滇西北普上含矿斑岩体的岩石地球化学及蚀变特征研究-岩石矿物学杂志-CSCIED科技核心评价数据库-手机版

滇西北普上含矿斑岩体的岩石地球化学及蚀变特征研究

Petrographic geochemistry and alteration characterization of ore-bearing porphyry bodies in Pushang, Northwest Yunnan, China

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DOI	10.20086/j.cnki.yskw.2024.0601
刊名	岩石矿物学杂志 Acta Petrologica et Mineralogica
年，卷(期)	2024, 43(6)
作者	莫雷，冷成彪*，邢新龙，李凯旋，陈喜连，余海军，王艳军，陈加杰,
作者单位	1. 东华理工大学核资源与环境国家重点实验室, 江西南昌 330013; 2. 东华理工大学地球科学学院, 江西南昌 330013; 3. 江西省地质局第三地质大队, 江西九江 332100; 4. 云南省地质调查院, 云南昆明 650216
摘要	滇西北中甸斑岩铜多金属成矿带是我国重要的铜资源基地,普上为该成矿带新发现的斑岩型铜点,含矿复式岩体主要由石英闪长玢岩和石英二长斑岩组成。为探讨该岩体成因、构造背景、物质迁移过程及成矿潜力等问题,本文对新鲜石英闪长玢岩和蚀变石英闪长玢岩分别开展了岩石化学和蚀变组分特征研究。结果显示,蚀变石英闪长玢岩的SiO₂(61.16%)和K₂O(4.20%)含量较新鲜石英闪长玢岩(分别为58.24%和3.06%)有所升高,而Al₂O₃和Na₂O的含量明显降低,但都具有大离子亲石元素(Rb、Ba、K、Sr)富集、高场强元素(Zr、Nb、Ta、Ti)亏损的特征,且具有较高的Ba/Nb值(分别为75.7和93.2)和较低的Ce/Pb值(分别为3.16和5.70),显示典型弧环境花岗岩的特征。普上新鲜石英闪长玢岩的(La/Sm)_N值较高(平均8.18),无明显的Eu负异常,SiO₂与Rb、Zr/Sm值之间表现出一定的正相关性,表明其经历了角闪石的分离结晶作用; Ba/Rb(＜50)和Nb/La(＜1)值较低,Th/La值(＞0.25)相对较高,Rb/Sr值(0.09)介于上地幔(0.034)与地壳(0.35)之间,表明岩浆源区与俯冲作用有关,岩浆来源为壳幔混源。蚀变石英闪长玢岩中大量迁入的组分包括Fe₂O₃^T、CaO、K₂O、Th、Ta、HREE和Cu、Mo、W、Ag等成矿元素,迁出的组分有Na₂O、MgO、MnO、Sr、Ba、U和LREE等,表明普上蚀变石英闪长玢岩受到了以钾交代为主的碱性蚀变作用的影响,引起矿物蚀变的成矿热液富含Cu、Mo等成矿金属。普上石英闪长玢岩中普遍发育角闪石斑晶且Sr/Y和V/Sc值较高,表明原始岩浆具有富水和高氧逸度的特征; 蚀变岩中绢云母化广泛发育,Cu巨量迁入,在岩石化学组成与金属成矿专属性判别图解中,所有样品均在Cu-Au成矿区域。综合以上特征,认为普上石英闪长玢岩体具有形成Cu-Au矿床的潜力。
Abstract	The Zhongdian porphyry copper polymetallic metallogenic belt in northwestern Yunnan is an important copper resource base in China. Pushang is a newly discovered porphyry copper spot in the metallogenic belt. The ore-bearing composite rock mass is mainly composed of quartz diorite porphyrite and quartz monzonite porphyry. In order to explore the genesis, tectonic setting, material migration process and metallogenic potential of the rock mass, this paper studies the petrochemistry and alteration component characteristics of fresh quartz diorite porphyrite and altered quartz diorite porphyrite respectively. The results show that the contents of SiO₂ (61.16%) and K₂O (4.20%) in the altered quartz diorite porphyrite are higher than those in the fresh quartz diorite porphyrite (58.24% and 3.06%, respectively), while the contents of Al₂O₃ and Na₂O are significantly lower. However, they all have the characteristics of enrichment of large ion lithophile elements (Rb, Ba, K, Sr) and depletion of high field strength elements (Zr, Nb, Ta, Ti), and have higher Ba/Nb values (75.7 and 93.2, respectively) and lower Ce/Pb values (3.16 and 5.70, respectively). It shows the characteristics of granite in typical arc environment. The (La/Sm)_N of the fresh quartz diorite porphyrite is high (average value is 8.18), and there is no obvious negative Eu anomaly. There is a positive correlation between SiO₂ and Rb, Zr/Sm ratios, indicating that it has experienced the fractional crystallization of hornblende. The ratios of Ba/Rb (<50) and Nb/La (<1) are low, the ratio of Th/La (>0.25) is relatively high, and the ratio of Rb/Sr (0.09) is between the upper mantle (0.034) and the crust (0.35), indicating that the magma source area is related to subduction, and the magma source is crust-mantle mixed source. A large number of components in the altered quartz diorite porphyrite include Fe₂O₃^T, CaO, K₂O, Th, Ta, HREE, Cu, Mo, W, Ag and other ore-forming elements, and the migrated components include Na₂O, MgO, MnO, Sr, Ba, U and LREE, indicating that the Pushang altered quartz diorite porphyrite was affected by alkaline alteration dominated by potassium metasomatism, and the ore-forming hydrothermal fluid causing mineral alteration was rich in Cu, Mo and other ore-forming metals. The hornblende phenocrysts with high Sr/Y and V/Sc ratios are widely developed in the quartz diorite porphyrite, indicating that the original magma is characterized by rich water and high oxygen fugacity. Sericitization is widely developed in altered rocks, and Cu migrates in a large amount. All samples are in the Cu-Au mineralized area in the lithochemical composition and metal mineralization exclusivity discrimination illustration. Based on the above characteristics, the Pushang quartz diorite porphyrite has the potential to form Cu-Au deposits.
