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世界地质 2018 37 (2): 436-446 ISSN: 1004-5589 CN: 22-1111/P |
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别子型火山成因块状硫化物矿床的地质和地球化学特征 |
郭云峰1,2, 安芳1,2 |
1. 西北大学 地质学系, 西安 710069; 2. 大陆动力学国家重点实验室, 西安 710069 |
收稿日期 2017-07-10 修回日期 2018-01-31 网络版发布日期 null |
参考文献 [1] Еремин Н И. Типизация фанерозойских колчеданных месторождений[R]. Москва:АН СССР, 1978:5-8. (in Russian) [2] 安伟, 曹志敏, 郑建斌,等. 古代与现代火山成因块状硫化物矿床研究进展[J]. 地球科学进展, 2003, 18(5):773-782. AN Wei, CAO Zhi-min, ZHENG Jian-bin, et al. The developments of study on ancient and modern volcanogenic massive sulfide deposit[J]. Advances in Earth Science, 2003, 18(5):773-782. [3] Еремин Н И. Дифференциация вулканогенного сульфидного оруденения (на примере колчеданных месторождений фанерозоя)[М]. Москва:Издательство Москвы, 1983:82-93. (in Russian) [4] Еремин Н И, Дергачев А Л, Сергеева Н Е. Типы колчеданных месторождений вулканической ассоциации[J]. Геология Рудных Месторождений, 2000, 42(2):177-190. (in Russian) [5] Еремин Н И, Дергачев А Л, Сергеева Н Е. Вулканогенние колчеданные месторождения в офиолитовых комплексах[C]//Улътра-базитбазитовые комплексных-ладчатых о6ластей и связанные с ними местороэвдения. Екатеринбург:УО РАН, 2009:169-173. (in Russian) [6] Patten C G C, Pitcairn I K, Teagle D A H. Hydrothermal mobilisation of Au and other metals in supra-subduction oceanic crust:insights from the Troodos ophiolite[J]. Ore Geology Reviews, 2017, 86(6):487-508. [7] 傅鹏, 陈守余, 赵江南, 等. 甘肃白银厂铜多金属矿田岩石地球化学特征及地质意义[J]. 地质与勘探, 2016, 52(1):14-24. FU Peng, CHEN Shou-yu, ZHAO Jiang-nan, et al. Geochemical characteristics of rocks from the Baiyinchang copper polymetallic ore field in Gansu Province and geological implications[J]. Geology and Prospecting, 2016, 52(1):14-24. [8] Nozaki T, Nakamura K, Awaji S, et al. Whole-rock geochemistry of basic schists from the Besshi area, Central Shikoku:implications for the tectonic setting of the Besshi sulfide deposit[J]. Resource Geology, 2010, 56(4):423-432. [9] Yamamoto M, Kase K, Tsutsumi M. Fractionation of sulfur isotopes and selenium between coexisting sulfide minerals from the Besshi deposit, Central Shikoku, Japan[J]. Mineralium Deposita, 1984, 19(3):237-242. [10] Sato K, Sasaki A. Lead isotopic feature of the Besshi-type deposits and its bearing on the ore lead evolution[J]. Geochemical Journal, 1980, 14(6):303-315. [11] Yoshida K, Hirajima T. Annular fluid inclusions from a quartz vein intercalated with metapelites from the Besshi area of the Sanbagawa belt, SW Japan[J]. Journal of Mineralogical & Petrological Sciences, 2012, 107(1):50-55. [12] 高珍权, 方维萱, 胡瑞忠, 等. 新疆阿舍勒铜矿英安——玄武——安山质火山岩的地球化学特征与构造背景[J]. 矿床地质, 2010, 29(2):218-228. GAO Zhen-quan, FANG Wei-xuan, HU Rui-zhong, et al. Tectonic setting and geochemical characteristics of dacite andesite-basalt volcanic rocks in Ashele copper deposit, Xinjiang[J]. Mineral Deposits, 2010, 29(2):218-228. [13] Sharman E R, Taylor B E, Minarik W G, et al. Sulfur isotope and trace element data from ore sulfides in the Noranda district (Abitibi, Canada):implications for volcanogenic massive sulfide deposit genesis[J]. Mineralium Deposita, 2015, 50(5):591-606. [14] 张增杰, 邢树文, 马玉波, 等. 辽宁红透山铜锌矿围岩黑云斜长角闪岩锆石U-Pb定年及其块状硫化物指示意义[J]. 吉林大学学报(地球科学版), 2013, 43(4):1159-1168. ZHANG Zeng-jie, XING Shu-wen, MA Yu-bo, et al. Zircon U-Pb dating of the biotite-bearing plagioclase amphibolite from Hongtoushan Cu-Zn deposit, Liaoning Province, China and its implications on the exploration of VMS[J]. Journal of Jilin Univcrsity(Earth Scicncc Edition), 2013, 43(4):1159-1168. [15] 郝明, 杨言辰, 张国宾, 等. 辽宁树基沟铜锌矿床地球化学特征及成因[J]. 