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    滇西漕涧地区崇山变质杂岩中崇山岩群的时代与构造属性

    黄亮 王冬兵 王晓林 刘小春 丛峰 朱勋早 方雄

    黄亮, 王冬兵, 王晓林, 刘小春, 丛峰, 朱勋早, 方雄, 2021. 滇西漕涧地区崇山变质杂岩中崇山岩群的时代与构造属性. 地球科学, 46(11): 3861-3879. doi: 10.3799/dqkx.2020.385
    引用本文: 黄亮, 王冬兵, 王晓林, 刘小春, 丛峰, 朱勋早, 方雄, 2021. 滇西漕涧地区崇山变质杂岩中崇山岩群的时代与构造属性. 地球科学, 46(11): 3861-3879. doi: 10.3799/dqkx.2020.385
    Huang Liang, Wang Dongbing, Wang Xiaolin, Liu Xiaochun, Cong Feng, Zhu Xunzao, Fang Xiong, 2021. Age and Tectonic Attributes of Chongshan Group in Chongshan Metamorphic Complex in Caojian Area, West Yunnan. Earth Science, 46(11): 3861-3879. doi: 10.3799/dqkx.2020.385
    Citation: Huang Liang, Wang Dongbing, Wang Xiaolin, Liu Xiaochun, Cong Feng, Zhu Xunzao, Fang Xiong, 2021. Age and Tectonic Attributes of Chongshan Group in Chongshan Metamorphic Complex in Caojian Area, West Yunnan. Earth Science, 46(11): 3861-3879. doi: 10.3799/dqkx.2020.385

    滇西漕涧地区崇山变质杂岩中崇山岩群的时代与构造属性

    doi: 10.3799/dqkx.2020.385
    基金项目: 

    中国地质调查局地质调查项目 DD20160345-02

    中国地质调查局地质调查项目 1212010000150007-26

    云南省地勘基金项目 D201901

    国家自然科学基金特提斯重大研究计划重点项目 92055207

    国家自然科学基金项目 420602005

    云南省科技厅-云南大学联合基金项目 CY21624103

    详细信息
      作者简介:

      黄亮(1985-), 男, 高级工程师, 主要从事区域地质调查, 研究方向为岩石学、构造地质方向.ORCID: 0000-0002-9929-8980.E-mail: 409090169@qq.com

    • 中图分类号: P58

    Age and Tectonic Attributes of Chongshan Group in Chongshan Metamorphic Complex in Caojian Area, West Yunnan

    • 摘要: 滇西崇山变质杂岩带位于三江造山带"峰腰"的北段,带内构造挤压变质作用强烈,主体由一套中-深变质岩系(崇山岩群)和晚期花岗岩组成.其中崇山岩群历来被认为是元古代的结晶基底,但至今无精确的年龄依据,其形成时代和构造属性存在较大争议,严重制约了对区域构造演化的认识.对滇西漕涧地区崇山岩群中的岩石组分开展了碎屑锆石U-Pb年代学及岩石地球化学研究,结果显示副变质岩中的锆石均具明显的磨圆特征和较大的岩浆核,其中3件样品的最小一组碎屑锆石年龄分别为366~412 Ma(平均值为395 Ma)、435~508 Ma(平均值为473 Ma)和673~704 Ma(平均值为689 Ma),指示了其原始沉积时代应不早于395 Ma;岩石地球化学表明,副变质岩是一套活动大陆边缘或被动大陆边缘构造背景有关的大陆岛弧碎屑岩,变质基性岩和变质中性岩为同源异相,均具活动大陆边缘的弧火山岩特征.结合副变质岩和两类正变质岩的构造属性相同以及普遍具相互伴生关系的特点,该3类岩石应属同一套地层系统的不同物质组分,崇山岩群主体为一套成岩于晚古生代(236~395 Ma)和形成于陆缘弧环境的火山-沉积地层单元;并与南东侧澜沧增生杂岩的志留纪弧火山岩组合成原-古特提斯洋盆东侧不同时代多岛弧的构造格局.综合研究认为,崇山变质杂岩带内的中-深变质岩系(崇山岩群)不(全)是前人认为的元古代结晶基底建造,应为原-古特提斯洋盆向东俯冲在兰坪-思茅地块西缘形成的一套火山-沉积地层系统;崇山岩群主要由年轻的(晚古生代)地层岩石组成,由于后期遭受中生代和新生代变质变形作用后形成了现今所见的"古老"岩石面貌的中-深变质系.

