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

彭智敏; 张辑; 关俊雷; 张璋; 韩文文; 付于真

doi:10.3799/dqkx.2018.102

Volume 43 Issue 8

Aug. 2018

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Article Navigation > Earth Science > 2018 > 43(8): 2571-2585

Peng Zhimin, Zhang Ji, Guan Junlei, Zhang Zhang, Han Wenwen, Fu Yuzhen, 2018. The Discovery of Early-Middle Ordovician Granitic Gneiss from the Giant Lincang Batholith in Sanjiang Area of Western Yunnan and Its Geological Implications. Earth Science, 43(8): 2571-2585. doi: 10.3799/dqkx.2018.102

Citation:

Peng Zhimin, Zhang Ji, Guan Junlei, Zhang Zhang, Han Wenwen, Fu Yuzhen, 2018. The Discovery of Early-Middle Ordovician Granitic Gneiss from the Giant Lincang Batholith in Sanjiang Area of Western Yunnan and Its Geological Implications. Earth Science, 43(8): 2571-2585. doi: 10.3799/dqkx.2018.102

Citation:

Peng Zhimin, Zhang Ji, Guan Junlei, Zhang Zhang, Han Wenwen, Fu Yuzhen, 2018. The Discovery of Early-Middle Ordovician Granitic Gneiss from the Giant Lincang Batholith in Sanjiang Area of Western Yunnan and Its Geological Implications. Earth Science, 43(8): 2571-2585. doi: 10.3799/dqkx.2018.102

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The Discovery of Early-Middle Ordovician Granitic Gneiss from the Giant Lincang Batholith in Sanjiang Area of Western Yunnan and Its Geological Implications

doi: 10.3799/dqkx.2018.102

1.
Chengdu Center of China Geological Survey, Chengdu 610081, China
2.
Institute No. 280 of CNNC, Guanghan 618300, China
3.
College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China

Received Date: 2018-05-08
Publish Date: 2018-08-15

Abstract

Abstract

There are little research on the Early Paleozoic magma events of the giant Lingcang batholith in Sangjiang area.Early Paleozoic granitic gneiss was recognized for the first time from the Lincang batholith in Shuangjiang area of western Yunnan.LA-ICP-MS U-Pb dating and Hf isotopic analysis of zircons, combined with geochemical characteristics of two granitic gneiss samples are applied in this paper.The zircon U-Pb ages of 476.9±1.9 Ma and 465.7±1.9 Ma are obtained from two samples, which indicates that two granitic gneisses were formed in Middle-Late Ordovician.SiO₂ content of the granitic gneisses ranges from 70.67% to 74.03%.The K₂O/Na₂O ratio is greater than 1, ranging from 1.04 to 1.55, and belonging to peraluminous S-type granitoids.They also enriched in LILEs (Rb, Th and U), but strongly depleted in HFSEs (Nb, Ta, Ti and Zr), showing strongly fractionated REE pattern, with apparently negative Eu anomalies.Their zircons have negative ε_Hf(t) values (-7.2 to -0.7, average -3.0), and Hf isotope crust model ages (t_DM^C) are basically the same (average 1 639 Ma, 1 630 Ma).It is suggested that granitic gneiss may have originated from partial melting of ancient crustal materials.Based on the above analyses, granitic gneiss is formed by partial melting of ancient crustal materials that was caused by the eastward subduction of the Paleo-Tethys, and is the response of the magmatic events during subduction of the Paleo-Tethys.It shows that there was subduction in the Changning-Menglian ocean in the Early Ordovician, and the evolution history of the Tethys in the Changning-Menglian combination can be traced back to the Early Ordovician.
- granitic gneiss,
- zircon U-Pb dating,
- Paleo-Tethys ocean,
- Changning-Menglian suture,
- western Yunnan,
- Sangjiang area,
- geochemistry,
- geochronology

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References(72)

References

Altherr, R., Holl, A., Hegner, E., et al., 2000.High-Potassium, Calc-Alkaline I-Type Plutonism in the European Variscides:Northern Vosges (France) and Northern Schwarzwald (Germany).Lithos, 50(1-3):51-73.https://doi.org/10.1016/s0024-4937(99)00052-3 doi: 10.1016/S0024-4937(99)00052-3

Blichert-Toft, J., Albarède, F., 1997.The Lu-Hf Isotope Geochemistry of Chondrites and the Evolution of the Mantle-Crust System.Earth and Planetary Science Letters, 148(1-2):243-258.https://doi.org/10.1016/s0012-821x(97)00040-x doi: 10.1016/S0012-821X(97)00040-X

