留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

青藏高原东缘龙门山前陆逆冲带复合结构与生长

颜丹平 孙铭 巩凌霄 周美夫 邱亮 李书兵 张森 古术航 木红旭

颜丹平, 孙铭, 巩凌霄, 等, 2020. 青藏高原东缘龙门山前陆逆冲带复合结构与生长. 地质力学学报, 26 (5): 615-633. DOI: 10.12090/j.issn.1006-6616.2020.26.05.054
引用本文: 颜丹平, 孙铭, 巩凌霄, 等, 2020. 青藏高原东缘龙门山前陆逆冲带复合结构与生长. 地质力学学报, 26 (5): 615-633. DOI: 10.12090/j.issn.1006-6616.2020.26.05.054
YAN Danping, SUN Ming, GONG Lingxiao, et al., 2020. Composite structure and growth of the Longmenshan foreland thrust belt in the eastern margin of the Qinghai-Tibet Plateau. Journal of Geomechanics, 26 (5): 615-633. DOI: 10.12090/j.issn.1006-6616.2020.26.05.054
Citation: YAN Danping, SUN Ming, GONG Lingxiao, et al., 2020. Composite structure and growth of the Longmenshan foreland thrust belt in the eastern margin of the Qinghai-Tibet Plateau. Journal of Geomechanics, 26 (5): 615-633. DOI: 10.12090/j.issn.1006-6616.2020.26.05.054

青藏高原东缘龙门山前陆逆冲带复合结构与生长

doi: 10.12090/j.issn.1006-6616.2020.26.05.054
基金项目: 

国家自然基金项目 41672216

国家自然基金项目 41972206

详细信息
    作者简介:

    颜丹平(1964-), 男, 教授, 从事构造地质学教学与研究工作。E-mail:yandp@cugb.edu.cn

  • 中图分类号: P542

Composite structure and growth of the Longmenshan foreland thrust belt in the eastern margin of the Qinghai-Tibet Plateau

  • 摘要: 位于青藏高原东缘的北东向龙门山逆冲带,研究已经证明是中生代与新生代前陆复合扩展和生长的结果。然而,2008年5·12汶川地震地表破裂、余震和滑坡等的单向和分段迁移现象,对龙门山复合逆冲带的结构认识提出了挑战。文章在已有研究成果基础上,针对龙门山复合生长下构建的特殊结构进行了野外调查和构造解析。结果表明,以中生代与新生代两期前陆逆冲带复合生长为基础,龙门山复合逆冲带具有特殊的、主要由前陆逆冲楔叠加后形成的复合结构,而且这种复合逆冲楔具有分级和时序特征;中生代前陆逆冲楔是以逆冲断层-褶皱为特征,并分别组合形成碧口厚皮逆冲推覆体、唐王寨薄皮逆冲推覆体和龙王庙逆冲推覆体,总体从晚三叠世以前开始,至~160 Ma向南递进扩展生长;新生代前陆逆冲楔由逆冲断层和逆冲岩片组成,分为约35~10 Ma和10 Ma以来两个阶段,向南东向递进扩展生长,并可能与川西盆地东侧龙泉山构造相连通。因此,龙门山逆冲带具有前陆逆冲带和生长过程的双重复合结构。

     

  • 图  1  青藏高原东部与扬子板块西部区域构造图(Yan et al., 2018b;底图据四川省区域地质志,1991和黄崇轲,2001修改)

    Figure  1.  Geological map of the eastern Qinghai-Tibet Plateau and the western Yangtze block (Yan et al., 2018b; Base map is modified after SBGMR, 1991; Huang, 2001)

    图  2  龙门山复合逆冲带逆冲推覆构造图及ABC构造剖面图(据Yan et al., 2018a修改)

    Figure  2.  Regional tectonic map of the Longmenshan Tectonic Complex and the ABC geological section (modified after Yan et al., 2018a)

    图  3  龙门山复合逆冲构造带及邻近各主要构造单元区域地层层序与接触关系(据Yan et al, 2018b四川省地质矿产局,1991修改)

    Figure  3.  Stratigraphic correlation diagram of the Longmenshan Tectonic Complex and its adjacent main structural units (modified after Yan et al, 2018b; SBGMR, 1991)

    图  4  碧口(a—d)、唐王寨(e—f)和龙王庙(g—h)逆冲推覆体构造样式照片与组构测量(照片位置见图 2;数据据Yan et al., 2018a)

    a—碧口群D1期不对称褶皱指示向南逆冲,褶皱并被D2期长英质岩脉切割;b—文县北侧三叠系中的断展褶皱指示向南的逆冲;c—WX-073花岗质糜棱岩及其S-C组构,沿组构生长的白云母单矿物用于40Ar/39Ar测年;d—推覆体下盘震旦系中发育的糜棱岩及其S-C组构,沿组构生长的白云母单矿物用于40Ar/39Ar测年(WX-103);e—泥盆系中脆韧性剪切带与S-C组构,指示向SW的逆冲构造;f—泥盆系中发育的小型断坪-断坡构造;g—泥盆系中发育的不对称至倒转背斜和沿倒转翼发育的三角带构造,指示可能转化为运动学向南的逆冲断层;h—龙王庙逆冲推覆体综合的小断层与擦痕线理等,总体指示向SSE—SW的逆冲构造

