Geochronological and Geochemical Characteristics of the Pushang Ore-bearing Porphyry in the Zhongdian Area of the Northwestern Yunnan and Its Geological Significances
DONG Tao1,2, JIANG Xiao-jun3*, LI Chao4, DUAN Zhao-yan1,2, CAO Xiao-min1,2, DU Bin1, DONG Hong-guo1, LI Bing1
1. Yunnan Geological Survey,Kunming 650216, China;
2. Key Laboratory of Sanjiang Metallogeny and Resources Exploration and Utilization, MNR,Kunming 650051, China;
3. Faculty of Land Resource Engineering, Kunming University of Science and Technology,Kunming 650093, China;
4. National Research Center for Geonalysis, Chinese Academy of Geological Sciences,Beijing 100037, China
Abstract：In recent years, the Geza area in the northwestern Yunnan has gradually become an important porphyry copper orefield and copper resources exploration and development base in China. Quartz diorite porphyrite and quartz monzonitic diorite emplaced within the quartz diorite porphyrite have recently been recognized in the Pushang intermediate-acid porphyry complex in the northern part of Lannitang-Xuejiping Cu polymetallic metallogenic belt. In order to explore diagenetic mechanism and tectonic dynamic background of the Pushang complex and the relationship between the complex and the copper mineralization, the U-Pb chronology, Hf isotopes, and geochemical characteristics of the complex have been studied in this paper. The results show that the copper mineralization was developed in the whole quartz diorite porphyrite, with apparent thickness of 35 m, Cu grades of 0.13%-4.66%, andu grades of 0.24-0.78 g/t for samples collected by using the channel sampling, indicating that the Pushang deposit has the potential to become another large porphyry Cu polymetallic deposit in the southern part of the Yidun arc. The U-Pb ages of (215.9 ±1.4)Ma and (217.6±1.4)Ma for zircons of two ore-bearing porphyry samples indicate that the ore-bearing porphyries are products ofthe Late Triassic magmatism. Combined with petrological, geochemical, and zircon Hf isotopic characteristics of the porphyry complex, it is believed that the Pushang ore-bearing porphyry was mainly formed by the magma derived from the partial melting of metasomatized lithospheric mantle by subducted fluid under the tectonic setting of the westward subduction of the Ganzi-Litang oceanic crust in the Late Triassic, with contamination of crust-derived sediments in the process of magma ascent.
董涛, 江小均, 李超, 段召艳, 曹晓民, 杜斌, 董红国, 李冰. 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, 2021, 40(4): 871-888.
DONG Tao, JIANG Xiao-jun, LI Chao, DUAN Zhao-yan, CAO Xiao-min, DU Bin, DONG Hong-guo, LI Bing. Geochronological and Geochemical Characteristics of the Pushang Ore-bearing Porphyry in the Zhongdian Area of the Northwestern Yunnan and Its Geological Significances. Acta Metallurgica Sinica, 2021, 40(4): 871-888.
