Tectonic Evolution of the Changning-Menglian Proto-Paleo Tethys Ocean in the Sanjiang Area, Southwestern China
-
摘要: 昌宁-孟连特提斯洋的构造演化及其原特提斯与古特提斯的转换方式一直是青藏高原及邻区基础地质研究中最热门的科学问题之一.根据新的地质调查资料、研究成果并结合分析数据，系统总结了三江造山系不同构造单元地质特征，讨论了昌宁-孟连特提斯洋早古生代-晚古生代的构造演化历史.通过对不同构造单元时空结构的剖析和对相关岩浆、沉积及变质作用记录的分析，认为昌宁-孟连结合带内共存原特提斯与古特提斯洋壳残余，临沧-勐海一带发育一条早古生代岩浆弧带，前人所划基底岩系"澜沧岩群"应为昌宁-孟连特提斯洋东向俯冲消减形成的早古生代构造增生杂岩，滇西地区榴辉岩带很可能代表了俯冲增生杂岩带发生了深俯冲，由于弧-陆碰撞而迅速折返就位，这一系列新资料及新认识表明昌宁-孟连结合带所代表的特提斯洋在早古生代至晚古生代很可能是一个连续演化的大洋.在此基础上，结合区域地质资料，构建了三江造山系特提斯洋演化的时空格架及演化历史，认为其经历了早古生代原特提斯大洋扩张、早古生代中晚期-晚古生代特提斯俯冲消减与岛弧带形成、晚二叠世末-早三叠世主碰撞汇聚、晚三叠世晚碰撞造山与盆山转换等阶段.Abstract: The tectonic evolution of the Changning-Menglian Tethys, as well as the transformation from Proto-Tethys to Paleo-Tethys, is one of hottest research topics concerning the geology of Qinghai-Tibetan Plateau and adjacent regions. Based on the recent geological findings and our new data, we summarized the geological features of the tectonic units from the Sanjiang orogenic system. Then we investigated the evolution history of the Changning-Menglian Tethys during the Early Paleozoic to Late Paleozoic. In view of the spatio-temporal structure of the different tectonic units, and the associated magmatism, sedimentary and metamorphic records. It is suggested in this study that (1) both crustal remnants of Proto-and Paleo-Tethys retain in the Changning-Menglian suture zone, (2) a magmatic arc belt developed from Lincang to Menghai in the Early Paleozoic, (3) the 'Lancang rock Group' was not the basement rock series, but Early Paleozoic tectonic-accretionary complexes formed by the eastward subduction of the Changning-Menglian Tethys Ocean, (4) the eclogite belt in western Yunnan might be the production of rapid exhumation after the deep subduction process of the accretionary complex during the arc-continent collision process. All new lines of evidence suggest that the Changning-Menglian Tethys probably was a continuous ocean from Early Paleozoic to Late Paleozoic. Combined the new findings with the regional geological data, the preliminary temporal-spatial framework and evolution process of the Sanjiang Tethys orogenic system are established, which mainly includes the following four stages:(1) Longmucuo-Shuanghu-Changning-Menglian proto-Tethys seafloor spreading in the Early Paleozoic, (2) the Tethys subduction and formation of the island arc belt from middle-late Early Paleozoic to Late Paleozoic, (3) the convergence and main collision processes from the end of Late Permian to Early Triassic, and (4) the late-collision orogeny and basin-mountain transition in the Late Triassic.
-
图 1 青藏高原构造格架简图(a)及西南三江地区大地构造单元划分(b)
据Wang et al.(2014a)修改.KL.阿尼玛卿-昆仑结合带；GL.甘孜-理塘结合带；JS.金沙江结合带；AL.哀牢山结合带；NL.北澜沧江结合带；SL.南澜沧江结合带；LS.龙木错-双湖结合带；CM.昌宁-孟连结合带；BN.班公湖-怒江结合带；YL.印度-雅鲁藏布江结合带
Fig. 1. Tectonic framework of the Tibetan Plateau (a) and tectonic unit division of the Sanjiang Orogen and surrounding areas (b)
图 2 三江南段昌宁-孟连弧盆系构造单元及前侏罗纪岩浆作用时空分布
数据引用同表 1
Fig. 2. Simplified geological map of the Changning-Menglian orogenic system, showing the temporal-spatial distribution of pre-Jurassic magmatic rocks
图 3 昌宁-孟连结合带铜厂街(a)、南汀河(b)、牛井山(c)和曼信(d)蛇绿混杂岩地质简图
图a据陈莉等(2015)；图b据云南省地质调查院(2017，中华人民共和国1:5万香竹林、勐勇、勐撒、懂过、耿马县、安雅、勐库7幅区域地质调查报告)；图c据王冬兵等(2016)；图d据云南省地质矿产局(1984，中华人民共和国1:20万孟连幅区域地质调查报告)
Fig. 3. Simple geological maps of the Tongchangjie (a), Nantinghe (b), Niujingshan (c) and Manxin (d) ophiolites in the Changning-Menglian suture zone
图 4 昌宁-孟连结合带蛇绿混杂岩基性岩构造环境图解
南汀河数据来自Wang et al.(2013a)；铜厂街数据来自陈莉等(2015)；干龙塘数据来自赖绍聪等(2010)
Fig. 4. Tectonic environments diagram of mafic rocks in the Changning-Menglian ophiolite mélange
图 5 昌宁-孟连蛇绿混杂岩基性岩REE配分及微量元素蛛网图
数据来源同图 4
Fig. 5. Chondrite-normalized REE pattern and primitive mantle normalized trace element spider diagram of mafic rocks in the Changning-Menglian ophiolite mélange
图 6 三江南段早古生代岩浆岩构造环境判别图解
大中河数据来自毛晓长等(2012)；惠民数据来自Nie et al.(2015)；大平掌数据来自Hehmann et al.(2013)；双江数据来自云南省地质调查院，2017.中华人民共和国1:5万香竹林、勐勇、勐撒、懂过、耿马县、安雅、勐库7幅区域地质调查报告
Fig. 6. Tectonic environments diagram of Early Paleozoic magmatic rocks in the southern part of Sanjiang River
图 7 昌宁-孟连蛇绿混杂岩基性岩REE配分模式(a)和微量元素蛛网图(b)
数据来源同图 6
Fig. 7. The chondrite-normalized REE pattern (a) and PM-normalized trace element spider diagram (b) of Early Paleozoic magmatic rocks of the Changning-Menglian area
图 8 西南三江昌宁-孟连弧盆系演化模式简图
据潘桂棠等(2012)修改
Fig. 8. Schematic illustrations of the characteristics and evolution of the Changning-Menglian Orogenic System in the Sanjiang River
表 1 三江南段早古生代蛇绿混杂岩及岩浆岩年龄信息统计
Table 1. Statistical of age information of Early Paleozoic ophiolite and magmatic rocks in the southern part of Sanjiang River