关键词	普上；石英闪长玢岩；地球化学；热液蚀变；物质迁移
KeyWord	Pushang; quartz diorite porphyrite; geochemistry; hydrothermal alteration; material migration
基金项目
页码	1339-1360

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Ai Jinbiao, Ma Shengming, Zhu Lixin, et al. 2013. Major elements migration regularity and mass change quantification of alteration zones in Matou porphyry Mo-Cu deposit, Anhui Province
[J]. Mineral Depo-sits, 32(6): 1 262~1 274 (in Chinese with English abstract). Blevin P L. 2004. Redox and compositional parameters for interpreting the granitoid metallogeny of Eastern Australia: Implications for gold-rich ore systems
[J]. Resource Geology, 54(3): 241~252. Brauhart W C, Huston L D and Groves I D. 2001. Geochemical mass-transfer patterns as indicators of the architecture of a complete volcanic-hosted massive sulfide hydrothermal alteration system, Panorama District, Pilbara, Western Australia
[J]. Economic Geology and the Bulletin of the Society of Economic Geologists, 96(5): 1 263~1 278. Cao Dianhua, Wang Anjian, Huang Yufeng, et al. 2009. SHRIMP geochronology and Hf isotope composition of zircons from Xuejiping porphyry copper deposit, Yunnan Province
[J]. Acta Geologica Sinica, 83(10): 1 430~1 435 (in Chinese with English abstract). Cao K, Yang Z M, Hou Z Q, et al. 2021. Contrasting porphyry Cu fertilities in the Yidun arc, eastern Tibet: Insights from zircon and apatite compositions and implications for exploration
[J]. Society of Economic Geologists, Inc (SEG Special Publications), 24(2): 231~255. Cao K, Yang Z M, Mavrogenes J, et al. 2019. Geology and genesis of the giant Pulang porphyry Cu-Au district, Yunnan, Southwest China
[J]. Economic Geology, 114(2): 275~301. Cao Kang, Xu Jifeng, Chen Jianlian, et al. 2014. Origin of porphyry intrusions hosting superlarge Pulang porphyry copper deposit in Yunnan Province: Implications for metallogenesis
[J]. Mineral Deposits, 33(2): 307~322 (in Chinese with English abstract). Castillo P R, Janney P E and Solidum R U. 1999. Petrology and geo chemistry of Camiguin Island, southern Philippines: Insights to the source of adakites and other lavas in a complex arc setting
[J]. Con-tributions to Mineralogy and Petrology, 134(1): 33~51. Chen Bin, He Jingbo, Chen Changjian, et al. 2013. Nd-Sr-Os isotopic data of the Baishiquan mafic-ultramafic complex from east Tianshan, and implications for petrogenesis
[J]. Acta Petrologica Sinica, 29(6): 294~302 (in Chinese with English abstract). Chen X L, Leng C B, Zou S H, et al. 2021. Geochemical compositions of apatites from the Xuejiping and Disuga porphyries in Zhongdian arc: Implications for porphyry Cu mineralization
[J]. Ore Geology Reviews, 130: 103 954. Defant M J and Drummond M S. 1990. Derivation of some morden arc magmas by of young subducted lithosphere
[J]. Nature, 347: 662~665. 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
[J]. Gondwana Research, 26: 419~437. Deng Jun, Yang Liqiang, Wang Changming, et al. 2011. Research advances of superimposed orogenesis and metallogenesis in the Sanjiang Tethys
[J]. Acta Petrologica Sinica, 27(9): 2 501~2 509 (in Chinese with English abstract). Dong Tao, Jiang Xiaojun, Li Chao, et al. 2021. Geochronological and geochemical characteristics of the Pushang ore-bearing porphyry in the Zhongdian area of the northwestern Yunnan and its geological significances
[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 40(4): 871~888 (in Chinese with English abstract). Dong Tao, Yu Haijun, Duan Zhaoyan, et al. 2020. Geochronology, geochemistry, and zircon Hf isotope characteristics and their geological significances of the Gaijixia ore-bearing intrusive rocks in the Shangri-La region, NW Yunnan, SW China