Batchelor R A, Bowden P. 1985. Petrogenetic interpretation of granitoid rock series using multicationic parameters. Chemical Geology, 48(1-4): 43-55
Blevin P L, Chappell B W. 1995. Chemistry, origin, and evolution of mineralized granites in the Lachlan fold belt, Australia; the metallogeny of I- and S-type granites. Economic Geology, 90(6): 1604-1619
Blevin P L. 2004. Redox and compositional parameters for interpreting the granitoid metallogeny of eastern Australia: Implications for gold-rich ore systems. Resource Geology, 54(3): 241-252
Blichert-Toft J, Chauvel C, Albarède F. 1997. Separation of Hf and Lu for high-precision isotope analysis of rock samples by magnetic sector-multiple collector ICP-MS. Contributions to Mineralogy and Petrology, 127(3): 248-260
Cao K, Yang Z M, Xu J F, Fu B, Li W K, Sun M Y. 2018. Origin of dioritic magma and its contribution to porphyry Cu-Au mineralization at Pulang in the Yidun arc, eastern Tibet. Lithos, 304-307: 436-449
Chappell B W, White A J R. 1974. Two contrasting granite types. Pacific Geology, 8: 173-174
Collins W J, Beams S D, White A J R, Chappell B W. 1982. Nature and origin of A-type granites with particular reference to southeastern Australia. Contributions to Mineralogy and Petrology, 80(2): 189-200
Condie K C. 1982. Plate tectonics and crustal evolution. 2nd ed. Oxford: Pergamon Press
Condie K C. 1986. Geochemistry and tectonic setting of Early Proterozoic supracrustal rocks in the southwestern United States. The Journal of Geology, 94(6): 845-864
Deng J, Wang Q F, Li G J, Li C S, Wang C M. 2014a. 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
Deng J, Wang Q F, Li G J, Santosh M. 2014b. Cenozoic tectono-magmatic and metallogenic processes in the Sanjiang region, southwestern China. Earth-Science Reviews, 138: 268-299
Deng J, Wang Q F, Li G J, Li C S, Wang C M. 2014c. 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
Deng J, Wang C M, Zi J W, Xia R, Li Q. 2018. Constraining subduction-collision processes of the Paleo-Tethys along the Changning-Menglian Suture: New zircon U-Pb ages and Sr-Nd-Pb-Hf-O isotopes of the Lincang Batholith. Gondwana Research, 62: 75-92
Elhlou S, Belousova E, Griffin W L, Pearson N J, O'Reilly S Y. 2006. Trace element and isotopic composition of GJ-red zircon standard by laser ablation. Geochimica et Cosmochimica Acta, 70(18S): A158
Ellam R M, Hawkesworth C J. 1988. Elemental and isotopic variations in subduction related basalts: Evidence for a three component model. Contributions to Mineralogy and Petrology, 98(1): 72-80
Gao X, Yang L Q, Meng J Y, Zhang L J. 2017. Zircon U-Pb, molybdenite Re-Os geochronology and Sr-Nd-Pb-Hf-O-S isotopic constraints on the genesis of Relin Cu-Mo deposit in Zhongdian, Northwest Yunnan, China. Ore Geology Reviews, 91: 945-962