构造单元 地点 样品编号 岩石名称 测试方法 年龄(Ma) 误差(Ma) 来源 昌宁-孟连结合带 南汀河 11NTH-4 辉长岩 LA-ICPMS 439.0 2.4 Wang et al.(2013a, 2013b) 11NTH-6 堆晶辉长岩 LA-ICPMS 443.6 4.0 12NTH-1 堆晶辉长岩 LA-ICPMS 439.0 5.8 Wang et al.(2013b) 12NTH-5 堆晶辉长岩 LA-ICPMS 453.9 5.6 双江勐库 PM029-17-1 堆晶斜长岩 LA-ICPMS 470.8 5.3 刘桂春等(2017) 牛井山 D0017-1 英云闪长岩 LA-ICPMS 468.0 2.0 王冬兵等(2016) 老南掌 D0010-1-2 玄武岩 LA-ICPMS 449.0 8.4 孙载波等(2017) 早古生代岩浆岩 惠民 D008 玄武岩 LA-ICPMS 456.0 3.0 Nie et al.(2015) D009 安山岩 LA-ICPMS 456.0 7.0 D010 英安岩 LA-ICPMS 459.0 14.0 大平掌 辉钼矿 WR Re-Os 442.4 5.6 李文昌等(2010) 辉钼矿 WR Re-Os 428.8 6.1 DP-103 花岗闪长斑岩 LA-ICPMS 401.0 1.7 汝珊珊等(2012) Y-1 英安岩 LA-ICPMS 428.9 1.5 Lehmann et al.(2013) 大中河 DZH01-1 凝灰岩 LA-ICPMS 418.0 5.1 毛晓长等(2012) 大中河 DZH01-1 凝灰岩 LA-ICPMS 421.0 双江 GMTK-1 绿片岩 LA-ICPMS 451.7 2.1 云南省地质调查院(2017) 双江 XSBD-1-1 绿片岩 LA-ICPMS 453.5 0.9 粟义 11ML-57H 变火山岩 LA-ICPMS 462.0 6.0 Xing et al.(2017) 
下载: 导出CSV
-
[1] Chen, F.K., Li, X.H., Wang, X.L., et al., 2007.Zircon Age and Nd-Hf Isotopic Composition of the Yunnan Tethyan Belt, Southwestern China.International Journal of Earth Sciences, 96(6):1179-1194. https://doi.org/10.1007/s00531-006-0146-y [2] Chen, L., Wang, L.Q., Wang, D, B., et al., 2015.Genesis of Tongchanjie Deposit in Changning-Menglian Suture Zone, Western Yunnan.Mineral Deposits, 34(3):617-631 (in Chinese with English abstract). [3] Cong, B.L., Wu, G.Y., Zhang, Q., et al., 1993.The Tectonic Evolution of the Rock in the Ancient Tethys, Western Yunnan.Science in China(Series B), 23(11):1201-1207 (in Chinese). [4] Cong, F., Lin S.L., Li, Z.H., et al., 2009.Ziron U-Pb Age of Gneissic Granites in the Tengchong Block, Western Yunnan.Acta Geologica Sinica, 83(5):651-658 (in Chinese with English abstract). https://www.researchgate.net/publication/284650463_Ziron_U-Pb_age_of_gneissic_granites_in_the_Tengchong_block_western_Yunnan [5] Dai, T.M., Zhu, B.Q., Zhang, Y.Q., et al., 1986.Collision and Thermal History of Indian-Sandaland-Eurasine Plates as Implicated by 40Ar/39Ar Age Spectra of Granodiorites.Geochimica, 15(2):97-107 (in Chinese with English abstract). [6] Deng, J., Wang, Q.F., Li, G.J., et al., 2014.Cenozoic Tectono-Magmatic and Metallogenic Processes in the Sanjiang Region, Southwestern China.Earth-Science Reviews, 138:268-299. https://doi.org/10.1016/j.earscirev.2014.05.015 [7] Deng, J., Wang, Q.F., Li, G.J., 2016.Superimposed Orogeny and Composite Metallogenic System:Case Study from the Sangjiang Tethyan Belt, SW China.Acta Petrologica Sinica, 32(8):2225-2247 (in Chinese with English abstract). https://www.researchgate.net/publication/307588563_Superimposed_orogeny_and_composite_metallogenic_system_Case_study_from_the_Sanjiang_Tethyan_belt_SW_China [8] Dong, M.L., Dong, G.C., Mo, X.X., et al., 2012.Geochronology and Geochemistry of the Early Palaeozoic Granitoids in Baoshan Block, Western Yunnan and Their Implications.Acta Petrological Sinica, 28(5):1453-1464 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=b708cff3cfeefd137bdde4c5bd722829&encoded=0&v=paper_preview&mkt=zh-cn [9] Duan, X.D., Zhang, Z.B., Wang, W., et al., 2003.New Discovery of Devonian Conodonts in the Dalongtang Area, Gengma, Southwestern Yunnan, and Their Stratigraphic Significance.Geological Bulletin of China, 22(3):182-185 (in Chinese with English abstract). [10] Fan, W.M., Wang, Y.J., Zhang, A.M., et al., 2010.Permian Arc-Back-Arc Basin Development along the Ailaoshan Tectonic Zone:Geochemical, Isotopic and Geochronological Evidence from the Mojiang Volcanic Rocks, Southwest China.Lithos, 119(3-4):553-568. https://doi.org/10.1016/j.lithos.2010.08.010 [11] Fan, W.M., Wang, Y.J., Zhang, Y.H., et al., 2015.Paleotethyan Subduction Process Revealed from Triassic Blueschists in the Lancang Tectonic Belt of Southwest China.Tectonophysics, 662:95-108. https://doi.org/10.1016/j.tecto.2014.12.021 [12] Fan, W.M., Peng, T.P., Wang, Y.J., 2009.Triassic Magmatism in the Southern Lancangjiang Zone, Southwestern China and Its Constraints on the Tectonic Evolution of Paleo-Tethys.Earth Science Frontiers, 16(6):291-302 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200906039.htm [13] Fang, N.Q., Liu, B.P., Feng, Q.L., et al., 1994.Late Palaeozoic and Triassic Deep-Water Deposits and Tectonic Evolution of the Palaeotethys in the Changning-Menglian and Lancangjiang Belts, Southwestern Yunnan.Journal of Southeast Asian Earth Sciences, 9(4):363-374. https://doi.org/10.1016/0743-9547(94)90048-5 [14] Feng, Q.L., Ye, M., Zhang, Z.J., 1997.Early Carboniferous Radiolarians from Western Yunnan.Acta Micropalaeontologica Sinica, 14(1):79-92 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/wtgswxb200201010 [15] Gehrels, G.E., Kapp, P., DeCelles, P.G., et al., 2011.Detrital Zircon Geochronology of Pre-Tertiary Strata in the Tibetan-Himalayan Orogen.Tectonics, 30(5):TC5016. https://doi.org/10.1029/2011tc002868 [16] Hennig, D., Lehmann, B., Frei, D., et