[J]. Acta Petrologica Sinica, 36(5): 1 369~1 388 (in Chinese with English abstract). Drummond M S and Defant M J. 1990. A model for trondhjemite-tonalite-dacite genesis and crustal growth via slab melting: Archean to modern comparisons
[J]. Journal of Geophysical Research, 95(B13): 21 503~21 521. Du Zezhong, Cheng Zhizhong, Yao Xiaofeng, et al. 2020. Element migration regularity during hydrothermal alteration in the Xiejiagou gold deposit, Eastern Shandong Province
[J]. Geological Bulletin of China, 39(8): 1 137~1 152 (in Chinese with English abstract). Fan Yuhua and Li Wenchang. 2006. Geological characteristics of the Pulang porphyry copper deposit, Yunnan
[J]. Geology in China, 33(2): 352~362 (in Chinese with English abstract). Grant J A. 1986. The isocon diagram—A simple solution to Gresens’equation for metasomatic alteration
[J]. Economic Geology, 81(8): 1 976~1 982. Grant J A. 2005. Isocon analysis: A brief review of the method and applications
[J]. Physics and Chemistry of the Earth, 30(17~18): 997~1 004. Gresens R L. 1967. Composition-volume relationships of metasomatism
[J]. Chemical Geology, 2: 47~65. Guo Shun,Ye Kai,Chen Yi,et al. 2013. Introduction of mass-balance calculation method for component transfer during the opening of a geological system
[J]. Acta Petrologica Sinica, 29(5): 1 486~1 498 (in Chinese with English abstract). Hezarkhani A, Williams-Jones A E and Gammons C H. 1999. Factors controlling copper solubility and chalcopyrite deposition in the Sungun porphyry copper deposit, Iran
[J]. Mineralium Deposita, 34 (8): 770~783. Hou Zengqian, Qu Xiaoming, Zhou Jirong, et al. 2001. Collision-orogenic processes of the Yidun arc in the Sanjiang region: Record of granites
[J]. Acta Geologica Sinica, 75(4): 484~497 (in Chinese with English abstract). Hou Z Q, Yang Z M, Qu X M, et al. 2009. The Miocene Gangdese porphyry copper belt generated during post-collisional extension in the Tibetan Orogen
[J]. Ore Geology Reviews, 36(1~3): 25~51. Hou Zengqian and Wang Tao. 2018. Isotopic mapping and deep material probing (Ⅱ): Imaging crustal architecture and its control on mineral systems
[J]. Earth Science Frontiers, 25(6): 20~41 (in Chinese with English abstract). Hou Zengqian, Yang Yueqing, Qu Xiaoming, et al. 2004. Tectonic evolution and mineralization systems of the Yidun arc orogen in Sanjiang region, China
[J]. Acta Geologica Sinica, 78 (1): 109~120 (in Chinese with English abstract). Huang Zhilong and Wang Liankui. 1997. The Regularity of element activity during the alteration and mineralization of lamprophyres in the Laowangzhai gold deposit, Yunnan province
[J]. Acta Petrologica et Mineralogica, 16(1): 11~22 (in Chinese with English abstract). Kelley K A and Cottrell E. 2009. Water and the oxidation state of subduc tion zone magmas
[J]. Science, 325(5 940): 605~607. Leng Chengbiao. 2017. Genesis of Hongshan Cu polymetallic large deposit in the Zhongdian area, NW Yunnan: Constraints from LA-ICPMS trace elements of pyrite and pyrrhotite
[J]. Earth Science Frontiers, 24(6): 162~175 (in Chinese with English abstract). Leng Chengbiao, Chen Xilian, Zhang Jingjing, et al. 2020. Lithogeochemical and mineral chemical footprints of porphyry Cu±Mo±Au deposits: A review
[J]. Acta Geologica Sinica, 94(11): 3 189~3 212 (in Chinese with English abstract). Leng C B, Cooke D R, Hou Z Q, et al. 2018a. Quantifying exhumation at the giant Pulang porphyry Cu-Au deposit using U-Pb-He dating
[J]. Economic Geology, 113(5): 1 077~1 092. Leng C B, Gao J F, Chen W T, et al. 2018b. Platinum-group elements, zircon Hf-O isotopes, and mineralogical constraints on magmatic evolution of the Pulang porphyry Cu-Au system, SW China