    Figure  4.  Photographs and structural fabrics of Bikou (a-d), Tangwangzhai (e-f) and Longwangmiao (g-h) thrust complex with locations in Fig. 2 (Data are from Yan et al., 2018a)

    图  5  D3期逆冲推覆样式与运动学(野外照片位置见图 2)

    a—歇马坪-清平断层和断层相关褶皱,以及断层在擦痕线理等指示向SE逆冲作用和右行走滑作用;b—断坡及断层岩组成;c—穿过龙门山复合逆冲带主要构造带的深地震反射剖面及构造解释(Feng et al., 2016, 位置见图 2剖面DE)

    Figure  5.  Structural style and kinematics of the D3 thrust (Photograph of locations are shown in Fig. 2)

    图  6  龙门山复合逆冲带形成时间

    a—WX-073白云母40Ar/39Ar测年结果;b—WX-103白云母40Ar/39Ar测年结果;c—据Yan et al., 2018a修改的各逆冲推覆体起始与结束时间关系图

    Figure  6.  Formation time of the Longmenshan Tectonic Complex

    图  7  龙门山复合生长逆冲带结构模式图

    Figure  7.  Tectonic model sketch of the Longmenshan Tectonic Complex

    表  1  40Ar/39Ar测年结果

    Table  1.   40Ar/39Ar dating results

      WX-073, 白云母, 38 mg, J=0.001969, 样品位置: 32°44′33″N, 105°20′29″E
    T/℃ (40Ar/39Ar)m (36Ar/39Ar)m (37Ar/39Ar)m (40Arr/39Ark)m 39Ar/×10-8ccSTP 39Ar/% 40Arr/40Art/% age/Ma ±aσ/Ma
    750 938.129 3.016 0.428 46.847 0.027 5.53 6.23 159.17 48.39
    850 267.953 0.591 0.089 93.355 0.091 18.51 35.69 304.41 5.30
    930 164.684 0.197 0.237 106.447 0.134 27.46 65.09 343.27 4.77
    980 144.210 0.119 0.301 109.207 0.081 16.50 76.03 351.36 7.34
    1020 143.939 0.104 0.380 113.165 0.073 14.97 78.88 362.89 5.65
    1060 213.086 0.330 1.181 115.860 0.028 5.83 54.92 370.71 13.52
    1100 378.614 0.858 3.250 125.493 0.011 2.28 33.93 398.36 49.91
    1140 481.734 1.047 2.782 173.061 0.008 1.65 36.68 529.00 52.84
    1180 602.156 1.683 3.540 105.500 0.005 1.10 18.55 340.49 151.07
    1220 684.689 1.865 2.932 134.222 0.005 1.00 20.61 423.05 79.06
    1280 753.303 1.889 5.283 196.163 0.006 1.29 26.90 589.18 115.34
    1340 322.537 0.915 5.533 52.803 0.008 1.72 17.39 178.44 69.01
    1400 230.617 0.636 4.505 43.227 0.011 2.16 19.74 147.36 30.31
      平均年龄=352 Ma, 等时线年龄=351±35 Ma
      WX-103, 白云母, 25.3 mg, J=0.001971, 样品位置: 32°17′53″N, 104°45′37″E
    750 56.294 0.098 0.046 27.463 0.175 3.56 49.45 95.10 1.78
    850 52.987 0.036 0.014 42.227 1.038 21.06 79.96 144.23 1.97
    930 53.396 0.006 0.007 51.487 1.344 27.29 96.47 174.37 2.36
    980 66.911 0.010 0.005 64.013 0.701 14.24 95.72 214.35 2.87
    1020 75.533 0.009 0.030 72.882 0.500 10.14 96.53 242.14 3.25
    1060 83.981 0.013 0.047 80.165 0.376 7.64 95.51 264.65 5.48
    1100 92.926 0.025 0.043 85.531 0.233 4.73 92.14 281.05 3.77
    1140 92.985 0.027 0.121 84.933 0.188 3.81 91.44 279.23 3.77
    1180 95.088 0.025 0.091 87.856 0.188 3.81 92.49 288.11 3.86
    1220 109.327 0.037 0.008 98.284 0.112 2.27 90.03 319.44 4.38
    1280 173.009 0.123 0.497 136.648 0.038 0.78 79.23 430.24 6.89
    1340 297.001 0.373 1.759 187.173 0.014 0.29 63.42 566.49 22.97
    1400 232.044 0.355 0.898 127.279 0.018 0.37 55.40 403.80 16.20
      总气体年龄=205.3 Ma, 反等时线年龄=223±27 Ma (steps 5~10)
    注:表中下标m=测量值,t=整体值,r=释放值
    下载: 导出CSV
  • AIRAGHI L, WARREN C J, DE SIGOYER J, et al., 2018. Influence of dissolution/reprecipitation reactions on metamorphic greenschist to amphibolite facies mica 40Ar/39Ar ages in the Longmen Shan (eastern Tibet)[J]. Journal of Metamorphic Geology, 36(7):933-958. doi: 10.1111/jmg.12420
    ARNE D, WORLEY B, WILSON C, et al., 1997. Differential exhumation in response to episodic thrusting along the eastern margin of the Tibetan Plateau[J]. Tectonophysics, 280(3-4):239-256. doi: 10.1016/S0040-1951(97)00040-1
    BAI D H, UNSWORTH M J, MEJU M A, et al., 2010. Crustal deformation of the eastern Tibetan plateau revealed by magnetotelluric imaging[J]. Nature Geoscience, 3(5):358-362. doi: 10.1038/ngeo830
    BILLEROT A, DUCHENE S, VANDERHAEGHE O, et al., 2017. Gneiss domes of the Danba metamorphic complex, Songpan Ganze, eastern Tibet[J]. Journal of Asian Earth Sciences, 140:48-74. doi: 10.1016/j.jseaes.2017.03.006
    BRUGUIER O, LANCELOT J R, MALAVIEILLE J, 1997. U-Pb dating on single detrital zircon grains from the Triassic Songpan-Ganze flysch (Central China):provenance and tectonic correlations[J]. Earth and Planetary Science Letters, 152(1-4):217-231. doi: 10.1016/S0012-821X(97)00138-6