       

    • 图  1  研究区地质简图和大地构造位置图

      Fig.  1.  Geological sketch and geotectonic location map of the study area

      图  2  崇山岩群野外露头及不同类型岩石

      a.崇山岩群呈包体状产于花岗岩中;b.石榴矽线黑云钾长片麻岩产出特征;c.斜长角闪岩;d.角闪斜长变粒岩

      Fig.  2.  Photographs of outcrop and various rocks of the Chongshan Group

      图  3  崇山岩群不同类型岩石显微结构特征

      a.石榴矽线黑云钾长片麻岩;b.石榴矽线黑云片岩;c.斜长角闪岩;d.角闪斜长变粒岩;Qtz.石英;Bt.黑云母;Sil.矽线石;Grt.石榴子石;Kfs.钾长石;Pl.斜长石;Amp.角闪石

      Fig.  3.  Microstructures of various type rocks of the Chongshan Group

      图  4  崇山岩群副变质岩中典型锆石阴极发光(CL)图像

      Fig.  4.  Cathodoluminescence (CL) images of representative zircons for the parablastesis from the Chongshan Group

      图  5  崇山岩群副变质岩LA-ICP-MS锆石年龄谐和图

      Fig.  5.  LA-ICP-MS zircon U-Pb concordia diagrams for the parablastesis from the Chongshan Group

      图  6  崇山岩群副变质岩LA-ICP-MS锆石U-Pb年龄分布图

      Fig.  6.  LA-ICP-MS zircon U-Pb histograms for the parablastesis from the Chongshan Group

      图  7  崇山岩群的稀土微量特征图解

      a,c.稀土元素球粒陨石标准化模式图;b,d. 微量元素原始地幔标准化图解(球粒陨石和原始地幔的值引自Sun and Mcdonough(1989)

      Fig.  7.  The diagrams of rare-earth and trace elements for the Chongshan Group

      图  8  崇山岩群正变质岩Harker图解

      Fig.  8.  Variations of major element for the orthometamorphite from the Chongshan Group

      图  9  崇山岩群副变质岩构造环境判别图解

      a. Hf-La/Th图解(据Floyd and Leveridge, 1987);b. La/Sc-Ti/Zr图解(据Bhatia,1983);c~e. Th-Sc-Zr/10图解、La-Sc-Th图解、Th-Co-Zr/10图解(据Bhatia and Crook, 1986

      Fig.  9.  Discrimination diagrams for the parametamorphic rocks from the Chongshan Group

      图  10  崇山岩群正变质岩判别图解

      a. Nb/Y-Zr/TiO2图解(据Winchester and Floyd, 1977);b. Zr-Y图解(据Simon and Bedard, 2009);c. 3Y-Zr-Ti/100图解(据Pearce and Cann, 1973);d. La-La/Nb图解(据Pearce,2003

      Fig.  10.  Discrimination diagrams of the orthometamorphite from the Chongshan Group

      图  11  变质中性岩的Ta/Yb-Th/Yb图解(据Gorton and Schandl, 2000

      Fig.  11.  Ta/Yb-Th/Yb diagram of the metamorphic intermediate rock (after Gorton and Schandl, 2000)

