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    Volume 43 Issue 6
    Jun.  2018
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    Article Navigation >  Earth Science  > 2018  >  43(6): 2019-2028
    Zhu Chuanbao, Sun Feifei, Yuan Wanming, Zhang Aikui, Zhang Daming, Ma Zhongyuan, Zhou Qinglu, Wang Shengming, Zhao Mengqi, Liu Guanglian, 2018. Apatite Fission Track Thermochronology and Tectonic Significance in Yemaquan Area, East Kunlun. Earth Science, 43(6): 2019-2028. doi: 10.3799/dqkx.2018.598
    Citation: Zhu Chuanbao, Sun Feifei, Yuan Wanming, Zhang Aikui, Zhang Daming, Ma Zhongyuan, Zhou Qinglu, Wang Shengming, Zhao Mengqi, Liu Guanglian, 2018. Apatite Fission Track Thermochronology and Tectonic Significance in Yemaquan Area, East Kunlun. Earth Science, 43(6): 2019-2028. doi: 10.3799/dqkx.2018.598
    shu

    Apatite Fission Track Thermochronology and Tectonic Significance in Yemaquan Area, East Kunlun

    doi: 10.3799/dqkx.2018.598
    • 1.

      No.3 Exploration Institute of Geology and Mineral Resources of Qinghai Province, Xining 810029, China

    • 2.

      Institute of Earth Sciences, China University of Geosciences, Beijing 100083, China

    • Received Date: 2018-01-17
    • Publish Date: 2018-06-15
      Abstract
    • We present the tectonic evolution characteristics of Yemaquan area, which is located in west of the East Kunlun Mountains, according to apatite fission track thermochronology analysis.The results show that apatite fission track ages mainly are divided into three groups, including 153.8 Ma, 106.8 to 81.0 Ma, and 48.7 to 44.4 Ma, respectively.The Bangonghu-Nujiang ocean closure event happened in 153.8 Ma, then the collision and combination of Lhasa block and Qiangtang block on the East Kunlun area mainly ranged from 106.8 to 81.0 Ma, and post-orogenic stretching events after the collision between the India-Eurasia occurred during 48.7 Ma and 44.4 Ma.In addition, the analysis results also indicate that three stages of thermal history of Yemaquan area are mainly ranged from 130 to 110 Ma, 110 to 14 Ma, and 14 Ma to now, respectively.The first stage, 130-110 Ma, corresponds to collision activity between the Lhasa and the Qiangtang block after the closed up of the Bangonghu-Nujiang oceanic basin.The second stage, 110-14 Ma, rised continuously, with strike-slip movement of Alkin fault and the ductile deformation of the Xidatan fault occurred during 110-90 Ma.And the last stage, 14 Ma to now, uplifted rapidly, and affected by strong tectonic activity of Tibetan plateau since Neogene.Uplift rates and uplift ranges for these three stages are estimated of 0.021 mm/a and 0.42 km, 0.01 mm/a and 1.0 km, and 0.1 mm/a and 1.43 km, respectively, with the average uplift rate and the total uplift height of 0.028 mm/a, and 2.86 km, respectively.

       

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    • Arnaud, N., Tapponnier, P., Roger, F., et al., 2003.Evidence for Mesozoic Shear along the Western Kunlun and Altyn-Tagh Fault, Northern Tibet (China).Journal of Geophysical Research:Solid Earth, 108(B1):2053-2064.https://doi.org/10.1029/2001jb000904
      Bai, Y.S., Ren, E.F., Fan, G.L., et al., 2008.Apatite Fission Track Evidence for the Miocene Rapid Uplift of the Qimantag Mountains on the Northwestern Margin of the Qinghai-Tibet Plateau.Geologcal Bulletin of China, 27(7):1044-1048(in Chinese with English abstract).
