摘要
四川木里梭罗沟金矿床是产于甘孜-理塘金矿带南端的大型金矿床。矿体产于近东西向断裂控制的构造蚀变带内,矿石类型主要为蚀变蚀变玄武岩矿石、凝灰岩矿石。由深部至浅部,依次发育硅化、黄铁绢英岩化、碳酸盐化蚀变。流体成矿过程包括早、中、晚3个阶段,分别以石英-他形黄铁矿组合、石英-五角十二面体黄铁矿-毒砂组合和石英-碳酸盐±少量立方体黄铁矿组合为标志。矿石矿物主要沉淀于中阶段,五角十二面体黄铁矿和毒砂是主要的载金矿物。早阶段热液石英中发育CO_2-H_2O型包裹体(C型)和水溶液包裹体(W型),中、晚阶段只发育水溶液包裹体(W型)。早阶段流体包裹体均一温度集中于251~371℃,盐度w(NaCleq)为3.3%~13.7%;中阶段流体包裹体均一温度集中于187~294℃,盐度w(NaCleq)为1.6%~13.9%;晚阶段流体包裹体均一温度集中于144~224℃,盐度w(NaCleq)介于0.2%~10.6%之间。估算的早阶段流体捕获压力为102~343 MPa,推测最大成矿深度为10~11 km。上述流体包裹体研究表明,成矿流体由早阶段中高温、富CO_2的变质热液演化至晚阶段的低温、贫CO_2的大气降水热液;流体温度降低、CO_2逃逸是控制成矿物质沉淀的主要因素。矿床地质及流体包裹体特征指示梭罗沟金矿床可能为断控造山型金矿床。
The Suoluogou Au deposit in Muli County of Sichuan Province is a large deposit in the Garze-Litang suture.Au mineralization occurs in the EW-trending fault, and the ores mainly include the altered basalt and tuff. The hydrothermal alteration is intense, ranging from silicification, beresitization to carbonatization with increasing depth. The hydrothermal ore-forming process includes the early, middle and late stages, characterized by mineral assemblages of quartz-allotriomorphic pyrite, quartz-pyritohedron pyrite-arsenopyrite and quartz-carbonate±cubic pyrite, respectively. Ore minerals were mainly precipitated in the middle stage, and the arsenopyrites and pyritohedron pyrites are the main gold-bearing minerals. The hydrothermal minerals in the early stage contain NaClH_2O(W-type) and CO_2-H_2O(C-type) fluid inclusions, while the middle-and late-stage hydrothermal quartz contains only NaCl-H_2O fluid inclusions(W-type). The homogeneous temperatures of the C-type and W-type fluid inclusions in the early stage are generally homogenized at temperatures of 251~371℃, with salinities w(NaCleq) of3.3%~13.7%. In the middle stage, the W-type fluid inclusions mainly have homogeneous temperatures of 187~294℃ and salinities w(NaCleq) of 1.6%~13.9%. W-type fluid inclusions in the late stage are homogenized at temperatures of 144~224℃, with salinities w(NaCleq) of 0.2%~10.6%. The estimated pressures range from 102~343 MPa in the early stage, with the formation depth of 10~11 km. In a word, the ore-forming fluids evolved from middle-high temperature, CO_2-bearing metamorphic fluid to low temperature, CO_2-poor meteoric fluid. It seems that temperature decreasing and CO_2 escaping caused the precipitation of metallogenic materials. The characteristics of the ore geology and fluid inclusions indicated that the Suoluogou Au deposit can be genetically assigned to the orogenic-type ore-system.
引文
Benning L G and Seward T M.1996.Hydrosulphide complexing of Au(I)in hydrothermal solutions from 150~400°C and 500~1500bar[J].Geochimica et Cosmochimica Acta,60(11):1849-1871.
Bodnar R J.1993.Revised equation and table for determining the freezing point depression of H2O-Na Cl solutions[J].Geochimica et Cosmochimica Acta,57(3):683-684.
Bowers T S and Helgson H C.1983.Calculation of the thermodynamic and geochemical consequences of nonideal mixing in the system H2O-CO2-Na Cl on phase relations in geologic systems:Equation of state for H2O-CO2-Na Cl fluids at high pressures and temperatures[J].Geochimica et Cosmochimica Acta,47:1247-1275.