al., 2009.Early Permian Seafloor to Continental Arc Magmatism in the Eastern Paleo-Tethys:U-Pb Age and Nd-Sr Isotope Data from the Southern Lancangjiang Zone, Yunnan, China.Lithos, 113(3-4):408-422. https://doi.org/10.1016/j.lithos.2009.04.031 [17] Hu, P.Y., Li, C., Wu, Y.W., et al., 2014.Opening of the Longmu Co-Shuanghu-Lancangjiang Ocean:Constraints from Plagiogranites.Chinese Science Bulletin, 59(25):3188-3199. https://doi.org/10.1007/s11434-014-0434-z [18] Huang, J.Q., Chen, G.M., Chen, B.W., 1987.The Evolution of the Tethys Sea in China and Its Neighbourhood.Geological Publishing House, Beijing (in Chinese). [19] Huang, X.X., Xu, J.F., Chen, J.L., et al., 2012.Geochronology, Geochemistry and Petrogenesis of Two Periods of Intermediate-Acid Intrusive Rocks from Hongshan Area in Zhongdian Arc.Acta Petrologica Sinica, 28(5):1493-1506 (in Chinese with English abstract). https://www.researchgate.net/publication/295636299_Geochronology_geochemistry_and_petrogenesis_of_two_periods_of_intermediate-acid_intrusive_rocks_from_Hongshan_area_in_Zhongdian_arc [20] Ji, W.H., Chen, S.J., Zhao, Z.M., et al., 2009.Discovery of the Cambiran Volcanic Rocks in the Xainza Area Gangdese Orogenic Belt, Tibet, China and Its Significance.Geological Bulletin of China, 28(9):1350-1354 (in Chinese with English abstract). [21] Jian, P., Wang, X.F., He, L.Q., et al., 1999.U-Pb Zircon Dating of Anothosite and Plagiogranite from the Jinshajiang Ophiolite Belt.Acta Petrologica Sinica, 15(4):590-593 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB199904011.htm [22] Jian, P., Liu, D.Y., Kröner, A., et al., 2009a.Devonian to Permian Plate Tectonic Cycle of the Paleo-Tethys Orogen in Southwest China (Ⅱ):Insights from Zircon Ages of Ophiolites, Arc/Back-Arc Assemblages and Within-Plate Igneous Rocks and Generation of the Emeishan CFB Province.Lithos, 113(3-4):767-784. https://doi.org/10.1016/j.lithos.2009.04.006 [23] Jian, P., Liu, D.Y., Kröner, A., et al., 2009b.Devonian to Permian Plate Tectonic Cycle of the Paleo-Tethys Orogen in Southwest China(Ⅰ):Geochemistry of Ophiolites, Arc/Back-Arc Assemblages and Within-Plate Igneous Rocks.Lithos, 113(3-4):748-766. https://doi.org/10.1016/j.lithos.2009.04.004 [24] Jian, P., Liu, D.Y., Sun, X.M., 2008.SHRIMP Dating of the Permo-Carboniferous Jinshajiang Ophiolite, Southwestern China:Geochronological Constraints for the Evolution of Paleo-Tethys.Journal of Asian Earth Sciences, 32(5-6):371-384. https://doi.org/10.1016/j.jseaes.2007.11.006 [25] Kong, H.L., Dong, G.C., Mo, X.X., et al., 2012.Petrogenesis of Lincang Granites in Sanjiang Area of Western Yunnan Province:Constraints from Geochemistry, Zircon U-Pb Geochronology and Hf Isotope.Acta Petrologica Sinica, 28(5):1438-1452 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=2b68cf1f7825af5d5f9cc8bab685aeb1&encoded=0&v=paper_preview&mkt=zh-cn [26] Lai, S.C., Qin, J.F., Li, X.J., ,et al.2010.Geochemistry of the OIB-Type Basalt from the Wumulong-Tongchangjie Area, Changning-Menglian Suture Zone:Its Petrogenesis and Tectonic Implications.Earth Science Frontiers, 17(3):44-52 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dxqy201003004 [27] Lehmann, B., Zhao, X.F., Zhou, M.F., et al., 2013.Mid-Silurian Back-Arc Spreading at the Northeastern Margin of Gondwana:The Dapingzhang Dacite-Hosted Massive Sulfide Deposit, Lancangjiang Zone, Southwestern Yunnan, China.Gondwana Research, 24(2):648-663. https://doi.org/10.1016/j.gr.2012.12.018 [28] Li, C., Dong, Y.S., Zhai, Q.G., et al., 2008.Discovery of Eopaleozoic Ophiolite in the Qiangtang of Tibet Plateau:Evidence from SHRIMP U-Pb Dating and Its Tectonic Implications.Acta Petrologica Sinica, 24(1):31-36 (in Chinese with English abstract). [29] Li, C., Wu, Y.W., Wang, M., et al., 2010.Significant Progress on Pan-African and Early Paleozoic Orogenic Events in Qinghai-Tibet Plateau-Discovery of Pan-African Orogenic Unconformity and Cambrian System in the Gangdise Area, Tibet, China.Geological Bulletin of China, 29(12):1733-1736 (in Chinese with English abstract). [30] Li, G.J., Wang, Q.F., Yu, L., et al., 2013.Closure Time of Ailaoshan Paleo-Tethys Ocean:Constraints from the Zircon U-Pb Dating and Geochemistry of the Late Permian Granitoids.Acta Petrologica Sinica, 29(11):3883-3900 (in Chinese with English abstract). https://www.researchgate.net/publication/282302442_Closure_time_of_the_Ailaoshan_Paleo-Tethys_Ocean_Constraints_from_the_zircon_U-Pb_dating_and_geochemistry_of_the_Late_Permian_granitoids [31] Li, J., Sun, Z.B., Huang, L., et al., 2017.P-T-t Path and Geological Significance of Retrograded Eclogites from Mengku Area in Western Yunnnan Province, China.Acta Petrologica Sinica, 33(7):2285-2301 (in Chinese with English