河南磨沟金矿床成因:地质、流体包裹体和H-O-S稳定同位素约束
|
摘要
豫西熊耳山地区的磨沟金矿床赋存于熊耳群火山岩中,矿体受NE向断裂控制。通过对矿区的地质特征、流体包裹体以及H-O-S稳定同位素研究,探讨磨沟金矿床的成矿物质、流体来源及成因机制。成矿期可划分为石英-黄铁矿、石英-多金属硫化物以及石英-碳酸盐3个阶段。流体包裹体有纯CO_2型、CO_2-H_2O型和H_2O-NaCl型3种。成矿流体具有中温(210℃~310℃)、低盐度(NaCl质量分数为3%~12%)的特征,成矿深度小于9km。氢、氧同位素分别为-107‰~-88‰和-1.7‰~4.3‰,硫同位素为-0.98‰~5.62‰。磨沟金矿床成矿流体主要为变质流体来源,晚阶段有大气降水参与;成矿物质主要来自变质结晶基底;属于造山型金矿床。
The ore bodies of Mogou Au deposit in the Xiong'er Mountains,western Henan Province,are controlled by the NE faults and hosted in volcanic rocks of the Xiong'er Group.On the basis of the geological characteristics,fluid inclusions and H-O-S stable isotope data,the metal and fluid sources,and ore-forming genesis of the Mogou Au deposit are studied.The hydrothermal activities ofmineralization can be divided into three stages:quartz-pyrite stage,quartz-polymetallic sulfide stage and quartz-carbonate vein stage.There are three types of fluid inclusions in the auriferous quartz veins,including the pure carbonic type, CO_2-H_2O type and H_2O-NaCl type inclusions.Homogenization temperature values obtained from the inclusions range from 210℃ to 310℃,corresponding to salinity values of fluid inclusions of 3%~12%,and the ore-forming depth is less than 9 km.The δDV-SMOW values range from -107‰ to -88‰,corresponding to δ~(18) O_(H_2O) values of-1.7‰~4.3‰,and δ~(34) SCDTvalues range from -0.98‰ to 5.62‰.H-O isotope results indicate that the ore-forming fluids are derived from metamorphic fluid,with minor meteoric water during the late stage,and S isotope data show that the ore-forming material is originated from metamorphic crystalline basement.Geological and fluid features and stable isotope results suggest that the Mogou Au deposit is an orogenic type gold deposit.
The ore bodies of Mogou Au deposit in the Xiong'er Mountains,western Henan Province,are controlled by the NE faults and hosted in volcanic rocks of the Xiong'er Group.On the basis of the geological characteristics,fluid inclusions and H-O-S stable isotope data,the metal and fluid sources,and ore-forming genesis of the Mogou Au deposit are studied.The hydrothermal activities ofmineralization can be divided into three stages:quartz-pyrite stage,quartz-polymetallic sulfide stage and quartz-carbonate vein stage.There are three types of fluid inclusions in the auriferous quartz veins,including the pure carbonic type, CO_2-H_2O type and H_2O-NaCl type inclusions.Homogenization temperature values obtained from the inclusions range from 210℃ to 310℃,corresponding to salinity values of fluid inclusions of 3%~12%,and the ore-forming depth is less than 9 km.The δDV-SMOW values range from -107‰ to -88‰,corresponding to δ~(18) O_(H_2O) values of-1.7‰~4.3‰,and δ~(34) SCDTvalues range from -0.98‰ to 5.62‰.H-O isotope results indicate that the ore-forming fluids are derived from metamorphic fluid,with minor meteoric water during the late stage,and S isotope data show that the ore-forming material is originated from metamorphic crystalline basement.Geological and fluid features and stable isotope results suggest that the Mogou Au deposit is an orogenic type gold deposit.
引文
[1]王伟,刘继顺,何美香,等.豫西金矿地质特征与构造控矿探讨[J].西北地质,2014,47(3):62-69.Wang W,Liu J S,He M X,et al.Discussion on geologic characteristics and structural ore-control of the gold deposits in western Henan[J].Northwestern Geology,2014,47(3):62-69.(in Chinese)
[2]王义天,毛景文,卢欣祥.嵩县祁雨沟金矿成矿时代的40 Ar-39 Ar年代学证据[J].地质论评,2001,47(5):551-555.Wang Y T,Mao J W,Lu X X.40 Ar-39 Ar and geochronological constraints on the ore-forming epoch of the Qiyugou gold deposit in Songxian County,Henan Province[J].Geological Review,2001,47(5):551-555.(in Chinese)
[3]Chen Y J,Pirajno F,Qi J P,et al.Ore geology,fluid geochemistry and genesis of the Shanggong gold deposit,Eastern Qinling Orogen,China[J].Resource Geology,2006,56(2):99-116.