      Brandon, M.T., 2002.Decomposition of Mixed Grain Age Distributions Using Binom Fit.On Track, 24:13-18. http://adsabs.harvard.edu/abs/2003SedG..162...39W
      Chen, H.W., Luo, Z.H., Mo, X.X., et al., 2006.SHRIMP Ages of Kayakedengtage Complex in the East Kunlun Mountains and Their Geological Implications.Acta Petrologica et Mineralogica, 25(1):25-32(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW200601002.htm
      Chen, N.S., Sun, M., Wang, Q.Y., et al., 2008.U-Pb Dating of Zircon from the Central Zone of the East Kunlun Orogen and Its Implications for Tectonic Evolution.Science China:Earth Sciences, 51(7):929-938. https://doi.org/10.1007/s11430-008-0072-x
      Chen, X.H., McRivette, M.W., Li, L., et al., 2011.Thermochronological Evidence for Multi-Phase Uplifting of the East Kunlun Mountains, Northern Tibetan Plateau.Geological Bulletin of China, 30(11):1647-1660(in Chinese with English abstract).
      Chen, X.N., Yuan, W.M., Zhang, A.K., et al., 2014.Apatite Fission Track Analysis for Revealing Tectonic Events of the Bayinguole Area in the West Section of Eastern Kunlun Mountains, Northern Qinghai-Tibet Plateau.Nuclear Techniques, 37(1):54-61(in Chinese with English abstract).
      Deng, J.F., Yang, J.J., Zhao, H.L., et al., 1996.Igneous Petrotectonic Assemblages and Geotectonic Evolution along Golmud Ejinaqi Geosciences Section.Geoscience, 10(3):330-343(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XDDZ603.005.htm
      Galbraith, R.F., 1981.On Statistical Models for Fission Track Counts:Reply.Journal of the International Association for Mathematical Geology, 13(6):485-488.https://doi.org/10.1007/bf01034500 doi: 10.1007/BF01034500
      Gao, Y.B., Li, W.Y., Qian, B., et al., 2014.Geochronology, Geochemistry and Hf Isotopic Compositions of the Granitic Rocks Related with Iron Mineralization in Yemaquan Deposit, East Kunlun, NW China.Acta Petrologica Sinica, 30(6):1647-1665(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201406009.htm
      Gleadow, A.J.W., Duddy, I.R., Green, P.F., et al., 1986.Confined Fission Track Lengths in Apatite:A Diagnostic Tool for Thermal History Analysis.Contributions to Mineralogy and Petrology, 94(4):405-415.https://doi.org/10.1007/bf00376334 doi: 10.1007/BF00376334
      Gleadow, A.J.W., Kohn, B.P., Brown, R.W., et al., 2002.Fission Track Thermotectonic Imaging of the Australian Continent.Tectonophysics, 349(1-4):5-21.https://doi.org/10.1016/s0040-1951(02)00043-4 doi: 10.1016/S0040-1951(02)00043-4
      Green, P.F., 1981.A New Look at Statistics in Fission-Track Dating.Nuclear Tracks, 5(1-2):77-86.https://doi.org/10.1016/0191-278x(81)90029-9 doi: 10.1016/0191-278X(81)90029-9
      Green, P.F., 1986.On the Thermo-Tectonic Evolution of Northern England:Evidence from Fission Track Analysis.Geological Magazine, 123(5):493-506.https://doi.org/10.1017/s0016756800035081 doi: 10.1017/S0016756800035081
      Guo, L., Xiao, P.X., Gao, X.F., et al., 2010.Chronology and Geochemistry of Acid Intrusions in Chulutaohai Iron Ore, Eastern Kunlun.Northwestern Geology, 43(4):159-167(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XBDI201004025.htm
      Guo, Z.F., Deng, J.F., Xu, Z.Q., et al., 1998.Late Palaeozoic-Mesozoic Intracontinental Orogenic Process and Intermedate-Acidic Igneous Rocks from the Eastern Kunlun Mountains of Northwestern China.Geoscience, 12(3):344-352 (in Chinese with English abstract).