    • Bailey, J. C., 1981. Geochemical Criteria for a Refined Tectonic Discrimination of Orogenic Andesites. Chemical Geology, 32(1): 139-154.
      Becker, H., Jochum, K.P., Carlson, R.W., 2000. Trace Element Fractionation during Dehydration of Eclogites from High-Pressure Terranes and the Implications for Element Fluxes in Subductions Zones. Chemical Geology, 163(1-4): 65-99. doi: 10.1016/S0009-2541(99)00071-6
      Bhatia, M.R., 1983. Plate Tectonics and Geochemical Composition of Sandstones. The Journal of Geology, 91(6): 611-627. doi: 10.1086/628815
      Bhatia, M. R., Crook, K. A. W., 1986. Trace Element Characteristics of Graywackes and Tectonic Setting Discrimination of Sedimentary Basins. Contributions to Mineralogy and Petrology, 92(2): 181-193. https://doi.org/10.1007/BF00375292
      Bureau of Geological Survey of Yunnan Province, 2013. Research Report on Metallogenic Geological Background in Yunnan Rrovince (in Chinese).
      Bureau of Geology and Mineral Resources of Yunnan Province, 1990. Regional Geology of Yunnan Province. Geological Publishing House, Beijing (in Chinese).
      Cai, Z.H., Xu, Z.Q., Duan, X.D., et al., 2013. Early Stage of Early Paleozoic Orogenic Event in Western Yunnan Province, Southeastern Margin of Tibet Plateau. Acta Petrologica Sinica, 29(6): 2123-2140 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201306020.htm
      Cao, Y., Kang, Z.Q., Xu, J.F., et al., 2020. Geochronology, Geochemistry and Geological Significance of Volcanic Rocks of the Dianzhong Formation, Shiquanhe Area, Western Lhasa Block. Earth Science, 45(5): 1573-1592 (in Chinese with English abstract).
      Compilation Group, Editorial Board of Sanjiang Geological Map, Ministry of Geology and Mineral Resources, 1986. The Regional Geological Map of Nujiang, Lancangjiang and Jinshajiang Area Instruction 1: 1 000 000. Geological Publishing House, Beijing (in Chinese).
      Condie, K.C., 2001. Mantle Plume and Their Record in Earth History. Cambridge University Press, London.
      Deng, J., Wang, Q.F., Li, G.J., et al., 2014. Tethys Tectonic Evolution and Its Bearing on the Distribution of Important Mineral Deposits in the Sanjiang Region, SW China. Gondwana Research, 26(2): 419-437. doi: 10.1016/j.gr.2013.08.002
      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 Petrologica Sinica, 28 (5): 1453-1464 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201205011.htm
      Floyd, P. A., Leveridge, B.E., 1987. Tectonic Environment of the Devonian Gramscatho Basin, South Cornwall: Framework Mode and Geochemical Evidence from Turbiditic Sandstones. Journal of the Geological Society, 144(4): 531-542. doi: 10.1144/gsjgs.144.4.0531
      Gao, F., Pei, X. Z., Li, R. B., et al., 2019. Detrital Zircon U-Pb Ages and Geological Significance of Low-Metamorphosed Liuling Sedimentary Assemblage in the Shangdan Area, Eastern Qinling Orogenic Belt. Earth Science, 44(7): 2519-2531 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX201907023.htm
      Glassley, W. E., 1974. Geochemistry and Tectonics of the Crescent Volcanic Rocks, Olympic Peninsula, Washington. Geological Society of America Bulletin, 85(5): 785-794. doi: 10.1130/0016-7606(1974)85<785:GATOTC>2.0.CO;2