[4]周珂,叶会寿,毛景文,等.豫西鱼池岭斑岩型钼矿床地质特征及其辉钼矿铼-锇同位素年龄[J].矿床地质,2009,28(2):170-184.Zhou K,Ye H S,Mao J W,et al.Geological characteristics and molybdenite Re-Os isotopic dating of Yuchiling porphyry Mo deposit in western Henan Province[J].Mineral Deposits,2009,28(2):170-184.(in Chinese)
[5]毛景文,郑榕芬,叶会寿,等.豫西熊耳山地区沙沟银铅锌矿床成矿的40 Ar-39 Ar年龄及其地质意义[J].矿床地质,2006,25(4):359-368.Mao J W,Zheng R F,Ye H S,et al.40 Ar-39 Ar dating of fuchsite and sericite from altered rocks close to ore veins in Shagou large-size Ag-Pb-Zn deposit of Xiongershan area,western Henan Province,and its significance[J].Mineral Deposits,2006,25(4):359-368.(in Chinese)
[6]叶会寿.华北陆块南缘中生代构造演化与铅锌银成矿作用[D].北京:中国地质科学院,2006.Ye H S.The Mesozoic Tectonic Evolution and PbZn-Ag Mineralization in South Margin of North China Craton[D].Beijing:Chinese Academy of Geological Sciences,2006.(in Chinese)
[7]Cao M P,Yao J M,Deng X H,et al.Diverse and multistage Mo,Au,Ag-Pb-Zn and Cu deposits in the Xionger Terrane,East Qinling:From Triassic Cu mineralization[J].Ore Geology Reviews,2017,81(2):565-574.
[8]范宏瑞,谢奕汉,王英兰.豫西花山花岗岩岩浆热液的性质及与金成矿的关系[J].岩石学报,1993,9(2):136-145.Fan H R,Xie Y H,Wang Y L.The properties of magmatic hydrothermal fluid of Huashan granitic batholith in western Henan Province and their relationship to gold mineralization[J].Acta Petrologica Sinica,1993,9(2):136-145.(in Chinese)
[9]范宏瑞,谢奕汉.豫西熊耳山地区岩石和金矿床稳定同位素地球化学研究[J].地质找矿论丛,1994,9(1):54-64.Fan H R,Xie Y H.Stable isotope geochemistry of rocks and gold deposit in the Xiongershan area,western Henan Province[J].Contributions to Geology and Mineral Resources Research,1994,9(1):54-64.(in Chinese)
[10]付治国,瓮纪昌,卢欣祥.小秦岭-熊耳山地区金矿硫同位素地球化学特征[J].物探与化探,2009,33(5):507-514.Fu Z G,Weng J C,Lu X X.Sulfur isotope geochemical characteristics of gold deposit in Xiaoqinling-Xionger Mountain area[J].Geophysical and Geochemical Exploration,2009,33(5):507-514.(in Chinese)
[11]王团华,谢桂青,叶安旺,等.豫西小秦岭-熊耳山地区金矿成矿物质来源研究——兼论中基性岩墙与金成矿作用关系[J].地球学报,2009,30(1):27-38.Wang T H,Xie G Q,Ye A W,et al.Material sources of gold deposits in Xiaoqinling-Xiongershan area of western Henan Province as well as the relationship between gold deposits and intermediatebasic dyke[J].Acta Geosicientia Sinica,2009,30(1):27-38.(in Chinese)
[12]卢欣祥,尉向东,于在平,等.小秦岭-熊耳山地区金矿的成矿流体特征[J].矿床地质,2003,22(4):377Lu X X,Yu X D,Yu Z P,et al.Characteristics of ore-forming fluids in gold deposits of XiaoqinlingXiongershan area[J].Mineral Deposits,2003,22(4):377-385.(in Chinese)
[13]卢欣祥.小秦岭-熊耳山地区金矿特征与地幔流体[M].北京:地质出版社,2004.Lu X X.The Characteristics of Gold Deposits and Mantle Fluid in Xiaoqinling-Xiongershan Area[M].Beijing:Geological Publishing House,2004.(in Chinese)
[14]Deng J,Yuan W M,Carranza E J M,et al.Geochronology and thermochronometry of the Jiapigou gold belt,northeastern China:New evidence for multiple episodes of mineralization[J].Journal of Asian Earth Sciences,2014,89(3):10-27.
[15]Wang C M,Bagas L,Lu Y J,et al.Terrane boundary and spatio-temporal distribution of ore deposits in the Sanjiang Tethyan Orogen:Insights from zircon Hf-isotopic mapping[J].Earth-Science Reviews,2016,156:39-65.