[J]. Gondwana Research, 62: 163~177. Leng C B, Wang D Z, Yu H J, et al. 2023. Mapping hydrothermal alteration zones with short wavelength infrared (SWIR) spectra and magnetic susceptibility at the Pulang porphyry Cu-Au deposit, Yunnan, SW China
[J]. Mineralium Deposita, 59: 699~716. Leng C B, Zhang X C, Hu R Z, et al. 2012. Zircon U-Pb and molybdenite Re-Os geochronology and Sr-Nd-Pb-Hf isotopic constraints on the genesis of the Xuejiping porphyry copper deposit in Zhongdian, Northwest Yunnan, China
[J]. Journal of Asian Earth Sciences, 60: 31~48. Leng Chengbiao, Zhang Xingchun, Wang Shouxu, et al. 2007. Geochemical characteristics of porphyry copper deposits in the Zhongdian area, Yunnan as exemplified by the Xuejiping and Pulang porphyry copper deposits
[J]. Acta Mineralogica Sinica, 27(3~4): 414~422 (in Chinese with English abstract). Leng Chengbiao, Zhang Xingchun, Wang Shouxu, et al. 2008. Sulfur and lead isotope compositions of the Xuejiping porphyry copper deposit in northwest Yunnan, China: Tracing for the source of metals
[J]. Journal of Mineralogy and Petrology, 28(4): 80~88 (in Chinese with English abstract). Li C and Ripley E M. 2009. Sulfur contents at sulfide-liquid or anhydrite saturation in silicate melts: Empirical equations and example applications
[J]. Economic Geology, 104(3): 405~412. Li Jiankang, Li Wenchang, Wang Denghong, et al. 2007. Re-Os dating for ore-forming event in the late of Yanshan Epoch and research of ore-forming regularity in Zhongdian Arc
[J]. Acta Petrologica Sinica, 23(10): 2 415~2 422 (in Chinese with English abstract). Li Jianping, Chen Huayong, Su Long, et al. 2019. Experimental study of high to intermediate temperature alteration in porphyry copper systems and geological implications
[J]. Science China Earth Sciences, 62: 550~570 (in Chinese with English abstract). Li Kaixuan, Liang Huangying, Huang Wenting, et al. 2019. Highly oxidized characteristics of Tongchanggou porphyry associated with skarn-porphyry Mo-Cu mineralization and key factors controlling the elemental association of porphyry deposits in northwestern Yunnan Province
[J]. Geochimica, 48(2): 101~113 (in Chinese with English abstract). Li Shoukui, Chen Jianhang, Liu Xuelong, et al. 2023. The law of ore-forming hydrothermal alteration and element transfer enrichment in the Tongchanggou porphyry Mo-Cu deposit in Shangri-La, Northwest Yunnan
[J]. Geology in China, 50(6): 1 745~1 763 (in Chinese with English abstract). Li W C, Yu H J, Gao X, et al. 2017. Review of mesozoic multiple magmatism and porphyry Cu-Mo(W) mineralization in the Yidun Arc, eastern Tibet Plateau
[J]. Ore Geology Reviews, 90: 795~812. Li W C, Zeng P S, Hou Z Q, et al. 2011. The Pulang porphyry copper deposit and associated felsic intrusions in Yunnan province, southwest China
[J]. Economic Geology, 106(1): 79~92. Li Wenchang, Liu Xuelong, Zeng Pusheng, et al. 2011. The characteristics of metallogenic rocks in the Pulang porphyry copper deposit of Yunnan Province
[J]. Geology in China, 38(2): 403~414 (in Chinese with English abstract). Li Wenchang, Yu Haijun and Yin Guanghou. 2013. Porphyry metallogenic system of Geza arc in the Sanjiang region,southwestern China
[J]. Acta Petrologica Sinica, 29(4): 1 129~1 144 (in Chinese with English abstract). Li Wenchang and Zeng Pusheng. 2007. Characteristics and metallogenic model of the Pulang superlarge porphyry copper deposit in Yunnan, China
[J]. Journal of Chengdu University of Technology (Science & Technology Edition), 34(4): 436~446 (in Chinese with English abstract). Li Xuefeng. 2016. Geochemistry and Ore-bearing Potential Research of the Indo-porphyries in Zhongdian Arc, SN Yunnan
