滇西兰坪皂角场新生代富碱斑岩体锆石U-Pb年代学及岩石地球化学特征

doi:10.13278/j.cnki.jjuese.20190229

Abstract

Abstract: Lanping basin in western Yunnan has attracted wide attention in geological circles because of its large scale resources and great prospecting potential, however,as one of the only three Cenozoic intrusions in the basin, the Zaojiaochang intrusion is rarely reported. To some extent, this not only affects the overall understanding of the basin evolution and metallogenic mechanism, but also is incomplete for the study of alkali-rich porphyry belt in western Yunnan. A study on petrography, zircon U-Pb chronology and elemental geochemistry, shows that the Zaojiaochang intrusion is composed of monzogranite (central facies) and granodiorite porphyry (marginal facies). The LA-ICP-MS zircon U-Pb dating shows that the emplacement age of the Zaojiaochang intrusion is about 34 Ma. The intrusion belongs to high-K calcium-alkali series, with high silicon (w(SiO₂)=71.49%-73.17%), peraluminous (A/CNK=1.12-1.32), and high total alkali (w(K₂O+Na₂O)=7.83%-9.10%). It is rich in LILEs (Rb, Ba, Th, U, K, Hf) and LREEs, relatively depleted of HFSEs (Ta, Nb, Ti and P), with no or weak negative Eu anomalies and special Nb/Ta and Th/U values. Based on the above mentioned data,it is suggested that the magma of the Zaojiaochang intrusion came from deep source, and the parent magmas originated from a metasomatic lithospheric mantle source, and mixed up with crust-source materials later. The comprehensive study shows that the intracontinental subduction of the Tibetan Plateau during the late collision period (40-26 Ma) induced the lateral flow of mantle material,the upwelling of deep asthenosphere, and the forming of the alkali-rich porphyry belt. The Zaojiaochang intrusion was formed in the Late Eocene Lanping basin transformation stage and the mountain intracontinental orogenic extrusion tectonic environment. In the center of the basin, the Lanping-Simao central axis fault with lithospheric fault property reached its peak in this period, and the magma rose along the fault and formed the super hypabyssal alkaline-rich porphyry under a brittle condition near the surface.

Key words: Zaojiaochang instrution, alkaline-rich porphyries, Lanping basin, zircon U-Pb dating, lithogeochemistry, petrogenesis

CLC Number:

P588.1

Li Shoukui, Zhang Shitao, Zhao Qinghong, Li Ming. Zircon U-Pb Chronology and Petrogeochemistry of Cenozoic Alkali-Rich Porphyry in Zaojiaochang, Lanping, Western Yunnan[J].Journal of Jilin University(Earth Science Edition), 2021, 51(1): 169-184.

References

[1] 曾普胜,杨伟光,喻学惠.滇西富碱斑岩带及其与金矿化的关系[J].地球学报,1999,20(增刊):367-372. Zeng Pusheng, Yang Weiguang, Yu Xuehui. Alkali-Rich Porphyry Zone and the Relationship Between the Porphyry and Gold Metallization in the Western Yunnan[J]. Acta Geographica Sinica, 1999, 20(Sup.):367-372.
[2] 曾普胜,莫宣学,喻学惠,等.滇西富碱斑岩带的Nd、Sr、Pb同位素特征及其挤压走滑背景[J].岩石矿物学杂志,2002,21(3):231-241. Zeng Pusheng, Mo Xuanxue, Yu Xuehui, et al. Nd, Sr and Pb Isotopic Characteristics of the Alkaline-Rich Porphyries in Western Yunnan and Its Compression Strike-Slip Setting[J]. Acta Petrologica et Mineralogica, 2002, 21(3):231-241.
[3] 王建,李建平,王江海,等.滇西剑川-大理地区新生代钾玄岩系中深源包体的地质意义[J].矿物学报,2002, 22(2):113-125. Wang Jian, Li Jianping, Wang Jianghai, et al. Geological Implications for the Mafic Enclaves of Deep-Derivation from Cenozoic Shoshonitic Rocks in Jianchuan-Dali Area, Western Yunnan[J]. Acta Mineralogica Sinica, 2002, 22(2):113-125.