abstract). [32] Li, P.W., Gao, R., Cui, J.W., et al., 2005.Paleomagnetic Results from the Three Rivers Region, SW China:Implications for the Collisional and Accretionary History.Acta Geoscientica Sinica, 26(5):387-404 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=cdfeee13d676d50ab58dd960b294801c&encoded=0&v=paper_preview&mkt=zh-cn [33] Li, S.Z., Zhao, S.J., Li, X.Y., 2016.Proto-Tehtys Ocean in East Asia(Ⅰ):Northern and Southern Border Faults and Subduction Polarity.Acta Petrologica Sinica, 32(9):2609-2627 (in Chinese with English abstract). https://www.researchgate.net/publication/309044481_Proto-Tehtys_Ocean_in_East_Asia_I_Northern_and_southern_border_faults_and_subduction_polarity [34] Li, W.C., Pan, G.T., Hou, Z.Q., et al., 2010.The Multi-Island Arc Basin-Collisional Orogenic Metallogenic Theory and Exploration Technology of "Three Rivers" in Southwest China.Science Publication, Beijing (in Chinese). [35] Li, X.H., Li, W.X., Li, Z.X., et al., 2008.850-790 Ma Bimodal Volcanic and Intrusive Rocks in Northern Zhejiang, South China:A Major Episode of Continental Rift Magmatism during the Breakup of Rodinia.Lithos, 102(1-2):341-357. https://doi.org/10.1016/j.lithos.2007.04.007 [36] Liu, B.P., Feng, Q.L., Chonglakmani, C., et al., 2002.Framework of Paleotethyan Archipelago Ocean of Western Yunnan and Its Elongation towards North and South.Earth Science Frontiers, 9(3):161-171 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=50ae29cf9c5f546ce79f84cef0e3bb4c&encoded=0&v=paper_preview&mkt=zh-cn [37] Liu, G.C., Sun, Z.B., Zeng, W.T., et al., 2017.The Age of Wanhe Ophiolitic Mélange from Mengku Area, Shuangjiang County, Western Yunnnan Province, and Its Geological Significance.Acta Petrologica et Mineralogica, 36(2):163-174 (in Chinese with English abstract). [38] Liu, J.P., Tian, S.M., Cong, F., et al., 2017.The Shale Granites from the Southern Part of the Lancangjiang Tectonic Belt, Western Yunnan:Zircon U-Pb Age, Geochemistry and Geological Implications.Sedimentary Geology and Tethyan Geology, 37(4):29-40 (in Chinese with English abstract). [39] Mao, X.C., Wang, L.Q., Li, B., et al., 2012.Discovery of the Late Silurian Volcanic Rocks in the Dazhonghe Area Yunxian-Jinghong Volcanic Arc Belt, Western Yunnan, China and Its Geological Significance.Acta Petrologica Sinica, 28(5):1517-1528 (in Chinese with English abstract). https://www.researchgate.net/publication/271520986_Discovery_of_the_Late_Silurian_volcanic_rocks_in_the_Dazhonghe_area_Yunxian-Jinggu_volcanic_arc_belt_western_Yunnan_China_and_its_geological_significance [40] Metcalfe, I., 2013.Gondwana Dispersion and Asian Accretion:Tectonic and Palaeogeographic Evolution of Eastern Tethys.Journal of Asian Earth Sciences, 66:1-33. https://doi.org/10.1016/j.jseaes.2012.12.020 [41] Mo, X.X., Lu, F.X., Shen, S.Y., et al., 1993.Tethys Volcanism and Mineralization in the Sanjiang Area.Geology Publication, Beijing:65-77 (in Chinese). [42] Nie, X.M., Feng, Q.L., Metcalfe, I., et al., 2016.Discovery of a Late Devonian Magmatic Arc in the Southern Lancangjiang Zone, Western Yunnan:Geochemical and Zircon U-Pb Geochronological Constraints on the Evolution of Tethyan Ocean Basins in SW China.Journal of Asian Earth Sciences, 118:32-50. https://doi.org/10.1016/jj.seaes.2015.12.026 [43] Nie, X.M., Feng, Q.L., Qian, X., et al., 2015.Magmatic Record of Prototethyan Evolution in SW Yunnan, China:Geochemical, Zircon U-Pb Geochronological and Lu-Hf Isotopic Evidence from the Huimin Metavolcanic Rocks in the Southern Lancangjiang Zone.Gondwana Research, 28(2):757-768. https://doi.org/10.1016/j.gr.2014.05.011 [44] Pan, G.T., Wang, L.Q., Li, R.S., et al., 2012.Tectonic Evolution of the Qinghai-Tibet Plateau.Journal of Asian Earth Sciences, 53:3-14. https://doi.org/10.1016/j.jseaes.2011.12.018 [45] Pan, G.T., Wang, L.Q., Li, R.S., et al., 2012.Tectonic Model of Archipelagic Arc-Basin Systems:The Key to the Continental Geology.Sedimentary Geology and Tethyan Geology, 32(3):1-20 (in Chinese with English abstract). https://www.researchgate.net/publication/311570518_Tectonic_Model_of_Archipelagic_Arc-Basin_Systems_The_Key_to_the_Continental_Geology [46] Pan, G, T., Wang, L, Q., Zhang, W, P., et al., 2013.Geotectonic Maps and Instructions for the Qinghai-Tibet Plateau and Adjacent Areas(1:1 500 000).Geology Publication, Beijing (in Chinese). [47] Peng, T.P., Wang, Y.J., Fan, W.M., et al., 2006.Zircon SHRIMPDating of Early Mesozoic Felsic Volcanic Rocks from the Southern Lancangjiang Zone and Tectonic Implications.Science in China(Series D), 36(2):123-132 (in Chinese). [48] Peng, T.P., Wang, Y.J., Zhao, G.C., et al., 2008.Arc-Like Volcanic Rocks from the Southern Lancangjiang Zone, SW China:Geochronological and Geochemical Constraints