[16]廖诗进,宁勇.河南磨沟金矿床地质特征及找矿方向[J].地质调查与研究,2010,33(2):142-148.Liao S J,Ning Y.Geological characteristics and ore prospecting of the Mogou gold deposit,Henan Province[J].Geological Survey and Research,2010,33(2):142-148.(in Chinese)
[17]卢焕章,郭迪江.流体包裹体研究的进展和方向[J].地质论评,2000,46(4):385-392.Lu H Z,Guo D J.Progress and trends of researches on fluid inclusions[J].Geological Review,2000,46(4):385-392.(in Chinese)
[18]倪培,蒋少涌,凌鸿飞,等.流体包裹体面的研究背景、现状及发展前景[J].地质论评,2001,47(4):398-404.Ni P,Jiang S Y,Ling H F,et al.The background,application and development of fluid inclusion planes research[J].Geological Review,2001,47(4):398-404.(in Chinese)
[19]池国祥,周义明,卢焕章.当前流体包裹体研究和应用概况[J].岩石学报,2003,19(2):201-212.Chi G X,Zhou Y M,Lu H Z.An overview on current fluid-inclusion research and application[J].Acta Petrologica Sinica,2003,19(2):201-212.(in Chinese)
[20]周慧,郗爱华,熊益学,等.流体包裹体的研究进展[J].矿物学报,2013,33(1):92-100.Zhou H,Xi A H,Xiong Y X,et al.Progress in the research on fluid inclusions[J].Acta Mineralogica Sinica,2013,33(1):92-100.(in Chinese)
[21]Farber K,Dziggel A,Meyer F M,et al.Fluid inclusion analysis of silicified Paleoarchean oceanic crust-A record of Archaean seawater[J].Precambrian Research,2015,266:150-164.
[22]Terrence M.A review of fluid inclusions in diagenetic systems[J].Acta Geologica Sinica,2015,89(3):697-714.
[23]郑永飞.稳定同位素体系理论模式及其矿床地球化学应用[J].矿床地质,2001,20(1):57-70.Zheng Y F.Theoretical modeling of stable isotope systems and its applications to geochemistry of hydrothermal ore deposits[J].Mineral Deposits,2001,20(1):57-70.(in Chinese)
[24]Tang K F,Li J W,Selby D,et al.Geology,mineralization,and geochronology of the Qianhe gold deposit,Xiongershan area,southern North China Craton[J].Mineralium Deposita,2013,48(6):729-747.
[25]Dong Y P,Santosh M.Tectonic architecture and multiple orogeny of the Qinling Orogenic Belt,Central China[J].Gondwana Research,2016,29(1):1-40.
[26]Wang C M,Deng J,Bagas L,et al.Zircon Hfisotopic mapping for understanding crustal architecture and metallogenesis in the Eastern Qinling Orogen[J].Gondwana Research,2017,50:293-310.
[27]张国伟,张本仁,袁学诚,等.秦岭造山带与大陆动力学[M].北京:科学出版社,2001.Zhang G W,Zhang B R,Yuan X C,et al.Qinling Orogenic Belt and Continental Dynamics[M].Beijing:Science Press,2001.(in Chinese)
[28]刘红樱,胡受奚,周顺之.豫西马超营断裂带的控岩控矿作用研究[J].矿床地质,1998,17(1):70-81.Liu H Y,Hu S X,Zhou S Z.A study of rockcontrolling and ore-controlling role of the Machaoying fault in western Henan[J].Mineral Deposits,1998,17(1):70-81.(in Chinese)
[29]张元厚,张世红,韩以贵,等.华熊地块马超营断裂走滑特征及演化[J].吉林大学学报(地球科学版),2006,36(2):169-176.Zhang Y H,Zhang S H,Han Y G,et al.Strik-slip features of the Machaoying fault zone and its evolution in the Huaxiong terrane,southern North China Craton[J].Journal of Jilin University(Earth Science Edition),2006,36(2):169-176.(in Chinese)
[30]卿敏,陈祥,关连绪.金矿与花岗岩类关系的“同源说”——以豫西外方山地区为例[J].黄金地质,1997,3(3):30-35.Qing M,Chen X,Guan L X.The theory of“cognate genesis”about relationships between granitoids and gold deposits:Taking example of Waifangshan area,western Henan Province[J].Gold Geology,1997,3(3):30-35.(in Chinese)
[31]卢仁,梁涛,白凤军,等.豫西磨沟正长岩LA-ICPMS锆石U-Pb年代学及Hf同位素[J].地质论评,2013,59(2):355-368.Lu R,Liang T,Bai F J,et al.LA-ICP-MS zircon age and Hf isotope composition of Mogou syenite,western Henan Province[J].Geological Review,2013,59(2):355-368.(in Chinese)
[32]郭保健,李永峰,王志光,等.熊耳山Au-Ag-Pb-Mo矿集区成矿模式与找矿方向[J].地质与勘探,2005,41(5):43-47.Guo B J,Li Y F,Wang Z G,et al.Type metallogenetic regularities mineralization and prospecting proposal in the Xiongershan district[J].Geology and Prospecting,2005,41(5):43-47.(in Chinese)
[33]Kr9ner A,Compston W,Zhang G W,et al.Age and tectonic setting of late Archean greenstonegneiss terrain in Henan Province,China,as revealed by single-grain zircon dating[J].Geology,1988,16:211-215.