    BURCHFIEL B C, CHEN Z L, LIU Y P, et al., 1995. Tectonics of the Longmen Shan and adjacent regions, central China[J]. International Geology Review, 37(8):661-735. doi: 10.1080/00206819509465424
    BURCHFIEL B C, MOLNAR P, ZHAO Z Y, et al., 1989. Geology of the Ulugh Muztagh area, northern Tibet[J]. Earth and Planetary Science Letters, 94(1-2):57-70. doi: 10.1016/0012-821X(89)90083-6
    BURCHFIEL B C, ROYDEN L H, VAN DER HILST R D, et al., 2008. A geological and geophysical context for the Wenchuan earthquake of 12 May 2008, Sichuan, People's Republic of China[J]. GSA Today, 18(7):4-11. doi: 10.1130/GSATG18A.1
    CAO W T, YAN D P, QIU L, et al., 2015. Structural style and metamorphic conditions of the Jinshajiang metamorphic belt:Nature of the Paleo-Jinshajiang orogenic belt in the eastern Tibetan Plateau[J]. Journal of Asian Earth Sciences, 113:748-765. doi: 10.1016/j.jseaes.2015.09.003
    CASTONGUAY S, RUFFET G, TREMBLAY A, 2007. Dating polyphase deformation across low-grade metamorphic belts:An example based on 40Ar/39Ar muscovite age constraints from the southern Quebec Appalachians, Canada[J]. GSA Bulletin, 119(7-8):978-992. doi: 10.1130/B26046.1
    CHANG E Z, 2000. Geology and tectonics of the Songpan-Ganzi fold belt, Southwestern China[J]. International Geology Review, 42(9):813-831. doi: 10.1080/00206810009465113
    CHEN S F, WILSON C J L, 1996. Emplacement of the Longmen Shan Thrust-Nappe belt along the eastern margin of the Tibetan Plateau[J]. Journal of Structural Geology, 18(4):413-430. http://www.sciencedirect.com/science/article/pii/019181419500096V
    CHEN S F, WILSON C J L, WORLEY B A, 1995. Tectonic transition from the Songpan-Ganzê fold belt to the Sichuan basin, south-western China[J]. Basin Research, 7(3):235-253. doi: 10.1111/j.1365-2117.1995.tb00108.x
    CLARK M K, ROYDEN L H, 2000. Topographic ooze:building the eastern margin of Tibet by lower crustal flow[J]. Geology, 28(8):703-706. doi: 10.1130/0091-7613(2000)28<703:TOBTEM>2.0.CO;2
    DE SIGOYER J, VANDERHAEGHE O, DUCHêNE S, et al., 2014. Generation and emplacement of Triassic granitoids within the Songpan Ganze accretionary-orogenic wedge in a context of slab retreat accommodated by tear faulting, Eastern Tibetan plateau, China[J]. Journal of Asian Earth Sciences, 88:192-216. doi: 10.1016/j.jseaes.2014.01.010
    DEWEY J F, SHACKLETON R M, CHANG C F, et al., 1988. The tectonic evolution of the Tibetan Plateau[J]. Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 327(1594):379-413. doi: 10.1098/rsta.1988.0135
    DIRKS P H G M, WILSON C J L, CHEN S, et al., 1994. Tectonic evolution of the NE margin of the Tibetan Plateau; evidence from the central Longmen mountains, Sichuan province, China[J]. Journal of Southeast Asian Earth Sciences, 9(1-2):181-192. doi: 10.1016/0743-9547(94)90074-4
    ENKELMANN E, WEISLOGEL A, RATSCHBACHER L, et al., 2007. How was the Triassic Songpan-Ganzi basin filled? A provenance study[J]. Tectonics, 26(4):TC4007.
    FENG S Y, ZHANG P Z, LIU B J, et al., 2016. Deep crustal deformation of the Longmen Shan, eastern margin of the Tibetan Plateau, from seismic reflection and Finite Element modeling[J]. Journal of Geophysical Research:Solid Earth, 121(2):767-787. doi: 10.1002/2015JB012352
    HARROWFIELD M J, WILSON C J L, 2005. Indosinian deformation of the Songpan Garzê fold belt, northeast Tibetan Plateau[J]. Journal of Structural Geology, 27(1):101-117. doi: 10.1016/j.jsg.2004.06.010
    HBGMR (Hubei Bureau of Geology and Mineral Resources), 1990. Regional geology of Hubei Province:Beijing. China[M]. Beijing:Geological Publishing House, 1-645. (in Chinese)
    HUANG C K, 2001. Spatial Database of 1: 2500000 Digital Geologic Map of People's Republic of China[G]. Geological Publishing House. (in Chinese)
    HUANG C K, YE T Z, CHEN K Q, et al., 2002. Geological map of the people's Republic of China (1:2500000)[M]. Xi'an:China Cartographic Publishing House. (in Chinese)
    HUANG M H, BUICK I S, HOU L W, 2003. Tectonometamorphic evolution of the Eastern Tibet plateau:evidence from the central Songpan-Ganzê orogenic belt, western China[J]. Journal of Petrology, 44(2):255-278. doi: 10.1093/petrology/44.2.255
