与勘探,2002,38(2):11-14.
[222]杨金中,沈远超,赵玉灵.层间滑动角砾岩型金矿床的地质特征及形成机制——以山东乳山蓬家夼金矿为例.黄金科学技术,1999,7(3):15-20.
[223]杨金中,沈远超,赵玉灵,等.胶莱盆地东北缘与低角度拆离有关的金成矿作用——以山东海阳郭城金矿为例.黄金科学技术,2000,8(4):13-20.
[224]邹为雷,沈远超,杨金中,等.浅析胶莱盆地边缘层间滑动断层构造及其控矿机制.地质地球化学,2001,29(2):58-65
[225]张连吕,沈远超,刘铁兵,等.胶东蓬家夼金矿床地质地球化学特征——一个与低角度层间滑动断层有关的金矿床.矿物岩石地球化学通报,2000,19(4):268-270.
[226]张岳桥,李金良,柳宗泉,等.胶莱盆地深部拆离系统及其区域构造意义.石油与天然气地质, 2006,27(4):505-511.
[227]刘建中,李三忠,周立宏,等.华北板块东部中生代构造变形与盆地格局.海洋地质与第四纪地质,2004,24(4):45-54.
[228]金振奎,刘泽荣,石占中.鲁西地区断裂构造类型及其形成机制.石油大学学报(自然科学版),1999,23(5):1-5.
[229]李三忠,王金铎,刘建中,等.鲁两地块中生代构造格局及其形成背景.地质学报,2005,79(4):487-497.
[230]单松炜,王淑霞,黄春慧.鲁西控煤构造特征及其演化分析.煤田地质与勘探,2000.28(1):6-8.
[231]翟明国,范洪瑞,杨进辉,等.非造山带型金矿--胶东型金矿的陆内成矿作用.地学前缘(中国地质大学,北京),2004,11(1):85-98.
[232]李厚民,毛景文,沈远超,等.胶西北东季金矿床钾长石和石英的Ar-Ar年龄及其意义.矿床地质,2003,22(1):72-77.
[233]杨金中,李光明.胶东中生代两期金矿化作用的对比研究及其意义.地质与勘探,2001,37(1):33-37
[234]Xiao'ou Zhang,PeterA.Cawood,Simon A.Wild,et al..Geology and timing of mineralization at the Cangshang gold deposit,north-western Jiaodong peninsula China.Mineralium deposita,2003,38:141-153.
[235]汪劲草,夏斌,汤静如.对玲珑-焦家矿集区几个关键地质问题的认识.大地构造与成矿学,2003,27(2):147-151.
[236]苗来成,罗镇宽,关康,等.胶东招掖金矿带控矿断裂演化规律.地质找矿论丛,1997,12(1):26-35.
[237]李厚民,沈远超,刘铁兵.胶东西北部焦家式与玲珑式金矿的成因联系.矿床地质,2002,21(增刊):621-624.
[238]李俊建,罗镇宽,刘晓阳,等.胶东中生代花岗岩及大型-超大型金矿床形成的地球动力学背景.矿床地质,2005,24(4):361-372.
[239]徐刚,郑达兴,温长顺.胶东焦家断裂带与金矿的成生关系.地质力学学报,1998,4(2):53-58.
[240]徐刚.焦家金矿田断裂构造与矿化特征的关系研究.矿床地质,2002,21(增刊):731-734.
[241]卢焕章,Guy Acambault,李院生,等.山东玲珑-焦家地区形变类型与金矿的关系.地质学报,1999,73(2):174-188.
[242]朱志澄,宋鸿林主编.构造地质学.武汉:中国地质大学出版社,1990,183-190.
[243]胡受奚,孙景贵,凌洪飞,等.中生代苏.鲁活动大陆边缘榴辉岩、煌斑岩、金矿及富集地幔间的成因联系.岩石学报,2001,17(3):425-435.
[244]李宏骥.胶北地区内生金矿成矿规律.山东地质,2002,18(3-4):72-77.
[245]沈远超.李厚民,刘铁兵,等.胶西北焦家式金矿化类型及其研究意义.地质与勘探,2001,37(1):48-51.
[246]王燕,卢作祥.山东焦掖金矿带焦家式金矿的矿床分带.地球科学--中国地质大学学报,1988,13(2):137-146.
[247]姚凤良,刘连登,孔庆存,等.胶东西北部脉状金矿.长春:吉林科学技术山版社,1990,234.
[248]吕古贤.山东玲珑金矿田和焦家金矿田成矿深度的测算与研究方法.中国科学,D辑,1997,27(4):338-342.
[249]李金祥,郭涛,吕古贤.试论胶东西北部金矿化类型及其与构造关系.贵金属地质,1999,8(2):87-91.
