[1]刘一鸣,李三忠,于胜尧.2019.青藏高原班公湖-怒江缝合带及周缘燕山期微地块聚合与增生造山过程.大地构造与成矿学,43(4):824-838.doi:10.16539/j.ddgzyckx.2019.04.013
 LIU Yiming,LI Sanzhong,YU Shengyao.2019.The Mesozoic Collage and Orogeny Process of Micro-blocks in Bangong-Nujiang Suture Zone, Tibetan Plateau.Geotectonica et Metallogenia,43(4):824-838.doi:10.16539/j.ddgzyckx.2019.04.013
点击复制

青藏高原班公湖-怒江缝合带及周缘燕山期微地块聚合与增生造山过程
分享到:

《大地构造与成矿学》[ISSN:ISSN 1001-1552/CN:CN 44-1595/P]

卷:
期数:
2019年43卷04期
页码:
824-838
栏目:
微板块构造专辑
出版日期:
2019-08-15

文章信息/Info

Title:
The Mesozoic Collage and Orogeny Process of Micro-blocks in Bangong-Nujiang Suture Zone, Tibetan Plateau
文章编号:
1001-1552(2019)04-0824-015
作者:
刘一鸣12 李三忠12* 于胜尧12 曹现志12 周 洁12 李 阳12 王誉桦12 徐林山3 郭润华12 周在征12
1.海底科学与探测技术教育部重点实验室, 中国海洋大学 海洋高等研究院和海洋地球科学学院, 山东 青岛 266100; 2.青岛海洋科学与技术国家实验室 海洋矿产资源评价与探测技术功能实验室, 山东 青岛 266237; 3.北京市地质工程设计研究院, 北京 100050
Author(s):
LIU Yiming12 LI Sanzhong12* YU Shengyao12 CAO Xianzhi12 ZHOU Jie12 LI Yang12 WANG Yuhua12 XU Linshan3 GUO Runhua12 and ZHOU Zaizheng12
1.Key Lab of Submarine Geosciences and Prospecting Techniques, MOE, Institute for Advanced Ocean Study and College of Marine Geosciences, Ocean University of China, Qingdao 266100, Shandong, China; 2.Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, Shandong, China; 3.Beijing Institute of Geological Engineering, Beijing 100050, China
关键词:
青藏高原 燕山期 微地块 聚合增生
Keywords:
Tibetan Plateau Yanshanian micro-blocks collage
分类号:
P542
DOI:
10.16539/j.ddgzyckx.2019.04.013
文献标志码:
A
摘要:
班公湖-怒江洋多岛弧盆体系的俯冲闭合过程对于研究青藏高原早期形成与演化具有重要意义。本文系统总结了羌南-保山地块与拉萨地块燕山期的岩浆岩、沉积序列以及变质变形特征, 详细探讨了其与班公湖-怒江洋俯冲闭合过程的联系。研究结果显示随着特提斯大洋的打开, 羌南-保山地块、拉萨地块、聂荣微地块和嘉玉桥微地块均作为裂生微地块从冈瓦纳大陆北缘裂解出来, 北拉萨地块是班公湖-怒江洋南向俯冲弧后扩张裂解的产物, 并随着大洋的南向俯冲, 逐渐演变为增生型微地块。随着洋盆的闭合这些微地块作为残生微地块碰撞拼贴在一起, 保留在造山带之中。班公湖-怒江洋在燕山期经历了复杂而漫长的多个微小地块的碰撞增生过程。该过程最早可能始于晚侏罗世, 并主体于早白垩世末期-晚白垩世初期汇聚消亡, 期间经历了纵向和横向的双重穿时性。印度-雅鲁藏布江洋的北向俯冲作用对于班公湖-怒江洋的汇聚消亡以及青藏高原现今主体构造格架形成至关重要。
Abstract:
The subduction and closure of the Bangong-Nujiang Ocean are recognized as significant events in the geotectonic evolution of Tibetan Plateau.This study focuses on the Mesozoic magmatic rocks, sedimentary strata, metamorphic and deformation features, and discusses their relation with the evolution of the Bangong-Nujiang Ocean in details.The Qiangnan-Baoshan, Lhasa, Nierong and Jiayuqiao micro-blocks rifted from the northern margin of the Gondwana as rifting-induced micro-blocks.The northern Lhasa micro-blocks was a product of the back-arc spreading of the Bangong-Nujiang Ocean, and evolved into an accretion-induced micro-blocks due to the southward subduction of the Bangong-Nujiang Ocean.All these micro-blocks collaged together as subduction-derived micro-blocks preserving in the orogenic belt.The Bangong-Nujiang Ocean experienced a complex and prolonged process of multiple collage and collision among micro-blocks during the Mesozoic period.This process may have started in the Late Jurassic and completed at the end of the Early Cretaceous to early Late Cretaceous.Both longitudinal and transverse diachronism occurred during the closure of the Bangong-Nujiang Ocean.The northward subduction of the Indus-Yarlung Zangbo Ocean is important to the closure of the Bangong-Nujiang Ocean, as well as the formation of the modern tectonic framework of Tibetan Plateau.

参考文献/References:

白建科, 陈隽璐, 闫臻, 唐卓, 徐学义, 李继亮.2015.西准噶尔南部玛依勒洋盆开启、闭合时限: 来自中泥盆统与下伏地质体之间角度不整合关系的证据.岩石学报, 31(1): 133-142.
杜德道, 曲晓明, 王根厚, 辛洪波, 刘治博.2011.西藏班公湖-怒江缝合带西段中特提斯洋盆的双向俯冲: 来自岛弧型花岗岩锆石U-Pb年龄和元素地球化学的证据.岩石学报, 27(7): 1993-2002.
范建军.2016.班公湖-怒江洋中西段晚中生代汇聚消亡时空重建.长春: 吉林大学博士学位论文: 1-225.
付佳俊, 丁林, 许强, 蔡福龙, 岳雅慧, 郭钰.2015.西藏改则洞错地区白垩纪火山岩锆石U-Pb年代学、Hf同位素组成及对班公-怒江洋俯冲闭合的制约.地质科学, 50(1): 182-202.
和钟铧, 杨德明, 王天武, 黄应聪.2006.西藏比如盆地竟柱山组沉积-火山岩形成环境及构造意义.沉积与特提斯地质, 26(1): 8-12.
李才.2008.青藏高原龙木错-双湖-澜沧江板块缝合带研究二十年.地质论评, 54(1): 105-119.
李才, 谢尧武, 沙绍礼, 董永胜.2008.藏东八宿地区泛非期花岗岩锆石 SHRIMP U-Pb 定年.地质通报, 27(1): 64-68.
李才, 翟庆国, 陈文, 董永胜, 于介江.2007.青藏高原龙木错-双湖板块缝合带闭合的年代学证据——来自果干加年山蛇绿岩与流纹岩Ar-Ar和SHRIMP年龄制约.岩石学报, 23(5): 911-918.
李才, 翟庆国, 程立人, 徐峰, 黄小鹏.2005.青藏高原羌塘地区几个关键地质问题的思考.地质通报, 24(4): 295-301.
李光明, 段志明, 刘波, 张晖, 董随亮, 张丽.2011.西藏班公湖-怒江结合带北缘多龙地区侏罗纪增生杂岩的特征及意义.地质通报, 30(8): 1256-1260.
李伟.2012.西藏改则地区去申拉组火山岩地球化学特征及锆石年代学制约.北京: 中国地质大学硕士学位论文: 1-64.
刘敏.2012.青藏高原中部聂荣微陆块侏罗纪早期富碱侵入岩的岩石成因及构造意义.北京: 中国地质大学硕士学位论文: 1-179.