      Hay, W.W., Shaw, C.A., Wold, C.N., 1989.Mass-Balanced Paleogeographic Reconstructions.Geologische Rundschau, 78(1):207-242.https://doi.org/10.1007/bf01988362 doi: 10.1007/BF01988362
      Hurford, A.J., Green, P.F., 1982.A Users' Guide to Fission Track Dating Calibration.Earth and Planetary Science Letters, 59(2):343-354.https://doi.org/10.1016/0012-821x(82)90136-4 doi: 10.1016/0012-821X(82)90136-4
      Ketcham, R.A., Donelick, R.A., Carlson, W.D., 1999.Variability of Apatite Fission-Track Annealing Kinetics; Ⅲ, Extrapolation to Geological Time Scales.American Mineralogist, 84(9):1235-1255. https://doi.org/10.2138/am-1999-0903
      Kohn, B.P., 2005.Visualizing Thermotectonic and Denudation Histories Using Apatite Fission Track Thermochronology.Reviews in Mineralogy and Geochemistry, 58(1):527-565. https://doi.org/10.2138/rmg.2005.58.20
      Kohn, B.P., Gleadow, A.J.W., Brown, R.W., et al., 2002.Shaping the Australian Crust over the Last 300 Million Years:Insights from Fission Track Thermotectonic and Denudation Studies of Key Terranes.Australian Journal of Earth Sciences, 49(4):697-717. https://doi.org/10.1046/j.1440-0952.2002.00942.x
      Li, H.B., Yang, J.S., Xu, Z.Q., et al., 2006.The Constraint of the Altyn Tagh Fault System to the Growth and Rise of the Northern Tibetan Plateau.Earth Science Frontiers, 13(4):59-79 (in Chinese with English abstract).
      Liu, Y.H., Mo, X.X, Yu, X.H., et al., 2006.Zircon SHRIMP U-Pb Dating of the Jingren Granite, Yemaquan Region of the East Kunlun and Its Geological Significance.Acta Petrologica Sinica, 22(10):2457-2463(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB200610005.htm
      Luo, Z.H., Deng, J.F., Cao, Y.Q., et al., 1999.On Late Paleozoic-Early Mesozoic Volcanism and Regional Tectonic Evolution of Eastern Kunlun, Qinghai Province.Geoscience, 13(1):51-56 (in Chinese with English abstract). http://kuscholarworks.ku.edu/handle/1808/17114?show=full
      Métivier, F., Gaudemer, Y., 1997.Mass Transfer between Eastern Tien Shan and Adjacent Basins (Central Asia):Constraints on Regional Tectonics and Topography.Geophysical Journal International, 128(1):1-17.https://doi.org/10.1111/j.1365-246x.1997.tb04068.x doi: 10.1111/gji.1997.128.issue-1
      Mo, X.X., Pan, G.T., 2006.From the Tethys to the Formation of the Qinghai-Tibet Plateau:Constrained by Tectono-Magmatic Events.Earth Science Frontiers, 13(6):43-51(in Chinese with English abstract).
      Mo, X.X., Luo, Z.H., Deng, J.F., et al., 2007a.Granitoids and Crustal Growth in the East-Kunlun Orogenic Belt.Geological Journal of China Universities, 13(3):403-414(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GXDX200703005.htm
      Mo, X.X., Zhao, Z.D., Zhou, S., et al., 2007b.On the Timing of India-Asia Continental Collision.Geological Bulletin of China, 26(10):1240-1244(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD200710004.htm
      Mock, C., Arnaud, N.O., Cantagrel, J.M., 1999.An Early Unroofing in Northeastern Tibet? Constraints from 40Ar/39Ar Thermochronology on Granitoids from the Eastern Kunlun Range (Qianghai, NW China).Earth and Planetary Science Letters, 171(1):107-122.https://doi.org/10.1016/s0012-821x(99)00133-8 doi: 10.1016/S0012-821X(99)00133-8
      Pichon, X.L., Henry, P., Goffé, B., 1997.Uplift of Tibet:From Eclogites to Granulites-Implications for the Andean Plateau and the Variscan Belt.Tectonophysics, 273(1-2):57-76.https://doi.org/10.1016/s0040-1951(96)00288-0 doi: 10.1016/S0040-1951(96)00288-0
      Vincent, S.J., Allen, M.B., 1999.Evolution of the Minle and Chaoshui Basins, China:Implications for Mesozoic Strike-Slip Basin Formation in Central Asia.Geological Society of America Bulletin, 111(5):725-742.https://doi.org/10.1130/0016-7606(1999)111<0725:eotmac>2.3.co; 2 doi: 10.1130/0016-7606(1999)111<0725:EOTMAC>2.3.CO;2
      Wang, A., Wang, G.C., Xie, D.F., et al., 2006.Fission Track Geochronology of Xiaonanchuan Pluton and the Morphotectonic Evolution of Eastern Kunlun since Late Miocene.Journal of Earth Science, 17(4):302-309.https://doi.org/10.1016/s1002-0705(07)60003-x http://www.sciencedirect.com/science/article/pii/S100207050760003X
      Wang, G.C., Xiang, S.Y., Wang, A., et al., 2007.Thermochronological Constraint to the Processes of the East Kunlun and Adjacent Areas in Mesozoic-Early Cenozoic.Earth Science, 32(5):605-614, 680(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200705005.htm
      Wang, P.J., Mattern, F., Schneider, W., et al., 2003.The Cretaceous of the Eastern Bangong-Nujiang Suture Zone(Tibet):Tectono-Sedimentation.Global Geology, 22(2):105-110, 118(in Chinese with English abstract).