[4] 赵欣,莫宣学,喻学惠,等.滇西六合地区新生代正长斑岩中深源包体的矿物学特征与成因意义[J].地学前缘,2003,10(3):93-104. Zhao Xin, Mo Xuanxue, Yu Xuehui, et al. Mineralogical Characteristics and Petrogenesis of Deep-Derived Xenoliths in Cenozoic Syenite-Porphyry in Liuhe, Western Yunnan Province[J]. Earth Science Frontiers, 2003, 10(3):93-104.
[5] 黄小龙,徐义刚,杨启军,等.滇西莴中新生代高镁富钾火山岩中橄榄石斑晶及其尖晶石包裹体的岩浆成因动力学意义[J].岩石学报,2006,22(6):1553-1564. Huang Xiaolong, Xu Yigang, Yang Qijun, et al. Olivine Phenocrysts and Spinel Inclusions in the Wozhong High-Mg and K-Rich Lavas from the Western Yunnan, China:Petrogenesis and Geodynamic Implications[J]. Acta Petrologica Sinica, 2006, 22(6):1553-1564.
[6] 黄小龙,徐义刚,杨启军,等.滇西莴中晚始新世高镁富钾火山岩中单斜辉石斑晶环带结构的成因:岩浆补给-混合过程[J].高校地质学报,2007,13(2):250-260. Huang Xiaolong, Xu Yigang, Yang Qijun, et al. Genesis of Compositional Zoning of Clinopyroxene Phenocrysts in the Wozhong Late Eocene High-Mg Ultrapotassic Lavas, Western Yunnan,China:Magma Replenishment-Mixing Process[J]. Geological Journal of China Universities, 2007, 13(2):250-260.
[7] 喻学惠,莫宣学,曾普胜,等.云南马关地区新生代碧玄岩中地幔包体研究[J].岩石学报,2006,22(3):621-630. Yu Xuehui, Mo Xuanxue, Zeng Pusheng, et al. A Study on the Mantle Xenoliths in the Cenozoic Volcanic Rocks from Maguan Area, Yunnan Province[J]. Acta Petrologica Sinica, 2006, 22(3):621-630.
[8] 张玉泉,谢应雯.哀牢山-金沙江富碱侵入岩年代学和Nd, Sr同位素特征[J].中国科学:D辑,1997,27(4):289-293. Zhang Yuquan, Xie Yingwen. Geochronology of Ailaoshan-Jinshajiang Alkali-Rich Intrusive Rocks and Their Sr and Nd Isotopic Characteristics[J]. Science in China:Series D, 1997, 27(4):289-293.
[9] Chung S L, Lee T Y, Lo C H, et al. Intraplate Extension Prior to Continental Extrusion Along the Ailao Shan-Red River Shear Zone[J]. Geology, 1997, 25(4):311-314.
[10] Chung S L, Lo C H, Lee T Y, et a1. Diachronous Uplift of the Tibetan Plateau Starting 40 Myr Ago[J]. Nature, 1998, 394:769-773.
[11] 王江海,尹安,Harrison T M,等.青藏东缘新生代两类高钾岩浆活动的热年代学研究[J].中国科学:D辑,2002,32(7):529-537. Wang Jianghai, Yin An, Harrison T M, et al. A Thermal Chronology Studies of Two Types Cenozoic High-Potassic Magmatism in Eastern Margin of Tibetan Plateau[J]. Science in China:Series D, 2002, 32(7):529-537.
[12] 董方浏,莫宣学,侯增谦,等.云南兰坪盆地喜马拉雅期碱性岩⁴⁰Ar/³⁹Ar年龄及地质意义[J].岩石矿物学杂志,2005,24(2):103-109. Dong Fangliu, Mo Xuanxue, Hou Zengqian, et al.⁴⁰Ar/³⁹Ar Ages of Himalayan Alkaline Rocks in Lanping Basin, Yunnan Province, and Their Geological Implications[J]. Acta Petrologica et Mineralogica, 2005, 24(2):103-109.