on Their Petrogenesis and Tectonic Implications.Lithos, 102(1-2):358-373. https://doi.org/10.1016/j.lithos.2007.08.012 [49] Peng, T.P., Wilde, S.A., Wang, Y.J., et al., 2013.Mid-Triassic Felsic Igneous Rocks from the Southern Lancangjiang Zone, SW China:Petrogenesis and Implications for the Evolution of Paleo-Tethys.Lithos, 168-169:15-32. https://doi.org/10.1016/j.lithos.2013.01.015 [50] Peng, T.P., Zhao, G.C., Fan, W.M., et al., 2014.Zircon Geochronology and Hf Isotopes of Mesozoic Intrusive Rocks from the Yidun Terrane, Eastern Tibetan Plateau:Petrogenesis and Their Bearings with Cu Mineralization.Journal of Asian Earth Sciences, 80:18-33. https://doi.org/10.1016/j.jseaes.2013.10.028 [51] Peng, T.P., Zhao, G.C., Fan, W.M., et al., 2015.Late Triassic Granitic Magmatism in the Eastern Qiangtang, Eastern Tibetan Plateau:Geochronology, Petrogenesis and Implications for the Tectonic Evolution of the Paleo-Tethys.Gondwana Research, 27(4):1494-1508. https://doi.org/10.1016/j.gr.2014.01.009 [52] Peng, X.J., Luo, W.L., 1982.Discovery of the Blue-Schist Belt in the Southern Section of Lancang River in Western Yunnan and Its Tectonic Significance.Regional Geology of China, 70(2):69-75 (in Chinese). [53] Ren, F., Pan, G.T., Yin, F.G., 2017.Oceanic Plate Stratigraphy and Tectonic Evolution of the Nujiang-Lancangjiang-Jinshajiang Area in Southwest China.Sedimentary Geology and Tethyan Geology, 37(4):9-16 (in Chinese with English abstract). [54] Ren, J.B., Xu, J.F., Chen, J.L., 2011.Zircon Geochronology and Geological Implications of Ore-Bearing Porphyries from Zhongdian Arc.Acta Petrologica Sinica, 27(9):2591-2599 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=471b48976d0988a33b4fbe3896b53da1&encoded=0&v=paper_preview&mkt=zh-cn [55] Ru, S.S, Li, F., Wu, J., et al., 2012.Geochemistry and Chronology of Granodiorite Porphyry in the Dapingzhang Cu Polymetallic Deposit.Acta Petrologica et Mineralogica, 31(4):531-540 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=f032bb5bebbd3c40bead4e2149f99be1&encoded=0&v=paper_preview&mkt=zh-cn [56] Shen, S.Y., Feng, Q.L., Wei, Q.R., et al., 2008.New Evidence for the Original Tethysan Island-Arc Volcanic Rocks in the Southern Segment of South Lancangjiang Belt.Journal of Mineralogy and Petrology, 28(4):59-63 (in Chinese with English abstract). [57] Sun, X.M., Nie, Z.T., Liang, D.Y., 1995.Determination of Sedimentary Environments and Tectonic Significance of Silicolites in Jinsha River Belt, NW Yunnan.Geological Review, 41(2):174-178 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP199502009.htm [58] Sun, Z.B.Li, J., Zhou, K., et al., 2017.Geochemical Characteristics and Geological Significance of Retrograde Eclogite in Mengku Area, Shuangjiang County, Western Yunnan Province, China.Geoscience, 31(4):746-756 (in Chinese with English abstract). [59] Wang, B.D., Wang, L.Q., Chen, J.L., et al., 2014a.Triassic Three-Stage Collision in the Paleo-Tethys:Constraints from Magmatism in the Jiangda-Deqen-Weixi Continental Margin Arc, SW China.Gondwana Research, 26(2):475-491. https://doi.org/10.1016/j.gr.2013.07.023 [60] Wang, X.S., Hu, R.Z., Bi, X.W., et al., 2014b.Petrogenesis of Late Cretaceous I-Type Granites in the Southern Yidun Terrane:New Constraints on the Late Mesozoic Tectonic Evolution of the Eastern Tibetan Plateau.Lithos, 208-209:202-219. https://doi.org/10.13039/501100005231 [61] Wang, B.D., Wang, L.Q., Chen, J.L., et al., 2017.Petrogenesis of Late Devonian-Early Carboniferous Volcanic Rocks in Northern Tibet:New Constraints on the Paleozoic Tectonic Evolution of the Tethyan Ocean.Gondwana Research, 41:142-156. https://doi.org/10.1016/j.gr.2015.09.007 [62] Wang, B.D., Wang, L.Q., Chung, S.L., et al., 2016.Evolution of the Bangong-Nujiang Tethyan Ocean:Insights from the Geochronology and Geochemistry of Mafic Rocks within Ophiolites.Lithos, 245:18-33. https://doi.org/10.1016/j.lithos.2015.07.016 [63] Wang, B.D., Wang, L.Q., Pan, G.T., et al., 2013a.U-Pb Zircon Dating of Early Paleozoic Gabbro from the Nantinghe Ophiolite in the Changning-Menglian Suture Zone and Its Geological Implication.Chinese Science Bulletin, 58(8):920-930. https://doi.org/10.1007/s11434-012-5481-8 [64] Wang, B.D., Wang, L.Q., Yin, F.G., et al., 2013b.Longmu Co-Shuanghu-Changning-Menglian Suture Zone:Residual of Uniform Early Paleozoic Tethys Ocean.Acta Geologica Sinica(English Edition), 87(z1):72-75. http://www.geojournals.cn/dzxben/ch/reader/create_pdf.aspx?file_no=dzxben2003z10040&year_id=2013&quarter_id=Z1&falg=1 [65] Wang, D.B., Luo, L., Tang, Y., et al., 2016.Zircon U-Pb Dating and Petrogenesis of Early Paleozoic Adakites from the Niujingshan Ophiolitic Mélange in the Changning-Menglian Suture Zone and Its Geological Implications.Acta