      Gorton, M. P., Schandl, E.S., 2000. From Continents to Island Arcs: A Geochemical Index of Tectonic Setting for Arc-Related and Within-Plate Felsic to Intermediate Volcanic Rocks. The Canadian Mineralogist, 38(5): 1065 -1073. doi: 10.2113/gscanmin.38.5.1065
      Hanchar, J. M., van Westrenen, W., 2007. Rare Earth Element Behavior in Zircon-Melt Systems. Elements, 3(1): 37-42. doi: 10.2113/gselements.3.1.37
      Harley, S. L., Kelly, N. M., 2007. Zircon: Tiny but Timely. Elements, 3(1): 13-18. doi: 10.2113/gselements.3.1.13
      Henderson, P., 1984. Rare Earth Element Geochemistry. Elsevier Science Publications, New York.
      Huang, L., Lü, B.Y., Wang, X.L., et al., 2021. Zircon U-Pb Age, Geochemical Characteristics, Hf Isotopic Composition and Indications of Pan-African Movement from the Two Types of Late Ordovician Superaluminum Granites in the Caojian Area, Western Yunnan Province. Geological Bulletin of China, in Press (in Chinese with English abstract).
      Huang, L., Wu, J.L., Wang, X.L., et al., 2020. The Discovery of Pegmatite of the Chongshan Orogenic Belt in the Caojian Area, Western Yunnan and Its Geological Significance. Acta Mineralogica Sinica, 40(5): 584-594 (in Chinese with English abstract).
      Lehmann, B., Zhao, X., Zhou, M., 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. doi: 10.1016/j.gr.2012.12.018
      Li, W.C., Pan, G.T., Hou, Z.Q., et al., 2010. Archipelagic-Basin, Forming Collision Theory and Prospecting Techniques along the Nujiang-Lancangjiang-Jinshajiang Area in Southwestern China. Geological Publishing House, Beijing (in Chinese).
      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://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200203027.htm
      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). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW201702003.htm
      Ludwig, K.R., 2003. ISOPLOT 3.00: A Geochronological Toolkit for Microsoft Excel. Berkeley Geochronology Center Special Publication, Berkeley.
      Mao, X.C., Wang, L.Q., Li, B., et al., 2012. Discovery of the Late Silurian Volcanic Rocks in the Dazhonghe Area, Yunxian-Jinggu Volcanic Arc Belt, Western Yunnan, China and Its Geological Significance. Acta Petrologica Sinica, 28(5): 1517-1528 (in Chinese with English abstract).
      Mao, X.C., Yin, F.G., Tang, Y., et al., 2014. Early Paleozoic Accretionary Orogenesis on Western Margin of Baoshan Block. Earth Science, 39(8): 1129-1139 (in Chinese with English abstract).
      McCulloch, M. T., Gamble, J. A., 1991. Geochemical and Geodynamical Constraints on Subduction Zone Magmatism. Earth and Planetary Science Letters, 102(3-4): 358-374. doi: 10.1016/0012-821X(91)90029-H
      Metcalfe, I., 2013. Gondwana Dispersion and Asian Accretion: Tectonic and Palaeogeography Evolution of Eastern Tetheys. Journal of Earth Sciences, 66: 1-33.
      Mo, X. X., Shen, S.Y., Zhu, Q.W., et al., 1998. Volcanics-Ophiolite and Mineralization of Middlesouthern Part in Shanjiang Area of Southwestern China. Geological Publishing House, Beijing, 1-128 (in Chinese).
      Nie, X.M., Feng, Q.L., Wang, Y.J., 2014. 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: 757-768. http://smartsearch.nstl.gov.cn/paper_detail.html?id=476ad36959b63d2bd71dd32f6cb5c631