刘通, 翟庆国, 王军, 苏犁, 康珍.2013.藏北羌塘盆地基底高级变质岩LA-ICP-MS锆石U-Pb年龄及其地质意义.地质通报, 32(11): 1691-1703.
吕杰.2010.青藏高原侏罗纪羌塘盆地构造-古地理和盆地演化.成都: 成都理工大学硕士学位论文: 1-87.
潘桂棠, 莫宣学, 侯增谦, 朱弟成, 王立全, 李光明, 廖忠礼.2006.冈底斯造山带的时空结构及演化.岩石学报, 22(3): 521-533.
曲晓明, 辛洪波, 赵元艺, 王瑞江, 樊兴涛.2010.西藏班公湖中特提斯洋盆的打开时间: 镁铁质蛇绿岩地球化学与锆石 U-Pb LA-ICP-MS定年结果.地学前缘, 17(3): 53-63.
曲永贵, 刘贵忠, 郑春子, 王永胜, 张树岐.2003.西藏北部班戈地层分区下白垩统郎山组、康曲组和余穷组地层层序研究.地层学杂志, 27(3): 220-226.
孙立新.2005.班公湖-怒江缝合带中段晚侏罗世-早白垩世碰撞作用的沉积响应.北京: 中国地质大学博士学位论文: 1-138.
孙振明.2015.西藏班-怒成矿带西段多龙矿集区铜金成矿作用与成矿规律.长春: 吉林大学博士学位论文: 1-170.
王立全, 潘桂棠, 丁俊, 姚冬生, 罗建宁, 颜仰基, 张克信.2013.青藏高原及邻区地质图及说明书(1∶1500000).北京: 地质出版社: 1-253.
吴福元, 黄宝春, 叶凯, 方爱民.2008.青藏高原造山带的垮塌与高原隆升.岩石学报, 24(1): 1-30.
解超明.2013.青藏高原聂荣微陆块构造演化——年代学与地球化学制约.长春: 吉林大学博士学位论文: 1-162.
谢国刚, 莫宣学, 赵志丹, 董国臣.2009.西藏班公湖地区侏罗纪-白垩纪沉积及古海洋盆地的演化.地学前缘, 16(4): 31-39.
辛洪波, 曲晓明.2006.藏西措勤县日阿与斑(玢)岩有关的铜矿床的矿床地质特征与成矿时代.矿床地质, 25(4): 477-482.
徐梦婧.2014.青藏高原狮泉河-永珠-嘉黎蛇绿混杂岩带的构造演化.长春: 吉林大学博士学位论文: 1-152.
许荣科, 郑有业, 赵平甲, 陕亮, 张雨莲, 曹亮, 代芳华.2007.西藏东巧北尕苍见岛弧的厘定及地质意义.中国地质, 34(5): 768-777.
许志琴, 杨经绥, 李海兵, 张建新, 曾令森, 姜枚.2006.青藏高原与大陆动力学——地体拼合、碰撞造山及高原隆升的深部驱动力.中国地质, 33(2): 221-238.
杨德明, 胡波, 董清水, 王天武.2009.西藏嘉黎巴嘎地区早白垩世多尼组地层特征与沉积环境.世界地质, 28(3): 280-283.
张硕, 史洪峰, 郝海健, 李德威, 吝岩, 冯旻譞.2014.青藏高原班公湖地区晚白垩世埃达克岩年代学、地球化学及构造意义.地球科学, 39(5): 509-524.
张玉修.2007.班公湖-怒江缝合带中西段构造演化.广州: 中国科学院广州地球化学研究所博士学位论文: 1-268.
张玉修, 张开均, 李勇, 李亚林, 谢尧武, 黎兵.2007.西藏羌塘盆地东部中-上侏罗统沉积特征及沉积相划分.大地构造与成矿学, 31(1): 52-62.
朱弟成, 潘桂棠, 王立全, 莫宣学, 赵志丹, 周长勇, 袁四化.2008.西藏冈底斯带侏罗纪岩浆作用的时空分布及构造环境.地质通报, 27(4): 458-468.