[13] 黄行凯,莫宣学,喻学惠,等.云南马关地区岩石圈地幔组成和年龄:地幔橄榄岩包体的Re-Os同位素限制[J].岩石学报,2011,27(9):2646-2654. Huang Xingkai, Mo Xuanxue, Yu Xuehui, et al. The Composition and Age of Subcontinental Lithospheric Mantle Beneath Maguan,Yunnan Province:Constraints from Re-Os Isotopes of Mantle-Derived Peridotitic Xenoliths[J]. Acta Petrologica Sinica, 2011, 27(9):2646-2654.
[14] 李勇,莫宣学,喻学惠,等.金沙江-哀牢山断裂带几个富碱斑岩体的锆石U-Pb定年及地质意义[J].现代地质,2011,25(2):189-200. Li Yong, Mo Xuanxue, Yu Xuehui, et al. Zircon U-Pb Dating of Several Selected Alkali-Rich Porphyries from the Jinshajiang-Ailaoshan Fault Zone and Geological Significance[J]. Geoscience, 2011, 25(2):189-200.
[15] 刘金宇,邓军,李龚健,等.滇西兰坪盆地莲花山岩体成因与构造意义:岩石地球化学、锆石U-Pb年代学及Hf同位素约束[J].岩石学报,2017,33(7):2115-2128. Liu Jinyu, Deng Jun, Li Gongjian,et al. Petrogenesis and Tectonic Significance of the Lianhuashan Intrusion in the Lanping Basin, Western Yunnan:Constraints from Bulk Element Composition, Zircon U-Pb Geochronology and Hf Isotopic Compositions[J]. Acta Petrologica Sinica, 2017, 33(7):2115-2128.
[16] 龙天祥,何小虎,刘飞,等.长安金矿区碱性岩锆石U-Pb年代学、微量元素、Hf同位素特征及其地质意义[J].吉林大学学报(地球科学版),2019,49(6):1607-1627. Long Tianxiang, He Xiaohu, Liu Fei,et al. Zircon U-Pb Geochronology, Trace Element, Hf Isotope of Alkaline Rocks from Chang'an Gold Deposit and Its Geological Implication[J]. Journal of Jilin University (Earth Science Edition), 2019, 49(6):1607-1627.
[17] 朱炳泉,张玉泉,谢应雯.滇西洱海东第三纪超K质火成岩系的Nd-Sr-Pb同位素特征与西南大陆地幔演化[J].地球化学,1992(3):201-212. Zhu Bingquan, Zhang Yuquan, Xie Yingwen. Nd, Sr and Pb Isotopic Characteristics of Cenozic Ultra-Potassic Volcanic Rocks from Eastern Erhai, Yunnan and Their Implications for Subcontinent-Mantle Evolution in Southwestern China[J]. Geochimica, 1992(3):201-212.
[18] 谢应雯,张玉泉,胡国相.哀牢山-金沙江富碱侵入岩带地球化学与成矿专属性初步研究[J].昆明工学院院报,1984(4):1-17. Xie Yingwen, Zhang Yuquan, Hu Guoxiang. A Preliminary Study on Geochemical Characteristics and Mineralization Specificity of Alkalirich Intrusive Belt in Ailaoshan-Jinshajiang[J]. Journal of Kunming Institute of Technology, 1984(4):1-17.
[19] 谢应雯,张玉泉.云南洱海东部新生代岩浆岩岩石化学[J].岩石学报,1995,11(4):423-433. Xie Yingwen, Zhang Yuquan. Petrochemistry of the Cenozoic Magmatic Rocks in the Eastern Erhai, Yunnan Province[J]. Acta Petrologica Sinica, 1995, 11(4):423-433.
[20] 张玉泉,谢应雯,李献华,等.青藏高原东部钾玄岩系岩浆岩同位素特征:岩石成因及其构造意义[J].中国科学:D辑,2000,30(5):493-498. Zhang Yuquan, Xie Yingwen, Li Xianhua, et al. Isotope Features of Magmatic Rocks of the Shoshonitic Series in the Eastern Qinghai-Tibetan Plateau:Origin of the Rocks and Their Tectonic Significance[J]. Science in China:Series D, 2000, 30(5):493-498.