Petrologica Sinica, 32(8):2317-2329 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201608006 [66] Wang, D.B., Luo, L., Tang, Y., et al., 2017.LA-ICP-MS Zircon U-Pb Age and Geochemical Signatures of the Amphibolites in the Changning-Menglian Suture Zone and Its Geological Implications.Sedimentary Geology and Tethyan Geology, 37(4):17-28 (in Chinese with English abstract). [67] Wang, D.B., Wang, L.Q., Yin, F.G., et al., 2012.Timing and Nature of the Jinshajiang Paleo-Tethys:Constraints from Zircon U-Pb Age and Hf Isotope of the Dongzhulin Layered Gabbro from Jinshajiang Ophiolite Belt, Northwestern Yunnan.Acta Petrologica Sinica, 28(5):1542-1550 (in Chinese with English abstract). http://www.oalib.com/paper/1475588 [68] Wang, F., Liu, F, L., Ji, L., et al., 2017.LA-ICP-MS U-Pb Dating of Detrital Zircon from Low-Grade Metamorphic Rocks of the Lancang Group in the Lancangjiang Complex and Its Tectonic Implications.Acta Petrologica Sinica, 33(9):2975-2985 (in Chinese with English abstract). [69] Wang, F., Liu, F.L., Liu, P.H., et al., 2014.Petrogenesis of Lincang Granites in the South of Lancangjiang Area:Constrain from Geochemistry and Zircon U-Pb Geochronology.Acta Petrologica Sinica, 30(10):3034-3050 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=1a4480bb2cf28b050e5975438afae466&encoded=0&v=paper_preview&mkt=zh-cn [70] Wang, L.Q., Pan, G.T., Ding, J., et al., 2013.Geotectonic Maps and Instructions for the Qinghai-Tibet Plateau and Adjacent Areas (1:1 500 000).Geological Publishing House, Beijing (in Chinese). [71] Wang, L.Q., Pan, G.T., Li, C., et al., 2008.SHRIMP U-Pb Zircon Dating of Eopaleozoic Cumulate in Guoganjianian Mt.from Central Qiangtang Area of Northern Tibet-Considering the Evolvement of Proto-and Paleo-Tethys.Geological Bulletin of China, 27(12):2045-2056 (in Chinese with English abstract). https://www.researchgate.net/publication/279556293_SHRIMP_U-Pb_zircon_dating_of_Eopaleozoic_cumulate_in_Guoganjianian_Mt_from_central_Qiangtang_area_of_northern_Tibet-Considering_the_evolvement_of_Proto-and_Paleo-Tethys [72] Wang, Y.Z., 2005.Remarks on the Upper Paleozoic Strata in the Menglian-Manxin Area of the Southern Part of the Changing-Menglian Belt, Western Yunnan.Geological Review, 51(1):1-10 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/OA000001895 [73] Wu, H.R., Li, H.S., 1989.The Carboniferous and Permian Radiolarian in the Menglian Area, Western Yunnan.Acta Micropalaeontologica Sinica, 6(4):337-343, 437 (in Chinese with English abstract). [74] Xing, X.W., Wang, Y.J., Cawood, P.A., et al., 2017.Early Paleozoic Accretionary Orogenesis along Northern Margin of Gondwana Constrained by High-Mg Metaigneous Rocks, SW Yunnan.International Journal of Earth Sciences, 106(5):1469-1486. https://doi.org/10.1007/s00531-015-1282-z [75] Yan, G.C., Wang, B.D., Liu, H., et al., 2018.Delineation of Middle Carboniferous Arc Volcanic Rocks in Jomda Area, Eastern Tibet and Its Tectonic Implications.Earth Science, 43(8):2715-2726 (in Chinese with English abstract). [76] Yang, J.W.1982.Discussion onOphiolite in Tongchangjie of Yunxian Area.Yunnan Geology, 1(1):59-71 (in Chinese with English abstract). [77] Yin, F.G., Wang, D.B., Wang, B.D., et al., 2017.Stratigraphic Classification in the Nujiang-Lancangjiang-Jinshajiang Orogenic Zone in Southwest China.Sedimentary Geology and Tethyan Geology, 37(4):1-8 (in Chinese with English abstract). [78] Yu, S.Y., Li, K.Q., Shi, Y.P., et al., 2003.A Study on the Granodiorite in the Middle Part of Lincang Granite Batholith.Yunnan Geology, 22(4):426-442 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=8f7bb3241af6dded30a3a6f328186cba&encoded=0&v=paper_preview&mkt=zh-cn [79] Yunnan Geological and Mineral Bureau, 1990.The Regional Geology of Yunnan Province.Geological Publishing House, Beijing (in Chinese). [80] Zhai, M.G., Cong, B.L., Zhang, R.Y., 1990.The Identification and Geological Significance of Two Types of Volcanic Rocks in Lancang Group in Yunnan Province.Science in China (Series B), (1):77-85 (in Chinese). [81] Zhai, Q.G., Jahn, B.M., Wang, J., et al., 2013.The Carboniferous Ophiolite in the Middle of the Qiangtang Terrane, Northern Tibet:SHRIMP U-Pb Dating, Geochemical and Sr-Nd-Hf Isotopic Characteristics.Lithos, 168-169:186-199. https://doi.org/10.1016/j.lithos.2013.02.005 [82] Zhai, Q.G., Jahn, B.M., Zhang, R.Y., et al., 2011.Triassic Subduction of the Paleo-Tethys in Northern Tibet, China:Evidence from the Geochemical and Isotopic Characteristics of Eclogites and Blueschists of the Qiangtang Block.Journal of Asian Earth Sciences, 42(6):1356-1370. https://doi.org/10.1016/j.jseaes.2011.07.023 [83] Zhai, Q.G., Wang, J., Li, C., et al., 2010.SHRIMP U-Pb Dating and Hf Isotopic Analyses of Middle