Brown P E.1989.Flincor:A microcomputer program for the reduction and investigation of fluid-inclusion data[J].American Mineralogist,74:1390-1393.
Chen Y J.2006.Orogenic-type deposits and their metallogenic model and exploration potential[J].Geology in China,33:1181-1196(in Chinese with English abstract).
Chen Y J,Pirajno F,Qi J P and Wang H H.2006.Ore geology,fluid geochemistry and genesis of the Shanggong gold deposit,East Qinling Orogen,China[J].Resource Geology,56(2):99-116.
Chen Y J,Ni P,Fan H R,Pirajno F,Lai Y,Su W C and Zhang H.2007.Diagnostic fluid inclusions of different types hydrothermal gold deposits[J].Acta Petrologica Sinica,23:2085-2108(in Chinese with English abstract).
Collins P L F.1979.Gas hydrates in CO2-bearing fluid inclusions and the use of freezing data for estimation of salinity[J].Econ.Geol.,74:1435-1444.
Deng J and Wang Q F.2016.Gold mineralization in China:Metallogenic provinces,deposit types and tectonic framework[J].Gondwana Research,36:219-274.
Du J R.2012.Geological character and primary study of genesis about the Suoluogou gold deposit,Muli County,Sichuan Province(Master degree thesis)[D].Chengdu:Chengdu University of Technology.1-59(in Chinese with English abstract).
Fan H R,Zhai M G,Xie Y H and Yang J H.2003.Ore-forming fluids associated with granite-hosted gold mineralization at Sanshandao deposit,Jiaodong gold province,China[J].Mineralium Deposita,38:739-750.
Fu X F and Ying H L.2003.Cenozoic tectonic movement and its relationship with gold mineralization in the northern segment of the Garze-Litang fault belt[J].Geology in China,30(4):413-418(in Chinese with English abstract).
Gibert F,Pascal M L and Pichavant M.1993.Solubility of gold in KC1(0.5 m)solution under hydrothermal conditions(350~450°C,500bar)(abstr.)[M].In:Cuney M and Cathelineau M,eds.Proc.4th International symposium on hydrothermal reactions[C].Institut Lorrain des Geoscience,65-68.
Goldfarb R J,Baker T,Dube B,Groves D I,Hart C J R and Gosselin P.2005.Distribution,character,and genesis of gold deposits in metamorphic terranes[J].Economic Geology 100th Anniversary Volume,407-450.
Groves D I,Goldfarb R J,Robert F and Hart C J R.2003.Gold deposits in metamorphic belts:Overview of current understanding,outstanding problems,future research,and exploration significance[J].Econ.Geol.,98:1-29.
Hagemann S G and Luders V.2003.P-T-X conditions of hydrothermal fluid and precipitation mechanism of stibnite-gold mineralization and the Wiluna lode-gold deposits,Western Australia:Conventional and infrared microthermometric constrains[J].Mineralium Deposita,38:936-952.
Hou Z Q,Qu X M,Zhou J R,Yang Y Q,Huang D H,LüQ T,Tang S H,Yu J J,Wang H P and Zhao J H.2001.Col1ision-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).
Huan W J,Li N,Yuan W M,Gong Q J,Zhang J and Wang Q F.2013.Fission track constrain on mineralization time and tectonic events in Ganzi-Litang gold belt,Tibet Plateau[J].Acta Petrologica Sinica,29(4):1338-1346(in Chinese with English abstract).
Kerrich R,Goldfarb R J,Groves D,Garwin S and Jia Y F.2000.The characteristics,origins and geodynamic settings of supergiant gold metallogenic provinces[J].Science in China Series D,43(Supp.):1-68.
Liu S S,Fan W Y,Nie F,Liu W W and Wang X F.2015.Geological characteristics and ore-controlling factors analysis of Suoluogou gold deposit,Muli County,Sichuan Province[J].Gold,6(36):8-13(in Chinese with English abstract).
Liu Y S,He Z W,Long X J and Feng X L.2011.Extraction of remote sensing alteration information and analysis of ore-searching Prospect in Jianglang Dome metallogenic zone[J].Journal of Sichuan Normal University(Natural Science),34(2):267-272(in Chinese with English abstract).