[21] 李献华,周汉文,韦刚健,等.滇西新生代超钾质煌斑岩的元素和Sr-Nd同位素特征及其对岩石圈地幔组成的制约[J].地球化学,2002,31(1):26-34. Li Xianhua, Zhou Hanwen, Wei Gangjian, et al. Geochemistry and Sr-Nd Isotopes of Cenozoic Ultrapotassic Lamprophyres in Western Yunnan:Constraints on the Composition of Sub-Continental Lithospheric Mantle[J]. Geochimica, 2002, 31(1):26-34.
[22] 董方浏,莫宣学,喻学惠,等.云南永平卓潘新生代碱性杂岩体的元素地球化学和Nd-Sr-Pb同位素特征及地质意义[J].岩石学报,2007,23(5):986-994. Dong Fangliu, Mo Xuanxue,Yu Xuehui, et al. Trace Elements Geochemical and Nd-Sr-Pb Isotopes Characteristics of the Zhuopan Alkaline Complex in Yongping, Yunnan Province and Its Geological Significance[J]. Acta Petrologica Sinica, 2007, 23(5):986-994.
[23] 黄小龙,徐义刚,杨启军,等.滇西晚始新世高镁富钾火山岩的地球化学特征及其岩石成因机制探讨[J].地球化学,2007,36(2):120-138. Huang Xiaolong, Xu Yigang, Yang Qijun, et al. Geochemistry of Late Eocene High-Mg Ultrapotassic Lavas from Western Yunnan, China:Constraints on Petrogenesis[J]. Geochimica, 2007, 36(2):120-138.
[24] Huang X L, Niu Y L, Xu Y G, et al. Mineralogical and Geochemical Constraints on the Petrogensis of Post-Collisional Potassic and Ultrapotassic Rocks from Western Yunnan China[J]. Journal of Petrology, 2010, 51(8):1617-1654.
[25] 李勇,莫宣学,喻学惠,等.滇西"三江"地区高镁钾质火山岩地球化学特征及其地质意义[J].岩石学报,2011,27(9):2510-2518. Li Yong, Mo Xuanxue, Yu Xuehui, et al. Geochemical and Geological Significance of the High-Mg Potassic Volcanic Rocks in Sanjiang Area,Western Yunnan[J]. Acta Petrologica Sinica, 2011, 27(9):2510-2518.
[26] 丁慧霞,侯青叶,曹铁宁,等.滇西银厂坪花岗斑岩岩体的地球化学及年代学特征[J].地学前缘,2012,19(3):240-251. Ding Huixia, Hou Qingye, Cao Tiening, et al. Geochronology, Geochemistry and Geological Significance of Yinchangping Granite Porphyry, Yunnan Province[J]. Earth Science Frontiers, 2012, 19(3):240-251.
[27] Lu Y J, Kerrich R, McCuaig T C, et al. Geochemical, Sr-Nd-Pb and Zircon Hf-O Isotopic Compositions of Eocene-Oligocene Shoshonitic and Potassic Adakite-Like Felsic Intrusions in Western Yunnan, SW China:Petrogenesis and Tectonic Implications[J]. Journal of Petrology, 2013, 54:1309-1348.
[28] 陈喜峰,曾普胜,张雪亭,等.云南永平卓潘碱性杂岩体岩石学和地球化学特征及成因研究[J].岩石学报,2015,31(9):2597-2608. Chen Xifeng, Zeng Pusheng, Zhang Xueting, et al. Petrologyand Geochemistry of the Zhuopan Alkaline Complex in Yongping,Yunnan Province:Constraints on Petrogenesis and Tectonic Setting[J]. Acta Petrologica Sinica, 2015, 31(9):2597-2608.
[29] 张玉泉,谢应雯,涂光炽.哀牢山-金沙江富碱侵入岩及其与裂谷构造关系初步研究[J].岩石学报,1987,3(1):17-25. Zhang Yuquan, Xie Yingwen, Tu Guangchi. Preliminary Study on Ailaoshan-Jinshajiang Alkali-Rich Intrusive Rocks and Their Relationship with Rift Structure[J]. Acta Petrologica Sinica, 1987, 3(1):17-25.