[D]. Beijing: China University of Geosciences (Beijing), 1~95 (in Chinese with English abstract). Li X F, Dong G C, He W Y, et al. 2014. Geochronology and geochemistry of the porphyries in Xuejiping deposit in northwestern Yunnan: Petrogenesis and implication for mineralization
[J]. Acta Geologica Sinica~English Edition, 88(S2): 563~564. Lin Zhenwen, Liang Zhipeng, Zhuang Wenming, et al. 2023. Characteristics of wall-rock alteration and element migration of the Yuanzhuding porphyry Cu-Mo deposit, Guangdong Province, China
[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 42(2): 325~339 (in Chinese with English abstract). Liu Xuelong, Li Wenchang, Yin Guanghouy, et al. 2013. The geochronology, mineralogy and geochemistry study of the Pulang porphyry copper deposits in Geza arc of Yunnan Province
[J]. Acta Petrologica Sinica, 29(9): 3 049~3 064 (in Chinese with English abstract). Liu Xuelong, Li Wenchang, Zhang Na, et al. 2014. Geochronological, geochemical characteristics of Disuga ore-forming I-type granitic porphyries in the Geza arc, Yunnan Province, and their geological significance
[J]. Geological Review, 60(1): 103~114 (in Chinese with English abstract). Liu Xuelong, Yang Fucheng, Zhang Changzhen, et al. 2018. Structural characteristics and mineralization of Xuejiping porphyry copper deposit in Northwest Yunnan
[J]. Gold Science and Technology, 26(4): 473~480 (in Chinese with English abstract). Loucks R R. 2014. Distinctive composition of copper-ore-forming arcmagmas
[J]. Australian Journal of Earth Sciences, 61 (1): 5~16. Maclean W H. 1990. Mass change calculations in altered rock series
[J]. Mineralium Deposita, 25: 44~49. Meng Xiangjin, Hou Zengqian, Gao Yongfeng, et al. 2004. The alteration zoning model of porphyry coppey deposit in collisional orogeny: Case studies of porphyry coppey deposits in gangdise belt, Xizang(Tibet)
[J]. Earth Science Frontiers, 11(1): 201~214 (in Chinese with English abstract). Mo Lei, Leng Chengbiao, Chen Xilian, et al. 2024a. Zircon trace elements and Hf-O isotopes of porphyries in the Zhongdian area of Yunnan Province and their implications for petrogenesis and mineralization
[J]. Acta Petrologica Sinica, 40(4): 1 163~1 184 (in Chinese with English abstract). Mo Lei, Shen Qiwu, Chen Xilian, et al. 2024b. Petrogeochemistry, chronology, Sr-Nd-Pb isotopic compositions, and geological significance of the ore-causative intrusion in the Langdu skarn deposit, northwest Yunnan
[J]. Sedimentary Geology and Tethyan Geology, 44(2): 421~436 (in Chinese with English abstract). Mungall J E. 2002. Roasting the mantle: Slab melting and the genesis of major Au and Au-rich Cu deposits
[J]. Geology, 30(10): 915~918. Pang Zhenshan, Du Yangsong, Wang Gongwen, et al. 2009. Single-grain zircon U-Pb isotopic ages, geochemistry and its implication of the Pulang complex in Yunnan Province, China
[J]. Acta Petrologica Sinica, 25(1): 159~165 (in Chinese with English abstract). Pearce J A, Harris N B W and Tindle A G. 1984. Trace element discrimination diagrams for the tectonic interpretation of granitic rocks
[J]. Journal of Petrology, 25(4): 956~983. Qu Xiaoming, Hou Zengqian and Tang Shaohua. 2003. Age of intraplate volcanism in the back-arc area of Yidun island arc and its significance
[J]. Acta Petrologica et Mineralogica, 22(2): 131~137 (in Chinese with English abstract). Ren Jiangbo, Xu Jifeng, Chen Jianlin, et al. 2011. Geochemistry and petrogenesis of Pulang porphyries in Sanjiang region
[J]. Acta Petrologica et Mineralogica, 30(4): 581~592 (in Chinese with English abstract). Ren Tao, Zhong Hong, Chen Jinfa, et al. 2011. Geochemical characteristics of the Langdu high-K intermediate-acid intrusive rocks in the Zhongdian area, northwest Yunnan province, P.R. China