    HUANG Y, WU J P, ZHANG T Z, et al., 2008. Relocation of the M8.0 Wenchuan earthquake and its aftershock sequence[J]. Science in China Series D:Earth Science, 51(12):1703-1711. doi: 10.1007/s11430-008-0135-z
    HUBBARD J, SHAW J H, 2009. Uplift of the Longmen Shan and Tibetan plateau, and the 2008 Wenchuan (M=7.9) earthquake[J]. Nature, 458(7235):194-197. doi: 10.1038/nature07837
    JIA D, LI Y Q, LIN A M, et al., 2010. Structural model of 2008 MW 7.9 Wenchuan earthquake in the rejuvenated Longmen Shan Thrust Belt, China[J]. Tectonophysics, 491(1-4):174-184. doi: 10.1016/j.tecto.2009.08.040
    JIA D, WEI G Q, CHEN Z X, et al., 2006. Longmen Shan fold-thrust belt and its relation to the western Sichuan basin in central China:New insights from hydrocarbon exploration[J]. AAPG Bulletin, 90(9):1425-1447. doi: 10.1306/03230605076
    JIN W Z, TANG L J, WAN G M, et al., 2010. Structural styles of Longmen mountain Thrust belt, SW China[J]. Journal of Earth Science, 21(1):19-31. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx-e201001003
    JOLIVET M, ROGER F, XU Z Q, et al., 2015. Mesozoic-Cenozoic evolution of the Danba dome (Songpan Garzê, East Tibet) as inferred from LA-ICPMS U-Pb and fission-track data[J]. Journal of Asian Earth Sciences, 102:180-204. doi: 10.1016/j.jseaes.2015.02.009
    KIRBY E, REINERS P W, KROL M A, et al., 2002. Late Cenozoic evolution of the eastern margin of the Tibetan Plateau:Inferences from 40Ar/39Ar and (U-Th)/He thermochronology[J]. Tectonics, 21(1):3-22.
    KIRSCHNER D L, COSCA M A, MASSON H, et al., 1996. Staircase 40Ar/39Ar spectra of fine-grained white mica:Timing and duration of deformation and empirical constraints on argon diffusion[J]. Geology, 24(8):747-750. doi: 10.1130/0091-7613(1996)024<0747:SAASOF>2.3.CO;2
    LANPHERE M A, BAADSGAARD H, 1997. The Fish Canyon tuff: A standard for geochronology[C]//American geophysical union, fall meeting 2011. AGU.
    LI J H, ZHANG Y Q, DONG S W, et al., 2013. Structural and geochronological constraints on the Mesozoic tectonic evolution of the North Dabashan zone, South Qinling, central China[J]. Journal of Asian Earth Sciences, 64:99-114. doi: 10.1016/j.jseaes.2012.12.001
    LI S Z, KUSKY T M, WANG L, et al., 2007. Collision leading to multiple-stage large-scale extrusion in the Qinling orogen:Insights from the Mianlue suture[J]. Gondwana Research, 12(1-2):121-143. doi: 10.1016/j.gr.2006.11.011
    LI W P, LIU S F, QIAN T, et al., 2014. Analysis of structural deformation in the North Dabashan thrust belt, South Qinling, central China[J]. International Geology Review, 56(10):1276-1294. doi: 10.1080/00206814.2014.935966
    LI X W, MO X X, HUANG X F, et al., 2015a. U-Pb zircon geochronology, geochemical and Sr-Nd-Hf isotopic compositions of the Early Indosinian Tongren Pluton in West Qinling:Petrogenesis and geodynamic implications[J]. Journal of Asian Earth Sciences, 97:38-50. doi: 10.1016/j.jseaes.2014.10.017
    LI Y, ALLEN A, DENSMORE A L, et al., 2003. Evolution of the Longmen Shan Foreland basin (Western Sichuan, China) during the Late Triassic Indosinian orogeny[J]. Basin Research, 15(1):117-138. doi: 10.1046/j.1365-2117.2003.00197.x
    LI Y, YANG J S, DILEK Y, et al., 2015b. Crustal architecture of the Shangdan suture zone in the early Paleozoic Qinling orogenic belt, China:Record of subduction initiation and backarc basin development[J]. Gondwana Research, 27(2):733-744. doi: 10.1016/j.gr.2014.03.006
    LIU H, YAN D P, WEI G Q, 2008. Deformation and metamorphism sequence of Bikou terrane in the northwest Margin of Yangtze plate:implications for extension collapse and transition of Songpan-Garze Orogenic belt[J]. Acta Geologica Sinica, 82(4):464-474. (in Chinese) http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE200804004.htm
    LIU S F, QIAN T, LI W P, et al., 2015. Oblique closure of the northeastern Paleo-Tethys in central China[J]. Tectonics, 34(3):413-434. doi: 10.1002/2014TC003784
    LUO Z L, 1984. A preliminary approach on C-subduction and its hydrocarbon prospecting[J]. Oil & Gas Geology, 5(4):315-324. (in Chinese with English abstract) http://www.researchgate.net/publication/288957803_A_preliminary_approach_on_C-subduction_and_its_hydrocarbon_prospecting
