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 - Tập 43 Số 1 - Trang 477-507 - 2015
Wenjiao Xiao1,2,3, Brian F. Windley4, Shu Sun5,6, Jiliang Li5,6, Baochun Huang7, Chunming Han8,6, Chao Yuan9, Min Sun10,5, Hanlin Chen11
1State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
2Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 100029, China
3Xinjiang Research Center for Mineral Resources, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China
4Department of Geology, University of Leicester, Leicester, LE1 7RH United Kingdom
5Department of Geosciences, National Taiwan University, Taipei, Taiwan
6State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics and
7School of Earth and Space Science, Peking University, Beijing 100871, China
8CAS Center for Excellence in Tibetan Plateau Earth Science, Chinese Academy of Sciences, Beijing 100029, China;
9Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, 510640, China
10Department of Earth Sciences, University of Hong Kong, Hong Kong, China
11Department of Earth Sciences, Zhejiang University, Hangzhou 310027, China

Tóm tắt

The Central Asian Orogenic Belt records the accretion and convergence of three collage systems that were finally rotated into two major oroclines. The Mongolia collage system was a long, N–S-oriented composite ribbon that was rotated to its current orientation when the Mongol-Okhotsk orocline was formed. The components of the Kazakhstan collage system were welded together into a long, single composite arc that was bent to form the Kazakhstan orocline. The cratons of Tarim and North China were united and sutured by the Beishan orogen, which terminated with formation of the Solonker suture in northern China. All components of the three collage systems were generated by the Neoproterozoic and were amalgamated in the Permo-Triassic. The Central Asian Orogenic Belt evolved by multiple convergence and accretion of many orogenic components during multiple phases of amalgamation, followed by two phases of orocline rotation.

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Tài liệu tham khảo

10.1016/j.tecto.2008.05.006

10.1016/j.tecto.2007.04.008

10.1080/10020070612330044

10.1016/j.gr.2010.01.004

10.1016/j.gr.2012.02.023

10.1016/j.gr.2009.11.014

10.1134/S001685211005002X

10.1016/S1367-9120(03)00131-7

Cai DS, 1995, Chin. Geol. Rev., 41, 432

10.1016/j.rgg.2011.11.014

Carroll AR, 2001, Geol. Soc. Am. Mem., 194, 47

10.1016/j.earscirev.2007.03.003

10.1016/j.jseaes.2008.05.007

10.1016/j.gr.2011.07.015

10.1007/s11434-013-5862-7

10.1016/j.earscirev.2007.02.001

10.1016/S0012-821X(00)00061-3

10.2475/10.2006.02

10.1073/pnas.0505516102

10.1098/rsta.1988.0135

Dobretsov NL, 2006, Russ. Geol. Geophys., 47, 424

10.1016/j.gr.2011.07.014

10.1016/j.gsf.2014.01.002

10.1002/2013TC003357

10.1016/j.gr.2012.11.001

10.1016/j.jseaes.2013.01.020

10.1016/0040-1951(95)00026-6

10.1016/S0024-4937(02)00153-6

Gao R, Hou H, Cai X, Knapp J, He R. 2013. Fine crustal structure beneath the junction of the southwest Tian Shan and Tarim Basin, NW China.Lithosphere5:382–92

10.1002/2013TC003501

10.1016/j.jseaes.2011.01.006

Geng YS, 2007, Geol. China, 34, 251

10.1016/j.gr.2011.03.003

Guo FX, 2000, Acta Geol. Sin., 74, 1, 10.1111/j.1755-6724.2000.tb00425.x

10.1016/j.gr.2013.03.014

10.1016/j.earscirev.2011.09.001

10.1016/j.gr.2012.10.015

10.2475/09.2010.07

10.1130/B30510.1

10.1016/S0040-1951(00)00176-1

10.1016/S1367-9120(03)00124-X

10.1016/j.earscirev.2014.02.006

10.1016/j.lithos.2007.07.005

Jian P, 2007, Abstract and Excursion Guidebook, Third International Workshop and Field Excursion for IGCP Project 480, 49

10.1016/S0012-821X(01)00516-7

Johnston ST, 2004, Geol. Soc. Am. Spec. Pap., 383, 225

10.1016/S0040-1951(03)00021-0

10.1130/B30765.1

10.1016/S0012-821X(02)00587-3

10.2205/2003ES000123

10.1134/S0016852110010024

10.1086/427666

10.1130/2007.1200(11)

10.2475/07.2010.02

10.1016/j.tecto.2003.09.013

10.1016/j.epsl.2007.02.025

10.1016/j.precamres.2010.12.001

Li Q, 2004, Acta Petrol. Sin., 20, 583

10.1016/j.earscirev.2013.06.001

Li XD, 1994, Comprehensive Survey of Geological Sections in the West Tianshan of Xinjiang, China, 126