[30] 邓万明,钟大赉.壳-幔过渡带及其在岩石圈构造演化中的地质意义[J].科学通报,1997,42(23):2472-2482. Deng Wanming, Zhong Dalai. Crust-Mantle Transitional Zone and Its Geological Significance in Tectonic Evolution of Lithosphere[J]. Chinese Science Bulletin, 1997, 42(23):2472-2482.
[31] Wang J H,Yin A,Harrison T M, et al. A Tectonic Model for Cenozoic Igneous Activities in the Eastern Indo-Asian Collision Zone[J]. Earth and Planetary Science Letters, 2001, 188:123-133.
[32] 夏萍,徐义刚.滇西岩石圈地幔域分区和富集机制:新生代两类超钾质火山岩的对比研究[J].中国科学:D辑,2004,34(12):1118-1128. Xia Ping, Xu Yigang. Mantle Zoning and Enrichment Mechanism of Lithosphere in Western Yunnan:A Comparative Study of Two Types of Superpotassic Volcanic Rocks in Cenozoic Ara[J]. Science in China:Series D, 2004, 34(12):1118-1128.
[33] Guo Z, Wilson M, Liu J,et a1. Post-Collisional, Potassic and Ultrapotassic Magmatism of the Northern Tibetan Plateau:Constraints on Characteristics of the Mantle Source, Geodynamic Setting and Uplift Mechanisms[J]. Journal of Petrology, 2006, 47(6):1177-1220.
[34] 杜斌.云南大莲花山和卓潘岩体岩浆源区及形成机制[D].北京:中国地质大学(北京),2017. Du Bin. Magma Source, Formation Mechanism and Tectonic Significance of the Dalianhuashan and Zhuopan Plutons, Yunan Province[D]. Beijing:China University of Geosciences (Beijing), 2017.
[35] 杜斌,王长明,杨立飞,等.西南三江永平卓潘碱性杂岩体源区与形成机制:全岩元素、锆石U-Pb年代学和Hf同位素联合约束[J].岩石学报,2018,34(5):1376-1396. Du Bin, Wang Changming, Yang Lifei, et al. Magma Source and Formation Mechanism of the Zhuopan Alkaline Complex in Yongping,Southwest China:Constraints from Geochemistry, Zircon U-Pb Geochronology and Hf Isotopes[J]. Acta Petrologica Sinica, 2018, 34(5):1376-1396.
[36] 侯增谦,王二七.印度-亚洲大陆碰撞成矿作用主要研究进展[J].地球学报,2008,29(3):275-292. Hou Zengqian, Wang Erqi. Metallogenesis of the Indo-Asian Collisional Orogen:New Advances[J]. Acta Geoscientica Sinica, 2008, 29(3):275-292.
[37] 刘显凡,战新志,高振敏,等.云南六合深源包体与富碱斑岩成岩成矿的关系[J].中国科学:D辑,1999,29(5):413-421. Liu Xianfan, Zhan Xinzhi, Gao Zhenmin, et al. Deep Xenoliths in Alkalic Porphyry,Liuhe, Yunnan, and Implications to Petrogenesis of Alkalic Porphyry and Associated Mineralizations[J]. Science in China:Series D, 1999, 29(5):413-421.
[38] 刘显凡,肖继雄,楚亚婷,等.滇西马厂箐多金属矿床系列成矿的深部过程与壳幔混染成因机制[J].矿物学报,2011,31(增刊):498-500. Liu Xianfan, Xiao Jixiong, Chu Yating, et al. Genesis Mechanism of Deep Processes and Crust-Mantle Contamination of Machangqing Polymetallic Deposit Series in West Yunnan[J]. Acta Mineralogica Sinica, 2011, 31(Sup.):498-500.
[39] 王强,许继峰,赵振华,等.中国埃达克岩或埃达克质岩及相关金属成矿作用[J].矿物岩石地球化学通报,2007,26(4):336-349. Wang Qiang, Xu Jifeng, Zhao Zhenhua, et al. Adakites or Adakitic Rocks and Associated Metal Metallogenesis in China[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2007, 26(4):336-349.
