吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (4): 1124-1138.doi: 10.13278/j.cnki.jjuese.201604112
石学法1,2, 李兵1, 鄢全树1,2, 叶俊1
Shi Xuefa1,2, Li Bing1, Yan Quanshu1,2, Ye Jun1
摘要:
岛弧-弧后盆地是海底热液硫化物发育的重要环境。本文总结了近几十年对西太平洋地区岛弧-弧后盆地热液活动调查及研究的成果,阐述了岛弧-弧后盆地热液活动的分布规律、构造环境、热液喷口水深和流体温度变化关系、相分离过程以及热液硫化物的金属元素组成特征,分析了成矿元素富集规律和控矿因素。研究认为,随着岛弧-弧后盆地热液喷口所处水深的增加,其最高喷口流体温度也相应增加,这与相分离过程有关;岛弧-弧后盆地热液硫化物与洋中脊硫化物不同,以Fe-Zn-Pb型硫化物为主,显著富集Zn、Pb、Au、Ag等金属元素;热液成矿作用主要受到岛弧及弧后扩张处的岩浆作用、相分离、基岩、弧后扩张速率、沉积物盖层等5类因素的制约。
中图分类号:
[1] Monecke T, Petersen S, Hannington M D. Constraints on Water Depth of Massive Sulfide Formation: Evidence from Modern Seafloor Hydrothermal Systems in Arc-Related Settings[J]. Economic Geology, 2014, 109(8): 2079-2101.[2] Hannington M, Jamieson J, Monecke T, et al. The Abundance of Seafloor Massive Sulfide Deposits[J]. Geology, 2011, 39:1155-1158.[3] Hoagland P, Beaulieu S, Tivey M A, et al. Deep-Sea Mining of Seafloor Massive Sulfides[J]. Marine Policy, 2010, 34(3): 728-732.[4] Kim J, Son S K, Son J W, et al. Venting Sites Along the Fonualei and Northeast Lau Spreading Centers and Evidence of Hydrothermal Activity at an Off-Axis Caldera in the Northeastern Lau Basin[J]. Geochemical Journal, 2009, 43(1): 1-13.[5] Fouquet Y, Charlou J, Stackelberg U V, et al. Metallogenesis in Back-Arc Environments: The Lau Basin Example[J]. Economic Geology (Plus the Bulletin of the Society of Economic Geologists), 1993, 88(8): 2154-2181.[6] Lisitsyn P, Malahoff A, Bogdanov Y A, et al. Hydrothermal Formations in the Northern Part of the Lau Basin, Pacific Ocean[J]. International Geology Review, 1992, 34(8): 828-847.[7] Verati C, Lancelot J, Fouquet Y. Pb Isotope Study of Mineralizations at Oceanic Hydrothermal Vent Fields and Heterogeneities in the North Fiji Back-Arc Basin (SW Pacific)[J]. Comptes Rendus De l Academie Des Sciences Serie Ⅱ, 1994, 319(8): 921-928.[8] Yukihiro N, Jun-Ichiro I, Takayoshi K, et al. Hydrothermal Plumes Along the North Fiji Basin Spreading Axis[J]. Nature, 1989, 342(6250): 667-670.[9] Halbach P, Hansmann W, Köppel V, et al. Whole-Rock and Sulfide Lead-Isotope Data from the Hydrothermal JADE Field in the Okinawa Back-Arc Trough[J]. Mineralium Deposita, 1997, 32(1): 70-78.[10] Kimura M, Uyeda S, Kato Y, et al. Active Hydrothermal Mounds in the Okinawa Trough Back-Arc Basin, Japan[J]. Tectonophysics, 1988, 145(3): 319-324.[11] Scott S D, Binns R A. Hydrothermal Processes and Contrasting Styles of Mineralization in the Western Woodlark and Eastern Manus Basins of the Western Pacific[J]. Geological Society London Special Publications, 1995, 87(1): 191-205.[12] Both R, Crook K, Taylor B, et al. Hydrothermal Chimneys and Associated Fauna in the Manus Back-Arc Basin, Papua New Guinea[J]. Eos, Transactions American Geophysical Union, 1986, 67(21): 489-490.[13] Horibe Y, Kim K R, Craig H. Hydrothermal Methane Plumes in the Mariana Back-Arc Spreading Center[J]. Nature, 1986, 324(6093): 131-133.[14] Baker E T, German C R. On the Global Distribution of Hydrothermal Vent Fields[C]// German C R, Lin J, Parson L M. Mid-Ocean Ridges: Hydrothermal Interactions Between the Lithosphere and Oceans:Geophysical Monograph Series 148.Washington, DC: American Geophysical Union, 2004: 245-266.[15] Beaulieu S E, Baker E T, German C R. Where Are the Undiscovered Hydrothermal Vents on Oceanic Spreading Ridges? [J].Deep Sea Research Part II: Topical Studies in Oceanography, 2015, 121: 202-212.[16] Halbach P Nakamura, Ko-ichi Wahsner M, et al. Probable Modern Analogue of Kuroko-Type Massive Sulphide Deposits in the Okinawa Trough Back-Arc Basin[J]. Nature, 1989, 338:496-499.[17] Iizasa K, Fiske R S, Ishizuka O, et al. A Kuroko-Type Polymetallic Sulfide Deposit in a Submarine Silicic Caldera[J]. Science, 1999, 283(5404):975-977.