世界地质, 2014, 33(2):337-347. HAO Ming, YANG Yan-chen, ZHANG Guo-bin, et al. Geochemical characteristics and genesis of Shujigou Cu-Zn deposit, Liaoning[J]. Global Geology, 2014, 33(2):337-347. [16] Yamada R, Yoshida T. Relationships between Kuroko volcanogenic massive sulfide (VMS) deposits, felsic volcanism, and island arc development in the Northeast Honshu arc, Japan[J]. Mineralium Deposita, 2011, 46(5/6):431-448. [17] 党院, 陈懋弘, 毛景文, 等. 基于构造解析重建的四川呷村银多金属矿床模型[J]. 矿床地质, 2013, 32(6):1077-1092. DANG Yuan, CHEN Mao-hong, MAO Jing-wen, et al. Deposit model reconstruction of Xiacun siliver polymetallic deposit in Sichuan Province based on tectonic analysis[J]. Mineral Deposit, 2013, 32(6):1077-1092. [18] 侯增谦,韩发,夏林圻, 等. 现代与古代海底热水成矿作用[M]. 北京:地质出版社, 2003:1-91. HOU Zeng-qian, HAN Fa, XIA Lin-qi, et al. Hydrothermal systems and metallogeny on the mordern and ancient sea-floor[M]. Beijing:Geological Publishing House, 2003:1-91. [19] 李文渊. 块状硫化物矿床的类型、分布和形成环境[J]. 地球科学与环境学报, 2007, 29(4):331-344. LI Wen-yuan. Classification, distribution and forming setting of massive sulfide deposits[J]. Journal of Earth Sciences and Environment, 2007, 29(4):331-344. [20] Layton-Matthews D, Peter J M, Scott S D, et al. Distribution, mineralogy, and geochemistry of selenium in felsic volcanic-hosted massive sulfide deposits of the Finlayson Lake District, Yukon Territory, Canada[J]. Economic Geology, 2008, 103(1):61-88. [21] Wardle R J, Ryan B, Ermanovics I. The eastern Churchill Province, Torngat and New Québec orogens:an overview[J]. Geoscience Canada, 1990,14(4):217-222. [22] Barrett T J, Wares R P, Fox J S. Two-stage hydrothermal formation of a Lower Proterozoic sediment-hosted massive sulfide deposit, northern Labrador, Quebec[J]. Canadian Mineralogist, 2014, 26(3):871-888. [23] Beaudoin G. Proterozoic Pb isotope evolution in the Belt-Purcell Basin; constraints from syngenetic and epigenetic sulfide deposits[J]. Economic Geology, 1997, 92(3):343-350. [24] Bending J S, Scales W G. New production in the Idaho cobalt belt:a unique metallogenic province[J]. Applied Earth Science, 2001, 110(110):81-87. [25] Gaboury D, Pearson V. Rhyolite geochemical signatures and association with volcanogenic massive sulfide deposits:examples from the Abitibi belt, Canada[J]. Economic Geology, 2008, 103(7):1531-1562. [26] Miller C. Geological and geochemical aspects of the Liontown VHMS deposit North eastern Queensland[J]. Library Home, 1996, 25(4):47-59. [27] Peter J M, Scott S D. Windy Craggy, northwestern British Columbia:the world's largest Besshi-type deposit[J].Economic Geology,1999,94(8):261-295. [28] Lodge R W D, Gibson H L, Stott G M, et al. Geodynamic setting, crustal architecture, and VMS metallogeny of ca. 2.[J]. Canadian Journal of Earth Sciences, 2014, 52(3):196-214. [29] 王登红. 新疆阿舍勒火山岩型块状硫化物铜矿床成矿机制与成矿模式:博士学位论文[D]. 北京:中国地质科学院, 1995. WANG Deng-hong. On the metallogenic mechanism and model of the Ashele volcanogenic massive sulfide copper deposit, Xinjiang:doctor's degree thesis[D]. Beijing:Chinese Academy of Geological Sciences, 1995. [30] Lobanov K, Yakubchuk A, Creaser R A. Besshi-type VMS deposits of the Rudny Altai (Central Asia)[J]. Economic Geology, 2014, 109(5):1403-1430. [31] Lobanov K V, Gaskov I V. The Karchiga copper massive sulfide deposit in the high-grade metamorphosed rocks of the Kurchum block:geologic structure, formation, and metamorphism (Rudny Altai)[J]. Russian Geology & Geophysics, 2012, 53(1):77-91. [32] Kase K, Yamamoto M, 张祖海. 日本三波川带别子型矿床矿石的矿物及地球化学特征[J]. 地球与环境, 1993(2):4-10. Kase K, Yamamoto M, ZHANG Zu-hai. Mineral and geochemical characteristics of Sanbagawa belt Besshi-type deposit, Japan[J]. Earth and Environment, 1993(2):4-10. [33] Lehuray A P. Lead and sulfur isotopes and a model for the origin of the Ducktown Deposit, Tennessee[J]. Economic Geology, 1984, 79(7):1561-1573. [34] 王文广. 