Baxter A T, Aitchison J C and Zyabrev S V.2009.Radio?larian age constraints on Mesotethyan ocean evolution, and their implications for development of the Bangong-Nujiang suture, Tibet.Journal of the Geological Society, 166: 689-694.
Chen W W, Zhang S H, Ding J K, Zhang J H, Zhao X X, Zhu L D, Yang W G, Yang T S, Li H Y and Wu H C.2015.Combined paleomagnetic and geochronological study on Cretaceous strata of the Qiangtang terrane, central Tibet.Gondwana Research, 41: 373-389.
Chen Y, Zhu D C, Zhao Z D, Meng F Y, Wang Q, Santosh M, Wang L Q, Dong G C and Mo X X.2014.Slab breakoff triggered ca.113 Ma magmatism around Xainza area of the Lhasa Terrane, Tibet.Gondwana Research, 26: 449-463.
DeCelles P G, Kapp P, Ding L and Gehrels G E.2007.Late Cretaceous to middle Tertiary basin evolution in the central Tibetan Plateau: Changing environments in response to tectonic partitioning, aridification, and regional elevation gain.Geological Society of America Bulletin, 119: 654-680.
Dewey J F, Shackleton R M and Chang C.1988.The tectonic development of the Tibetan Plateau.Philoso?phical Transactions of the Royal Society, 327: 379-413.
Fan J J, Li C, Liu Y M and Xu J X.2015.Age and nature of the late Early Cretaceous Zhaga Formation, northern Tibet: Constraints on when the Bangong-Nujiang Neo-Tethys Ocean closed.International Geology Review, 57: 342-353.
Fan J J, Li C, Wang M and Xie C M.2018.Reconstructing in space and time the closure of the middle and western segments of the Bangong-Nujiang Tethyan Ocean in the Tibetan Plateau.International Journal of Earth Sciences, 107: 231-249.
Fan J J, Li C, Xie C M and Wang M.2014b.Petrology geochemistry and geochronology of the Zhonggang ocean island northern Tiber: Implications for the evolution of the Bangongco-Nujiang oceanic arm of Neo-Tethys.International Geology Review, 56: 1504-1520.
Fan J J, Li C, Xu J X and Wang M.2014a.Petrology geochemistry and geological significance of the Nadong ocean island Banggong-Nujiang suture Tibetan Plateau.International Geology Review, 56: 915-928.
Guynn J H, Kapp P, Pullen A, Gehrels G E, Heizler M and Ding L.2006.Tibetan basement rocks near Amdo reveal “missing” Mesozoic tectonism along the Bangong suture, central Tibet.Geology, 34: 505-508.
Guynn J H, Tropper P, Kapp P and Gehrels G.2013.Metamorphism of the Amdo metamorphic complex, Tibet: Implications for the Jurassic tectonic evolution of the Bangong suture zone.Journal of Metamorphic Geology, 31: 705-727.
Hao L L, Wang Q, Wyman D A, Ou Q, Dan W, Jiang Z Q, Yang J H, Li J and Long X P.2016.Andesitic crustal growth via mélange partial melting: Evidence from Early Cretaceous arc dioritic/andesitic rocks in southern Qiangtang, central Tibet.Geochemistry Geophysics Geosystems, 17: 1641-1659.
Harris N B W, Xu R H, Lewis C L and Jin C W.1988.Plutonic rocks of the 1985 Tibet Geotraverse, Lhasa to Golmud.Philosophical Transactions of the Royal Society of London, Series A, Mathematical and Physical Sciences, 327: 145-168.
Ji W Q, Wu F Y, Chung S L, Li J X and Liu C Z.2009.Zircon U-Pb geochronology and Hf isotopic constraints on petrogenesis of the Gangdese batholith, southern Tibet.Chemical Geology, 262: 229-245.
Jordan T E and Gardeweg M.1989.Tectonic evolution of the Late Cenozoic Central Andes (20°-33°S) // Ben-Avraham Z.Oxford Monographs on Geology and Geophysics 8: The Evolution of the Pacific Ocean Margins.Oxford: Clarendon Press: 193-207.
Kapp P, DeCelles P G, Gehrels G E, Heizler M and Ding L.2007.Geological records of the Lhasa-Qiangtang and Indo-Asian collisions in the Nima area of central Tibet.Geological Society of America Bulletin, 119: 917-932.
Kapp P, Muupy M A, Yin A, Harrison T M, Ding L and Guo J.2003.Mesozoic and Cenozoic tectonic evolution of the Shiquanhe area of western Tibet.Tectonics, 22: 3-23.
Kapp P, Yin A, Harrison T M and Ding L.2005.Cretaceous-Tertiary shortening, basin development, and volcanism in central Tibet.Geological Society of America Bulletin, 117: 865-878.
Li G M, Qin K Z, Li J X, Evans N J, Zhao J X, Cao M J and Zhang X N.2017a.Cretaceous magmatism and metallogeny in the Bangong-Nujiang metallogenic belt, central Tibet: Evidence from petrogeochemistry, zircon U-Pb ages, and Hf-O isotopic compositions.Gondwana Research, 41: 110-127.
Li H Q, Xu Z Q, Webb A A G, Li T F, Ma S W and Huang X M.2017b.Early Jurassic tectonism occurred within the Basu metamorphic complex, eastern central Tibet: Implications for an archipelago-accretion orogenic model.Tectonophysics, 702: 29-41.
Li J X, Qin K Z, Li G M, Richards J P, Zhao J X and Cao M J.2014.Geochronology, geochemistry, and zircon Hf isotopic compositions of Mesozoic intermediate-felsic intrusions in central Tibet: Petrogenetic and tectonic implications.Lithos, 198: 77-91.
Li Y L, He J, Wang C S, Santosh M, Dai J G, Zhang Y X, Wei Y S and Wang J G.2013.Late Cretaceous K-rich magmatism in central Tibet: Evidence for early elevation of the Tibetan plateau? Lithos, 160: 1-13.
Liu D L, Shi R D, Ding L, Huang Q S, Zhang X R, Yue Y H and Zhang L Y.2017c.Zircon U-Pb age and Hf isotopic compositions of Mesozoic granitoids in southern Qiangtang, Tibet: Implications for the subduction of the Bangong-Nujiang Tethyan Ocean.Gondwana Research, 41: 157-172.
Liu Y M, Li C, Xie C M, Wang M and Fan J J.2017b.Geochronology of the Duguer range metamorphic rocks, Central Tibet: Implications for the changing tectonic setting of the South Qiangtang subterrane.International Geology Review, 59: 29-44.
Liu Y M, Li S Z, Santosh M, Cao H H, Yu S Y, Wang Y H, Zhou J and Zhou Z Z.2019b.The generation and reworking of continental crust during early Paleozoic in Gondwanan affinity terranes from the Tibet Plateau.Earth-Science Reviews, 190: 486-497.
Liu Y M, Wang M, Li C, Li S Z, Xie C M, Zeng X W, Dong Y C and Liu J H.2019a.Late Cretaceous tectono-magmatic activity in the Nize region, central Tibet: Evidence for lithospheric delamination beneath the Qiangtang-Lhasa collision zone.International Geology Review, 61: 562-583.
Liu Y M, Wang M, Li C, Xie C M, Chen H Q, Li Y B, Fan J J, Li X K, Xu W and Sun Z M.2017a.Cretaceous structures in the Duolong region of central Tibet: Evidence for an accretionary wedge and closure of the Bangong-Nujiang Neo-Tethys Ocean.Gondwana Research, 48: 110-123.