[J]. Acta Mineralogica Sinica, 31(1): 43~54 (in Chinese with English abstract). Richards J P and Kerrich R. 2007. Special paper: Adakite-like rocks: Their diverse origins and questionable role in metallogenesis
[J]. Economic Geology, 102(4): 537~576. Richards J P. 2003. Tectono-magmatic precursors for porphyry Cu(Mo-Au) deposit formation
[J]. Economic Geology, 98(8): 1 515~1 533. Richards J P. 2011. High Sr/Y arc magmas and porphyry Cu±Mo±Au deposits: Just add water
[J]. Economic Geology, 106(7): 1 075~1 081. Richards J P. 2014. The oxidation state,and sulfur and Cu contents of arc magmas: Implications for metallogeny
[J]. Lithos, 233: 27~45. Rooney T O, Franceschi P and Hall C M. 2011. Water-saturated magmas in the Panama Canal region: A precursor to adakite-like magma gen eration?
[J]. Contributions to Mineralogy and Petrology, 161(3): 373~388. Sawka W N. 1998. REE and trace element variations in accessory minerals and hornblende from the strongly zoned MaMurry Meadows pluton, California
[J]. Transactions of the Royal Society of Edinburgh: Earth Sciences, 79(2~3): 157168. Schütte P, Chiaradia M, Barra F, et al. 2012. Metallogenic features of Miocene porphyry Cu and porphyry-related mineral deposits in Ecuador revealed by Re-Os, ⁴⁰Ar/³⁹Ar, and U-Pb geochronology
[J]. Mineralium Deposita, 47(4): 383~410. Sillitoe R H. 2010. Porphyry copper systems
[J]. Economic Geology, 105(1): 3~41. Stern R J. 2002. Subduction zones
[J]. Reviews of Geophysics, 40: 1 012. Sun S S and McDonough W F. 1989. Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and processes
[C]//Saunders A D and Norry M J. Magmatism in the Ocean Basins. Geological Society, London, Special Publications, 42(1): 313~345. Wang B Q, Zhou M F, Li J W, et al. 2011. Late Triassic porphyritic intrusions and associated volcanic rocks from the Shangri-La region, Yidun terrane, Eastern Tibetan Plateau: Adakitic magmatism and porphyry copper mineralization
[J]. Lithos, 127(1~2): 24~38. Wang Chengyang, Zhang Ziwei, Huang Jingyi, et al. 2023. Elements mobilization of the Early Triassic altered porphyry in the Shuangjianzishan deposit in Inner Mongolia, China
[J]. Mineral Exploration, 14(4): 553~562 (in Chinese with English abstract). Wang Cuiyun,Li Xiaofeng,Xiao Rong,et al. 2012. Elements mobilization of mineralized porphyry rocks during hydrothermal alteration at Zhushahong porphyry copper deposit,Dexing district,South China
[J]. Acta Petrologica Sinica,28(12): 3 869~3 886 (in Chinese with English abstract). Wang P, Dong G C, Zhao G C, et al. 2018. Petrogenesis of the Pulang porphyry complex, southwestern China: Implications for porphyry copper metallogenesis and subduction of the Paleo-Tethys Oceanic lithosphere
[J]. Lithos, 304: 280~297. Wang R, Richards J P, Hou Z Q, et al. 2014a. Increased magmatic water content-the key to Oligo-Miocene porphyry Cu-Mo Au formation in the eastern Gangdese belt, Tibet
[J]. Economic Geology, 109: 1 315~1 339. Wang R, Richards J P, Hou Z Q, et al. 2014b. Increasing magmatic oxidation state from Paleocene to Miocene in the Eastern Gangdese belt, Tibet: Implication for collision-related porphyry Cu-Mo-Au mineralization
[J]. Economic Geology, 109: 1 943~1 965. Wang R, Richards J P, Hou Z Q, et al. 2015. Zircon U-Pb age and Sr-Nd-Hf-O isotope geochemistry of the Paleocene-Eocene igneous rocks in western Gangdese: Evidence for the timing of Neo-Tethyan slab breakoff
[J]. Lithos, 224~225: 179~194. Wang Rui, Li Xia, Dong Cheng, et al. 2010. Migration regularity of major elements and REE in Wenglang structural altered rock type gold deposit, Congjiang County
[J]. Mineral Deposits, 29(3): 489~500(in Chinese with English abstract). Wang Shouxu, Zhang Xingchun, Qin Chaojian, et al. 2007. Fluid inclusions in quartz veins of Pulang porphyry copper deposit, Zhongdian, northwestern Yunnan, China