      Pearce, J.A., 1983. Role of the Sub-Continental Lithosphere in Magma Genesis at Active Continental Margins. In: Hawkesworth, C.J., Norry, M.J., eds., Continental Basalts and Mantle Xenoliths. Shiva Publishing, Nantwich, Cheshire, 230-249.
      Pearce, J.A., 2003. Supra-Subduction Zone Ophiolites: The Search for Modern Analogues. In: Pearce, J. A., ed., Special Paper 373: Ophiolite Concept and the Evolution of Geological Thought. Geological Society of America, New York, 269-293.
      Pearce, J.A., Cann, J.R., 1973. Tectonic Setting of Basic Volcanic Rocks Determined Using Trace Element Analyses. Earth and Planetary Science Letters, 19(2): 290-300. doi: 10.1016/0012-821X(73)90129-5
      Pearce, J. A., Harris, N. B. W., Tindle, A. G, 1984. Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks. Journal of Petrology, 25(4): 956-983. https://doi.org/10.1093/petrology/25.4.956
      Peng, Z.M., Zhang, J., Guan, J.L., et al., 2018. The Discovery of Early-Middle Ordovician Granitic Gneiss from the Giant Lincang Batholith in Sanjiang of Western Yunnan and Its Geological Implications. Earth Science, 43(8): 2571-2585 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX201808003.htm
      Rubatto, D., Hermann, J., 2007. Zircon Behaviour in Deeply Subducted Rocks. Elements, 3(1): 31-35. doi: 10.2113/gselements.3.1.31
      Rudnick, R.L., Gao, S., 2003. Composition of the Continental Crust. Elsevier-Pergamon, Oxford, 3: 1-64.
      Sadofsky, S.J., Bebout, G.E., 2003. Record of Forearc Devolatilization in Low-T, High-P/T Metasedimentary Suites: Significance for Models of Convergent Margin Chemical Cycling. Geochemistry, Geophysics, Geosystems, 4(4): 9003.
      Simon, R.P., Bedard, J.H., 2009. Magmatic Affinity of Modern and Ancient Subalkaline Volcanic Rocks Determined Trace-Element Discriminant Diagrams. Canadian Journal of Earth Science, 46(11): 823-839. doi: 10.1139/E09-054
      Sun, S.S., McDonough, W.F., 1989. Chemical and Isotopic Systematics of Oceanic Basalts: Implications for Mantle Composition and Processes. Geological Society, London, Special Publications, 42: 313-345. doi: 10.1144/GSL.SP.1989.042.01.19
      Volcanic Rock Formation in Rock Teaching and Research Section of Chengdu Institute of Geology, 1980. Discovery and Metamorphism of Marine Volcanic Rocks of Chongshan Group in Caojian Area, Western Yunnan. Mineral Rock, 1: 32-41 (in Chinese).
      Wang, B.D., Wang, L.Q., Wang, D.B., et al., 2018. Tectonic Evolution of the Changning-Menglian Proto-Paleo Tethys Ocean in the Sanjiang Area, Southwestern China. Earth Science, 43(8): 2527-2550 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX201808001.htm
      Wang, D.B., Yin, F.G., Luo, L., et al., 2015. U-Pb Dating of Detrital Zircons from the Damenglong Group in the Niujinshan Area of Changning-Menglian Tectonicbelt and Its Geological Significance. Mineralogy and Petrology, 35(3): 72-80 (in Chinese with English abstract).
      Wang, D.D., Li, B.L., Ji, J.Q., et al., 2014. Zircon SHRIMP U-Pb Geochronology and Its Tectonic Implication of the Metamorphic Rocks in Southern Lancang River Tectonic Zone, West Yunnan Province. Acta Petrologica Sinica, 30(9): 2725-2738 (in Chinese with English abstract).