      Xu, D.Z., Zhu, C.B., Meng, X.G., et al., 2016.Fault Activity Characteristics in the Northern Margin of the Tibetan Plateau before the Menyuan Ms6.4 Earthquake.Geodesy and Geodynamics, 7(4):261-267. https://doi.org/10.1016/j.geog.2016.07.001
      Yuan, W.M., Dong, J.Q., Wang, S.C., et al., 2005.Apatite Fission Track Analysis for Revealing Tectonic Evolution of the South-Block in Eastern Kunlun Mountains, Northern Qinghai-Tibet Plateau.Nuclear Techniques, 28(9):707-711(in Chinese with English abstract).
      Yuan, W.M., Dong, J.Q., Wang, S.C., et al., 2006.Apatite Fission Track Evidence for Neogene Uplift in the Eastern Kunlun Mountains, Northern Qinghai-Tibet Plateau, China.Journal of Asian Earth Sciences, 27(6):847-856. https://doi.org/10.1016/j.jseaes.2005.09.002
      Yuan, W.M., Mo.X.X., Yu, X.H., et al., 2000a.The Record of Indosinian Tectonic Setting from the Granotoid of Eastern Kunlun Mountains.Geological Review, 46(2):203-211(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP200002012.htm
      Yuan, W.M., Wang, S.C., Wang, L.F., 2000b.Application of Fission Track Thermochronology to Hongshuihe Gold Mineralization Ages.Atomic Energy Science and Technology, 34(Suppl.):57-60(in Chinese with English abstract).
      Yuan, W.M., Mo, X.X., Zhang, A.K., et al., 2013.Fission Track Thermochronology Evidence for Multiple Periods of Mineralization in the Wulonggou Gold Deposits, Eastern Kunlun Mountains, Qinghai Province.Journal of Earth Science, 24(4):471-478. https://doi.org/10.1007/s12583-013-0362-x
      Yuan, W.M., Zhang, X.T., Dong, J.Q., et al., 2003.A New Vision of the Intracontinental Evolution of the Eastern Kunlun Mountains, Northern Qinghai-Tibet Plateau, China.Radiation Measurements, 36(1-6):357-362.https://doi.org/10.1016/s1350-4487(03)00151-3 doi: 10.1016/S1350-4487(03)00151-3
      Yuan, W.M., Zhang, X.T., Dong, J.Q., et al., 2004.Apatite Fission Track Evidence on the Uplifting of Eastern Kunlun Mountains.Atomic Energy Science and Technology, 38(2):166-168(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YZJS200402016.htm
      Zhang, A. K., 2012. Studies on Late Paleozoic-Early Mesozoic Magmatism and Mineralization in Yemaquan Area, Qinghai Province(Dissertation). China University of Geosciences, Beijing(in Chinese with English abstract).
      Zhang, K.X., Wang, G.C., Cao, K., et al., 2008.The Main Uplift Events of Tibet Plateau during Cenozoic:The Response of Sedimentation and the Record of Thermochronology.Science in China (Series D), 38(12):1575-1588(in Chinese).