Murphy M A, Yin A, Harrison T M, Dürr S B, Chen Z, Ryerson F J, Kidd W S F, Wang X and Zhou X.1997.Did the Indo-Asian collision alone create the Tibetan Plateau? Geology, 25: 719-722.
Pan G T, Wang L Q, Li R S, Yuan S H, Ji W H, Yin F G, Zhang W P and Wang B D.2012.Tectonic evolution of the Qinghai-Tibet plateau.Journal of Asian Earth Sciences, 53: 3-14.
Pullen A, Kapp P, Gehrels G E, Ding L and Zhang Q H.2011.Metamorphic rocks in central Tibet: Lateral variations and implications for crustal structure.Geological Society of America Bulletin, 123: 585-600.
Qu X M, Wang R J, Xin H B, Jiang J H and Chen H.2012.Age and petrogenesis of A-type granites in the middle segment of the Bangonghu-Nujiang suture, Tibetan plateau.Lithos, 146-147: 264-275.
Robinson A C, Yin A, Manning C E, Harrison T M, Zhang S H and Wang X F.2004.Tectonic evolution of the northeastern Pamir: Constraints from the northern portion of the Cenozoic Kongur Shan extensional system, western China.Geological Society of America Bulletin, 116: 953-973.
Shi R D, Yang J S, Xu Z Q and Qi X X.2008.The Bangong Lake ophiolite (NW Tibet) and its bearing on the tectonic evolution of the Bangong-Nujiang suture zone.Journal of Asian Earth Sciences, 32: 438-457.
Sui Q L, Wang Q, Zhu D C, Zhao Z D, Chen Y, Santosh M, Hu Z C, Yuan H L and Mo X X.2013.Compositional diversity of ca.110 Ma magmatism in the northern Lhasa Terrane, Tibet: Implications for the magmatic origin and crustal growth in a continent-continent collision zone.Lithos, 168-169: 144-159.
Sun G Y, Hu X M, Sinclair H D, BouDagher-Fadel M K and Wang J G.2015.Late Cretaceous evolution of the Coqen Basin (Lhasa terrane) and implications for early topographic growth on the Tibetan Plateau.Geological Society of America Bulletin, 127: 1001-1020.
Tapponnier P, Zhiqin X, Roger F, Meyer B, Arnaud N, Wittlinger G and Jingsui Y.2001.Oblique stepwise rise and growth of the Tibet Plateau.Science, 294: 1671-1677.
Volkmer J E, Kapp P, Guynn J H and Lai Q.2007.Cretaceous-Tertiary structural evolution of the north central Lhasa Terrane, Tibet.Tectonics, 26: 1-18.
Volkmer J E, Kapp P, Horton B K, Gehrels G E, Minervini J M and Ding L.2014.Northern Lhasa thrust belt of central Tibet: Evidence of Cretaceous-Early Cenozoic shortening within a passive roof thrust system? Geological Society of America Special Papers, 507: 59-70.
Wallis S, Tsujimori T, Aoya M, Kawakami T, Terada K, Suzuki K and Hyodo H.2003.Cenozoic and Mesozoic metamorphism in the Longmenshan orogen: Implica?tions for geodynamic models of eastern Tibet.Geology, 31: 745-748.
Wang B D, Wang L Q, Chung S L, Chen J L, Yin F G, Liu H and Chen L K.2016.Evolution of the Bangong-Nujiang Tethyan ocean: Insights from the geochronology and geochemistry of mafic rocks within ophiolites.Lithos, 245: 18-33.
Wang Q, Zhu D C, Zhao Z D, Liu S A, Chung S L, Li S M, Liu D, Dai J G, Li G M and Mo X X.2014.Origin of the ca.90 Ma magnesia-rich volcanic rocks in SE Nyima, central Tibet: Products of lithospheric delami?na?tion beneath the Lhasa-Qiangtang collision zone.Lithos, 198: 24-37.