[40] 和文言,莫宣学,喻学惠,等.滇西马厂箐斑岩型铜钼(金)矿床成岩成矿时代研究[J].地学前缘,2011,18(1):207-215. He Wenyan, Mo Xuanxue, Yu Xuehui, et al. Geochronological Study of Magmatic Intrusions and Mineralization of Machangqing Porphyry Cu-Mo-Au Deposit, Western Yunnan Province[J]. Earth Science Frontiers, 2011, 18(1):207-215.
[41] 麻菁.滇西卓潘碱性杂岩基本特征及其构造与资源意义[D].北京:中国地质大学(北京),2016. Ma Jing. The Basic Characteristics of the Zhuopan Alkaline Complex in West Yunnan, SW China, and Its Significances on Tectonics and Resuorces[D]. Beijing:China University of Geosciences (Beijing), 2016.
[42] Lu Y J, Kerrich R, Kemp A I S, et al. Intracontinental Eocene-Oligocene Porphyry Cu Mineral Systems of Yunnan, Western Yangtze Craton, China:Compositional Characteristics, Sources, and Implications for Continental Collision Metallogeny[J]. Economic Geology, 2013, 108:1541-1576.
[43] Wang C M, Bagas L, Lu Y J, et al. Terrane Boundary and Spatio-Temporal Distribution of Ore Deposits in the Sanjiang Tethyan Orogen:Insights from Zircon Hf-Isotopic Mapping[J]. Earth Science Reviews, 2016, 156:39-65.
[44] Deng J, Wang Q F, Li G J, et al. Cenozoic Tectono-Magmatic and Metallogenic Processes in the Sanjiang Region, Southwestern China[J]. Earth Science Reviews, 2014, 138:268-299.
[45] 莫宣学,赵志丹,喻学惠,等.青藏高原新生代碰撞-后碰撞火成岩[M].北京:地质出版社,2009:1-396. Mo Xuanxue, Zhao Zhidan, Yu Xuehui, et al. Cenozoic Collision and Post-Collision Igneous of Tibet Plateau[M]. Beijing:Geological Publishing House, 2009:1-396.
[46] 邓万明,黄萱,钟大赉.滇西金沙江带北段的富碱斑岩及其与板内变形的关系[J].中国科学:D辑,1998,28(2):111-117. Deng Wanming, Huang Xuan, Zhong Dalai. Alkali-Rich Porphyry and Its Relation with Intraplate Deformation of North Part of Jinsha River Belt in Western Yunnan, China[J]. Science in China:Series D, 1998, 28(2):111-117.
[47] 葛良胜,邹依林,邢俊兵,等.滇西北与喜马拉雅期富碱斑岩有关的金矿成矿系统[J].黄金地质,2004,10(1):39-47. Ge Liangsheng, Zou Yilin, Xing Junbing, et al. Gold Mineralization System Related to Alkali-Rich Porphyries in Himalayan, the Northwestern Part of Yunnan[J]. Gold Geology, 2004, 10(1):39-47.
[48] 薛传东,侯增谦,刘星,等.滇西北北衙金多金属矿田的成岩成矿作用:对印-亚碰撞造山过程的响应[J].岩石学报,2008,24(3):457-472. Xue Chuandong, Hou Zengqian, Liu Xing, et al. Petrogenesis and Metallogenesis of the Beiya Gold-Polymetallic Ore District,Northwestern Yunnan Province, China:Responses to the Indo-Asian Collisional Processes[J]. Acta Petrologica Sinica, 2008, 24(3):457-472.
[49] 李兴振,刘文均,王义昭,等.西南三江地区特提斯构造演化与成矿:总论[M].北京:地质出版社,1999:230-232. Li Xingzhen, Liu Wenjun, Wang Yizhao, et al. Tectonic Evolution of the Tethys and Mineralization in the Sanjiang Region, SW China:A General Introduction[M]. Beijing:Geological Publishing House, 1999:230-232.
[50] 王立全,李定谋,潘桂棠,等.青藏高原矿产及成矿地质背景图及说明书[M].成都:成都地图出版社,2015:85-91. Wang Liquan, Li Dingmou, Pan Guitang, et al. Mineral and Metallogenic Geological Background Map and Instructions for the Qinghai-Tibet Plateau[M]. Chengdu:Chengdu Cartographic Publishing House, 2015:85-91.