    LUO Z L, 1991. The dynamical model of the lithospheric evolution in Longmenshan orogenic belt[J]. Journal of Chengdu College of Geology, 18(1):1-7. (in Chinese with English abstract) http://ci.nii.ac.jp/naid/10003542881
    LV S, YAN D P, WANG Y, et al., 2010. Geochemical and geochronological constraints on the Mashan and Mupi plutons in the South Qinling orogenic belt:Implications for tectonic nature of the Bikou terrane[J]. Acta Petrologica Sinica, 26(6):1889-1991. (in Chinese with English abstract)
    MATTAUER M, MALAVIEILLE J, CALASSOU S, et al., 1992. The Songpan-Ganze Triassic belt of west Sichuan and eastern Tibet-a decollement fold belt on passive margin[J]. Comptes Rendus de I' Academie des Sciences Serie II, 314:619-626. http://www.mendeley.com/research/songpan-garze-triassic-belt-west-sechuan-eastern-tibet-decollement-fold-belt-passive-margin/
    MENG Q R, WANG E, HU J M, 2005. Mesozoic sedimentary evolution of the northwest Sichuan basin:implication for continued clockwise rotation of the South China block[J]. GSA Bulletin, 117(3-4):396-410. http://www.onacademic.com/detail/journal_1000035248171110_a399.html
    MENG Q R, ZHANG G W, 2000. Geologic framework and tectonic evolution of the Qinling orogen, central China[J]. Tectonophysics, 323(3-4):183-196. doi: 10.1016/S0040-1951(00)00106-2
    MU H X, YAN D P, QIU L, et al., 2019. Formation of the Late Triassic western Sichuan foreland basin of the Qinling Orogenic Belt, SW China:sedimentary and geochronological constraints from the Xujiahe Formation[J]. Journal of Asian Earth Sciences, 183:103938. doi: 10.1016/j.jseaes.2019.103938
    NIE S Y, YIN A, ROWLEY D B, et al., 1994. Exhumation of the Dabie Shan ultra-high-pressure rocks and accumulation of the Songpan-Ganzi flysch sequence, central China[J]. Geology, 22(11):999-1002. doi: 10.1130/0091-7613(1994)022<0999:EOTDSU>2.3.CO;2
    ONSTOTT T C, PEACOCK M W, 1987. Argon retentivity of hornblendes:A field experiment in a slowly cooled metamorphic terrane[J]. Geochimica et Cosmochimica Acta, 51(11):2891-2903. doi: 10.1016/0016-7037(87)90365-6
    PARSONS T, JI C, KIRBY E, 2008. Stress changes from the 2008 Wenchuan earthquake and increased hazard in the Sichuan basin[J]. Nature, 454(7203):509-510. doi: 10.1038/nature07177
    QIN X H, CHEN Q C, MENG W, et al., 2018. Evaluating measured in-situ stress state changes associated with earthquakes and its implications:a case study in the Longmenshan fault zone[J]. Journal of Geomechanics, 24(3):309-320. (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTotal-DZLX201803005.htm
    RAO R B, XU J F, CHEN Y M, et al., 1987. The Triassic system of the Qianghai-Xizang Plateau[M]. Beijing:Geological Publishing House. (in Chinese)
    RATSCHBACHER L, HACKER B R, CALVERT A, et al., 2003. Tectonics of the Qinling (Central China):tectonostratigraphy, geochronology, and deformation history[J]. Tectonophysics, 366(1-2):1-53. doi: 10.1016/S0040-1951(03)00053-2
    RICHARDSON N J, DENSMORE A L, SEWARD D, et al., 2008. Extraordinary denudation in the Sichuan Basin:Insights from low-temperature thermochronology adjacent to the eastern margin of the Tibetan Plateau[J]. Journal of Geophysical Research:Solid Earth, 113(B4):B04409.
    ROGER F, JOLIVET M, CATTIN R, et al., 2011. Mesozoic-Cenozoic tectonothermal evolution of the eastern part of the Tibetan Plateau (Songpan-Garzê, Longmen Shan area):insights from thermochronological data and simple thermal modelling[J]. Geological Society, London, Special Publications, 353(1):9-25. doi: 10.1144/SP353.2
    ROGER F, JOLIVET M, MALAVIEILLE J, 2008. Tectonic evolution of the Triassic fold belts of Tibet[J]. Comptes Rendus Geoscience, 340(2-3):180-189. doi: 10.1016/j.crte.2007.10.014
    ROGER F, JOLIVET M, MALAVIEILLE J, 2010. The tectonic evolution of the Songpan-Garzê (North Tibet) and adjacent areas from Proterozoic to Present:A synthesis[J]. Journal of Asian Earth Sciences, 39(4):254-269. doi: 10.1016/j.jseaes.2010.03.008
    ROGER F, MALAVIEILLE J, LELOUP H, et al., 2004. Timing of granite emplacement and cooling in the Songpan-Ganzê fold belt (eastern Tibetan Plateau) with tectonic implications[J]. Journal of Asian Earth Sciences, 22(5):465-481. doi: 10.1016/S1367-9120(03)00089-0