Wu Z H, Barosh P J, Ye P S and Hu D G.2015.Late Cretaceous tectonic framework of the Tibetan Plateau.Journal of Asian Earth Sciences, 114: 693-703.
Xu W, Li C, Wang M, Fan J J, Wu H and Li X.2017.Subduction of a spreading ridge within the Bangong Co-Nujiang Tethys Ocean: Evidence from Early Cretaceous mafic dykes in the Duolong porphyry Cu-Au deposit, western Tibet.Gondwana Research, 41: 128-141.
Yin A and Harrison T M.2000.Geologic evolution of the Himalayan-Tibetan orogen.Annual Review of Earth and Planetary Sciences, 28: 211-280.
Zahirovic S, Matthews K J, Flament N, Müller R D, Hill K C, Seton M and Gurnis M.2016.Tectonic evolution and deep mantle structure of the eastern Tethys since the latest Jurassic.Earth-Science Reviews, 162: 293-337.
Zhang K J, Xia B, Zhang Y X, Liu W L, Zeng L, Li J F and Xu L F.2014.Central Tibetan Meso-Tethyan oceanic plateau.Lithos, 210-211: 278-288.
Zhang K J, Zhang Y X, Tang X C, Xie Y W, Sha S L and Peng X J.2008.First report of eclogites from central Tibet, China: Evidence for ultradeep continental subduction prior to the Cenozoic India-Asian collision.Terra Nova, 20: 302-308.
Zhang X R, Shi R D, Huang Q S, Liu D L, Cidan S L, Yang J S and Ding L.2010.Finding of high-pressure mafic granulites in the Amdo terrane, central Tibet.Chinese Science Bulletin, 55: 3694-3702.
Zhang X Z, Wang Q, Dong Y S, Zhang C, Li Q Y, Xia X P and Xu W.2017.High-pressure granulite facies overprinting during the exhumation of eclogites in the Bangong-Nujiang suture zone, central Tibet: Link to flat-slab subduction.Tectonics, 36: 2918-2935.
Zhang Y X, Li Z W, Zhu L D, Zhang K J, Yang W G and Jin X.2015.Newly discovered eclogites from the Bangong Meso-Tethyan suture zone (Gaize, central Tibet, western China): Mineralogy, geochemistry, geochronology, and tectonic implications.International Geology Review, 58: 574-587.
Zhang Z M, Dong X, Liu F, Lin Y H, Yan R and Santosh M.2012.Tectonic evolution of the Amdo terrane, central Tibet: Petrochemistry and zircon U-Pb geochronology.Journal of Geology, 120: 431-451.
Zhu D C, Li S M, Cawood P A, Wang Q, Zhao Z D, Liu S A and Wang L Q.2016.Assembly of the Lhasa and Qiangtang terranes in central Tibet by divergent double subduction.Lithos, 245: 7-17.
Zhu D C, Zhao Z D, Niu Y L, Dilek Y, Hou Z Q and Mo X X.2013.The origin and pre-Cenozoic evolution of the Tibetan Plateau.Gondwana Research, 23: 1429-1454.
Zhu D C, Zhao Z D, Niu Y L, Mo X X, Chung S L, Hou Z Q, Wang L Q and Wu F Y.2011.The Lhasa Terrane: Record of a microcontinent and its histories of drift and growth.Earth and Planetary Science Letters, 301: 241-255.

相似文献/References:

[1]马润勇,席先武,彭建兵.青藏高原递进式隆升的力学模式.大地构造与成矿学,2005.29(4):451.
 MA Runyong,XI Xianwu,PENG Jianbing.MECHANICS MODEL OF PROGRESSIVE UPLIFT OF QINGHAI-TIBET PLATEAU.Geotectonica et Metallogenia,2005.43(4):451.
[2]滕吉文.青藏高原地区地壳—上地幔结构与巨厚地壳的形成.大地构造与成矿学,1990.14(4):333.