[250]邓军.山东招掖金矿带断裂构造分带与蚀变矿化分带关系研究.矿床地质,1994,13(增刊):17-19.
[251]张连昌,曾庆栋,沈远超,等.胶西北红布金矿地质特征及构造解析[J].地质与勘探,2002,38(3):18-22.
[252]张锐,曾庆栋.焦家金矿3~#脉成矿规律探讨.黄金科学技术,2004,12(2):16-21.
[253]李三忠,周立宏,刘建中,等.华北板块东部新生代断裂构造特征与盆地成因.海洋地质与第四纪地质,2004,24(3):57-66.
[254]王颖,赵锡奎,高博禹.济阳坳陷构造演化特征.成都理工学院院报,2002,29(2):181-187.
[255]杨超,陈清华.济阳坳陷构造演化及其构造层的划分.油气地质与采收率,2005,12(2):9-22.
[256]李理,戴俊生.埕岛地区中生界和古生界构造应力场数值模拟及裂缝分析.石油大学学报(自然科学版),2000,24(1):6-11.
[257]戴俊生.埕岛油田古生界构造特征及演化.中国海上油气(地质),2000,14(3):174-175.
[258]宗国洪,肖焕钦,李常宝,等.济阳坳陷构造演化及其大地构造意义.高效地质学报,1999,5(3):275-282.
[259]王毅,陆克政,任安身.济阳坳陷东北部中生构造运动和代火山活动及盆地演化.石油大学学报(自然科学版),1994,18(2):1-7.
[260]侯方辉,李三忠,张志珣,等.济阳坳陷陡坡带构造特征--以东营凹陷北坡为例.海洋地质动态,2006,22(2),6-8.
[261]张宇.济阳缓坡带构造特征及分类.断块油气田,2005,12(3):22-24.
[262]付谨平,郑和荣,孙红蕾.东营坳陷断裂构造特征及其与油气成藏的关系.复式油气田,1995,6(2):5-11.
[263]刘朝露,夏斌.济阳坳陷中生代原型盆地初步恢复及主控因素.天然气地球科学,2006,17(1):60-63.
[264]郑德顺,吴智平,李伟,等.济阳坳陷中、新生代盆地转型期断裂特征及其对盆地的控制作用.地质学报,2005,79(3):386-394.
[265]王世虎,夏斌,陈根文,等.济阳凹陷构造特征及形成机制讨论.大地构造与成矿学,2004,28(4):428-434.
[266]郝雪峰,宗国洪,李传华,等.济阳坳陷正反转构造初步分析.油气地质与采收率,2001,8(3):8-10.
[267]夏斌,刘朝露,陈根文.渤海湾盆地中新生代构造演化.天然气工业,2006,26(12):57-60.
[268]吴智平,李伟,任拥军,等.济阳坳陷中生代盆地演化及其与新生代盆地的叠合关系探讨.地质学报,2003,77(2):280-286.
[269]田在艺,张庆春.中国含油气盆地岩相古地理与油气.北京:地质出版社,1997.
[270]王同和,李洪革,张功成.渤海湾盆地构造演化与油气分布规律,中国含油气盆地构造.北京:石油工业出版社,1999,187-200.
[271]朱炎铭,秦勇,范炳恒,等.渤海湾盆地三叠系沉积厚度分布及其意义.中国矿业大学学报,2001,30(2):195-200.
[272]陈杰,董冬.邱明文.济阳坳陷内的负反转构造及其石油地质意义.石油试验地质,1999,21(3):201-206.
[273]陈广军.胜利油区长堤潜山区域构造关系探讨.新疆石油学院学报,2001,13(3):15-18.
[274]黄朋,付永涛,李安春,等.山东蓬莱大黑山岛碱性玄武岩地球化学特征.海洋与湖沼,2007, 38(1):91-96.
[275]郭华,夏斌,陈根文,等.惠民凹陷渐新世玄武岩地球化学特征及大地构造意义.大地构造与成矿学,2005,29(3):303-315.
[276]余晓露,郑建平.复杂的山东昌乐新生代玄武岩辉石岩捕虏体及其岩石圈演化意义.现代地质,2007,21(2):318-326.
[277]王志才,石荣会,晁洪太,等.鲁中南隆起区第四纪晚期断裂活动特征.海洋地质与第四纪地质,2001,21(4):100-108.
[278]周本刚,冉勇康,环文林,等.山东海阳断裂东石兰沟断晚更新世以来地表错断特征与最大潜在地震估计,地震地质,2002,24(2):159-166.
[279]马保起,舒赛兵,刘光勋.山东半岛东北部发现近东西向活断层.地震地质,2004,26(4):638-644.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |