西伯利亚板块与华北克拉通碰撞带地电结构及对深部缝合边界的讨论
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摘要
西伯利亚板块与华北克拉通碰撞导致古亚洲洋闭合,形成了幅员辽阔的中亚造山带,该带内记录了丰富的板块碰撞信息,揭示深部缝合边界对于研究洋-陆俯冲到陆-陆碰撞的深部动力学过程具有重要的科学意义.本文对查干敖包—化德410km大地电磁测深(MT)剖面数据进行反演,获得二维电性结构,为研究西伯利亚板块与华北克拉通碰撞带深部构造形迹、碰撞边界问题提供地电结构的依据.结合人工反射地震及地质资料获得以下认识:(1)西伯利亚板块与华北克拉通碰撞带地壳存在多组"U"型低阻异常,多对应弧型、倾斜或"鳄鱼嘴"状反射界面.莫霍面存在两处错断现象,并与深部电性梯度带对应.岩石圈地幔除白乃庙岛弧呈低阻块体外,均为高阻块体,这些电性结构特征反映了南北汇聚所形成的构造形迹.(2)碰撞带可分为二连—贺根山和索伦—西拉木伦河两个不同时期的汇聚体系,晚泥盆世—晚石炭世早期形成的二连—贺根山汇聚体系由二连—贺根山增生杂岩带、宝力岛弧地体及断裂带组成,深部缝合边界位于二连浩特.而晚二叠—早三叠的索伦—西拉木伦河汇聚体系由二道井子增生杂岩带和温都尔庙增生杂岩带及断裂带组成,深部缝合边界位于苏尼特右旗.(3)在锡林浩特地区软流圈内部存在高阻异常,可能为俯冲消失的洋壳或碰撞造山后拆离的岩石圈残片.
The collision between the Siberia plate and the North China Craton led to the closure of the ancient Asian Ocean and the formation of a vast central Asian orogenic belt,which recorded abundant plate collision information and evidences that the deep suture boundary is of great significance to the study on the deep dynamic process from oceanic-continent subduction to continent-continent collision.To further address this issue,this paper presents an inversion of MT data along the 410 km-long Chagan Obo-Huade profile,thus to delineate a two-dimensional electrical structure beneath it.It provides evidence for the study of the deep structure and collision boundary between the Siberian plate and the North China Craton collision zone.Combining with seismic reflection and geological data we can obtain the following conclusions:(1)There are many groups of"U"-shaped low-resistance anomalies in the crust of the Siberian plate and the North China Craton collision zone which are correspond to arc-like and"crocodile mouth"-shaped reflection interfaces.Two dislocations on the Moho surface can be recognized,consistent with the deep electrical gradients.In addition to the low-resistivity blocks beneath the Bainaimiao island arc,the lithosphere of highresistivity.These physical characteristics reflect the structural traces formed by the north-south convergence.(2)The collision zone can be divided into two different converging systems:Erenhot-Hegenshan and Soren-Xilamulun.The Erenhot-Hegenshan convergence system which formed in the Late Devonian-Late Carboniferous is composed of the renhot-Hegenshan accretion complex belt,Baolidao Island arc geological body and fault zone,of which the deep suture boundary is located in Erenhot.And the Late Permian-Early Triassic Soren-Xilamulun convergence system consists of the Erdaojingzi accretional complex belt and the Wenduermiao accretion complex belt and the fault zone,of which the deep suture boundary is located in Sonid Zuoqi.(3)There are high resistivity anomalies in asthenosphere beneath the Xilinhaote area,which may be the fragments of subducted oceanic crust or detachment lithosphere after collision orogeny.
The collision between the Siberia plate and the North China Craton led to the closure of the ancient Asian Ocean and the formation of a vast central Asian orogenic belt,which recorded abundant plate collision information and evidences that the deep suture boundary is of great significance to the study on the deep dynamic process from oceanic-continent subduction to continent-continent collision.To further address this issue,this paper presents an inversion of MT data along the 410 km-long Chagan Obo-Huade profile,thus to delineate a two-dimensional electrical structure beneath it.It provides evidence for the study of the deep structure and collision boundary between the Siberian plate and the North China Craton collision zone.Combining with seismic reflection and geological data we can obtain the following conclusions:(1)There are many groups of"U"-shaped low-resistance anomalies in the crust of the Siberian plate and the North China Craton collision zone which are correspond to arc-like and"crocodile mouth"-shaped reflection interfaces.Two dislocations on the Moho surface can be recognized,consistent with the deep electrical gradients.In addition to the low-resistivity blocks beneath the Bainaimiao island arc,the lithosphere of highresistivity.These physical characteristics reflect the structural traces formed by the north-south convergence.(2)The collision zone can be divided into two different converging systems:Erenhot-Hegenshan and Soren-Xilamulun.The Erenhot-Hegenshan convergence system which formed in the Late Devonian-Late Carboniferous is composed of the renhot-Hegenshan accretion complex belt,Baolidao Island arc geological body and fault zone,of which the deep suture boundary is located in Erenhot.And the Late Permian-Early Triassic Soren-Xilamulun convergence system consists of the Erdaojingzi accretional complex belt and the Wenduermiao accretion complex belt and the fault zone,of which the deep suture boundary is located in Sonid Zuoqi.(3)There are high resistivity anomalies in asthenosphere beneath the Xilinhaote area,which may be the fragments of subducted oceanic crust or detachment lithosphere after collision orogeny.
引文
Bai L B,Li Y X,Liu J J.2004.Characteristics and tectonic settings of the Devonian basic volcanic rocks in Mandula,inner Mongolia.Geology and Mineral Resources of South China(in Chinese),(3):50-54.
Bai W J,Yang J S,Zhou M F,et al.1995.Tectonic evolution of different dating ophiolites in the western Junggar,Xinjiang.Acta Petrologica Sinica(in Chinese),11(S1):62-72.
Buchan C A.2001.Tectonic evolution of the Bayankhongor Ophiolite,Central Mongolia:Implications for the Palaeozoic crustal growth of Central Asia.Leicester:University of Leicester.
Cai J T,Chen X B.2010.Refined techniques for data processing and two-dimensional inversion in magnetotelluricⅡ:Which data polarization mode should be used in 2Dinversion.Chinese Journal of Geophysics(in Chinese),53(11):2703-2714,doi:10.3969/j.issn.0001-5733.2010.11.018.
Cai J T,Chen X B,Zhao G Z.2010.Refined techniques for data processing and two-dimensional inversion in magnetotelluricⅠ:Tensor decomposition and dimensionality analysis.Chinese Journal of Geophysics(in Chinese),53(10):2516-2526,doi:10.3969/j.issn.0001-5733.2010.10.025.
Cai Z H,Xu Z Q,Tang Z M,et al.2009.Exhumation kinetics of northern Sulu ultrahigh-pressure metamorphic belt,Rongcheng Area.Acta Petrologica Sinica(in Chinese),25(7):1627-1638.
Chen B,Jahn B M,Tian W.2009.Evolution of the Solonker suture zone:Constraints from zircon U-Pb ages,Hf isotopic ratios and whole-rock Nd-Sr isotope compositions of subduction-and collision-related magmas and forearc sediments.Journal of Asian Earth Sciences,34(3):245-257.
Chen B,Zhao G C,Wilde S.2001.Subduction-and Collision-related granitoids from southern Sonidzuoqi,inner Mongolia:Isotopic ages and tectonic implications.Geological Review(in Chinese),47(4):361-367.
Chen X B,Guo C L.2017.Refined techniques for data processing and two-dimensional inversion in magnetotelluric(V):Detecting the linear structures of the Earth by impedance tensor imaging.Chinese Journal of Geophysics(in Chinese),60(2):766-777,doi:10.6038/cjg20170227.
Deng S H,Wan C B,Yang J G.2007.Discovery of a Late Permian Angara-Cathaysia mixed flora from Acheng of Heilongjiang,China,with discussions on the closure of the Paleoasian Ocean.Science in China Series D:Earth Sciences,52(11):1746-1755.
Dilek Y,Furnes H.2011.Ophiolite genesis and global tectonics:Geochemical and tectonic fingerprinting of ancient oceanic lithosphere.GSA Bulletin,123(3-4):387-411.
Dong Z Y,Tang J,Chen X B,et al.2016.Deep electric structure beneath northeastern boundary areas of the North China craton.SeismologyandGeology(in Chinese),38(1):107-120.
Egbert G D.1997.Robust multiple-station magnetotelluric data processing.Geophysical Journal International,130(2):475-496.
Farquharson C G,Oldenburg D W.2004.A comparison of automatic techniques for estimating the Regularisation parameter in non-linear inverse problems.Geophysical Journal International,156(3):411-425.
Groom R W,Bailey R C.1989.Decomposition of magnetotelluric impedance tensors in the presence of local three-dimensional galvanic distortion.Journal of Geophysical Research:Solid Earth,94(B2):1913-1925.
He Z J,Liu S W,Ren J S,et al.1997.Late Permian-early Triassic sedimentary evolution and tectonic setting of the Linxi region.Regional Geology of China(in Chinese),16(4):403-409,427.
Hu X,Niu S Y,Zhang Y T.1987.The middle-late Silurian flysch in the Bainaimiao area,Nei Monggol.Regional Geology of China(in Chinese),(4):47-54.
Hu Y C,Li T L,Fan C S,et al.2015.Three-dimensional tensor controlled-source electromagnetic modeling based on the vector finite-element method.Applied Geophysics,12(1):35-46.
Huang B,Fu D,Li S C,et al.2016.The age and tectonic implications of the Hegenshan ophiolite in Inner Mongolia.Acta Petrologica Sinica(in Chinese),32(1):158-176.
Huang Z,Yang J S,Zhu Y W,et al.2015.The discovery of diamonds and deep mantle minerals in chromitites of Hegenshan ophiolite,Inner Mongolia.Geology in China(in Chinese),42(5):1493-1514.
Jian P,Liu D Y,Kr9ner A,et al.2008.Time scale of an early to mid-Paleozoic orogenic cycle of the long-lived Central Asian Orogenic Belt,Inner Mongolia of China:Implications for continental growth.Lithos,101(3-4):233-259.
Khain E V,Bibikova E V,Salnikova E B,et al.2003.The PalaeoAsian ocean in the Neoproterozoic and early Palaeozoic:new geochronologic data and palaeotectonic reconstructions.Precambrian Research,122(1-4):329-358.
Li L,Sun F Y,Li B L,et al.2016.Early Mesozoic southward subduction of the eastern Mongol-Okhotsk oceanic plate:evidence from zircon U-Pb-Hf isotopes and whole-rock geochemistry of Triassic granitic rocks in the Mohe Area,NE China.Resource Geology,66(4):386-403.
Li P W,Gao R,Guan Y,et al.2006.Palaeomagnetic constraints on the final closure time of Solonker-Linxi suture.Journal of Jilin University(Earth Science Edition)(in Chinese),36(5):744-758.
Li P W,Gao R,Guan Y,et al.2007.Paleomagnetic constraints on the collision of Siberian and north china blocks,with a discussion on the tectonic origin of the ultrahigh-pressure metamorphism in the Sulu-Dabie region.Acta Geoscientica Sinica(in Chinese),28(3):234-252.
Li R B,Xu B,Zhao P,et al.2014.The discovery of blueschistfacies rock in Airgin Sum area,Erenhot,Inner Mongolia and its tectonic significance.Chinese Science Bulletin(in Chinese),59(1):66-71.
Li S Z,Zhao S J,Yu S,et al.2016.Proto-Tehtys Ocean in East Asia(Ⅱ):Affinity and assmbly of Early Paleozoic microcontinental blocks.Acta Petrologica Sinica(in Chinese),32(9):2628-2644.
Li X P,Zhang L F,Wilde S A,et al.2010.Zircons from rodingite in the Western Tianshan serpentinite complex:Mineral chemistry and U-Pb ages define nature and timing of rodingitization.Lithos,118(1-2):17-34.
Li Y J,Wang J F,Li H Y,et al.2015.Recognition of Meilaotewula ophiolite in Xi U Jimqin Banner,Inner Mongolia.Acta Petrologica Sinica(in Chinese),31(5):1461-1470.
Liang H D,Gao R,Hou H S,et al.2015.Post-collisional extend record at crustal scale:Revealed by the deep electrical structure from the southern margin of the central Asian orogenic belt to the northern margin of the North China Craton.Chinese Journal of Geology(in Chinese),50(2):643-652.
Liu J F,Li J Y,Sun L X,et al.2016.Zircon U-Pb dating of the Jiujingzi ophiolite in Bairin Left Banner,Inner Mongolia:Constraints on the formation and evolution of the Xar Moron River suture zone.Geology in China(in Chinese),43(6):1947-1962.
Liu J Y,Li C Y,Xiao X C.1985.Study on ophiolite suite and its tectonic significance in the inner Mongolian hegen mountain area(in Chinese).∥Proceedings of the Chinese Academy of Geological Sciences,176-177.
Liu L S,Liu F L,Liu P H,et al.2015.Geochemical characteristics and metamorphic evolution of meta-mafic rocks from Haiyangsuo area,Sulu ultrahigh-pressure metamorphic belt.Acta Petrologica Sinica(in Chinese),31(10):2863-2888.
Liu R C,Jiang Y J,Li B.2016.Effects of intersection and dead-end of fractures on nonlinear flow and particle transport in rock fracture networks.Geosciences Journal,20(3):415-426.
Liu X J,Xu J F,Wang S Q,et al.2009.Geochemistry and dating of E-MORB type mafic rocks from Dalabute ophiolite in West Junggar,Xinjiang and geological implications.Acta Petrologica Sinica(in Chinese),25(6):1373-1389.
Ma C,Zhao G P,Xiao W J,et al.2011.Emplacement of ophiolites:Mechanisms and timing.Chinese Journal of Geology(in Chinese),46(3):865-874.
McNeice G W,Jones A G.2012.Multisite,multifrequency tensor decomposition of magnetotelluric data.Geophysics,66(1):158-173.
Mei S W,Wang Y M,Du X F,et al.2016.Geochemical characteristics of the serpentinized peridotite in the Wenduermiao Area,Inner Mongolia,China and their geological significance.Bulletin of Mineralogy,Petrology and Geochemistry(in Chinese),35(2):212-221.
Miao L C,Fan W M,Liu D Y,et al.2008.Geochronology and geochemistry of the Hegenshan ophiolitic complex:Implications for late-stage tectonic evolution of the Inner Mongolia-Daxinganling Orogenic Belt,China.Journal of Asian Earth Sciences,32(5-6):348-370.
Rodi W,Mackie R L.2000.Nonlinear conjugate gradients algorithm for2-D magnetotelluric inversion.Geophysics,66(1):174-187.
Shi G R,Chen Z Q.2006.Lower Permian oncolites from South China:Implications for equatorial sea-level responses to Late Palaeozoic Gondwanan glaciation.Journal of Asian Earth Sciences,26(3-4):424-436.
Smith J T,Booker J R.2012.Rapid inversion of two-and threedimensional magnetotelluric data.Journal of Geophysical Research:Solid Earth,96(B3):3905-3922.
Tian C L,Cao C Z,Yang F L.1989.Geochemical features of ophiolite in the fold belt on the north side of the Sino-Korean platform.Bulletin of the Chinese Academy of Geological Science(in Chinese),11:107-129.
Wang H,Wang Y J,Chen Z Y,et al.2005.Discovery of the Permian radiolarians from the Bayanaobao area,Inner Mongolia.Journal of Stratigraphy(in Chinese),29(4):368-371.
Wang S Q,Xu J F,Liu X J,et al.2008.Geochemistry of the Chaokeshan ophiolite:Product of intra-oceanic back-arc basin?.Acta Petrologica Sinica(in Chinese),24(12):2869-2879.
Windley B F,Alexeiev D,Xiao W J,et al.2007.Tectonic models for accretion of the Central Asian Orogenic Belt.Journal of the Geological Society,164:31-47.
Wu F Y,Sun D Y,Li H M,et al.2002.A-type granites in northeastern China:Age and geochemical constraints on their petrogenesis.Chemical Geology,187(1-2):143-173.
Xiao W J.2004.Paleozoic accretionary and collisional tectonics of the eastern Tianshan(China):Implications for the continental growth of central Asia.Social Compass,304(1):85-98.
Xiao W J,Brian F,Windley,et al.2002.Arc-ophiolite obduction in the Western Kunlun Range(China):Implications for the Palaeozoic evolution of Central Asia.J Geol Soc Lond.Journal of the Geological Society,159(13):517-528.
Xiao W J,Brian F.Windley,Hao J,et al.2003.Accretion leading to collision and the Permian Solonker suture,Inner Mongolia,China:Termination of the central Asian orogenic belt.Tectonics,22(6):8-1-8-20.
Xiao W J,Windley B F,Huang B C,et al.2009.End-Permian to midTriassic termination of the accretionary processes of the southern Altaids:Implications for the geodynamic evolution,Phanerozoic continental growth,and metallogeny of Central Asia.International Journal of Earth Sciences,98(6):1189-1217.
Xiao W J,Windley B F,Sun S,et al.2015.A tale of amalgamation of three permo-triassic collage systems in Central Asia:Oroclines,Sutures,and Terminal Accretion.Annual Review of Earth and Planetary Sciences,43(1):477-507.
Xu B,Charvet J,Chen Y,et al.2013.Middle Paleozoic convergent orogenic belts in western Inner Mongolia(China):framework,kinematics,geochronology and implications for tectonic evolution of the Central Asian Orogenic Belt.Gondwana Research,23(4):1342-1364.
Xu B,Charvet J,Zhang F Q.2001.Primary study on petrology and geochrononology of blueschists in Sunitezuoqi,Northern Inner Mongolia.Chinese Journal of Geology(in Chinese),36(4):424-434.
Xu B,Chen B.1997.Framework and evolution of the middle Paleozoic orogenic belt between Siberian and North China Plates in northern Inner Mongolia.Science in China Series D:Earth Sciences,40(5):463-469.
Xu G Y.1993.The tectonic evolution of Paleo-Asian Ocean in Northeast Asia.Jilin Geology(in Chinese),12(3):1-8.
Xu L B,Wei W B,Jin S,et al.2017.Study of deep electrical structure along aprofile from northern Ordos block to Yinshan orogenic belt.Chinese Journal of Geophysics(in Chinese),60(2):575-584,doi:10.6038/cjg20170212.
Xu X,Zhu Y F,Chen B.2007.Petrology of the Kamste ophiolite mélange from East Junggar,Xinjiang,NW China.Acta Petrologica Sinica(in Chinese),23(7):1603-1610.
Xu X X,Li J J,Liu J C,et al.2011.The crust-upper mantle electrical structure along Xilinhot-Dongwuqi section.Chinese Journal of Geophysics(in Chinese),54(5):1031-1039,doi:10.3969/j.issn.0001-5733.2011.05.019.
Xu Z Q.2007.Continental deep subduction and exhumation dynamics:Evidence from the main hole of the Chinese Continental Scientific Drilling and the Sulu HP-UHP metamorphic terrane.Acta Petrologica Sinica(in Chinese),23(12):3041-3053.
Yang W C,Yang W Y,Jin Z M,et al.2004.Lithospheric seismic fabrics of Sulu ultrahigh-pressure metamorphic belt.Science in China Series D:Earth Sciences,48(5):585-600.
Yuan X C.2007.Mushroom structure of the lithospheric mantle and its genesis at depth:Revisited.Geology in China(in Chinese),34(5):737-758.
Zhang S B,Tang J,Zheng Y F.2014.Contrasting Lu-Hf isotopes in zircon from Precambrian metamorphic rocks in the Jiaodong Peninsula:Constraints on the tectonic suture between North China and South China.Precambrian Research,245:29-50.
Zhang S H,Gao R,Li H Y,et al.2014.Crustal structures revealed from a deep seismic reflection profile across the Solonker suture zone of the Central Asian Orogenic Belt,northern China:An integrated interpretation.Tectonophysics,612-613:26-39.
Zhang Y S,Zhang J C.2017.Lithology-dependent minimum horizontal stress and in-situ stress estimate.Tectonophysics,703-704:1-8.
Zheng P,Zhang Y Z,Li Z X,et al.2008.Geochemical characteristics and forming environment of the carboniferous gabbro in yaduwula mountain area,middle Daxinganling.Geology and Resources(in Chinese),17(4):250-253,272.
Zheng Y F,Gao T S,Wu Y B,et al.2007.Fluid flow during exhumation of deeply subducted continental crust:zircon U-Pb age and O-isotope studies of a quartz vein within ultrahigh-pressure eclogite.Journal of Metamorphic Geology,25(2):267-283.
Zhou Z G,Gu Y C,Liu C F,et al.2010.Discovery of Early-Middle Permian cathaysian flora in Manduhubaolage area,Dong Ujimqin Qi,Inner Mongolia,China and its geological significance.Geological Bulletin of China(in Chinese),29(1):21-25.
Zhu Y F,Xu X.2006.The discovery of Early Ordovician ophiolite mélange in Taerbahatai Mts.Xinjiang,NW China.Acta Petrologica Sinica(in Chinese),22(12):2833-2842.
白立兵,李玉玺,刘俊杰.2004.内蒙古满都拉泥盆纪基性火山岩特征及其形成环境.华南地质与矿产,(3):50-54.
白文吉,杨经绥,周美付等.1995.西准噶尔不同时代蛇绿岩及其构造演化.岩石学报,11(S1):62-72.
蔡军涛,陈小斌.2010.大地电磁资料精细处理和二维反演解释技术研究(二)---反演数据极化模式选择.地球物理学报,53(11):2703-2714,doi:10.3969/j.issn.0001-5733.2010.11.018.
蔡军涛,陈小斌,赵国泽.2010.大地电磁资料精细处理和二维反演解释技术研究(一)---阻抗张量分解与构造维性分析.地球物理学报,53(10):2516-2526,doi:10.3969/j.issn.0001-5733.2010.10.025.
蔡志慧,许志琴,唐哲民等.2009.北苏鲁荣成地区超高压变质带的形成与折返动力学.岩石学报,25(7):1627-1638.
陈斌,赵国春,Wilde S.2001.内蒙古苏尼特左旗南两类花岗岩同位素年代学及其构造意义.地质论评,47(4):361-367.
陈小斌,郭春玲.2017.大地电磁资料精细处理和二维反演解释技术研究(五)---利用阻抗张量成像识别大地线性构造.地球物理学报,60(2):766-777,doi:10.6038/cjg20170227.
董泽义,汤吉,陈小斌等.2016.华北克拉通东北边界带深部电性结构特征.地震地质,38(1):107-120.
和政军,刘淑文,任纪舜等.1997.内蒙古林西地区晚二叠世-早三叠世沉积演化及构造背景.地质通报,16(4):403-409,427.
胡骁,牛树银,张英涛.1987.内蒙古白乃庙地区中晚志留世复理石.地质通报,(4):47-54.
黄波,付冬,李树才等.2016.内蒙古贺根山蛇绿岩形成时代及构造启示.岩石学报,32(1):158-176.
黄竺,杨经绥,朱永旺等.2015.内蒙古贺根山蛇绿岩的铬铁矿中发现金刚石等深部地幔矿物.中国地质,(5):1493-1514.
李朋武,高锐,管烨等.2006.内蒙古中部索伦-林西缝合带封闭时代的古地磁分析.吉林大学学报(地球科学版),36(5):744-758.
李朋武,高锐,管烨等.2007.华北与西伯利亚地块碰撞时代的古地磁分析---兼论苏鲁-大别超高压变质作用的构造起因.地球学报,28(3):234-252.
李瑞彪,徐备,赵盼等.2014.二连浩特艾力格庙地区蓝片岩相岩石的发现及其构造意义.科学通报,59(1):66-71.
李三忠,赵淑娟,余珊等.2016.东亚原特提斯洋(Ⅱ):早古生代微陆块亲缘性与聚合.岩石学报,32(9):2628-2644.
李英杰,王金芳,李红阳等.2015.内蒙古西乌旗梅劳特乌拉蛇绿岩的识别.岩石学报,31(5):1461-1470.
梁宏达,高锐,候贺晟等.2015.碰撞后的地壳尺度伸展记录---中亚造山带南缘-华北克拉通北缘深部电性结构的揭露.地质科学,50(2):643-652.
刘家义,李春昱,肖序常.1985.内蒙贺根山地区蛇绿岩套研究及构造意义.∥中国地质科学院文集(1982中英文合订本),176-177.
刘建峰,李锦轶,孙立新等.2016.内蒙古巴林左旗九井子蛇绿岩锆石U-Pb定年:对西拉木伦河缝合带形成演化的约束.中国地质,43(6):1947-1962.
刘利双,刘福来,刘平华等.2015.苏鲁超高压变质带中海阳所地区变基性岩的地球化学性质及变质演化特征.岩石学报,31(10):2863-2888.
刘希军,许继峰,王树庆等.2009.新疆西准噶尔达拉布特蛇绿岩E-MORB型镁铁质岩的地球化学、年代学及其地质意义.岩石学报,25(6):1373-1389.
马冲,赵桂萍,肖文交等.2011.蛇绿岩就位机制及时限.地质科学,46(3):865-874.
梅盛旺,汪玉梅,杜显锋等.2016.内蒙古温都尔庙地区蛇纹石化橄榄岩地球化学特征及其地质意义.矿物岩石地球化学通报,35(2):212-221.
田昌烈,曹从周,杨芳林.1989.中朝陆台北侧褶皱带(中段)蛇绿岩的地球化学特征.中国地质科学院院报,11:107-129.
王惠,王玉净,陈志勇等.2005.内蒙古巴彦敖包二叠纪放射虫化石的发现.地层学杂志,29(4):368-371.
王树庆,许继峰,刘希军等.2008.内蒙朝克山蛇绿岩地球化学:洋内弧后盆地的产物?岩石学报,24(12):2869-2879.
魏文博,叶高峰,金胜等.2008.华北地区东部岩石圈导电性结构研究-减薄的华北岩石圈特点.地学前缘,15(4):204-216.
徐备,陈斌.1997.内蒙古北部华北板块与西伯利亚板块之间中古生代造山带的结构及演化.中国科学(D辑),27(3):227-232.
徐备,Charvet J,张福勤.2001.内蒙古北部苏尼特左旗蓝片岩岩石学和年代学研究.地质科学,36(4):424-434.
徐公愉.1993.东北亚地区古亚洲洋的构造演化特点.吉林地质,12(3):1-8.
许林斌,魏文博,金胜等.2017.鄂尔多斯地块北部至阴山造山带
深部电性结构特征研究.地球物理学报,60(2):575-584,doi:10.6038/cjg20170212.
徐新,朱永峰,陈博.2007.卡姆斯特蛇绿混杂岩的岩石学研究及其地质意义.岩石学报,2007,23(7):1603-1610.
徐新学,李俊健,刘俊昌等.2011.内蒙古锡林浩特-东乌旗剖面壳幔电性结构研究.地球物理学报,54(5):1301-1309,doi:10.3969/j.issn.0001-5733.2011.05.019.
许志琴.2007.深俯冲和折返动力学:来自中国大陆科学钻探主孔及苏鲁超高压变质带的制约.岩石学报,23(12):3041-3053.
杨文采,杨午阳,金振民等.2004.苏鲁超高压变质带岩石圈的地震组构.中国科学D辑地球科学,34(4):307-319.
袁学诚.2007.再论岩石圈地幔蘑菇云构造及其深部成因.中国地质,34(5):737-758.
郑萍,张永正,李振祥等.2008.大兴安岭中段牙都乌拉山地区石炭纪辉长岩特征及形成环境.地质与资源,17(4):250-253,272.
周志广,谷永昌,柳长峰等.2010.内蒙古东乌珠穆沁旗满都胡宝拉格地区早-中二叠世华夏植物群的发现及地质意义.地质通报,29(1):21-25.
朱永峰,徐新.2006.新疆塔尔巴哈台山发现早奥陶世蛇绿混杂岩.岩石学报,22(12):2833-2842.
Bai W J,Yang J S,Zhou M F,et al.1995.Tectonic evolution of different dating ophiolites in the western Junggar,Xinjiang.Acta Petrologica Sinica(in Chinese),11(S1):62-72.
Buchan C A.2001.Tectonic evolution of the Bayankhongor Ophiolite,Central Mongolia:Implications for the Palaeozoic crustal growth of Central Asia.Leicester:University of Leicester.
Cai J T,Chen X B.2010.Refined techniques for data processing and two-dimensional inversion in magnetotelluricⅡ:Which data polarization mode should be used in 2Dinversion.Chinese Journal of Geophysics(in Chinese),53(11):2703-2714,doi:10.3969/j.issn.0001-5733.2010.11.018.
Cai J T,Chen X B,Zhao G Z.2010.Refined techniques for data processing and two-dimensional inversion in magnetotelluricⅠ:Tensor decomposition and dimensionality analysis.Chinese Journal of Geophysics(in Chinese),53(10):2516-2526,doi:10.3969/j.issn.0001-5733.2010.10.025.
Cai Z H,Xu Z Q,Tang Z M,et al.2009.Exhumation kinetics of northern Sulu ultrahigh-pressure metamorphic belt,Rongcheng Area.Acta Petrologica Sinica(in Chinese),25(7):1627-1638.
Chen B,Jahn B M,Tian W.2009.Evolution of the Solonker suture zone:Constraints from zircon U-Pb ages,Hf isotopic ratios and whole-rock Nd-Sr isotope compositions of subduction-and collision-related magmas and forearc sediments.Journal of Asian Earth Sciences,34(3):245-257.
Chen B,Zhao G C,Wilde S.2001.Subduction-and Collision-related granitoids from southern Sonidzuoqi,inner Mongolia:Isotopic ages and tectonic implications.Geological Review(in Chinese),47(4):361-367.
Chen X B,Guo C L.2017.Refined techniques for data processing and two-dimensional inversion in magnetotelluric(V):Detecting the linear structures of the Earth by impedance tensor imaging.Chinese Journal of Geophysics(in Chinese),60(2):766-777,doi:10.6038/cjg20170227.
Deng S H,Wan C B,Yang J G.2007.Discovery of a Late Permian Angara-Cathaysia mixed flora from Acheng of Heilongjiang,China,with discussions on the closure of the Paleoasian Ocean.Science in China Series D:Earth Sciences,52(11):1746-1755.
Dilek Y,Furnes H.2011.Ophiolite genesis and global tectonics:Geochemical and tectonic fingerprinting of ancient oceanic lithosphere.GSA Bulletin,123(3-4):387-411.
Dong Z Y,Tang J,Chen X B,et al.2016.Deep electric structure beneath northeastern boundary areas of the North China craton.SeismologyandGeology(in Chinese),38(1):107-120.
Egbert G D.1997.Robust multiple-station magnetotelluric data processing.Geophysical Journal International,130(2):475-496.
Farquharson C G,Oldenburg D W.2004.A comparison of automatic techniques for estimating the Regularisation parameter in non-linear inverse problems.Geophysical Journal International,156(3):411-425.
Groom R W,Bailey R C.1989.Decomposition of magnetotelluric impedance tensors in the presence of local three-dimensional galvanic distortion.Journal of Geophysical Research:Solid Earth,94(B2):1913-1925.
He Z J,Liu S W,Ren J S,et al.1997.Late Permian-early Triassic sedimentary evolution and tectonic setting of the Linxi region.Regional Geology of China(in Chinese),16(4):403-409,427.
Hu X,Niu S Y,Zhang Y T.1987.The middle-late Silurian flysch in the Bainaimiao area,Nei Monggol.Regional Geology of China(in Chinese),(4):47-54.
Hu Y C,Li T L,Fan C S,et al.2015.Three-dimensional tensor controlled-source electromagnetic modeling based on the vector finite-element method.Applied Geophysics,12(1):35-46.
Huang B,Fu D,Li S C,et al.2016.The age and tectonic implications of the Hegenshan ophiolite in Inner Mongolia.Acta Petrologica Sinica(in Chinese),32(1):158-176.
Huang Z,Yang J S,Zhu Y W,et al.2015.The discovery of diamonds and deep mantle minerals in chromitites of Hegenshan ophiolite,Inner Mongolia.Geology in China(in Chinese),42(5):1493-1514.
Jian P,Liu D Y,Kr9ner A,et al.2008.Time scale of an early to mid-Paleozoic orogenic cycle of the long-lived Central Asian Orogenic Belt,Inner Mongolia of China:Implications for continental growth.Lithos,101(3-4):233-259.
Khain E V,Bibikova E V,Salnikova E B,et al.2003.The PalaeoAsian ocean in the Neoproterozoic and early Palaeozoic:new geochronologic data and palaeotectonic reconstructions.Precambrian Research,122(1-4):329-358.
Li L,Sun F Y,Li B L,et al.2016.Early Mesozoic southward subduction of the eastern Mongol-Okhotsk oceanic plate:evidence from zircon U-Pb-Hf isotopes and whole-rock geochemistry of Triassic granitic rocks in the Mohe Area,NE China.Resource Geology,66(4):386-403.
Li P W,Gao R,Guan Y,et al.2006.Palaeomagnetic constraints on the final closure time of Solonker-Linxi suture.Journal of Jilin University(Earth Science Edition)(in Chinese),36(5):744-758.
Li P W,Gao R,Guan Y,et al.2007.Paleomagnetic constraints on the collision of Siberian and north china blocks,with a discussion on the tectonic origin of the ultrahigh-pressure metamorphism in the Sulu-Dabie region.Acta Geoscientica Sinica(in Chinese),28(3):234-252.
Li R B,Xu B,Zhao P,et al.2014.The discovery of blueschistfacies rock in Airgin Sum area,Erenhot,Inner Mongolia and its tectonic significance.Chinese Science Bulletin(in Chinese),59(1):66-71.
Li S Z,Zhao S J,Yu S,et al.2016.Proto-Tehtys Ocean in East Asia(Ⅱ):Affinity and assmbly of Early Paleozoic microcontinental blocks.Acta Petrologica Sinica(in Chinese),32(9):2628-2644.
Li X P,Zhang L F,Wilde S A,et al.2010.Zircons from rodingite in the Western Tianshan serpentinite complex:Mineral chemistry and U-Pb ages define nature and timing of rodingitization.Lithos,118(1-2):17-34.
Li Y J,Wang J F,Li H Y,et al.2015.Recognition of Meilaotewula ophiolite in Xi U Jimqin Banner,Inner Mongolia.Acta Petrologica Sinica(in Chinese),31(5):1461-1470.
Liang H D,Gao R,Hou H S,et al.2015.Post-collisional extend record at crustal scale:Revealed by the deep electrical structure from the southern margin of the central Asian orogenic belt to the northern margin of the North China Craton.Chinese Journal of Geology(in Chinese),50(2):643-652.
Liu J F,Li J Y,Sun L X,et al.2016.Zircon U-Pb dating of the Jiujingzi ophiolite in Bairin Left Banner,Inner Mongolia:Constraints on the formation and evolution of the Xar Moron River suture zone.Geology in China(in Chinese),43(6):1947-1962.
Liu J Y,Li C Y,Xiao X C.1985.Study on ophiolite suite and its tectonic significance in the inner Mongolian hegen mountain area(in Chinese).∥Proceedings of the Chinese Academy of Geological Sciences,176-177.
Liu L S,Liu F L,Liu P H,et al.2015.Geochemical characteristics and metamorphic evolution of meta-mafic rocks from Haiyangsuo area,Sulu ultrahigh-pressure metamorphic belt.Acta Petrologica Sinica(in Chinese),31(10):2863-2888.
Liu R C,Jiang Y J,Li B.2016.Effects of intersection and dead-end of fractures on nonlinear flow and particle transport in rock fracture networks.Geosciences Journal,20(3):415-426.
Liu X J,Xu J F,Wang S Q,et al.2009.Geochemistry and dating of E-MORB type mafic rocks from Dalabute ophiolite in West Junggar,Xinjiang and geological implications.Acta Petrologica Sinica(in Chinese),25(6):1373-1389.
Ma C,Zhao G P,Xiao W J,et al.2011.Emplacement of ophiolites:Mechanisms and timing.Chinese Journal of Geology(in Chinese),46(3):865-874.
McNeice G W,Jones A G.2012.Multisite,multifrequency tensor decomposition of magnetotelluric data.Geophysics,66(1):158-173.
Mei S W,Wang Y M,Du X F,et al.2016.Geochemical characteristics of the serpentinized peridotite in the Wenduermiao Area,Inner Mongolia,China and their geological significance.Bulletin of Mineralogy,Petrology and Geochemistry(in Chinese),35(2):212-221.
Miao L C,Fan W M,Liu D Y,et al.2008.Geochronology and geochemistry of the Hegenshan ophiolitic complex:Implications for late-stage tectonic evolution of the Inner Mongolia-Daxinganling Orogenic Belt,China.Journal of Asian Earth Sciences,32(5-6):348-370.
Rodi W,Mackie R L.2000.Nonlinear conjugate gradients algorithm for2-D magnetotelluric inversion.Geophysics,66(1):174-187.
Shi G R,Chen Z Q.2006.Lower Permian oncolites from South China:Implications for equatorial sea-level responses to Late Palaeozoic Gondwanan glaciation.Journal of Asian Earth Sciences,26(3-4):424-436.
Smith J T,Booker J R.2012.Rapid inversion of two-and threedimensional magnetotelluric data.Journal of Geophysical Research:Solid Earth,96(B3):3905-3922.
Tian C L,Cao C Z,Yang F L.1989.Geochemical features of ophiolite in the fold belt on the north side of the Sino-Korean platform.Bulletin of the Chinese Academy of Geological Science(in Chinese),11:107-129.
Wang H,Wang Y J,Chen Z Y,et al.2005.Discovery of the Permian radiolarians from the Bayanaobao area,Inner Mongolia.Journal of Stratigraphy(in Chinese),29(4):368-371.
Wang S Q,Xu J F,Liu X J,et al.2008.Geochemistry of the Chaokeshan ophiolite:Product of intra-oceanic back-arc basin?.Acta Petrologica Sinica(in Chinese),24(12):2869-2879.
Windley B F,Alexeiev D,Xiao W J,et al.2007.Tectonic models for accretion of the Central Asian Orogenic Belt.Journal of the Geological Society,164:31-47.
Wu F Y,Sun D Y,Li H M,et al.2002.A-type granites in northeastern China:Age and geochemical constraints on their petrogenesis.Chemical Geology,187(1-2):143-173.
Xiao W J.2004.Paleozoic accretionary and collisional tectonics of the eastern Tianshan(China):Implications for the continental growth of central Asia.Social Compass,304(1):85-98.
Xiao W J,Brian F,Windley,et al.2002.Arc-ophiolite obduction in the Western Kunlun Range(China):Implications for the Palaeozoic evolution of Central Asia.J Geol Soc Lond.Journal of the Geological Society,159(13):517-528.
Xiao W J,Brian F.Windley,Hao J,et al.2003.Accretion leading to collision and the Permian Solonker suture,Inner Mongolia,China:Termination of the central Asian orogenic belt.Tectonics,22(6):8-1-8-20.
Xiao W J,Windley B F,Huang B C,et al.2009.End-Permian to midTriassic termination of the accretionary processes of the southern Altaids:Implications for the geodynamic evolution,Phanerozoic continental growth,and metallogeny of Central Asia.International Journal of Earth Sciences,98(6):1189-1217.
Xiao W J,Windley B F,Sun S,et al.2015.A tale of amalgamation of three permo-triassic collage systems in Central Asia:Oroclines,Sutures,and Terminal Accretion.Annual Review of Earth and Planetary Sciences,43(1):477-507.
Xu B,Charvet J,Chen Y,et al.2013.Middle Paleozoic convergent orogenic belts in western Inner Mongolia(China):framework,kinematics,geochronology and implications for tectonic evolution of the Central Asian Orogenic Belt.Gondwana Research,23(4):1342-1364.
Xu B,Charvet J,Zhang F Q.2001.Primary study on petrology and geochrononology of blueschists in Sunitezuoqi,Northern Inner Mongolia.Chinese Journal of Geology(in Chinese),36(4):424-434.
Xu B,Chen B.1997.Framework and evolution of the middle Paleozoic orogenic belt between Siberian and North China Plates in northern Inner Mongolia.Science in China Series D:Earth Sciences,40(5):463-469.
Xu G Y.1993.The tectonic evolution of Paleo-Asian Ocean in Northeast Asia.Jilin Geology(in Chinese),12(3):1-8.
Xu L B,Wei W B,Jin S,et al.2017.Study of deep electrical structure along aprofile from northern Ordos block to Yinshan orogenic belt.Chinese Journal of Geophysics(in Chinese),60(2):575-584,doi:10.6038/cjg20170212.
Xu X,Zhu Y F,Chen B.2007.Petrology of the Kamste ophiolite mélange from East Junggar,Xinjiang,NW China.Acta Petrologica Sinica(in Chinese),23(7):1603-1610.
Xu X X,Li J J,Liu J C,et al.2011.The crust-upper mantle electrical structure along Xilinhot-Dongwuqi section.Chinese Journal of Geophysics(in Chinese),54(5):1031-1039,doi:10.3969/j.issn.0001-5733.2011.05.019.
Xu Z Q.2007.Continental deep subduction and exhumation dynamics:Evidence from the main hole of the Chinese Continental Scientific Drilling and the Sulu HP-UHP metamorphic terrane.Acta Petrologica Sinica(in Chinese),23(12):3041-3053.
Yang W C,Yang W Y,Jin Z M,et al.2004.Lithospheric seismic fabrics of Sulu ultrahigh-pressure metamorphic belt.Science in China Series D:Earth Sciences,48(5):585-600.
Yuan X C.2007.Mushroom structure of the lithospheric mantle and its genesis at depth:Revisited.Geology in China(in Chinese),34(5):737-758.
Zhang S B,Tang J,Zheng Y F.2014.Contrasting Lu-Hf isotopes in zircon from Precambrian metamorphic rocks in the Jiaodong Peninsula:Constraints on the tectonic suture between North China and South China.Precambrian Research,245:29-50.
Zhang S H,Gao R,Li H Y,et al.2014.Crustal structures revealed from a deep seismic reflection profile across the Solonker suture zone of the Central Asian Orogenic Belt,northern China:An integrated interpretation.Tectonophysics,612-613:26-39.
Zhang Y S,Zhang J C.2017.Lithology-dependent minimum horizontal stress and in-situ stress estimate.Tectonophysics,703-704:1-8.
Zheng P,Zhang Y Z,Li Z X,et al.2008.Geochemical characteristics and forming environment of the carboniferous gabbro in yaduwula mountain area,middle Daxinganling.Geology and Resources(in Chinese),17(4):250-253,272.
Zheng Y F,Gao T S,Wu Y B,et al.2007.Fluid flow during exhumation of deeply subducted continental crust:zircon U-Pb age and O-isotope studies of a quartz vein within ultrahigh-pressure eclogite.Journal of Metamorphic Geology,25(2):267-283.
Zhou Z G,Gu Y C,Liu C F,et al.2010.Discovery of Early-Middle Permian cathaysian flora in Manduhubaolage area,Dong Ujimqin Qi,Inner Mongolia,China and its geological significance.Geological Bulletin of China(in Chinese),29(1):21-25.
Zhu Y F,Xu X.2006.The discovery of Early Ordovician ophiolite mélange in Taerbahatai Mts.Xinjiang,NW China.Acta Petrologica Sinica(in Chinese),22(12):2833-2842.
白立兵,李玉玺,刘俊杰.2004.内蒙古满都拉泥盆纪基性火山岩特征及其形成环境.华南地质与矿产,(3):50-54.
白文吉,杨经绥,周美付等.1995.西准噶尔不同时代蛇绿岩及其构造演化.岩石学报,11(S1):62-72.
蔡军涛,陈小斌.2010.大地电磁资料精细处理和二维反演解释技术研究(二)---反演数据极化模式选择.地球物理学报,53(11):2703-2714,doi:10.3969/j.issn.0001-5733.2010.11.018.
蔡军涛,陈小斌,赵国泽.2010.大地电磁资料精细处理和二维反演解释技术研究(一)---阻抗张量分解与构造维性分析.地球物理学报,53(10):2516-2526,doi:10.3969/j.issn.0001-5733.2010.10.025.
蔡志慧,许志琴,唐哲民等.2009.北苏鲁荣成地区超高压变质带的形成与折返动力学.岩石学报,25(7):1627-1638.
陈斌,赵国春,Wilde S.2001.内蒙古苏尼特左旗南两类花岗岩同位素年代学及其构造意义.地质论评,47(4):361-367.
陈小斌,郭春玲.2017.大地电磁资料精细处理和二维反演解释技术研究(五)---利用阻抗张量成像识别大地线性构造.地球物理学报,60(2):766-777,doi:10.6038/cjg20170227.
董泽义,汤吉,陈小斌等.2016.华北克拉通东北边界带深部电性结构特征.地震地质,38(1):107-120.
和政军,刘淑文,任纪舜等.1997.内蒙古林西地区晚二叠世-早三叠世沉积演化及构造背景.地质通报,16(4):403-409,427.
胡骁,牛树银,张英涛.1987.内蒙古白乃庙地区中晚志留世复理石.地质通报,(4):47-54.
黄波,付冬,李树才等.2016.内蒙古贺根山蛇绿岩形成时代及构造启示.岩石学报,32(1):158-176.
黄竺,杨经绥,朱永旺等.2015.内蒙古贺根山蛇绿岩的铬铁矿中发现金刚石等深部地幔矿物.中国地质,(5):1493-1514.
李朋武,高锐,管烨等.2006.内蒙古中部索伦-林西缝合带封闭时代的古地磁分析.吉林大学学报(地球科学版),36(5):744-758.
李朋武,高锐,管烨等.2007.华北与西伯利亚地块碰撞时代的古地磁分析---兼论苏鲁-大别超高压变质作用的构造起因.地球学报,28(3):234-252.
李瑞彪,徐备,赵盼等.2014.二连浩特艾力格庙地区蓝片岩相岩石的发现及其构造意义.科学通报,59(1):66-71.
李三忠,赵淑娟,余珊等.2016.东亚原特提斯洋(Ⅱ):早古生代微陆块亲缘性与聚合.岩石学报,32(9):2628-2644.
李英杰,王金芳,李红阳等.2015.内蒙古西乌旗梅劳特乌拉蛇绿岩的识别.岩石学报,31(5):1461-1470.
梁宏达,高锐,候贺晟等.2015.碰撞后的地壳尺度伸展记录---中亚造山带南缘-华北克拉通北缘深部电性结构的揭露.地质科学,50(2):643-652.
刘家义,李春昱,肖序常.1985.内蒙贺根山地区蛇绿岩套研究及构造意义.∥中国地质科学院文集(1982中英文合订本),176-177.
刘建峰,李锦轶,孙立新等.2016.内蒙古巴林左旗九井子蛇绿岩锆石U-Pb定年:对西拉木伦河缝合带形成演化的约束.中国地质,43(6):1947-1962.
刘利双,刘福来,刘平华等.2015.苏鲁超高压变质带中海阳所地区变基性岩的地球化学性质及变质演化特征.岩石学报,31(10):2863-2888.
刘希军,许继峰,王树庆等.2009.新疆西准噶尔达拉布特蛇绿岩E-MORB型镁铁质岩的地球化学、年代学及其地质意义.岩石学报,25(6):1373-1389.
马冲,赵桂萍,肖文交等.2011.蛇绿岩就位机制及时限.地质科学,46(3):865-874.
梅盛旺,汪玉梅,杜显锋等.2016.内蒙古温都尔庙地区蛇纹石化橄榄岩地球化学特征及其地质意义.矿物岩石地球化学通报,35(2):212-221.
田昌烈,曹从周,杨芳林.1989.中朝陆台北侧褶皱带(中段)蛇绿岩的地球化学特征.中国地质科学院院报,11:107-129.
王惠,王玉净,陈志勇等.2005.内蒙古巴彦敖包二叠纪放射虫化石的发现.地层学杂志,29(4):368-371.
王树庆,许继峰,刘希军等.2008.内蒙朝克山蛇绿岩地球化学:洋内弧后盆地的产物?岩石学报,24(12):2869-2879.
魏文博,叶高峰,金胜等.2008.华北地区东部岩石圈导电性结构研究-减薄的华北岩石圈特点.地学前缘,15(4):204-216.
徐备,陈斌.1997.内蒙古北部华北板块与西伯利亚板块之间中古生代造山带的结构及演化.中国科学(D辑),27(3):227-232.
徐备,Charvet J,张福勤.2001.内蒙古北部苏尼特左旗蓝片岩岩石学和年代学研究.地质科学,36(4):424-434.
徐公愉.1993.东北亚地区古亚洲洋的构造演化特点.吉林地质,12(3):1-8.
许林斌,魏文博,金胜等.2017.鄂尔多斯地块北部至阴山造山带
深部电性结构特征研究.地球物理学报,60(2):575-584,doi:10.6038/cjg20170212.
徐新,朱永峰,陈博.2007.卡姆斯特蛇绿混杂岩的岩石学研究及其地质意义.岩石学报,2007,23(7):1603-1610.
徐新学,李俊健,刘俊昌等.2011.内蒙古锡林浩特-东乌旗剖面壳幔电性结构研究.地球物理学报,54(5):1301-1309,doi:10.3969/j.issn.0001-5733.2011.05.019.
许志琴.2007.深俯冲和折返动力学:来自中国大陆科学钻探主孔及苏鲁超高压变质带的制约.岩石学报,23(12):3041-3053.
杨文采,杨午阳,金振民等.2004.苏鲁超高压变质带岩石圈的地震组构.中国科学D辑地球科学,34(4):307-319.
袁学诚.2007.再论岩石圈地幔蘑菇云构造及其深部成因.中国地质,34(5):737-758.
郑萍,张永正,李振祥等.2008.大兴安岭中段牙都乌拉山地区石炭纪辉长岩特征及形成环境.地质与资源,17(4):250-253,272.
周志广,谷永昌,柳长峰等.2010.内蒙古东乌珠穆沁旗满都胡宝拉格地区早-中二叠世华夏植物群的发现及地质意义.地质通报,29(1):21-25.
朱永峰,徐新.2006.新疆塔尔巴哈台山发现早奥陶世蛇绿混杂岩.岩石学报,22(12):2833-2842.
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