[J]. Geochimica, 36(5): 467~478 (in Chinese with English abstract). Wang T R, Peng H J, Xia Y, et al. 2022. Magmatic processes of granitoids in the Hongniu-Hongshan porphyry-skarn copper deposit, southern Yidun Terrane, China: Evidence from mineral geochemistry
[J]. Minerals, 12(12): 1 559. Wang X S, Hu R Z, Bi X W, et al. 2014. 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
[J]. Lithos, 208~209: 202~219. Wang Xinsong, Bi Xianwu, Hu Ruizhong, et al. 2015. S-Pb isotopic geochemistry of Xiuwacu magmatic hydrothermal Mo-W deposit in Zhongdian area, NW Yunnan: Constrains on the sources of metal
[J]. Acta Petrologica Sinica, 31(11): 3 171~3 188 (in Chinese with English abstract). Xie B, Song H, Song S W, et al. 2022. Geochemical, zircon U-Pb-Hf-O isotopic evidence and molybdenite Re-Os dating from the Cuojiaoma batholith, eastern Tibetan Plateau: Implications for molybdenum potential and tectonic evolution
[J]. Ore Geology Reviews, 144: 104810. Xue Chuandong, Luo Shaoyong, Song Yucai, et al. 2010. Zircon SHRIMP U-Pb dating and its geological significance of Lujiacun quartz-monzonite porphyry in Shangri-la County, northwestern Yunnan Province, China
[J]. Acta Petrologica Sinica, 26(6): 1 845~1 855 (in Chinese with English abstract). Yang Yueqing, Hou Zengqian, Huang Dianhao, et al. 2002. Collision orogenic process and magmatic metallogenic system in Zhongdian Arc
[J]. Acta Geoscientia Sinica, 23(1): 17~24 (in Chinese with English abstract). Zeng Pusheng, Li Wenchang, Wang Haiping, et al. 2006. The Indosinian Pulang superlarge porphyry copper deposit in Yunnan, China: Petrology and chronology
[J]. Acta Petrologica Sinica, 22(4): 989~1 000 (in Chinese with English abstract). Zeng Pusheng, Mo Xuanxue, Yu Xuehui, et al. 1999. Preliminary research on the intermediate-acidic porphyries and their ore-bearing in Zhongdian area, northwest Yunnan
[J]. Acta Geoscientica Sinica, 20(Z): 359~366 (in Chinese with English abstract). Zeng Pusheng, Wang Haiping, Mo Xuanxue, et al. 2004. Tectonic setting and prospects of porphyry copper deposits in Zhongdian island arc belt
[J]. Acta Geoscientica Sinica, 25(5): 535~540 (in Chinese with English abstract). Zeng Pusheng, Mo Xuanxue, Yu Xuehui, et al. 2003. Porphyries and porphyry copper deposits in Zhongdian area, northwestern Yunnan
[J]. Mineral Deposits, 22(4): 393~400 (in Chinese with English abstract). Zhang Keqing and Yang Yong. 2002. Multiple precursor systems and mass balance of alteration
[J]. Bulletin of Geological Science and Technology, 21(2): 61~64 (in Chinese with English abstract). Zhang Xiangfei, Li Wenchang, Yin Guanghou, et al. 2017. Geological and mineralized characteristics of the composite complex in Xiuwacu W-Mo mining district, NW Yunnan, China: Constraints by geochronology, oxygen fugacity and geochemistry
[J]. Acta Petrologica Sinica, 33(7): 2 018~2 036 (in Chinese with English abstract). Zhou Xiaodan, Yang Fan, Wu Jing, et al. 2018. Petrogenesis of porphyry body in the periphery of Pulang porphyry copper deposit, Yunnan
[J]. Geological Science and Technology Information, 37(4): 39~50 (in Chinese with English abstract). 艾金彪, 马生明, 朱立新, 等. 2013. 安徽马头斑岩型钼铜矿床蚀变带常量元素迁移规律及其定量计算
[J]. 矿床地质, 32(6): 1 262~1 274. 曹殿华, 王安建, 黄玉凤, 等. 2009. 中甸弧雪鸡坪斑岩铜矿含矿斑岩锆石SHRIMP U-Pb年代学及Hf同位素组成
[J]. 地质学报, 83(10): 1 430~1 435. 曹康, 许继峰, 陈建林, 等. 2014. 云南普朗超大型斑岩铜矿床含矿斑岩成因及其成矿意义
[J]. 矿床地质, 33(2): 307~322. 陈斌, 贺敬博, 陈长健, 等. 2013. 东天山白石泉镁铁-超镁铁杂岩体的Nd-Sr-Os同位素成分及其对岩浆演化的意义
[J]. 岩石学报, 29(6): 294~302. 邓军, 杨立强, 王长明. 2011. 三江特提斯复合造山与成矿作用研究进展
[J]. 岩石学报, 27(9): 2 501~2 509. 董涛, 江小均, 李超, 等. 2021. 滇西北中甸地区普上含矿斑岩锆石U-Pb年代学和地球化学特征及其地质意义
[J]. 矿物岩石地球化学通报, 40(4): 871~888. 董涛, 余海军, 段召艳, 等. 2020. 云南香格里拉盖吉夏含矿石英二长闪长玢岩年代学、地球化学、锆石Hf同位素特征及其地质意义