[51] 张治波,朱志军,王文锋,等.滇西兰坪盆地中-新生代蒸发岩元素地球化学特征及其形成环境[J].吉林大学学报(地球科学版),2019,49(2):356-379. Zhang Zhibo, Zhu Zhijun, Wang Wenfeng,et al. Geochemical Characteristics and Formation Environment of Mesozoic and Cenozoic Evaporative Rocks in Lanping Basin, Western Yunnan[J]. Journal of Jilin University (Earth Science Edition), 2019, 49(2):356-379.
[52] 李兴振,杜德勋,王义昭.盆山转换及其成矿作用:以昌都-思茅盆地和金沙江-哀牢山带为例[J].特提斯地质,1998,22:1-16. Li Xingzhen, Du Dexun, Wang Yizhao. The Basin-Range Transition and Mineralization Examples from the Qamdo-Simao Basin and Jinshakoamg-Ailao Orogenic Belt in Southwestern China[J]. Tethyan Geology, 1998, 22:1-16.
[53] 牟传龙,王建,余谦,等.兰坪中新生代沉积盆地演化[J].矿物岩石,1999,19(3):30-36. Mou Chuanlong, Wang Jian, Yu Qian, et al. The Evolution of the Sedimentary Basin in Lanping Area During Mesozoic-Cenozoic[J]. Journal of Mineralogy and Petrology, 1999, 19(3):30-36.
[54] 罗君烈,杨友华,赵准,等.滇西特提斯的演化及主要金属矿床的成矿作用[M].北京:地质出版社,1994:149-239. Luo Junlie, Yang Youhua, Zhao Zhun, et al. Evolution of the Tethys in Western Yunnan and Mineralization for Main Metal Deposits[M]. Beijing:Geological Publishing House, 1994:149-239.
[55] Liu Y S, Hu Z C, Zong K Q, et al. Reappraisement and Refinement of Zircon U-Pb Isotope and Trace Element Analyses by LA-ICP-MS[J]. Chinese Science Bulletin, 2010, 55(15):1535-1546.
[56] Hu Z C, Liu Y S, Chen L, et al. Contrasting Matrix Induced Elemental Fractionation in NIST SRM and Rock Glasses During Laser Ablation ICP-MS Analysis at High Spatial Resolution[J]. Journal of Analytical Atomic Spectrometry, 2011,26(2):425-430.
[57] Liu Y S, Gao S, Hu Z C, et al. Continental and Oceanic Crust Recycling-Induced Melt-Peridotite Interactions in the Trans-North China Orogen:U-Pb Dating, Hf Isotopes and Trace Elements in Zircons from Mantle Xenoliths[J]. Journal of Petrology,2010, 51(1/2):537-571.
[58] Hoskin P W O,Black L P. Metamorphic Zircon Formation by Solid-State Recrystallization of Protolith Igneous Zircon[J]. Journal of Metamorphic Geology, 2000, 18(4):423-439.
[59] Corfu F, Hanchar J M, Hoskin P, et al. Atlas of Zircon Textures[J]. Reviews in Mineralogy and Geochemistry, 2003, 53(1):469.
[60] 吴元保,郑永飞.锆石成因矿物学研究及其对U-Pb年龄解释的制约[J].科学通报,2004,49(16):1589-1604. Wu Yuanbao, Zheng Yongfei. Genesis of Zircon and Its Constraints on Interpretation of U-Pb Age[J]. Chinese Science Bulletin, 2004, 49(16):1589-1604.
[61] Middlemost E A K. Naming Materials in the Magma/Igneous Rock System[J]. Earth-Science Reviews, 1994, 37(3/4):215-224.
[62] Irvine T N J, Baragar W R A. A Guide to the Chemical Classification of the Common Volcanic Rocks[J]. Canadian Journal of Earth Sciences, 1971, 8(5):523-548.
[63] Streckeisen A L. Classification of the Common Igneous Rocks by Means of Their Chemical Composition:A Provisional Attempt[J]. Neues Jahrbuch fur Mineralogie, Monatshefte, 1976, 1:1-15.