Gao X, Yang L Q, Orovan E A. 2018. The lithospheric architecture of two subterranes in the eastern Yidun Terrane, East Tethys: Insights from Hf-Nd isotopic mapping. Gondwana Research, 62: 127-143
Griffin W L, Pearson N J, Belousova E, Jackson S E, van Achterbergh E, O'Reilly S Y, Shee S R. 2000. The Hf isotope composition of cratonic mantle: LAM-MC-ICPMS analysis of zircon megacrysts in kimberlites. Geochimica et Cosmochimica Acta, 64(1): 133-147
Hoskin P W O, Black L P. 2000. Metamorphic zircon formation by solid-state recrystallization of protolith igneous zircon. Journal of Metamorphic Geology, 18(4): 423-439
Kelley K A, Cottrell E. 2009. Water and the oxidation state of subduction zone magmas. Science, 325(5940): 605-607
Kinny P D, Maas R. 2003. Lu-Hf and Sm-Nd isotope systems in zircon. Reviews in Mineralogy and Geochemistry, 53(1): 327-341
Li W C, Zeng P S, Hou Z Q, White N C. 2011. The Pulang porphyry copper deposit and associated felsic intrusions in Yunnan province, southwest China. Economic Geology, 106(1): 79-92
Li W C, Yin G H, Yu H J, Liu X L. 2014. The Yanshanian granites and associated Mo-polymetallic mineralization in the Xiangcheng-Luoji area of the Sanjiang-Yangtze conjunction zone in southwest China. Acta Geologica Sinica (English Edition), 88(6): 1742-1756
Li W C, Yu H J, Gao X, Liu X L, Wang J H. 2017. Review of Mesozoic multiple magmatism and porphyry Cu-Mo (W) mineralization in the Yidun Arc, eastern Tibet Plateau. Ore Geology Reviews, 90: 795-812
Liu Y S, Hu Z C, Gao S, Günther D, Xu J, Gao G H, Chen H H. 2008. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard. Chemical Geology, 257(1-2): 34-43
Lu Y J, Kerrich R, Kemp A I S, McCuaig T C, Hou Z Q, Hart C J R, Li Z X, Cawood P A, Bagas L, Yang Z M, Cliff J, Belousova E A, Jourdan F, Evans N J. 2013. Intracontinental Eocene-Oligocene porphyry Cu mineral systems of Yunnan, western Yangtze craton, China: Compositional characteristics, sources, and implications for continental collision metallogeny. Economic Geology, 108(7): 1541-1576
Maniar P D, Piccoli P M. 1989. Tectonic discrimination of granitoids. Geological Society of America Bulletin, 101(5): 635-643
Middlemost E A K. 1985. Magmas and magmatic rocks: An introduction to igneous petrology. London: Longman, 1-266
Middlemost E A K. 1994. Naming materials in the magma/igneous rock system. Earth-Science Reviews, 37(3-4): 215-224
Miller C F. 1985. Are strongly peraluminous magmas derived from pelitic sedimentary sources?. The Journal of Geology, 93(6): 673-689