Lu H Z,Fan H R,Ni P,Ou G X,Shen K and Zhang W H.2004.Fluid inclusion[M].Beijing:Science Press(in Chinese).
Mernagh T P,Bastrakov E N,Zaw K,Wygralak A S and Wyborn L A I.2007.Comparison of fluid inclusion data and mineralization processes for Australian orogenic gold and intrusion-related gold systems[J].Acta Petrologica Sinica,23(1):21-32.
Pan G T,Chen Z L and Li X Z.1997.Geological-Tectonic evolution in the Eastern Tethys[M].Beijing:Geological Publishing House.23-29(in Chinese)
Wang Z C,Gou Y D,Fan X and Luo T.2012.Typomorphic characteristics and its geological significance from pyrite of the Suoluogou gold deposit,Muli County,Sichuan Province[J].Computing Techniques for Geophysical and Geochemical Exploration,34(6):729-735(in Chinese with English abstract).
Wei Y F and Luo S L.2003.Geological features of ophiolite in the middle Garze-Litang plate junction[J].Acta Geologica Sichuan,23(3):134-140(in Chinese with English abstract).
Wei Y F and Luo S L.2004.Division and composition of the non-Smithian strata in the middle part of the Garze-Litang suture zone,western Sichuan[J].Sedimentary Geology and Tethyan Geology,24(4):21-30(in Chinese with English abstract).
Xiao J,Sun C M,Liu Y S,Ma Z N,Yang H Z,Zhou Q L and Sun Y.2008.Wallrock alteration and relationwith gold mineralization of Ajialongwa gold deposit in the central Ganzi-Litang fault zone,Sichuan[J].Geology and Prospecting,44(6):8-12(in Chinese with English abstract).
Yan N,Zhang J,Yuan W M,Gong Q J,Wang Q F and Luo J H.2013.Characteristics of isotopic geochemistry and metallogenesis of the Gala gold deposit in Ganzi-Litang suture zone,western Sichuan Province,China[J].Acta Petrologica Sinica,29(4):1347-1357(in Chinese with English abstract).
Yan Z G.2006.Geological characteristics of gold deposits in GanziLitang fault and preliminary discussion on their ore control factors[J].Contributions to Geology and Mineral Resources Research,21:52-57(in Chinese with English abstract).
Yang W S,Hu Z W and He D R.2007.Geochemical model for mineral prospecting of the Ajialongwa gold deposit in the central segment of the Garzê-Litang fault zone in Sichuan[J].Geology in China,34(1):123-131(in Chinese with English abstract).
Yang Y P and Yang L Y.2007.Geological features and prospecting potential of the Ajialongwa-Yahuo Au-(Cu)ore zone,Litang,Sichuan[J].Acta Geologica Sichuan,27(3):170-76(in Chinese with English abstract).
Yu A G,Lu M G,Song X H and Liu W W.2014.Geological features of the Suoluogou Au deposit in Muli,Sichuan[J].Acta Geologica Sichuan,34(4):514-516(in Chinese with English abstract).
Zhang L T,Yuan W M,Li N,Huan W J,Zhang J,Wang Q F and Gong Q J.2015.Apatite fission track constrains on tectonic activities in Ganzi-Litang gold belt,Qinghai-Tibet Plateau[J].Acta Petrologica Sinica,31(11):3353-3362(in Chinese with English abstract).
Zhang W L,Cao H W,Yang Z M,Xi X Y,Liu W W,Peng S M and Zheng L.2015.Geochemical characteristics and genesis of lamprophyres of the Cenozoic from the Suoluogou gold deposit,Sichuan Province,China[J].Bulletin of Mineralogy,Petrology and Geochemistry,34(1):110-119(in Chinese with English abstract).
Zhang Y,Wang Q F,Zhang J,Gong Q J and Cheng W B.2012.Geological characteristics and genesis of Ajialongwa gold deposit in Ganzi-Litang suture zone,West Sichuan[J].Acta Petrologica Sinica,28(2):691-701(in Chinese with English abstract).