Chappell, B.W., 1999.Aluminium Saturation in I-and S-Type Granites and the Characterization of Fractionated Haplogranites.Lithos, 46(3):535-551.https://doi.org/10.1016/s0024-4937(98)00086-3 doi: 10.1016/S0024-4937(98)00086-3

Chen, J.C., 1989.Tectonic Surroundings Forming West Yunnan Granitoids and Their Rock Characters.Yunnan Geology, 8(3-4):205-212 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YNZD1989Z1001.htm

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). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201707008

Ferry, J.M., Watson, E.B., 2007.New Thermodynamic Models and Revised Calibrations for the Ti-in-Zircon and Zr-in-Rutile Thermometers.Contributions to Mineralogy and Petrology, 154(4):429-437. https://doi.org/10.1007/s00410-007-0201-0

Griffin, W.L., Wang, X., Jackson, S.E., et al., 2002.Zircon Chemistry and Magma Mixing, SE China:In-Situ Analysis of Hf Isotopes, Tonglu and Pingtan Igneous Complexes.Lithos, 61(3-4):237-269.https://doi.org/10.1016/s0024-4937(02)00082-8 doi: 10.1016/S0024-4937(02)00082-8

Griffin, W.L., Belousova, E.A., Shee, S.R., et al., 2004.Archean Crustal Evolution in the Northern Yilgarn Craton:U-Pb and Hf Isotope Evidence from Detrital Zircons.Precambrian Research, 131(3-4):231-282. https://doi.org/10.1016/j.precamres.2003.12.011

Hu, P.Y., Li, C., Su, L., et al., 2010.Zircon U-Pb Dating of Granitic Gneiss in Wugong Mountain Area, Central Qiangtang, Qinghai-Tibet Plateau:Age Records of Pan-African Movement and Indo-China Movement.Geology in China, 37(4):1050-1061 (in Chinese with English abstract).

Huang, Y., Hao, J.X., Bai, L., et al., 2012.Stratigraphic and Petrologic Response to Late Pan-African Movement in Shidian Area, Western Yunnan Province.Geologcal Bulletin of China, 31(2):306-313 (in Chinese with English abstract). https://www.researchgate.net/publication/289747078_Stratigraphic_and_petrologic_response_to_Late_Pan-African_movement_in_Shidian_area_western_Yunnan_Province

King, P.L., White, A.J.R., Chappell, B.W., et al., 1997.Characterization and Origin of Aluminous A-Type Granites from the Lachlan Fold Belt, Southeastern Australia.Journal of Petrology, 38(3):371-391. https://doi.org/10.1093/petroj/38.3.371

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

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

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). http://en.cnki.com.cn/Article_en/CJFDTotal-ZQYD201012002.htm

Li, X.L., 1996.Basic Characteristics and Formation Structural Environment of Lincang Composite Granite Batholith.Yunnan Geology, 15(1):1-18 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YNZD601.000.htm

Liu, B.P., Feng, Q.L., Fang, N.Q., et al., 1993.Tectonic Evolution of Palaeo-Tethys Poly-Island-Ocean in Changning-Menglian and Lancangjiang Belts, Southwestern Yunnan, China.Earth Science, 18(5):529-539 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX199305000.htm

Liu, C.S., Zhu, J.C., Xu, X.S., et al., 1989.Study on the Characteristics of Linchang Composite Granite Batholith in West Yunnan.Yunnan Geology, 8(3-4):189-204 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YNZD1989Z1000.htm

Liu, D.L., Liu, J.S., Zhang, C.H., et al., 2008.Geological Characteristics and Tectonic Setting of Yunxian Granite in the Northern Part of South Lancangjiang Convergent Margin, Western Yunnan Province.Acta Petrologica et Mineralogica, 27(1):23-31 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=9ac04cc0521227dbb059bc378306426b&encoded=0&v=paper_preview&mkt=zh-cn

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).

Liu, Q., Deng, Y.B., Xiang, S.Y., et al., 2017.Early Ordovician Tectono-Thermal Event in Zhongba Terrane and Its Geological Significance.Earth Science, 42(6):881-890 (in Chinese with English abstract).https://doi.org/dqkx.2017.076 http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX201706003.htm

Liu, Y.S., Hu, Z.C., Zong, K.Q., et al., 2010.Reappraisement and Refinement of Zircon U-Pb Isotope and Trace Element Analyses by LA-ICP-MS.Chinese Science Bulletin, 55(15):1535-1546. https://doi.org/10.1007/s11434-010-3052-4

Ludwig, K.R., 2003.User's Manual for Isoplot 3.0: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). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201205014

Middlemost, E.A.K., 1985.Magmas and Magmatic Rocks.Longman, London.