Nasdala L, Hofmeister W, Norberg N, Martinson J M, Corfu F, Dörr W, Kamo S L, Kennedy A K, Kronz A, Reiners P W, Frei D, Kosler J, Wan Y S, Götze J, Häger T, Kröner A, Valley J W. 2008. Zircon M257- a homogeneous natural reference material for the ion microprobe U-Pb analysis of zircon. Geostandards and Geoanalytical Research, 32(3): 247-265
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
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
Richards J P. 2015. The oxidation state, and sulfur and Cu contents of arc magmas: Implications for metallogeny. Lithos, 233: 27-45
Scherer E, Münker C, Mezger K. 2001. Calibration of the lutetium-hafnium clock. Science, 293(5530): 683-687
Sun S S, McDonough W F. 1989. Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and processes. Geological Society, London, Special Publication, 42(1): 313-345
Sun W D, Huang R F, Li H, Hu Y B, Zhang C C, Sun S J, Zhang L P, Ding X, Li C Y, Zartman R E, Ling M X. 2015. Porphyry deposits and oxidized magmas. Ore Geology Reviews, 65: 97-131
Taylor S R, McLennan S M. 1995. The geochemical evolution of the continental crust. Reviews of Geophysics, 33(2): 241-265
Wang B Q, Zhou M F, Li J W, Yan D P. 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. Lithos, 127(1-2): 24-38
Wang C M, Bagas L, Lu Y J, Santosh M, Du B, McCuaig T C. 2016. Terrane boundary and spatio-temporal distribution of ore deposits in the Sanjiang Tethyan Orogen: Insights from zircon Hf-isotopic mapping. Earth-Science Reviews, 156: 39-65
Wang X S, Bi X W, Leng C B, Zhong H, Tang H F, Chen Y W, Yin G H, Huang D Z, Zhou M F. 2014a. Geochronology and geochemistry of Late Cretaceous igneous intrusions and Mo-Cu-(W) mineralization in the southern Yidun Arc, SW China: Implications for metallogenesis and geodynamic setting. Ore Geology Reviews, 61: 73-95
Wang X S, Hu R Z, Bi X W, Leng C B, Pan L C, Zhu J J, Chen Y W. 2014b. Petrogenesis of Late Cretaceous I-type granites in the southern Yidun Terrane: New constraints on the Late Mesozoic tectonic evolution of the eastern Tibetan Plateau. Lithos, 208-209: 202-219
Yang L Q, Deng J, Gao X, He W Y, Meng J Y, Santosh M, Yu H J, Yang Z, Wang D. 2017a. Timing of formation and origin of the Tongchanggou porphyry-skarn deposit: Implications for Late Cretaceous Mo-Cu metallogenesis in the southern Yidun Terrane, SE Tibetan Plateau. Ore Geology Reviews, 81: 1015-1032
Yang L Q, Gao X, Shu Q H. 2017b. Multiple Mesozoic porphyry-skarn Cu (Mo-W) systems in Yidun Terrane, east Tethys: Constraints from zircon U-Pb and molybdenite Re-Os geochronology. Ore Geology Reviews, 90: 813-826
Yang L Q, He W Y, Gao X, Xie S X, Yang Z. 2018. Mesozoic multiple magmatism and porphyry-skarn Cu-polymetallic systems of the Yidun Terrane, Eastern Tethys: Implications for subduction- and transtension-related metallogeny. Gondwana Research, 62: 144-162