[18] 侯增谦. 现代与古代海底热水成矿作用[M]. 北京:地质出版社, 2003. Hou Zengqian. Modern and Ancient Submarine Hydrothermal Mineralization[M]. Beijing:Geological Publishing House,2003.[19] Horibe Y, Kim K R, Craig H. Hydrothermal Methane Plumes in the Mariana Back-Arc Spreading Center[J]. Nature, 1986, 324(6093):131-133.[20] Sakai H, Gamo T, Kim E-S, et al. Venting of Carbon Dioxide-Rich Fluid and Hydrate Formation in Mid-Okinawa Trough Back-Arc Basin[J]. Science, 1990,248(4959):1093-1096.[21] Fouquet Y, Stackelberg U, Von Charlou J, et al. Hydrothermal Activity and Metallogenesis in the Lau Back-Arc Basin[J]. Nature, 1991, 349(6312): 778-781.[22] 吴世迎.世界海底热液硫化物资源[M]. 北京:海洋出版社, 2000. Wu Shiying. Global Submarine Hydrothermal Sulfide Resources[M]. Beijing: Ocean Press, 2000.[23] 吴世迎.马里亚纳海槽海底热液烟囱物研究[M]. 北京:海洋出版社, 1995. Wu Shiying. Study of Hydrothermal Chimneys in the Mariana Trough[M] . Beijing: Ocean Press, 1995.[24] 曾志刚. 海底热液地质学[M]. 北京:科学出版社,2011. Zeng Zhigang. Submarine Hydrothermal Geology[M]. Beijing: Science Press, 2011.[25] Beaulieu, Stace E. InterRidge Vents Database[DB/OL]. https://www.interridge. org /zh-hans/IRvents_database, 2015.[26] Koschinsky A, Garbe-Schönberg D, Sander S, et al. Hydrothermal Venting at Pressure-Temperature Conditions Above the Critical Point of Seawater, 5°S on the Mid-Atlantic Ridge[J]. Geology, 2008, 36(8): 615-618.[27] Foustoukos D I , Seyfried W E. Fluid Phase Separation Processes in Submarine Hydrothermal Systems[J]. Reviews in Mineralogy and Geochemistry, 2007, 65(1):213-239.[28] Bischoff J L, Rosenbauer R J. Liquid-Vapor Relations in the Critical Region of the System NaCl-H2O from 380 to 415℃: A Refined Determination of the Critical Point and Two-Phase Boundary of Seawater[J]. Geochimica et Cosmochimica Acta, 1988, 52(8): 2121-2126.[29] Ellis A J, Golding R M. The Solubility of Carbon Dioxide Above 100°C in Water and in Sodium Chloride Solutions[J]. American Journal of Science, 1963, 261:47-60.[30] Hannington M D, Ronde C, Petersen S. Seafloor Tectonics and Submarine Hydrothermal Systems[J]. Economic Geology, 2005,100 : 111-141.[31] Fouquet Y, Cambon P, Etoubleau J, et al. Geodiversity of Hydrothermal Processes Along the Mid-Atlantic Ridge and Ultramafic-Hosted Mineralization: A New Type of Oceanic Cu-Zn-Co-Au Volcanogenic Massive Sulfide Deposit[C]// Peter A Rona, Colin W Devey, Jérôme Dyment, et al. Geophysical Monograph Series 188.Washington, DC: American Geophysical Union , 2010: 321-367.[32] Hannington M D, Alan G, Herzig P M, et al. Comparation of the TAG Mound and Stockwork Complex with Cyprus-Type[J]. Proceedings of the Ocean Drilling Program: Scientific Results, 1998, 158: 389-415.[33] Petersen S, Herzig P M, Hannington M D, et al. Submarine Vein-Type Gold Mineralization Near Lihir Island, New Ireland Fore-Arc, Papua New Guinea[J]. Economic Geology, 2002, 97: 1795-1813.[34] Yang K, Scott S D. Possible Contribution of a Metal-Rich Magmatic Fluid to a Sea-Floor Hydrothermal System[J]. Nature, 1996, 383(6599): 420-423.[35] Susan E Humphris, Robert A Zierenberg, Lauren S Mullineaux, et al. Subseafloor Processes in Mid-Ocean Ridge Hydrothermal Systems[C]//Alt J C. Seafloor Hydrothermal Systems: Physical, Chemical, Biological, and Geological Interactions:Geophysical Monograph Series 91.Washington, D C: American Geophysical Union, 1995: 85-114.[36] 曾志刚, 蒋富清, 翟世奎,等. 冲绳海槽Jade热液活动区块状硫化物的铅同位素组成及其地质意义[J]. 地球化学, 2000, 29(3): 239-245. Zeng Zhigang, Jiang Fuqing, Zhai Shikui, et al. Lead Isotopic Compositions of Massive Sulfides from the Jade Hydrothermal Filed in the Okinawa Trough and Its Geological Implications[J]. Geochimica,2000, 29(3): 239-245. |
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