      Wang, G.Z., Liu, D.Z., Zhu, L.D., et al., 2000. Analysis of the Undating Metamorphics in West Yunnan and Determination of Its Age. Regional Geology of China, 19(1): 32-37 (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTotal-ZQYD200001005.htm
      Wei, G.Y., Feng, G.R., Luo, Z.W., et al., 1984. Stratigraphic Sequences of the Lancang and Chongshan Groups in Western Yunnan and Their Volcanism and Metamorphism. Journal of Chengdu University of Technology, (2): 12-20 (in Chinese). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CDLG198402001.htm
      Whittington, A.G., Treloar, P.J., 2002. Crustal Anatexis and Its Relation to the Exhumation of Collisional Orogenic Belts, with Particular Reference to the Himalaya. Mineralogical Magazine, 66(1): 53-91. doi: 10.1180/0026461026610015
      Wilson, M., 1989. Igneous Petrogenesis: A Global Tectonic Approach. Unwin Hyman, London, 1-466.
      Winchester, J.A., Floyd, P.A., 1977. Geological Discrimination of Different Magma Series and Their Differentiation Products Using Immobile Elements. Chemical Geology, 20: 325-343. doi: 10.1016/0009-2541(77)90057-2
      Winter, J.D., 2001. An Introduction Igneous and Metamorphic Petrology. Printice Hall, New Jersey, 1-697.
      Wu, Y.B., Zheng, Y.F., 2004. Genesis of Zircon and Its Constraints on Interpretation of U-Pb Age. Chinese Science Bulletin, 49(16): 1554-1569 (in Chinese). doi: 10.1007/BF03184122
      Xiong, J.Y., 1989. The Summary of Strata in Yunnan Province. Yunnan Regional Geology, 7: 10-31 (in Chinese with English abstract).
      Xu, Y.F., Liu, J.P., Cong, F., et al., 2018. LA-ICP-MS Zircon U-Pb Dating of the Chongshan Group in the Xiaowan Area along the Southern Section of the Lancang River in Western Yunnan and Its Geological Significance. Geological Bulletin of China, 37(6): 1006-1014 (in Chinese with English abstract).
      Yin, A., Harrison, T.M., 2000. Geologic Evolution of the Himalayan-Tibetan Orogen. Annual Reviews Earth Planet Science, 28(1): 211-280. doi: 10.1146/annurev.earth.28.1.211
      Yunnan Institute of Geological Survey, 2008.1: 250 000 Dali Regional Geological Survey Report (in Chinese).
      Yunnan Institute of Geological Survey, 2011.1: 50 000 Regional Geological and Mineral Survey Report of Baoshan, Banqiao, Huayao, Shanyang, Jinji, Yongping, Changjie and Longjie in Yunnan Province (in Chinese).
      Yunnan Institute of Geological Survey, 2019.1: 50 000 Regional Geological Survey of Guizhou, Baofeng, Caojian and Gongguo Street in Yunnan Province (in Chinese).
      Zhai, M.G., Cong, B.L., Qiao, G.S., et al., 1990. Sm-Nd and Rb-Sr Geochronology of Metamorphic Rocks from SW Yunnan Orogenic Zones, China. Acta Petrologica Sinica, 6(4): 1-11(in Chinese with English abstract).
      Zhang, B., Zhang, J.J., Zhong, D.L., 2010. Structure, Kinematics and Ages of Transpression during Strain-Partitioning in the Chongshan Shear Zone, Western Yunnan, China. Journal of Structural Geology, 32(4): 445-463. doi: 10.1016/j.jsg.2010.02.001
      Zhang, Q., 2012. Commengt on Harke Diagram of the Granite. Acta Petrologica et Mineralogica, 31(3): 425-431 (in Chinese with English abstract).