Zotov A V and Baranova N N.1995.The solubility of Au2S and AuAg S in near-neutral sulphide solutions at temperatures of 25 and80°C and pressures of 1 and 500 bars[A].In:Kharaka Y K and Chudaev O V,eds.Water-rock interaction-8[M].Balkema Press.773-776.
陈衍景.2006.造山型矿床、成矿模式及找矿潜力[J].中国地质,33:1181-1196.
陈衍景,倪培,范宏瑞,Pirajno F,赖勇,苏文超,张辉.2007.不同类型热液金矿系统的流体包裹体特征[J].岩石学报,23(9):2085-2108.
杜金锐.2012.四川梭罗沟金矿床地质特征与成因初探[D].硕士学位论文,成都:成都理工大学.1-59.
付小方,应汉龙.2003.甘孜-理塘断裂带北段新生代构造特征及金矿成矿作用[J].中国地质,30(4):413-418.
侯增谦,曲晓明,周继荣,杨岳清,黄典豪,吕庆田,唐绍华,余今杰,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[J].地质学报,75(4):484-497.
郇伟静,李娜,袁万明,龚庆杰,张静,王庆飞.2013.四川甘孜-理塘金成矿带成矿时代与构造活动的裂变径迹研究[J].岩石学报,29(4):1338-1346.
刘书生,范文玉,聂飞,刘文武,王显峰.2015.四川木里梭罗沟金矿地质特征及控矿因素分析[J].黄金,6(36):8-13.
刘严松,何政伟,龙晓君,冯孝良.2011.江浪穹隆成矿区遥感蚀变信息提取及找矿远景分析[J].四川师范大学学报(自然科学版),34(2):267-272.
卢焕章,范宏瑞,倪培,欧光习,沈昆,张文淮.2004.流体包裹体[M].北京:科学出版社.1-487.
潘桂棠,陈智梁,李兴振.1997.东特提斯地质构造形成演化[M].北京:地质出版社.23-29.
王兆成,勾永东,范晓,罗涛.2012.四川木里梭罗沟金矿黄铁矿标型特征及地质意义[J].物化探计算技术,34(6):729-735.
魏永峰,罗森林.2003.甘孜-理塘结合带中段蛇绿岩的地质特征[J].四川地质学报,23(3):134-140.
魏永峰,罗森林.2004.甘孜-理塘结合带中段非史密斯地层的划分及组分特征[J].四川地质学报,24(4):21-30.
肖军,孙传敏,刘严松,马子宁,杨弘忠,周庆磊,孙遥.2008.四川甘孜-理塘断裂带中段阿加隆洼金矿围岩蚀变特征及与金矿化关系[J].地质与勘探,44(6):8-12.
燕旎,张静,袁万明,龚庆杰,王庆飞,罗建宏.2013.川西甘孜-理塘结合带嘎拉金矿床同位素特征及成矿作用研究[J].岩石学报,29(4):1347-1357.
晏子贵.2006.甘孜-理塘断裂带金矿成矿地质特征和控矿因素浅析[J].地质找矿论丛,21(增刊):52-57.
杨伟寿,胡正文,何德润.2007.四川甘孜-理塘断裂带中段阿加隆洼金矿床地球化学找矿模式[J].中国地质,34(1):123-131.
杨永鹏,杨露云.2007.四川理塘阿加隆洼-亚火金(铜)矿带地质特征及找矿前景[J].四川地质学报,27(3):170-76.
喻安光,卢玫瑰,宋晓华,刘文武.2014.四川木里梭罗沟金矿床特征[J].四川地质学报,34(4):514-516.
张丽婷,袁万明,李娜,郇伟静,张静,王庆飞,龚庆杰.2015.甘孜-理塘金成矿带构造活动的磷灰石裂变径迹年代学制约[J].岩石学报,31(11):3353-3362.
张文林,曹华文,杨志民,席孝义,刘文武,彭仕冕,郑硌.2015.四川梭罗沟大型金矿区新生代碱性煌斑岩脉地球化学特征及其地质意义[J].矿物岩石地球化学通报,34(1):110-119.
张玙,王庆飞,张静,龚庆杰,程文斌.2012.川西甘孜-理塘缝合带阿加隆洼金矿床地质特征及成因探讨[J].岩石学报,28(2):691-701.