[J].岩石学报, 36(5): 1 369~1 388. 杜泽忠, 程志中, 姚晓峰, 等. 2020. 胶东谢家沟金矿热液蚀变作用过程的元素迁移规律
[J]. 地质通报, 39(8): 1 137~1 152. 范玉华, 李文昌. 2006. 云南普朗斑岩铜矿床地质特征
[J]. 中国地质, 33(2): 352~362. 郭顺, 叶凯, 陈意, 等. 2013. 开放地质体系中物质迁移质量平衡计算方法介绍
[J]. 岩石学报, 29(5): 1 486~1 498. 侯增谦, 曲晓明, 周继荣, 等. 2001. 三江地区义敦岛弧碰撞造山过程: 花岗岩记录
[J]. 地质学报, 75(4): 484~497. 侯增谦, 王涛. 2018. 同位素填图与深部物质探测(Ⅱ): 揭示地壳三维架构与区域成矿规律
[J]. 地学前缘, 25(6): 20~41. 侯增谦, 杨岳清, 曲晓明, 等. 2004. 三江地区义敦岛弧造山带演化和成矿系统
[J]. 地质学报, 78(1): 109~120. 黄智龙, 王联魁. 1997. 云南老王寨金矿煌斑岩蚀变、矿化过程中元素活动规律
[J]. 岩石矿物学杂志, 16(1): 11~22. 冷成彪. 2017. 滇西北红山铜多金属矿床的成因类型: 黄铁矿和磁黄铁矿LA-ICP-MS微量元素制约
[J]. 地学前缘, 24(6): 162~175. 冷成彪, 陈喜连, 张静静, 等. 2020. 斑岩型Cu±Mo±Au矿床的勘查标志: 岩石化学和矿物化学指标
[J]. 地质学报, 94(11): 3 189~3 212. 冷成彪, 张兴春, 王守旭, 等. 2007. 云南中甸地区两个斑岩铜矿容矿斑岩的地球化学特征——以雪鸡坪和普朗斑岩铜矿床为例
[J]. 矿物学报, 27(3~4): 414~422. 冷成彪, 张兴春, 王守旭, 等. 2008. 滇西北雪鸡坪斑岩铜矿S、Pb同位素组成及对成矿物质来源的示踪
[J]. 矿物岩石, 28(4): 80~88. 李建康, 李文昌, 王登红, 等. 2007. 中甸弧燕山晚期成矿事件的Re-Os定年及成矿规律研究
[J]. 岩石学报, 23(10): 2 415~2 422. 李建平, 陈华勇, 苏龙, 等. 2019. 斑岩型铜矿床高-中温蚀变过程实验研究及其地质意义
[J]. 中国科学: 地球科学, 49(4): 611~634. 李凯旋, 梁华英, 黄文婷, 等. 2019. 滇西北铜厂沟夕卡岩~斑岩型Mo-Cu矿床成矿岩体的高氧逸度特征及区内斑岩矿床成矿元素组合差异控制因素分析
[J]. 地球化学, 48(2): 101~113. 李守奎, 陈建航, 刘学龙, 等. 2023. 滇西北香格里拉铜厂沟斑岩型钼铜矿成矿热液蚀变与元素迁移富集规律
[J]. 中国地质, 50(6): 1 745~1 763. 李文昌, 刘学龙, 曾普胜, 等. 2011. 云南普朗斑岩型铜矿成矿岩体的基本特征
[J].中国地质, 38(2): 403~414. 李文昌, 余海军, 尹光候. 2013. 西南"三江"格咱岛弧斑岩成矿系统
[J]. 岩石学报, 29(4): 1 129~1 144. 李文昌, 曾普胜. 2007. 云南普朗超大型斑岩铜矿特征及成矿模型
[J]. 成都理工大学学报(自然科学版), 34(4): 436~446. 李雪峰. 2016. 滇西北中甸弧印支期斑岩地球化学特征及含矿性研究
[D]. 北京: 中国地质大学(北京), 1~95. 林振文, 梁志鹏, 庄文明, 等. 2023. 广东圆珠顶斑岩型铜钼矿床蚀变及元素迁移特征分析
[J]. 矿物岩石地球化学通报, 42(2): 325~339. 刘学龙, 李文昌, 尹光侯, 等. 2013. 云南格咱岛弧普朗斑岩型铜矿年代学、岩石矿物学及地球化学研究
[J]. 岩石学报, 29(9): 3 049~3 064. 刘学龙, 李文昌, 张娜, 等. 2014. 云南格咱岛弧地苏嘎成矿岩体I型花岗岩年代学、地球化学特征及地质意义
[J]. 地质论评, 60(1): 103~114. 刘学龙, 杨富成, 张昌振, 等. 2018. 滇西北雪鸡坪斑岩型铜矿构造特征与成矿作用研究
[J]. 黄金科学技术, 26(4): 473~480. 孟祥金, 侯增谦, 高永丰, 等. 2004. 碰撞造山型斑岩铜矿蚀变分带模式——以西藏冈底斯斑岩铜矿带为例
[J]. 地学前缘, 11(1): 201~214. 莫雷, 冷成彪, 陈喜连, 等. 2024a. 云南中甸地区斑岩体锆石微量元素与Hf-O同位素特征及其对成岩成矿的启示
[J]. 岩石学报, 40(4): 1 163~1 184. 莫雷, 沈啟武, 陈喜连, 等. 2024b. 滇西北浪都夕卡岩矿床致矿岩体的岩石地球化学、年代学、Sr-Nd-Pb同位素组成及其地质意义
[J]. 沉积与特提斯地质, 44(2): 421~436. 庞振山, 杜杨松, 王功文, 等. 2009. 云南普朗复式岩体锆石U-Pb年龄和地球化学特征及其地质意义
[J]. 岩石学报, 25(1): 159~165. 曲晓明, 侯增谦, 唐绍华. 2003. 义敦岛弧带弧后区板内岩浆作用的时代及意义
[J]. 岩石矿物学杂志, 22(2): 131~137. 任江波, 许继峰, 陈建林, 等. 2011."三江"地区中甸弧普朗成矿斑岩地球化学特征及其成因
[J]. 岩石矿物学杂志, 30(4): 581~592. 任涛, 钟宏, 陈金法, 等. 2011. 云南中甸地区浪都高钾中酸性侵入岩的地球化学特征
[J]. 矿物学报, 31(1): 43~54. 王承洋, 张紫薇, 黄静宜, 等. 2023. 内蒙古双尖子山矿区早三叠世蚀变斑岩的物质迁移特征研究
[J]. 矿产勘查, 14(4): 553~562. 王翠云, 李晓峰, 肖荣, 等. 2012. 德兴朱砂红斑岩铜矿热液蚀变作用及元素地球化学迁移规律
[J]. 岩石学报, 28(12): 3 869~3 886. 王睿, 李霞, 董成, 等. 2010. 从江翁浪地区蚀变岩型金矿床常量元素及稀土元素迁移规律研究
[J]. 矿床地质, 29(3): 489~500. 王守旭, 张兴春, 秦朝建, 等. 2007. 滇西北中甸普朗斑岩铜矿流体包裹体初步研究
[J]. 地球化学, 36(5): 467~478. 王新松, 毕献武, 胡瑞忠, 等. 2015. 滇西北中甸地区休瓦促岩浆热液型Mo-W矿床S、Pb同位素对成矿物质来源的约束
[J]. 岩石学报, 31(11): 3 171~3 188. 薛传东, 骆少勇, 宋玉财, 等. 2010. 滇西北中甸陆家村石英二长斑岩的锆石SHRIMP定年及其意义
[J]. 岩石学报, 26(6): 1 845~1 855. 杨岳清, 侯增谦, 黄典豪, 等. 2002. 中甸弧碰撞造山作用和岩浆成矿系统
[J]. 地球学报, 23(1): 17~24. 曾普胜, 李文昌, 王海平, 等. 2006. 云南普朗印支期超大型斑岩铜矿床: 岩石学及年代学特征
[J]. 岩石学报, 22(4): 989~1 000. 曾普胜, 莫宣学, 喻学惠, 等. 1999. 滇西北中甸地区中－酸性斑岩及其含矿性初步研究
[J]. 地球学报, 20(增刊): 359~366. 曾普胜, 莫宣学, 喻学惠, 等. 2003. 滇西北中甸斑岩及斑岩铜矿
[J]. 矿床地质, 22(4): 393~400. 曾普胜, 王海平, 莫宣学, 等. 2004. 中甸岛弧带构造格架及斑岩铜矿前景
[J]. 地球学报, 25(5): 535~540. 张可清, 杨勇. 2002. 蚀变作用的多原岩系统及质量平衡
[J]. 地质科技情报, 21(2): 61~64. 张向飞, 李文昌, 尹光候, 等. 2017. 滇西北休瓦促钨钼矿区复式岩体地质及其成矿特征——来自年代学、氧逸度和地球化学的约束
[J]. 岩石学报, 33(7): 2 018~2 036. 周晓丹, 杨帆, 吴静, 等. 2018. 云南普朗斑岩型铜矿床外围斑岩体成因探讨
[J]. 地质科技情报, 37(4): 39~50.

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莫雷，冷成彪*，邢新龙，李凯旋，陈喜连，余海军，王艳军，陈加杰. 滇西北普上含矿斑岩体的岩石地球化学及蚀变特征研究 [J]. 岩石矿物学杂志. 2024; 43; (6). 1339 - 1360.

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