      Zhang, W., Zhou, H.W., Zhu, Y.H., et al., 2016.The Evolution of Triassic Granites Associated with Mineralization within East Kunlun Orogenic Belt:Evidence from the Petrology, Geochemistry and Zircon U-Pb Geochronology of the Mohexiala Pluton.Earth Science, 41(8):1334-1348(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2016.520 doi: 10.1007/s12583-017-0808-7
      Zhang, X. T., 2006. Study on the Tectonic Framework of Qinghai(Dissertation). China University of Geosciences, Beijing(in Chinese with English abstract).
      Zhang, Y.F., 1994.Preliminary Approach on Geologic Structure Evolution in Qinghai Province and Its Adjacent Area.Earthquake Research in Plateau, 6(3):10-16(in Chinese with English abstract). http://www.irgrid.ac.cn/handle/1471x/626838
      Zhao, F.F., Sun, F.Y., Liu, J.L., 2017.Zircon U-Pb Geochronology and Geochemistry of the Gneissic Granodiorite in Manite Area from East Kunlun, with Implications for Geodynamic Setting.Earth Science, 42(6):927-940, 1044 (in Chinese with English abstract).https://doi.org/10.3799/dqkx.2017.073
      Zhong, D.L., Ding, L., 1996.Study on the Process and Mode of Uplift in Tibet Plateau.Science in China (Series D), 26(4):289-295(in Chinese).
      Zhu, Y.H., Lin, Q.X., Jia, C.X., et al., 2006.SHRIMP Zircon U-Pb Age and Significance of Early Paleozoic Volcanic Rocks in East Kunlun Orogenic Belt, Qinghai Province, China.Science in China (Series D), 49(1):88-96. https://doi.org/10.1007/s11430-004-5317-8
      拜永山, 任二峰, 范桂兰, 等, 2008.青藏高原西北缘祁漫塔格山中新世快速抬升的磷灰石裂变径迹证据.地质通报, 27(7):1044-1048. http://www.cqvip.com/qk/95894A/200807/27776364.html
      谌宏伟, 罗照华, 莫宣学, 等, 2006.东昆仑喀雅克登塔格杂岩体的SHRIMP年龄及其地质意义.岩石矿物学杂志, 25(1):25-32. http://www.cqvip.com/QK/94932X/2006001/21189467.html
      陈小宁, 袁万明, 张爱奎, 等, 2014.东昆仑西段巴音郭勒地区构造事件的磷灰石裂变径迹分析.核技术, 37(1):54-61. http://www.cnki.com.cn/Article/CJFDTotal-YZJS201402033.htm
      陈宣华, McRivette, M.W., 李丽, 等, 2011.东昆仑造山带多期隆升历史的地质热年代学证据.地质通报, 30(11):1647-1660. doi: 10.3969/j.issn.1671-2552.2011.11.001
      邓晋福, 杨建军, 赵海玲, 1996.格尔木-额济纳旗断面走廊域火成岩-构造组合与大地构造演化.现代地质, 10(3):330-343. http://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ603.005.htm
      高永宝, 李文渊, 钱兵, 等, 2014.东昆仑野马泉铁矿相关花岗质岩体年代学、地球化学及Hf同位素特征.岩石学报, 30(6):1647-1665. http://industry.wanfangdata.com.cn/yj/Detail/Periodical?id=Periodical_ysxb98201406009
      过磊, 校培喜, 高晓峰, 等, 2010.东昆仑楚鲁套海酸性侵入体年代学及地球化学特征.西北地质, 43(4):159-167. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xbdz201004019
      郭正府, 邓晋福, 许志琴, 等, 1998.青藏东昆仑晚古生代末-中生代中酸性火成岩与陆内造山过程.现代地质, 12(3):344-352. http://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ803.006.htm