10.1016/j.jseaes.2010.09.009

10.1016/j.lithos.2014.05.022

10.2475/02.2014.08

10.1029/2007TC002128

10.1016/j.precamres.2007.04.025

10.1016/j.lithos.2012.02.005

10.1017/S0016756811000811

10.1111/j.1440-1738.1997.tb00042.x

10.1016/j.gr.2009.07.002

10.1016/j.gr.2008.07.001

10.1016/j.gr.2010.02.004

10.1007/BF03183519

10.1144/SP280.11

10.1016/j.jseaes.2007.11.005

10.1144/GSL.SP.1996.106.01.08

10.1016/j.tecto.2005.04.011

10.1016/j.gr.2005.06.014

Niu H, 2007, Acta Petrol. Sin., 23, 1627

10.1111/j.1502-3931.1995.tb01592.x

10.1111/j.1502-3931.1982.tb01131.x

10.1016/S1342-937X(05)71063-7

10.1016/j.gr.2012.10.008

10.1016/j.gr.2009.02.008

Seltmann R, 2005, Super Porphyry Copper and Gold Deposits: A Global Perspective, 467

Şengör AMC, 1996, The Tectonic Evolution of Asia, 486

10.1146/annurev.earth.24.1.263

10.1038/364299a0

10.1360/04wd0069

Shu LS, 2003, Geol. Rev., 49, 408

10.1016/j.rgg.2008.04.001

10.2205/2003ES000125

10.1016/S0012-8252(97)00019-6

Su B, Qin K, Zhou M, Sakyi P, Thakurta J. 2014. Petrological, geochemical and geochronological constraints on the origin of the Xiadong Ural-Alaskan type complex in NW China and tectonic implication for the evolution of the southern Central Asian Orogenic Belt.Lithos200–1:226–40

10.1016/j.chemgeo.2007.10.026

10.1111/j.1440-1738.1995.tb00150.x

10.1016/j.jsg.2013.03.016

Tian ZH, Xiao WJ, Sun JM, Windley BF, Glen R, et al. 2015. Early–Late Triassic deformation of Permian–Early Triassic arc-related sediments in the Beishan (NW China): last pulse of the accretionary orogenesis in the southernmost Altaids?Tectonophysics. In press. doi: 10.1016/j.tecto.2015.01.009

10.1016/j.gr.2013.06.012

10.1144/0016-764903-098

10.1016/j.tecto.2006.08.008

10.1144/GSL.SP.1998.143.01.17

10.1016/S0024-4937(99)00019-5

10.1016/j.rgg.2006.12.008

10.1016/j.jseaes.2004.04.004

10.1130/L234.1

10.1016/j.epsl.2007.08.037

10.1029/TC005i007p01073

10.1016/j.gsf.2012.02.002

Wang YJ, 1997, Acta Palaeontol. Sin., 36, 58

10.1016/j.earscirev.2012.04.001

10.1144/0016-76492006-022

10.1016/j.gr.2014.01.008

10.1029/2002TC001484

10.1144/0016-764903-165

10.2475/ajs.304.4.370

10.1016/j.jseaes.2007.10.008

10.2475/03.2009.02

10.1144/SP338.3

10.1016/j.gr.2010.01.007

10.2475/10.2010.12

10.1016/j.gr.2012.01.012

Xie L, 2014, Geol. Bull. China, 33, 691

10.1016/j.gr.2012.05.015

10.1016/j.earscirev.2013.08.005

10.1016/j.jseaes.2004.01.006

10.1016/j.gr.2011.07.029

10.1016/j.lithos.2012.01.026

10.1016/j.gr.2013.11.006

10.1146/annurev.earth.28.1.211

Yin A, 1996, The Tectonic Evolution of Asia, 442

10.1016/j.gr.2009.05.011

Yuan W, Yang Z. 2015a. The Alashan terrane did not amalgamate with North China block by the Late Permian: evidence from Carboniferous and Permian paleomagnetic results.J. Asian Earth Sci.In press

10.1016/j.gr.2013.12.009

Yue Y, 2001, Geol. Soc. Am. Mem., 194, 101

10.1016/j.lithos.2006.09.012

10.1016/j.tecto.2013.11.035

10.1007/s00531-008-0368-2

10.1016/j.gr.2006.08.001

10.1016/j.gr.2013.05.011

10.1016/j.gr.2012.10.001

10.1016/j.tecto.2010.12.009

10.1029/GD021

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Annual Review of Earth and Planetary Sciences

Tập 43 Số 1

477-507

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