Ordovician Meta-Cumulate Gabbro in Central Qiangtang, Northern Tibetan Plateau.Science in China(Series D), 40(5):565-573 (in Chinese). doi: 10.1007%2Fs11430-010-0063-6 [84] Zhang, K.J., Cai, J.X., Zhang, Y.X., et al., 2006.Eclogites from Central Qiangtang, Northern Tibet(China) and Tectonic Implications.Earth and Planetary Science Letters, 245(3-4):722-729. https://doi.org/10.1016/j.epsl.2006.02.025 [85] Zhang, Q., Li, D.Z., Zhang, K.W., 1985.Preliminary Study on Tongchangjie Ophiolitic Melange from Yun County, Yunnan Province.Acta Petrologica Sinica, 1(3):1-14 (in Chinese with English abstract). [86] Zhou, W.Q., Lin, W.X., 1982.The Features of the Glaucophane Schist in the Southern Part of the Lancang Jiang Metamorphic Belt.Geological Bulletin of China, (2):76-85 (in Chinese with English abstract). [87] Zhu, D.C., Zhao, Z.D., Niu, Y.L., et al., 2012.Cambrian Bimodal Volcanism in the Lhasa Terrane, Southern Tibet:Record of an Early Paleozoic Andean-Type Magmatic Arc in the Australian Proto-Tethyan Margin.Chemical Geology, 328:290-308. https://doi.org/10.1016/j.chemgeo.2011.12.024 [88] Zhu, T.X., Zhang, Q.Y., Dong, H., 2006.Discovery of the Late Devonian and Late Permian Radiolarian Cherts in Tectonic Mélanges in the Cêdo Caka Area, Shuanghu, Northern Tibet, China.Geological Bulletin of China, 25(12):1413-1418 (in Chinese with English abstract). https://www.researchgate.net/publication/279626220_Discovery_of_the_Late_Devonian_and_Late_Permi-an_radioiarian_cherts_in_tectonic_melanges_in_the_Cedo_Caka_area_Shuanghu_northern_Tibet [89] Zi, J.W., Cawood, P.A., Fan, W.M., et al., 2012.Contrasting Rift and Subduction-Related Plagiogranites in the Jinshajiang Ophiolitic Mélange, Southwest China, and Implications for the Paleo-Tethys.Tectonics, 31(2):TC2012. https://doi.org/10.1029/2011tc002937 [90] 陈莉, 王立全, 王保弟, 等, 2015.滇西昌宁-孟连缝合带铜厂街矿床成因探讨.矿床地质, 34(3):617-631. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=KCDZ201503013&dbname=CJFD&dbcode=CJFQ [91] 从柏林, 吴根耀, 张旗, 等, 1993.中国滇西古特提斯构造带岩石大地构造演化.中国科学(B辑), 23(11):1201-1207. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=JBXK199311012&dbname=CJFD&dbcode=CJFQ [92] 丛峰, 林仕良, 李再会, 等, 2009.滇西腾冲地块片麻状花岗岩的锆石U-Pb年龄.地质学报, 83(5):651-658. doi: 10.3321/j.issn:0001-5717.2009.05.006 [93] 戴橦谟, 朱炳泉, 张玉泉, 等, 1986.从花岗闪长岩的40Ar/39Ar年龄谱分析探讨印度-欧亚板块碰撞与热动力作用历史.地球化学, 15(2):97-107. doi: 10.3321/j.issn:0379-1726.1986.02.001 [94] 邓军, 王庆飞, 李龚健, 2016.复合造山和复合成矿系统:三江特提斯例析.岩石学报, 32(8):2225-2247. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=YSXB201608001&dbname=CJFD&dbcode=CJFQ [95] 董美玲, 董国臣, 莫宣学, 等, 2012.滇西保山地块早古生代花岗岩类的年代学、地球化学及意义.岩石学报, 28(5):1453-1464. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=YSXB201205011&dbname=CJFD&dbcode=CJFQ [96] 段向东, 张志斌, 王伟, 等, 2003.滇西南耿马地区泥盆纪牙形石的发现.地质通报, 22(3):182-185. doi: 10.3969/j.issn.1671-2552.2003.03.006 [97] 范蔚茗, 彭头平, 王岳军, 2009.滇西古特提斯俯冲-碰撞过程的岩浆作用记录地学前缘, 16(6):291-302. doi: 10.3321/j.issn:1005-2321.2009.06.031 [98] 冯庆来, 叶玫, 章正军, 1997.滇西早石炭世放射虫化石.微体古生物学报, 14(1):79-92. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=WSGT701.008&dbname=CJFD&dbcode=CJFQ [99] 黄汲清, 陈国铭, 陈炳蔚, 1987.中国及邻区特提斯海的演化.北京:地质出版社. [100] 黄肖潇, 许继峰, 陈建林, 等, 2012.中甸岛弧红山地区两期中酸性侵入岩的年代学、地球化学特征及其成因.岩石学报, 28(5):1493-1506. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=YSXB201205014&dbname=CJFD&dbcode=CJFQ [101] 计文化, 陈守建, 赵振明, 等, 2009.西藏冈底斯构造带申扎一带寒武系火山岩的发现及其地质意义.地质通报, 28(9):1350-1354. doi: 10.3969/j.issn.1671-2552.2009.09.026 [102] 简平, 汪啸风, 何龙清, 等, 1999.金沙江蛇绿岩中斜长岩和斜长花岗岩的U-Pb年龄及地质意义.岩石学报, 15(4):590-593. doi: 10.3321/j.issn:1000-0569.1999.04.012 [103] 孔会磊, 董国臣, 莫宣学, 等, 2012.滇西三江地区临沧花岗岩的岩石成因:地球化学、锆石U-Pb年代学及Hf同位素约束.岩石学报, 28(5):1438-1452. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=YSXB201205010&dbname=CJFD&dbcode=CJFQ [104] 赖绍聪, 秦江锋, 李学军, 等, 2010.昌宁-孟连缝合带乌木龙-铜厂街洋岛型火山岩地球化学特征及其大地构造意义.地学前缘, 17(3):44-52. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=DXQY201003006&dbname=CJFD&dbcode=CJFQ [105] 李才, 董永胜, 翟庆国, 等, 2008.青藏高原羌塘早古生代蛇绿岩——堆晶辉长岩的锆石SHRIMP定年及其意义.岩石学报, 24(1):31-36. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=YSXB200801003&dbname=CJFD&dbcode=CJFQ [106] 李才, 吴彦旺, 王明, 等, 2010.青藏高原泛非-早古生代造山事件研究重大进展——冈底斯地区寒武系和泛非造山不整合的发现.地质通报, 29(12):1733-1736. doi: 10.3969/j.issn.1671-2552.2010.12.001 [107] 李龚健, 王庆飞, 禹丽, 等, 2013.哀牢山古特提斯洋缝合时限:晚二叠世花岗岩类锆石U-Pb年代学与地球化学制约.岩石学报, 29(11):3883-3900. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=YSXB201311020&dbname=CJFD&dbcode=CJFQ [108] 李静, 孙载波, 黄亮, 等, 2017.滇西勐库退变质榴辉岩的P-T-t轨迹及地质意义.岩石学报, 33(7):2285-2301. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=YSXB201707022&dbname=CJFD&dbcode=CJFQ [109] 李朋武, 高锐, 崔军文, 等, 2005.西藏和云南三江地区特提斯洋盆演化历史的古地磁分析.地球学报, 26(5):387-404. doi: 10.3321/j.issn:1006-3021.2005.05.001 [110] 李三忠, 赵淑娟, 李玺瑶, 等, 2016.东亚原特提斯洋(Ⅰ):南北边界和俯冲极性.岩石学报, 32(9):2609-2627. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=YSXB201609002&dbname=CJFD&dbcode=CJFQ [111] 李文昌, 潘桂棠, 侯增谦, 等, 2010.西南"三江"多岛弧盆-碰撞造山成矿理论与勘查技术.北京:地质出版社. [112] 刘本培, 冯庆来, Chonglakmani C., 等, 2002.滇西古特提斯多岛洋的结构及其南北延伸.地学前缘, 9(3):161-171. doi: 10.3321/j.issn:1005-2321.2002.03.020 [113] 刘桂春, 孙载波, 曾文涛, 等.2017.滇西双江县勐库地区湾河蛇绿混杂岩的形成时代、岩石地球化学特征及地质意义.岩石矿物学杂志, 36(2):163-174. doi: 10.3969/j.issn.1000-6524.2017.02.003 [114] 刘军平, 田素梅, 丛峰, 等, 2017.滇西澜沧江构造带南段沙乐花岗岩的锆石U-Pb年龄、地球化学特征及其地质意义.沉积与特提斯地质, 37(4):29-40. doi: 10.3969/j.issn.1009-3850.2017.04.005 [115] 毛晓长, 王立全, 李冰, 等, 2012.云县-景谷火山弧带大中河晚志留世火山岩的发现及其地质意义.岩石学报, 28(5):1517-1528. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=YSXB201205016&dbname=CJFD&dbcode=CJFQ [116] 莫宣学, 路凤香, 沈上越, 等, 1993.三江特提斯火山作用与成矿.北京:地质出版社, 65-77. [117] 潘桂棠, 王立全, 李荣社, 等, 2012.多岛弧盆系构造模式:认识大陆地质的关键.沉积与特提斯地质, 32(3):1-20. doi: 10.3969/j.issn.1009-3850.2012.03.001 [118] 潘桂棠, 王立全, 张万平, 等, 2013.青藏高原及邻区大地构造图及说明书(1:1500000).北京:地质出版社. [119] 彭头平, 王岳军, 范蔚茗, 等, 2006.澜沧江南段早中生代酸性火成岩SHRIMP锆石U-Pb定年及构造意义.中国科学(D辑), 36(2):123-132. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=JDXK200602001&dbname=CJFD&dbcode=CJFQ [120] 彭兴阶, 罗万林, 1982.滇西澜沧江南段蓝闪片岩带的发现及其大地构造意义.中国区域地质, 70(2):69-75. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ZQYD198202007&dbname=CJFD&dbcode=CJFQ [121] 任飞, 潘桂棠, 尹福光, 等, 2017.西南三江地区洋板块地层特征及构造演化.沉积与特提斯地质, 37(4):9-16. doi: 10.3969/j.issn.1009-3850.2017.04.003 [122] 任江波, 许继峰, 陈建林, 2011.中甸岛弧成矿斑岩的锆石年代学及其意义.岩石学报, 27(9):2591-2599. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=YSXB201109010&dbname=CJFD&dbcode=CJFQ [123] 汝珊珊, 李峰, 吴静, 等, 2012.云南大平掌铜多金属矿区花岗闪长斑岩地球化学特征及年代学研究.岩石矿物学杂志, 31(4):531-540. doi: 10.3969/j.issn.1000-6524.2012.04.006 [124] 沈上越, 冯庆来, 魏启荣, 等, 2008.南澜沧江带南段原特提斯岛弧火山岩新证据.矿物岩石, 28(4):59-63. doi: 10.3969/j.issn.1001-6872.2008.04.011 [125] 孙晓猛, 聂泽同, 梁定益, 1995.滇西北金沙江带硅质岩沉积环境的确定及大地构造意义.地质论评, 41(2):174-178. doi: 10.3321/j.issn:0371-5736.1995.02.010 [126] 孙载波, 李静, 周坤, 等, 2017.滇西双江县勐库地区退变质榴辉岩的岩石地球化学特征及其地质意义.现代地质, 31(4):746-756. doi: 10.3969/j.issn.1000-8527.2017.04.009 [127] 王冬兵, 罗亮, 唐渊, 等, 2016.昌宁-孟连结合带牛井山早古生代埃达克岩锆石U-Pb年龄、岩石成因及其地质意义.岩石学报, 32(8):2317-2329. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=YSXB201608006&dbname=CJFD&dbcode=CJFQ [128] 王冬兵, 罗亮, 唐渊, 等, 2017.昌宁-孟连结合带斜长角闪岩锆石U-Pb年龄、地球化学特征及其地质意义.沉积与特提斯地质, 37(4):17-28. doi: 10.3969/j.issn.1009-3850.2017.04.004 [129] 王冬兵, 王立全, 尹福光, 等, 2012.滇西北金沙江古特提斯洋早期演化时限及其性质:东竹林层状辉长岩锆石U-Pb年龄及Hf同位素约束.岩石学报, 28(5):1542-1550. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=YSXB201205018&dbname=CJFD&dbcode=CJFQ [130] 王舫, 刘福来, 冀磊, 等, 2017.澜沧江杂岩带澜沧群浅变质岩系碎屑锆石LA-ICP-MS U-Pb年代学及其构造意义.岩石学报, 33(9):2975-2985. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=YSXB201709020&dbname=CJFD&dbcode=CJFQ [131] 王舫, 刘福来, 刘平华, 等, 2014.澜沧江南段临沧花岗岩的锆石U-Pb年龄及构造意义.岩石学报, 30(10):3034-3050. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=YSXB201410018&dbname=CJFD&dbcode=CJFQ [132] 王立全, 潘桂棠, 丁俊, 等, 2013.青藏高原及邻区地质图及说明书(1:1 500 000).北京:地质出版社. [133] 王立全, 潘桂棠, 李才, 等, 2008.藏北羌塘中部果干加年山早古生代堆晶辉长岩的锆石SHRIMP U-Pb年龄——兼论原-古特提斯洋的演化.地质通报, 27(12):2045-2056. doi: 10.3969/j.issn.1671-2552.2008.12.010 [134] 王义昭, 2005.滇西昌宁-孟连带南部孟连-曼信地区晚古生代地层若干问题.地质论评, 51(1):1-9. doi: 10.3321/j.issn:0371-5736.2005.01.001 [135] 吴浩若, 李红生, 1989.滇西孟连地区的石炭纪和二叠纪放射虫化石.微体古生物学报, 6(4):337-343, 437. http://www.cnki.com.cn/Article/CJFD1989-WSGT198904002.htm [136] 徐桂香, 曾文涛, 孙载波, 等, 2016.滇西双江县勐库地区(退变)榴辉岩的岩石学、矿物学特征.地质通报, 35(7):1035-1045. doi: 10.3969/j.issn.1671-2552.2016.07.001 [137] 闫国川, 王保弟, 刘函, 等, 2018.藏东江达中石炭世弧火山岩的厘定及其构造意义.地球科学, 43(8):2715-2726. http://earth-science.net/WebPage/Article.aspx?id=3907 [138] 杨嘉文, 1982.对云县铜厂街蛇绿岩的探讨.云南地质, 1(1):59-71. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=YNZD198201012&dbname=CJFD&dbcode=CJFQ [139] 尹福光, 王冬兵, 王保弟, 等, 2017.西南三江造山带地层区划.沉积与特提斯地质, 37(4):1-8. doi: 10.3969/j.issn.1009-3850.2017.04.002 [140] 俞赛赢, 李昆琼, 施玉萍, 等, 2003.临沧花岗岩基中段花岗闪长岩类研究.云南地质, 22(4):426-442. doi: 10.3969/j.issn.1004-1885.2003.04.009 [141] 云南省地质矿产局.1990.云南省区域地质志.北京:地质出版社. [142] 翟明国, 从柏林, 张儒媛, 1990.滇西澜沧群两类火山岩系的识别及其地质意义.中国科学(B辑), (1):77-85. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=JBXK199001012&dbname=CJFD&dbcode=CJFQ [143] 翟庆国, 王军, 李才, 等, 2010.青藏高原羌塘中部中奥陶世变质堆晶辉长岩锆石SHRIMP年代学及Hf同位素特征.中国科学(D辑), 40(5):565-573. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=JDXK201005006&dbname=CJFD&dbcode=CJFQ [144] 张旗, 李达周, 张魁武, 1985.云南省云县铜厂街蛇绿混杂岩的初步研究.岩石学报, 1(3):1-14. doi: 10.3321/j.issn:1000-0569.1985.03.001 [145] 周维全, 林文信, 1982.澜沧江变质带南段蓝闪石片岩特征.中国区域地质, (2):76-85. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ZQYD198202008&dbname=CJFD&dbcode=CJFQ [146] 朱同兴, 张启跃, 董瀚, 等, 2006.藏北双湖地区才多茶卡一带构造混杂岩中发现晚泥盆世和晚二叠世放射虫硅质岩.地质通报, 25(12):1413-1418. doi: 10.3969/j.issn.1671-2552.2006.12.009 -
点击查看大图
图(8) / 表(1)
计量
- 文章访问数: 3803
- HTML全文浏览量: 1350
- PDF下载量: 106
- 被引次数: 0