Yu H J, Li W C, Yin G H, Lu Y X, Cao X M, Huang D Z, Dong T, Zhang Y M. 2014. Zircon U-Pb ages of the granodioritic porphyry in the laba molybdenum deposit, Yunnan, SW China and its geological implication. Acta Geologica Sinica (English Edition), 88(4): 1183-1194
Yu H J, Jiang J W, Li W C. 2020. Controls of variable crustal thicknesses on Late Triassic mineralization in the Yidun Arc, Eastern Tibet. Journal of Asian Earth Sciences, 195: 104285, doi: 10.1016/j.jseaes.2020.104285
曹殿华. 2007. 中甸地区斑岩铜矿成矿模式与综合勘查评价技术研究. 博士学位论文. 北京: 中国地质科学院
曹殿华, 王安建, 黄玉凤, 张维, 侯可军, 李瑞萍, 李以科. 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. 地质学报, 83(10): 1430-1435
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. 岩石学报, 27(9): 2501-2509
邓军, 王长明, 李文昌, 杨立强, 王庆飞. 2014. 三江特提斯复合造山与成矿作用研究态势及启示. 地学前缘, 21(1): 52-64
邓军, 王庆飞, 李龚健. 2016. 复合造山和复合成矿系统: 三江特提斯例析. 岩石学报, 32(8): 2225-2247
董涛, 余海军, 段召艳, 魏坤, 吴俊, 兰文达, 刘晓波, 杜斌. 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. 岩石学报, 36(5): 1369-1388
董毅. 2013. 云南香格里拉阿热岩体年代学与地球化学. 硕士学位论文. 成都: 成都理工大学
范玉华, 李文昌. 2006. 云南普朗斑岩铜矿床地质特征. 中国地质, 33(2): 352-362
侯可军, 李延河, 邹天人, 曲晓明, 石玉若, 谢桂青. 2007. LA-MC-ICP-MS锆石Hf同位素的分析方法及地质应用. 岩石学报, 23(10): 2595-2604
侯可军, 李延河, 田有荣. 2009. LA-MC-ICP-MS锆石微区原位U-Pb定年技术. 矿床地质, 28(4): 481-492
侯增谦, 莫宣学. 1991. “三江”地区义敦岛弧构造-岩浆演化特征. 见: 地质矿产部青藏高原地质文集编委会. 青藏高原地质文集21. 北京: 地质出版社, 153-165
侯增谦, 曲晓明, 周继荣, 杨岳清, 黄典豪, 吕庆田, 唐绍华, 余金杰, 王海平, 赵金花. 2001. 三江地区义敦岛弧碰撞造山过程: 花岗岩记录. 地质学报, 75(4): 484-497
侯增谦, 杨岳清, 王海平, 曲晓明, 吕庆田, 黄曲豪, 吴宣志, 余金杰, 唐绍华, 赵金花. 2003. 三江义敦岛弧碰撞造山过程与成矿系统. 北京: 地质出版社, l-345
侯增谦, 杨岳清, 曲晓明, 黄典豪, 吕庆田, 王海平, 余金杰, 唐绍华. 2004. 三江地区义敦岛弧造山带演化和成矿系统. 地质学报, 78(1): 109-120
胡清华, 张世权, 尹静, 黄定柱, 伍建兢, 孟青, 杨丽梅, 罗光明. 2010. 中甸普朗斑岩型铜矿床围岩蚀变初步研究. 矿物岩石地球化学通报, 29(2): 192-201
黄肖潇, 徐继峰, 陈建林, 任江波. 2012. 中甸岛弧红山地区两期中酸性侵入岩的年代学、地球化学特征及其成因. 岩石学报, 28(5): 1493-1506
姜丽莉, 薛传东, 侯增谦, 向坤. 2015. 滇西北甭哥正长岩体成因: 锆石U-Pb年龄、Hf同位素和地球化学证据. 岩石学报, 31(11): 3234-3246
江小均, 陈政宇, 李文昌, 余海军, 李超, 张向飞, 严清高. 2019. 滇西北休瓦促晚白垩世岩浆-成矿作用动力学机制探讨. 地学前缘, 26(2): 137-156
冷成彪, 张兴春, 王守旭, 秦朝建, 苟体忠. 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. 矿物学报, 27(3-4): 414-422
冷成彪, 张兴春, 王守旭, 秦朝建, 苟体忠, 王外全. 2008a. 滇西北中甸松诺含矿斑岩的锆石SHRIMP U-Pb年龄及地质意义. 大地构造与成矿学, 32(1): 124-130
冷成彪, 张兴春, 王守旭, 王外全, 秦朝建, 吴孔文, 任涛. 2008b. 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. 矿物岩石, 28(4): 80-88
李建康, 李文昌, 王登红, 卢映祥, 尹光侯, 薛顺荣. 2007. 中甸弧燕山晚期成矿事件的Re-Os定年及成矿规律研究. 岩石学报, 23(10): 2415-2422
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. 成都理工大学学报(自然科学版), 34(4): 436-446
李文昌, 潘桂棠, 侯增谦, 莫宣学, 王立全, 丁俊. 2010a. 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