    ROYDEN L H, BURCHFIEL B C, KING R W, et al., 1997. Surface deformation and lower crustal flow in eastern Tibet[J]. Science, 276(5313):788-790. doi: 10.1126/science.276.5313.788
    SBGMR (Sichuan Bureau of Geology and Mineral Resources), 1991. Regional geology of Sichuan Province:Beijing, China[M]. Beijing:Geological Publishing House:680. (in Chinese)
    SUN C, JIA D, YIN H W, et al., 2016. Sandbox modeling of evolving thrust wedges with different preexisting topographic relief:Implications for the Longmen Shan Thrust Belt, eastern Tibet[J]. Journal of Geophysical Research:Solid Earth, 121(6):4591-4614. doi: 10.1002/2016JB013013
    SUN M, 2018. Typical Cenozoic tectonic association and its formation mechanism in the eastern margin of Tibetan publication[D]. Beijing: China University of Geosciences: 121. (in Chinese with English abstract)
    SUN M, YIN A, YAN D P, et al., 2018. Role of pre-existing structures in controlling the Cenozoic tectonic evolution of the eastern Tibetan plateau:New insights from analogue experiments[J]. Earth and Planetary Science Letters, 491:207-215. doi: 10.1016/j.epsl.2018.03.005
    SUN W H, ZHOU M F, GAO J F, et al., 2009. Detrital zircon U-Pb geochronological and Lu-Hf isotopic constraints on the Precambrian magmatic and crustal evolution of the western Yangtze Block, SW China[J]. Precambrian Research, 172(1-2):99-126. doi: 10.1016/j.precamres.2009.03.010
    TIAN Y T, KOHN B P, HU S B, et al., 2015. Synchronous fluvial response to surface uplift in the eastern Tibetan Plateau:implications for crustal dynamics[J]. Geophysical Research Letters, 42(1):29-35. doi: 10.1002/2014GL062383
    TIAN Y T, LI R, TANG Y, et al., 2018. Thermochronological constraints on the late Cenozoic morphotectonic evolution of the Min Shan, the eastern margin of the Tibetan Plateau[J]. Tectonics, 37(6):1733-1749. doi: 10.1029/2017TC004868
    WANG E, KIRBY E, FURLONG K P, et al., 2012. Two-phase growth of high topography in eastern Tibet during the Cenozoic[J]. Nature Geoscience, 5(9):640-645. doi: 10.1038/ngeo1538
    WANG X B, YU N, ZHU Y T, et al., 2008. Preliminary result of magnetotelluric sounding in the Longmen thrust belt of West Sichuan, China[J]. Journal of Chengdu University of Technology (Science & Technology Edition), 35(4):398-403. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cdlgxyxb200804009
    WANG X X, WANG T, ZHANG C L, 2013. Neoproterozoic, Paleozoic, and Mesozoic granitoid magmatism in the Qinling Orogen, China:Constraints on orogenic process[J]. Journal of Asian Earth Sciences, 72:129-151. doi: 10.1016/j.jseaes.2012.11.037
    WEI C J, 1994. Metamorphism and its geological significance of the Bikou Group in the Shanxi-Gansu-Sichuan border region[J]. Acta Geologica Sinica, 68(3):241-254. (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199400057171
    WEISLOGEL A L, GRAHAM S A, CHANG E Z, et al., 2006. Detrital zircon provenance of the Late Triassic Songpan-Ganzi complex:Sedimentary record of collision of the North and South China blocks[J]. Geology, 34(2):97-100. http://ci.nii.ac.jp/naid/10026141046
    WEISLOGEL A L, GRAHAM S A, CHANG E Z, et al., 2010. Detrital zircon provenance from three turbidite depocenters of the Middle-Upper Triassic Songpan-Ganzi complex, central China:Record of collisional tectonics, erosional exhumation, and sediment production[J]. GSA Bulletin, 122(11-12):2041-2062. doi: 10.1130/B26606.1
    WELLER O M, ST-ONGE M R, WATERS D J, et al., 2013. Quantifying Barrovian metamorphism in the Danba Structural Culmination of eastern Tibet[J]. Journal of Metamorphic Geology, 31(9):909-935. doi: 10.1111/jmg.12050
    WORLEY B A, WILSON C J L, 1996. Deformation partitioning and foliation reactivation during transpressional orogenesis, an example from the central Longmen Shan, China[J]. Journal of Structural Geology, 18(4):395-411. doi: 10.1016/0191-8141(95)00095-U
    XIAO L, ZHANG H F, CLEMENS J D, et al., 2007. Late Triassic Granitoids of the eastern margin of the Tibetan Plateau:geochronology, petrogenesis and implications for tectonic evolution[J]. Lithos, 96(3-4):436-452. doi: 10.1016/j.lithos.2006.11.011