 TENG Jiwen.THE STRUCTURE OF CRUST AND UPPER MANTLE AND FORMATION OF HUGE THICK CRUST IN QINGHAI-XIZANG PLATEAU, CHINA.Geotectonica et Metallogenia,1990.43(4):333.
[3]陈国达.青藏高原隆升的历史背景和机因.大地构造与成矿学,1997.21(2):095.
 CHEN Guoda.MECHANISM AND HISTORICAL BACKGROUND OF THE UPLIFT OF THE QINHAI-XIZANG (TIBET) PLATEAU.Geotectonica et Metallogenia,1997.43(4):095.
[4]李相博,王新民,袁剑英.青藏高原东北部旋卷(扭)构造变形及其形成地质条件分析──兼评法国地质学家Tapponnier的“走向滑移线场和构造逃逸理论”.大地构造与成矿学,2001.25(2):120.
 LI Xiangbo,WANG Xinmin,YUAN Jianying.STUDY ON THE VORTEX STRUCTURE DEFORMATION AND ITS FORMING MECHANISM IN THE NORTHEASTERN QINGHAI-TIBET PLATEAU──Additionally Discussing French Geologist Tapponnier’s Theories of “strike-slip line field and sructure escaping”.Geotectonica et Metallogenia,2001.43(4):120.
[5]呼建雄,陈建林,张占武.青藏高原南部谢通门侏罗纪埃达克质岩地球化学特征及其形成机制.大地构造与成矿学,2013.37(2):320.
 HU Jianxiong,CHEN Jianlin,ZHANG Zhanwu.Geochemistry and Genesis of Middle Jurassic Adakitic Rocks in the Xietongmen Area of Southern Tibet.Geotectonica et Metallogenia,2013.43(4):320.
[6]刘 锐,吴昌雄 祝莉玲,赵新福.北大别南部存在巨量隐伏燕山期岩浆作用: 岩浆岩锆石U-Pb 年龄、元素及Sr-Nd-Hf 同位素地球化学证据.大地构造与成矿学,2018.优先出版:001.doi:10.16539/j.ddgzyckx.2018.06.015
 LIU Rui,WU Changxiong,ZHU Liling and ZHAO Xinfu.Giant Unexposed Yanshanian Magmatism in Southern North Dabie Terrane: Evidence from Zircon U-Pb Age, Elemental and Sr-Nd-Hf Isotope Geochemistry of Magmatic Rocks.Geotectonica et Metallogenia,2018.43(4):001.doi:10.16539/j.ddgzyckx.2018.06.015
[7]刘一鸣,李三忠,于胜尧.青藏高原班公湖?江缝合带及周缘燕山期微地块聚合与增生造山过程.大地构造与成矿学,2018.优先出版:824.doi:10.16539/j.ddgzyckx.2019.04.013
 LIU Yiming,LI Sanzhong,YU Shengyao.The Mesozoic Collage and Orogeny Process of Micro-blocks in Bangong-Nujiang Suture Zone, Tibetan Plateau.Geotectonica et Metallogenia,2018.43(4):824.doi:10.16539/j.ddgzyckx.2019.04.013

备注/Memo

备注/Memo:
收稿日期: 2018-08-31; 改回日期: 2019-05-14
项目资助: 国家重点研发计划项目(2017YFC0601401)、博士后创新人才支持计划项目(BX201700216)、青岛海洋科学与技术国家实验室鳌山科技创新计划项目(2016ASKJ13、2017ASKJ02)、中国博士后科学基金项目(2017M622273)、国家自然科学基金项目(41802232、41702050、41325009)和青岛市博士后应用研究项目联合资助。
第一作者简介: 刘一鸣(1989-), 男, 博士, 从事海洋地质研究。Email: michael_yatmingliu@foxmail.com
通信作者: 李三忠(1968-), 男, 教授, 博士生导师, 从事海洋地质学及构造地质学研究。Email: sanzhong@ouc.edu.cn
更新日期/Last Update: 2019-08-15