李文昌, 尹光候, 卢映祥, 王彦斌, 余海军, 曹晓民, 张世权. 2010b. 西南“三江”格咱火山-岩浆弧中红山-属都蛇绿混杂岩带的厘定及其意义. 岩石学报, 26(6): 1661-1671
李文昌, 尹光侯, 余海军, 卢映祥, 刘学龙. 2011. 滇西北格咱火山-岩浆弧斑岩成矿作用. 岩石学报, 27(9): 2541-2552
李文昌, 余海军, 尹光侯, 曹晓民, 黄定柱, 董涛. 2012. 滇西北铜厂沟钼多金属矿床辉钼矿Re-Os同位素年龄及其成矿环境. 矿床地质, 31(2): 282-292
李文昌, 余海军, 尹光候. 2013. 西南“三江”格咱岛弧斑岩成矿系统. 岩石学报, 29(4): 1129-1144
李文昌, 尹光侯, 卢映祥, 余海军, 施玉北, 朱俊, 刘学龙, 薛顺荣, 蒋成兴. 2016. 西南三江南段有色、贵金属成矿带成矿规律及矿产预测. 北京: 地质出版社
林清茶, 夏斌, 张玉泉. 2006. 云南中甸地区雪鸡坪同碰撞石英闪长玢岩锆石SHRIMP U-Pb定年及其意义. 地质通报, 25(1-2): 133-137
刘学龙, 李文昌. 2013. 云南格咱岛弧印支期岩浆作用的锆石年龄和铪同位素证据. 地学前缘, 20(5): 57-74
刘学龙, 李文昌, 张娜. 2016. 云南卓玛成矿斑岩体锆石U-Pb年龄及地球化学特征. 矿物岩石地球化学通报, 35(1): 109-117
刘颖, 刘海臣, 李献华. 1996. 用ICP-MS准确测定岩石样品中的40余种微量元素. 地球化学, 25(6): 552-558
莫宣学, 路凤香, 沈上越, 朱勤文, 侯增谦, 杨开辉, 邓晋福, 刘祥品, 何昌祥. 1993. 三江特提斯火山作用与成矿. 北京: 地质出版社
潘桂棠, 徐强, 侯增谦, 王立全, 杜德勋, 莫宣学, 李定谋, 汪名杰, 李兴振, 江新胜, 胡云中. 2003. 西南“三江”多岛弧造山过程成矿系统与资源评价. 北京: 地质出版社, 11-30
任江波, 许继峰, 陈建林, 张世权, 梁华英. 2011a. “三江”地区中甸弧普朗成矿斑岩地球化学特征及其成因. 岩石矿物学杂志, 30(4): 581-592
任江波, 许继峰, 陈建林. 2011b. 中甸岛弧成矿斑岩的锆石年代学及其意义. 岩石学报, 27(9): 2591-2599
王新松, 毕献武, 冷成彪, 唐永永, 兰江波, 齐有强, 沈能平. 2011. 滇西北中甸红山铜多金属矿床花岗斑岩锆石LA-ICP-MS U-Pb定年及其地质意义. 矿物学报, 31(3): 315-321
王新松. 2014. 滇西北中甸地区燕山晚期花岗岩浆系统成岩成矿作用. 博士学位论文. 北京: 中国科学院大学
王新松, 毕献武, 胡瑞忠, 冷成彪, 余海军, 尹光侯. 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. 岩石学报, 31(11): 3171-3188
吴福元, 李献华, 郑永飞, 高山. 2007a. Lu-Hf同位素体系及其岩石学应用. 岩石学报, 23(2): 185-220
吴福元, 李献华, 杨进辉, 郑永飞. 2007b. 花岗岩成因研究的若干问题. 岩石学报, 23(6): 1217-1238
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): 1589-1604
肖庆辉, 邓晋福, 马大铨, 洪大卫, 莫宣学, 卢欣祥, 李志昌, 汪雄武, 马昌前, 吴福元, 罗照华, 王涛. 2002. 花岗岩研究思维与方法. 北京: 地质出版社, 230
徐兴旺, 蔡新平, 屈文俊, 宋保昌, 秦克章, 张宝林. 2006. 滇西北红山晚白垩世花岗斑岩型Cu-Mo成矿系统及其大地构造学意义. 地质学报, 80(9): 1422-1433
薛传东, 骆少勇, 宋玉财, 杨志明, 韩艳伟, 黄琴辉, 李敬, 魏爱英. 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. 岩石学报, 26(6): 1845-1855
杨帆, 邹国富, 吴静, 李峰, 姜永果, 赵向东. 2011. 中甸春都铜矿区岩体成岩时代及地质意义. 大地构造与成矿学, 35(2): 307-314
杨立强, 高雪, 和文言. 2015. 义敦岛弧晚白垩世斑岩成矿系统. 岩石学报, 31(11): 3155-3170
尹光候, 李文昌, 蒋成兴, 许东, 李建康, 杨舒然. 2009. 中甸火山-岩浆弧燕山期热林复式岩体演化与Ar-Ar定年及铜钼矿化. 地质与勘探, 45(4): 385-394
余海军, 李文昌, 尹光候, 王建华, 姜文涛, 吴松, 唐忠. 2015. 滇西北铜厂沟Mo-Cu矿床岩体年代学、地球化学及其地质意义. 岩石学报, 31(11): 3217-3233
余海军, 李文昌. 2016. 滇西北休瓦促Mo-W矿区印支晚期和燕山晚期岩浆活动与成矿作用: 来自锆石U-Pb年代学和地球化学的证据. 岩石学报, 32(8): 2265-2280
余海军. 2018. 格咱斑岩带复合成矿系统及找矿方向. 博士学位论文. 武汉: 中国地质大学
云南省地质调查院. 2018. 云南香格里拉格咱地区铜多金属矿整装勘查区矿产调查与找矿预测成果报告(内部报告)
曾普胜, 莫宣学, 喻学惠, 卢振权. 1999. 滇西北中甸地区中-酸性斑岩及其含矿性初步研究. 地球学报, 20(增刊): 359-366
曾普胜, 莫宣学, 喻学惠, 侯增谦, 徐启东, 王海平, 李红, 杨朝志. 2003. 滇西北中甸斑岩及斑岩铜矿. 矿床地质, 22(4): 393-400
曾普胜, 王海平, 莫宣学, 喻学惠, 李文昌, 李体刚, 李红, 杨朝志. 2004. 中甸岛弧带构造格架及斑岩铜矿前景. 地球学报, 25(5): 535-540
曾普胜, 李文昌, 王海平, 李红. 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. 岩石学报, 22(4): 989-1000
张向飞, 李文昌, 尹光侯, 杨镇, 唐忠. 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. 岩石学报, 33(7): 2018-2036