Middlemost, E.A.K., 1994.Naming Materials in the Magma/Igneous Rock System.Earth-Science Reviews, 37(3-4):215-224. https://doi.org/10.1016/0012-8252(94)90029-9

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/10.13039/501100001809 doi: 10.1016/j.gr.2014.05.011

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

Peccerillo, A., Taylor, S.R., 1976.Geochemistry of Eocene Calc-Alkaline Volcanic Rocks from the Kastamonu Area, Northern Turkey.Contributions to Mineralogy and Petrology, 58(1):63-81.https://doi.org/10.1007/bf00384745 doi: 10.1007/BF00384745

Peng, T.P., Wang, Y.J., Fan, W.M., et al., 2006.SHRIMP Zircon U-Pb Geochronology of Early Mesozoic Felsic Igneous Rocks from the Southern Lancangjiang and Its Tectonic Implications.Science in China (Series D), 36(2):123-132 (in Chinese). https://www.researchgate.net/profile/Yuruo_Shi/publication/226663314_SHRIMP_ziron_U-Pb_geochronology_of_early_Mesozoic_felsic_igneous_rocks_from_the_southern_Lancangjiang_and_its_tectonic_implications/links/53e8c1be0cf21cc29fdc94cf.pdf?origin=publication_list

Peng, Z.M., Geng, Q.R., Wang, L.Q., et al., 2014.Zircon U-Pb Ages and Hf Isotopic Characteristics of Granitic Gneiss from Bunsumco, Central Qiangtang, Qinghai-Tibet Plateau.Chinese Science Bulletin, 59(26):2621-2629 (in Chinese). doi: 10.1360/N972014-00014

Söderlund, U., Patchett, P.J., Vervoort, J.D., et al., 2004.The ¹⁷⁶Lu Decay Constant Determined by Lu-Hf and U-Pb Isotope Systematics of Precambrian Mafic Intrusions.Earth and Planetary Science Letters, 219(3-4):311-324.https://doi.org/10.1016/s0012-821x(04)00012-3 doi: 10.1016/S0012-821X(04)00012-3

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(1):313-345.https://doi.org/10.1144/gsl.sp.1989.042.01.19 doi: 10.1144/GSL.SP.1989.042.01.19

Sun, Z.B., Zeng, W.T., Zhou, K., et al., 2017.Identification of Ordovician Oceanic Island Basalt in the Changning-Menglian Suture Zone and Its Tectonic Implications:Evidence from Geochemical and Geochronological Data.Geological Bulletin of China, 36(10):1760-1771 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD201710008.htm

Sylvester, P.J., 1998.Post-Collisional Strongly Peraluminous Granites.Lithos, 45(1-4):29-44.https://doi.org/10.1016/s0024-4937(98)00024-3 doi: 10.1016/S0024-4937(98)00024-3

Wang, B.D., Wang, L.Q., Pan, G.T., et al., 2013.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(4):344-354(in Chinese). http://cn.bing.com/academic/profile?id=e5c57d4e44a3e491a9308cfefd5ae46f&encoded=0&v=paper_preview&mkt=zh-cn

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

Wang, H.L., Lin, F.C., Cong, F., et al., 2016.Yunnan Fengqing Mang Street Leucogranite LA-ICP-MS Zircon U-Pb Age and Its Geological Significance.World Nonferrous Metals, (7):59-61 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-COLO201607024.htm

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

Watson, E.B., Harrison, T.M., 1983.Zircon Saturation Revisited:Temperature and Composition Effects in a Variety of Crustal Magma Types.Earth and Planetary Science Letters, 64(2):295-304.https://doi.org/10.1016/0012-821x(83)90211-x doi: 10.1016/0012-821X(83)90211-X

Wu, S. L., 2010. Charcteristics, Geochronology of Lincang Granite in the Southern Langcangjiang, Sanjiang Area and Implication for Tectonics (Dissertation). China University of Geosciences, Beijing (in Chinese with English abstract).

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

Xing, X.W., Zhang, Y.Z., Wang, Y.J., et al., 2015.Zircon U-Pb Geochronology and Hf Isotopic Composition of the Ordovician Granitic Gneisses in Ximeng Area, West Yunnan Province.Geotectonica et Metallogenia, 39(3):470-480 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=69f696ee0255c7c73807e65e56693f10&encoded=0&v=paper_preview&mkt=zh-cn

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

Zeng, W.T., Liu, G.C., Feng, Q.L., et al., 2017.The Relationship between Lincang Block and Provenance of Nanduan Formation:Evidence of Detrital Zircon U-Pb Dating from Metasandstone of Devonian-Carboniferous Nanduan Formation.Geological Bulletin of China, 36(7):1175-1187 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-ZQYD201707008.htm

Zhang, W.H., Qin, Y.J., Wang, Y., 1991.Discussion on the Causation Type and Its Source of Lincang Granite Belt in West Yunnan.Bulletin of Mineralogy, Petrology and Geochemistry, 10(4):240-243 (in Chinese with English abstract).