别子型块状硫化物矿床的地质特征构造环境及其在我国的找矿意义[J]. 矿产与勘查, 1990(1):17-23. WANG Wen-guang. The geological characteristics of the tectonic environment of Besshi type massive sulfide deposits in China and its prospecting significance[J]. Mineral Exploration, 1990(1):17-23. [35] Fox J S. Besshi-type volcanogenic sulfide deposits:a review[J]. Canadian Mining & Metallurgical Bulletin, 1984, 77(1):57-68. [36] Maghfouri S, Rastad E, Mousivand F. Nudeh deposit, Besshi-type volcanogenic massive sulfide deposit in the Sabzevar back-arc basin[C]//Proceedings of the 33rd National Symposium on Earth Sciences. Tehran:Geological Publishing House, 2012:68-74. [37] Mousivand F, Rastad E, Meffre S, et al. Age and tectonic setting of the Bavanat Cu-Zn-Ag Besshi-type volcanogenic massive sulfide deposit, southern Iran[J]. Mineralium Deposita, 2012, 47(8):911-931. [38] Maghfouri S, Rastad E, Mousivand F, et al. Geology, ore facies and sulfur isotopes geochemistry of the Nudeh Besshi-type volcanogenic massive sulfide deposit, southwest Sabzevar Basin, Iran[J]. Journal of Asian Earth Sciences, 2016, 125:1-21. [39] 慕生禄. 西昆仑昆盖山火山岩构造环境与典型矿床研究:博士学位论文[D]. 北京:中国科学院大学, 2016. MU Sheng-lu. Volcanic rocks tectonic environments and metallogenesis of typical mineral deposits in Kungai mountains, West Kunlun:doctor's degree thesis[D].Beijing:University of Chinese Academy of Sciences, 2016. [40] Barber A, Craw D. Lithology, geochemistry, and structure of Moke Creek sulphide deposit host rocks, Otago Schist, New Zealand[J]. New Zealand Journal of Geology & Geophysics, 2002, 45(2):193-205. [41] Huston D L, Large R R, 王楠. 火山成因块状硫化物矿床中金富集的化学模式[J]. 地球与环境, 1991(1):1-13. Huston D L, Large R R, WANG Nan. Chemical model of gold enrichment in VMS deposits[J]. Earth and Environment, 1991(1):1-13. [42] Peter J M, Layton M D, Piercey S, et al. Volcanic-hosted massive sulphide deposits of the Finlayson Lake District, Yukon[M]. Special Publication 5, Mineral Deposits Division. Ottawa:Geological Association of Canada, 2007:471-508. [43] Sebert C. A note on preliminary lithogeochemistry of the Fire Lake area[J]. Yukon Exploration & Geology, 1998, 1(20):195-203. [44] Nold J L. The Idaho cobalt belt, northwestern United States:a metamorphosed Proterozoic exhalative ore district[J]. Mineralium Deposita, 1990, 25(3):163-168. [45] Kusakabe M, Mayeda S, Nakamura E. S, O and Sr isotope systematics of active vent materials from the Mariana backarc basin spreading axis at 18°N[J]. Earth & Planetary Science Letters, 1990, 100(1):275-282. [46] Peter J M, Scott S D. Fluid inclusion and light stable isotope geochemistry of the Windy Craggy Besshi-type massive sulfide deposit, northwestern British Columbia[J]. Journal of Geological Engineering, 1993, 20:229-248. [47] Sato K, Sasaki A. Lead isotopic feature of the Besshi-type deposits and its bearing on the ore lead evolution.[J]. Geochemical Journal, 1980, 14(6):303-315. [48] Fox J S, Farquhar R, Rui I, et al. Genesis of basalt-hosted massive sulphide deposits from the Trondheim and Sulitjelma districts, Norway:ore lead isotopic considerations[J]. Mineralium Deposita, 1988, 23(4):276-285. [49] 宋学信, 郭月敏, 徐珏,等. 筏子坝别子型铜锌矿床构造环境与演化[J]. 矿床地质, 2002, 21(增刊1):453-458. SONG Xue-xin, GUO Yue-min, XU Yu, et al. Tectonic setting and evolutive model of Besshi-typle Cu-Zn deposit at Faziba, SE Gansu, NE China[J]. Mineral Deposits, 2002, 21(Suppl.1):453-458. |
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通讯作者: 安芳(1984-),副教授,主要从事矿床地球化学方面的研究.E-mail:anfang_china@163.com |
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