      Zhong, D.L., 1998. Paleotethyan Orogenic Belts in Yunnan and Western Sichuan. Science Press, Beijing (in Chinese).
      云南省地质调查局, 2013. 云南省成矿地质背景研究报告.
      云南省地质矿产局, 1990. 云南省区域地质志. 北京: 地质出版社.
      蔡志慧, 许志琴, 段向东, 等, 2013. 青藏高原东南缘滇西早古生代早期造山事件. 岩石学报, 29(6): 2123-2140. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201306020.htm
      曹延, 康志强, 许继峰, 等, 2020. 拉萨地块西部狮泉河地区典中组火山岩年代学、地球化学特征及其构造意义. 地球科学, 45(5): 1573-1592. doi: 10.3799/dqkx.2019.161
      地质矿产部三江地质编委会地质图编图组, 1986. 怒江、澜沧江、金沙江区域地质图(1: 100万)说明书. 北京: 地质出版社.
      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. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201205011.htm
      高峰, 裴先治, 李瑞保, 等, 2019. 东秦岭商丹地区刘岭群浅变质沉积岩系碎屑锆石U-Pb年龄及其地质意义. 地球科学, 44(7): 2519-2531. doi: 10.3799/dqkx.2018.164
      黄亮, 吕勃烨, 王晓林, 等, 2021. 滇西漕涧地区两类晚奥陶世强过铝花岗岩的锆石U-Pb年龄、地球化学特征、Hf同位素组成及对泛非运动的指示. 地质通报, 待刊.
      黄亮, 吴嘉林, 王晓林, 等, 2020. 滇西漕涧地区崇山造山带伟晶岩的发现与地质意义. 矿物学报, 40(5): 584-594. https://www.cnki.com.cn/Article/CJFDTOTAL-KWXB202005006.htm
      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.
      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
      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
      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. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201205016.htm
      毛晓长, 尹福光, 唐渊, 等, 2014. 保山地块西缘早古生代增生造山作用. 地球科学, 39(8): 1129-1139. doi: 10.3799/dqkx.2014.099
      莫宣学, 沈上越, 朱勤文, 等, 1998. 三江中南段火山岩-蛇绿岩与成矿. 北京: 地质出版社, 1-128.
      彭智敏, 张辑, 关俊雷, 等, 2018. 滇西"三江" 地区临沧花岗岩基早-中奥陶世花岗质片麻岩的发现及其意义. 地球科学, 43(8): 2571-2585. doi: 10.3799/dqkx.2018.102
      成都地质学院岩石教研室火山岩组, 1980. 滇西漕涧地区崇山岩群海相火山岩的发现及其变质作用. 矿物岩石, 1: 32-41. https://www.cnki.com.cn/Article/CJFDTOTAL-KWYS198001003.htm
      王保弟, 王立全, 王冬兵, 等, 2018. 三江昌宁-孟连带原-古特提斯构造演化. 地球科学, 43(8): 2527-2550. doi: 10.3799/dqkx.2018.160
      王丹丹, 李宝龙, 季建清, 等, 2014. 澜沧江构造带南段变质岩系锆石U-Pb年代学及构造涵义. 岩石学报, 30(9): 2725-2738. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201409021.htm
      王冬兵, 尹福光, 罗亮, 等, 2015. 昌宁-孟连构造带牛井山地区大勐龙岩群碎屑锆石U-Pb定年及其地质意义. 矿物岩石, 35(3): 72-80. https://www.cnki.com.cn/Article/CJFDTOTAL-KWYS201503010.htm
      王国芝, 刘登忠, 朱利东, 等, 2000. 滇西时代不明变质岩系的解体和时代厘定. 中国区域地质, 19(1): 32-37. doi: 10.3969/j.issn.1671-2552.2000.01.006
      卫管一, 冯国荣, 罗再文, 等, 1984. 滇西澜沧群、崇山群地层层序及其火山作用和变质作用. 成都地质学院学报(自然科学版), (2): 12-20. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG198402001.htm
      吴元保, 郑永飞, 2004. 锆石成因矿物学研究及其对U-Pb年龄解释的制约. 科学通报, 49(16): 1554-1569. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200416001.htm
      熊家镛, 1989. 云南地层概述. 云南区域地质, 7: 10-31. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201402004.htm
      徐云飞, 刘军平, 丛峰, 等, 2018. 滇西澜沧江南段小湾地区崇山岩群LA-ICP-MS锆石U-Pb年龄及其地质意义. 地质通报, 37(6): 1006-1014. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201806005.htm
      云南省地质调查院, 2008.1: 25万大理幅区域地质调查报告.
      云南省地质调查院, 2011. 云南省1: 5万保山、板桥、瓦窑、杉阳、金鸡、永平、厂街、龙街8幅区域地质矿产调查报告.
      云南省地质调查院, 2019. 云南省1: 5万归州、宝丰、漕涧、功果街幅区域地质调查报告.
      翟明国, 从柏林, 乔广生, 等, 1990. 中国滇西南造山带变质岩的Sm-Nd和Rb-Sr同位素年代学. 岩石学报, 6(4): 1-11. doi: 10.3321/j.issn:1000-0569.1990.04.001
      张旗, 2012. 评花岗岩的哈克图解. 岩石矿物学杂志, 31(3): 425-431. doi: 10.3969/j.issn.1000-6524.2012.03.012
      钟大赉, 1998. 滇川西部古特提斯造山带. 北京: 科学出版社.
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