[64] Peccerillo A, Taylor S R. Geochemistry of Eocene Calc-Alkaline Volcanic Rocks from the Kastamonu Area, Northern Turkey[J]. Contributions to Mineralogy and Petrology, 1976, 58(1):63-81.
[65] Taylor S R, Mclennan S M. The Geochemical Evolution of the Continental Crust[J]. Reviews of Geophysics, 1995, 33:241-265.
[66] 徐平,吴福元,谢烈文,等.U-Pb同位素定年标准锆石的Hf同位素[J].科学通报,2004,49(14):1403-1410. Xu Ping, Wu Fuyuan, Xie Liewen, et al. Hf Isotopic Compositions of the Standard Zircons for U-Pb Dating[J]. Chinese Science Bulletin, 2004, 49(14):1403-1410.
[67] Weyer S, Munker C, Rehkamper M, et al. Determination of Ultra-Low Nb, Ta, Zr and Hf Concentrations and the Chondritic Zr/Hf and Nb/Ta Ratios by Isotope Dilution Analyses with Multiple Collector ICP-MS[J]. Chemical Geology, 2002, 187(3):295-313.
[68] Jochum K P, Seufert H M, Spettel B, et al. The Solar-System Abundances of Nb, Ta, and Y, and the Relative Abundances of Refractory Lithophile Elements in Differentiated Planetary Bodies[J]. Geochimica et Cosmochimica Acta, 1986, 50(6):1173-1183.
[69] Green T H. Significance of Nb/Ta As an Indicator of Geochemical Processes in the Crust-Mantle System[J]. Chemical Geology, 1995, 120(3/4):347-359.
[70] Sun S S, McDonou G H. Cheminal and Istopic Systematic of Oceanic Basalts:Implications for Mantle Composition and Processes[M]//Msaunders A D, Norry M J. Mamatism in the Ocean Basin.London:Black-Well Scientific, Geological Society Special Publication, 1989:313-345.
[71] Rudnick R L, Gao S. Composition of the Continental Crust[M]//Rudnick R L.The Crust, Treaties on Geochemistry. Oxford:Elsevier Pergramon, 2003:1-64.
[72] 邱家骧.火山岩成分与板块构造环境[J].地质科技情报, 1983(1):6-16. Qiu Jiaxiang. Volcanic Rock Composition and Plate Tectonic Environment[J]. Geological Science and Technology Information, 1983(1):6-16.
[73] 邱家骧.应用岩浆岩岩石学[M].武汉:中国地质大学出版社,1987:1-418. Qiu Jiaxiang. Applied Magmatic Petrology[M]. Wuhan:China University of Geosciences Press, 1987:1-418.
[74] 潘桂棠,徐强,侯增谦,等.西南三江多岛弧造山过程成矿系统与资源评价[M].北京:地质出版社,2003:54-58. Pan Guitang, Xu Qiang, Hou Zengqian, et al. Mineralization System and Resource Evaluation of Multi-Island Arc Orogenic Process in Sanjiang, Southwest China[M]. Beijing:Geological Publishing House, 2003:54-58.
[75] 张旗.大陆花岗岩的地球动力学意义[J].岩石矿物学杂志,2014,33(4):785-798. Zhang Qi. Geodynamic Implications of Continental Granites[J]. Acta Petrologica et Mineralogica, 2014, 33(4):785-798.
[76] Searle M P, Godin L. The South Tibetan Detachment and the Manaslu Leucogranite:A Structural Reinterpretation and Restoration of the Annapurna-Manaslu Himalaya, Nepal[J]. Journal of Geology, 2003, 111:505-523.
[77] 尹汉辉,范蔚茗,林炯,等.滇西地洼构造与成矿[M].长沙:中南矿业大学出版社,1993:1-137. Yin Hanhui, Fan Yuming, Lin Jiong, et al. Geodepression Structure and Mineralization in Western Yunnan[M]. Changsha:Central South University of Mining and Technology Press, 1993:1-137.

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Zircon U-Pb Chronology and Petrogeochemistry of Cenozoic Alkali-Rich Porphyry in Zaojiaochang, Lanping, Western Yunnan

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