      李海兵, 杨经绥, 许志琴, 等, 2006.阿尔金断裂带对青藏高原北部生长、隆升的制约.地学前缘, 13(4):59-79. https://www.wenkuxiazai.com/doc/90b126506f1aff00bfd51e2b-2.html
      刘云华, 莫宣学, 喻学惠, 等, 2006.东昆仑野马泉地区景忍花岗岩锆石SHRIMP U-Pb定年及其地质意义.岩石学报, 22(10):2457-2463. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=2006010264&journal_id=ysxb
      罗照华, 邓晋福, 曹永清, 等, 1999.青海省东昆仑地区晚古生代-早中生代火山活动与区域构造演化.现代地质, 13(1):51-56. http://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ901.007.htm
      莫宣学, 潘桂棠, 2006.从特提斯到青藏高原形成:构造-岩浆事件的约束.地学前缘, 13(6):43-51. http://industry.wanfangdata.com.cn/dl/Detail/Periodical?id=Periodical_dxqy200606007
      莫宣学, 罗照华, 邓晋福, 等, 2007a.东昆仑造山带花岗岩及地壳生长.高校地质学报, 13(3):403-414. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200703005.htm
      莫宣学, 赵志丹, 周肃, 等, 2007b.印度-亚洲大陆碰撞的时限.地质通报, 26(10):1240-1244. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200710004.htm
      王国灿, 向树元, 王岸, 等, 2007.东昆仑及相邻地区中生代-新生代早期构造过程的热年代学记录.地球科学, 32(5):605-614, 680. http://www.earth-science.net/WebPage/Article.aspx?id=3520
      王璞珺, Mattern, F., Schneider, W., 等, 2003.西藏班公湖-怒江缝合带白垩系沉积特征及其构造意义.世界地质, 22(2):105-110, 118. http://d.old.wanfangdata.com.cn/Periodical/sjdz200302001
      袁万明, 董金泉, 王世成, 等, 2005.东昆仑南部带磷灰石裂变径迹分析的地质意义.核技术, 28(9):707-711. https://www.wenkuxiazai.com/doc/af5cfe446c85ec3a87c2c5b2-3.html
      袁万明, 莫宣学, 喻学惠, 等, 2000a.东昆仑印支期区域构造背景的花岗岩记录.地质论评, 46(2):203-211. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlp200002012
      袁万明, 王世成, 王兰芬, 2000b.裂变径迹法在洪水河金矿化时代研究中的应用.原子能科学技术, 34(增刊):57-60. doi: 10.3969/j.issn.1000-6931.2000.z1.016
      袁万明, 张雪亭, 董金泉, 等, 2004.东昆仑隆升作用的裂变径迹研究.原子能科学技术, 38(2):166-168. http://www.cnki.com.cn/Article/CJFDTOTAL-YZJS200402016.htm
      张爱奎, 2012. 青海省野马泉地区晚古生代-早中生代岩浆作用与成矿研究(博士学位论文). 北京: 中国地质大学.
      张克信, 王国灿, 曹凯, 等, 2008.青藏高原新生代主要隆升事件:沉积响应与热年代学记录.中国科学(D辑), 38(12):1575-1588. doi: 10.3321/j.issn:1006-9267.2008.12.011
      张炜, 周汉文, 朱云海, 等, 2016.东昆仑与成矿有关的三叠纪花岗岩演化:基于莫河下拉岩体岩石学、地球化学和锆石U-Pb年代学的证据.地球科学, 41(8):1334-1348.https://doi.org/10.3799/dqkx.2016.520 http://www.earth-science.net/WebPage/Article.aspx?id=3341
      张雪亭, 2006. 青海省大地构造格架研究(博士学位论文). 北京: 中国地质大学.
      张以茀, 1994.青海及邻近地区地质构造演化初探.高原地震, 6(3):10-16. http://www.cnki.com.cn/Article/CJFDTOTAL-GYDZ403.001.htm
      赵菲菲, 孙丰月, 刘金龙, 2017.东昆仑马尼特地区片麻状花岗闪长岩锆石U-Pb年代学、地球化学及其构造背景.地球科学, 42(6):927-940, 1044.https://doi.org/10.3799/dqkx.2017.073 http://www.earth-science.net/WebPage/Article.aspx?id=3588
      钟大赉, 丁林, 1996.青藏高原的隆起过程及其机制探讨.中国科学(D辑), 26(4):289-295. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK199604000.htm
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