    XU C G, WELLS M L, YAN D P, et al., 2020. Phase equilibria and geochronology of the Bikou blueschist:Insight into the Mesozoic evolution of the northwestern margin of the Yangtze Block[J]. Journal of Asia Earth Sciences, under revision. http://www.sciencedirect.com/science/article/pii/S1367912020303060
    XU J F, ZHANG B R, HAN Y W, 2008a. Geochemistry of the Mian-Lue ophiolites in the Qinling Mountains, central China:constraints on the evolution of the Qinling orogenic belt and collision of the North and South China Cratons[J]. Journal of Asian Earth Sciences, 32(5-6):336-347. doi: 10.1016/j.jseaes.2007.11.004
    XU Z Q, HOU L W, WANG C Q, et al., 1992. Orogenic processes of the Songpan Ganze orogenic belt of China[M]. Beijing:Geological Publishing House, 137. (in Chinese with English abstract)
    XU Z Q, JI S C, LI H B, et al., 2008b. Uplift of the Longmen Shan range and the Wenchuan earthquake[J]. Episodes, 31(3):291-301. doi: 10.18814/epiiugs/2008/v31i3/002
    YAN D P, LI S B, CAO W T, et al., 2010. Multi-layer detachment crustal structure in the Longmen Mountains:Evidences from neo-tectonic deformation and geophysical data[J]. Earth Science Frontiers, 17(5):106-116. (in Chinese with English abstract) http://www.ingentaconnect.com/content/el/18725791/2010/00000017/00000005/art00010
    YAN D P, QIU L, WELLS M L, et al., 2018a. Structural and geochronological constraints on the early Mesozoic north Longmen Shan Thrust Belt:Foreland fold-thrust propagation of the SW Qinling orogenic belt, northeastern Tibetan plateau[J]. Tectonics, 37(12):4595-4624. doi: 10.1029/2018TC004986
    YAN D P, ZHANG B, ZHOU M F, et al., 2009. Constraints on the depth, geometry and kinematics of blind detachment faults provided by fault-propagation folds:an example from the Mesozoic fold belt of South China[J]. Journal of Structural Geology, 31(2):150-162. doi: 10.1016/j.jsg.2008.11.005
    YAN D P, ZHOU M F, LI S B, et al., 2011. Structural and geochronological constraints on the Mesozoic-Cenozoic tectonic evolution of the Longmen Shan Thrust Belt, eastern Tibetan Plateau[J]. Tectonics, 30(6):TC6005. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=f54d673cb445673442129868bcf533de
    YAN D P, ZHOU M F, SONG H L, et al., 2003a. Structural Style and tectonic significance of the Jianglang dome in the Eastern Margin of the Tibetan Plateau, China[J]. Journal of Structural Geology, 25(5):765-779. doi: 10.1016/S0191-8141(02)00059-7
    YAN D P, ZHOU M F, SONG H L, et al., 2003b. Origin and tectonic significance of a Mesozoic multi-layer over-thrust system within the Yangtze Block (South China)[J]. Tectonophysics, 361(3-4):239-254. doi: 10.1016/S0040-1951(02)00646-7
    YAN D P, ZHOU M F, WEI G Q, et al., 2008a. The Pengguan tectonic dome of Longmen Mountains, Sichuan Province:Mesozoic denudation of a Neoproterozoic magmatic arc-basin system[J]. Science in China Series D:Earth Sciences, 51(11):1545-1559. doi: 10.1007/s11430-008-0126-0
    YAN D P, ZHOU M F, WEI G Q, et al., 2008b. Collapse of Songpan-Ganzê Orogenic belt resulted from Mesozoic middle-crustal ductile channel flow:evidences from deformation and metamorphism within Sinian-Paleozoic strata in hinterland of Longmenshan foreland thrust belt[J]. Earth Science Frontiers, 15(3):186-198. doi: 10.1016/S1872-5791(08)60066-4
    YAN D P, ZHOU Y, QIU L, et al., 2018b. The Longmenshan tectonic complex and adjacent tectonic units in the eastern margin of the Tibetan Plateau:A review[J]. Journal of Asian Earth Sciences, 164:33-57. doi: 10.1016/j.jseaes.2018.06.017
    YIN A, HARRISON T M, 2000. Geologic evolution of the Himalayan-Tibetan orogen[J]. Annual Review of Earth and Planetary Sciences, 28:211-280. doi: 10.1146/annurev.earth.28.1.211
    YIN A, NIE S Y, 1993. An indentation model for the North and South China collision and the development of the Tan-lu and Honam fault systems, eastern Asia[J]. Tectonics, 12(4):801-813. doi: 10.1029/93TC00313
    YUAN C, ZHOU M F, SUN M, et al., 2010. Triassic granitoids in the eastern Songpan Ganzi Fold Belt, SW China:Magmatic response to geodynamics of the deep lithosphere[J]. Earth and Planetary Science Letters, 290(3-4):481-492. doi: 10.1016/j.epsl.2010.01.005