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

陈吉琛, 1989.滇西花岗岩类形成的构造环境及岩石特征.云南地质, 8(3-4):205-212. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=YNZD1989Z1001&dbname=CJFD&dbcode=CJFQ

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://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000001581745

胡培远, 李才, 苏犁, 等, 2010.青藏高原羌塘中部蜈蚣山花岗片麻岩锆石U-Pb定年——泛非与印支事件的年代学记录.中国地质, 37(4):1050-1061. doi: 10.3969/j.issn.1000-3657.2010.04.019

黄勇, 郝家栩, 白龙, 等, 2012.滇西施甸地区晚泛非运动的地层学和岩石学响应.地质通报, 31(2):306-313. doi: 10.3969/j.issn.1671-2552.2012.02.013

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://d.old.wanfangdata.com.cn/Periodical/ysxb98201205008

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

李兴林, 1996.临沧复式花岗岩基的基本特征及形成构造环境的研究.云南地质, 15(1):1-18. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199600616589

刘本培, 冯庆来, 方念乔, 等, 1993.滇西南昌宁-孟连带和澜沧江带古特提斯多岛洋构造演化.地球科学, 18(5):529-539. http://earth-science.net/WebPage/Article.aspx?id=68

刘昌实, 朱金初, 徐夕生, 等, 1989.滇西临沧复式岩基特征研究.云南地质, 8(3-4):189-204. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000003601932

刘德利, 刘继顺, 张彩华, 等, 2008.滇西南澜沧江结合带北段云县花岗岩的地质特征及形成环境.岩石矿物学杂志, 27(1):23-31. doi: 10.3969/j.issn.1000-6524.2008.01.003

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

刘强, 邓玉彪, 向树元, 等, 2017.藏南仲巴地体早奥陶世构造-热事件及其地质意义.地球科学, 42(6):881-890.https://doi.org/dqkx.2017.076 http://earth-science.net/WebPage/Article.aspx?id=3585

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://d.old.wanfangdata.com.cn/Periodical/ysxb98201205014

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

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://d.old.wanfangdata.com.cn/Periodical/zgkx-cd200602002

彭智敏, 耿全如, 王立全, 等, 2014.青藏高原羌塘中部本松错花岗质片麻岩锆石U-Pb年龄、Hf同位素特征及地质意义.科学通报, 59(26):2621-2629. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=KXTB201426014&dbname=CJFD&dbcode=CJFQ

孙载波, 曾文涛, 周坤, 等, 2017.昌宁-孟连结合带奥陶纪洋岛玄武岩的识别及其构造意义——来自地球化学和锆石U-Pb年龄的证据.地质通报, 36(10):1760-1771. doi: 10.3969/j.issn.1671-2552.2017.10.008

王保弟, 王立全, 潘桂棠, 等, 2013.昌宁-孟连结合带南汀河早古生代辉长岩锆石年代学及地质意义.科学通报, 58(4):344-354. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=YNZD1989Z1001&dbname=CJFD&dbcode=CJFQ

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://d.old.wanfangdata.com.cn/Periodical/ysxb98201608006

王海林, 林方成, 丛峰, 等, 2016.云南凤庆漭街淡色花岗岩LA-ICP-MS锆石U-Pb年龄及其地质意义.世界有色金属, (7):59-61. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=COLO201607024&dbname=CJFD&dbcode=CJFQ

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

吴随录, 2010. 三江地区南澜沧江临沧花岗岩的特点、时代及区域构造意义(硕士学位论文). 北京: 中国地质大学.

邢晓婉, 张玉芝, 王岳军, 等, 2015.西盟地区奥陶纪花岗片麻岩的锆石U-Pb年代学、Hf同位素组成特征及其大地构造意义.大地构造与成矿学, 39(3):470-480. http://d.old.wanfangdata.com.cn/Periodical/ddgzyckx201503012

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

曾文涛, 刘桂春, 冯庆来, 等, 2017.临沧地体亲缘性及南段组物源——来自泥盆纪-石炭纪南段组碎屑锆石U-Pb年龄的证据.地质通报, 36(7):1175-1187. doi: 10.3969/j.issn.1671-2552.2017.07.008

张雯华, 秦元季, 王毅, 1991.滇西临沧花岗岩带的成因类型及其物源的讨论.矿物岩石地球化学通讯, 10(4):240-243. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=KYDH199104001&dbname=CJFD&dbcode=CJFQ

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