    ZHANG G W, DONG Y P, LAI S C, et al., 2004. Mianlue tectonic zone and Mianliie suture zone on southern margin of Qinling-Dabie orogenic belt[J]. Science in China Series D-Earth Science-English Edition, 47(4):300-316. doi: 10.1360/02YD0526
    ZHANG H F, PARRISH R, ZHANG L, et al., 2007. A-type granite and adakitic magmatism association in Songpan-Garze fold belt, eastern Tibetan Plateau:Implication for lithospheric delamination[J]. Lithos, 97(3-4):323-335. doi: 10.1016/j.lithos.2007.01.002
    ZHANG H F, ZHANG L, HARRIS N, et al., 2006. U-Pb zircon ages, geochemical and isotopic compositions of granitoids in Songpan-Garze fold belt, eastern Tibetan Plateau:constraints on petrogenesis and tectonic evolution of the basement[J]. Contributions to Mineralogy and Petrology, 152(1):75-88. doi: 10.1007/s00410-006-0095-2
    ZHANG K J, LI B, WEI Q G, et al., 2008. Proximal provenance of the western Songpan-Ganzi turbidite complex (Late Triassic, eastern Tibetan plateau):Implications for the tectonic amalgamation of China[J]. Sedimentary Geology, 208(1-2):36-44. doi: 10.1016/j.sedgeo.2008.04.008
    ZHENG Y, LI H B, SUN Z M, et al., 2016. New geochronology constraints on timing and depth of the ancient earthquakes along the Longmen Shan fault belt, eastern Tibet[J]. Tectonics, 35(12):2781-2806. doi: 10.1002/2016TC004210
    ZHOU D, GRAHAM S A, 1996. The Songpan-Ganzi complex of the western Qinling Shan as a Triassic remnant ocean basin[M]//YIN A, HARRISON T M. The tectonic evolution of Asia. Cambridge: Cambridge University Press: 281-299.
    ZHOU M F, YAN D P, KENNEDY A K, et al., 2002. SHRIMP U-Pb zircon geochronological and geochemical evidence for Neoproterozoic arc-magmatism along the western margin of the Yangtze Block, South China[J]. Earth and Planetary Science Letters, 196(1-2):51-67. doi: 10.1016/S0012-821X(01)00595-7
    ZHOU M F, YAN D P, VASCONCELOS P M, et al., 2008. Structural and geochronological constraints on the tectono-thermal evolution of the Danba domal terrane, eastern margin of the Tibetan plateau[J]. Journal of Asian Earth Sciences, 33(5-6):414-427. doi: 10.1016/j.jseaes.2008.03.003
    ZHOU M F, YAN D P, WANG C L, et al., 2006. Subduction-related origin of the 750 Ma Xuelongbao adakitic complex (Sichuan Province, China):Implications for the tectonic setting of the giant Neoproterozoic magmatic event in South China[J]. Earth and Planetary Science Letters, 248(1-2):286-300. doi: 10.1016/j.epsl.2006.05.032
    富云莲, 罗修泉, 张思红等, 1988. 40Ar/39Ar定年法的实验技术与一些地质样品年龄的测定[J].中国地质科学院地质研究所文集, 1: 85-107.
    国家汶川地震专家委员会, 2008.汶川地震灾区地震地质灾害图集[M].北京:地图出版社:105.
    湖北省地质矿产局, 1990.湖北省区域地质志[M].北京:地质出版社:1-645.
    黄崇轲, 2001.中华人民共和国1: 250万数字地质图空间数据库[G].地质出版社.
    金文正, 汤良杰, 杨克明, 等, 2007.川西龙门山褶皱冲断带分带性变形特征[J].地质学报, 08:1072-1080. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb200708007
    刘鹤, 颜丹平, 魏国庆, 2008.扬子板块西北缘碧口地块变形变质作用序列:松潘-甘孜造山带伸展垮塌事件的意义[J].地质学报, 82(4):464-474.
    罗志立, 1984.试论中国型(C-型)冲断带及其油气勘探问题[J].石油与天然气地质, 5(4):315-324. http://www.cnki.com.cn/Article/CJFDTotal-SYYT198404001.htm
    罗志立, 1991.龙门山造山带岩石圈演化的动力学[J].成都地质学院学报, 18(1):1-7. http://www.cqvip.com/QK/91405X/19911/455388.html
    吕崧, 颜丹平, 王焰, 等, 2010.碧口地块麻山、木皮岩体岩石地球化学与地质年代学:对构造属性的指示意义[J].岩石学报, 26(6):1889-1991. http://d.wanfangdata.com.cn/Periodical/ysxb98201006021
    秦向辉, 陈群策, 孟文, 等, 2018.大地震前后实测地应力状态变化及其意义:以龙门山断裂带为例[J].地质力学学报, 24(3):309-320. https://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20180303&journal_id=dzlxxb
    四川省地质矿产局, 1991.四川省区域地质志[M].北京:地质出版社:680.
    孙铭, 2018.青藏高原东缘典型新生代构造组合与形成机制研究[D].北京: 中国地质大学(北京): 121.
    魏春景, 1994.陕甘川交界区碧口群的变质作用及其地质意义[J].地质学报, 68(3):241-254. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199400057171
    许志琴, 侯立伟, 王崇起, 等, 1992.中国松潘-甘孜造山带的造山过程[M].北京:地质出版社:137.
    颜丹平, 刘鹤, 魏国庆, 等, 2008.龙门山后山震旦系-古生界变形变质作用:松潘-甘孜造山带中生代伸展垮塌下的中地壳韧性流壳层[J].地学前缘, 03:186-198.
    颜丹平, 李书兵, 曹文涛, 等, 2010.龙门山多层分层拆离地壳结构:新构造变形与深部构造证据[J].地学前缘, 17(5):106-116. http://d.wanfangdata.com.cn/Periodical/dxqy201005010
  • 加载中
图(7) / 表(1)
计量
  • 文章访问数:  392
  • HTML全文浏览量:  148
  • PDF下载量:  52
  • 被引次数: 0
出版历程
  • 收稿日期:  2020-07-20
  • 修回日期:  2020-08-24
  • 刊出日期:  2020-10-28

目录

    /

    返回文章
    返回