[34]薛良伟,原振雷,张荫树,等.鲁山太华群Sm-Nd同位素年龄及其意义[J].地球化学,1995,24(增刊1):92-97.Xue L W,Yuan Z L,Zhang Y S,et al.The Sm-Nd isotope age of Taihua Group in Lushan area and their implications[J].Geochimica,1995,24(S1):92-97.(in Chinese)
[35]倪志耀,王仁民,童英,等.河南洛宁太华岩群斜长角闪岩的锆石207 Pb/206 Pb和角闪石40 Ar/39 Ar年龄[J].地质论评,2003,49(4):361-366.Ni Z Y,Wang R M,Tong Y,et al.207Pb/206Pb age of zircon and 40 Ar/39 Ar of amphibole from plagioclase amphibolite in the Taihua Group,Luoning,Henan,China[J].Geological Review,2003,49(4):361-366.(in Chinese)
[36]杨长秀.河南鲁山地区早前寒武纪变质岩系的锆石SHRIMP U-Pb年龄、地球化学特征及环境演化[J].地质通报,2008,27(4):517-533.Yang C X.Zircon SHRIMP U-Pb ages,geochemical characteristics and environmental evolution of the early Precambrian metamorphic series in the Lushan area,Henan,China[J].Geological Bulletin of China,2008,27(4):517-533.(in Chinese)
[37]侯万荣,肖荣阁,张汉成,等.熊耳裂谷火山岩系金-多金属矿床成矿模式[J].黄金地质,2003,9(2):22Hou W R,Xiao R G,Zhang H C,et al.The genesis model of the gold-polymetal deposit from the volcanic rocks in the Xionger rift[J].Gold Geology,2003,9(2):22-27.(in Chinese)
[38]任富根,丁士应,李增慧,等.豫西元古宙盆岭构造及其形成机制[J].中国区域地质,1996(3):239-243.Ren F G,Ding S Y,Li Z H,et al.The Proterozoic basin-range structure and its formation mechanism,western Henan[J].Regional Geology of China,1996(3):239-243.(in Chinese)
[39]赵太平,周美夫,金成伟,等.华北陆块南缘熊耳群形成时代讨论[J].地质科学,2001,36(3):326-334.Zhao T P,Zhou M F,Jin C W,et al.Discussion on age of the Xionger Group in southern margin of Northern China Craton[J].Chinese Journal of Geology,2001,36(3):326-334.(in Chinese)
[40]赵太平,翟明国,夏斌,等.熊耳群火山岩锆石SHRIMP年代学研究:对华北克拉通盖层发育初始时间的制约[J].科学通报,2004,49(22):2342-2349.Zhao T P,Zhai M G,Xia B,et al.The study of Zircon SHRIMP geochronology about the Precambrian volcano rock:Constraints on the overlying strata developmental initial time,North China Craton[J].Chinese Science Bulletin,2004,49(22):2342-2349.(in Chinese)
[41]王长明,邓军,张寿庭.河南熊耳山地区花山花岗岩与金矿化的关系[J].现代地质,2006,20(2):315-321.Wang C M,Deng J,Zhang S T.Relationship between Huashan granite and gold mineralization in Xiongershan area,Henan[J].Geoscience,2006,20(2):315-321.(in Chinese)
[42]Peng P,Zhai M G,Ernst R E,et al.A 1.78Ga large igneous province in the North China Craton:The Xionger volcanic province and the North China dyke swarm[J].Lithos,2008,101(3/4):260-280.
[43]柳晓艳,蔡剑辉,阎国翰.华北克拉通南缘熊耳群眼窑寨组次火山岩岩石地球化学与年代学研究及其意义[J].地质学报,2011,85(7):1134-1145.Liu X Y,Cai J H,Yan G H.Lithogeochemistry and geochronology of Xionger Group Yanyaozhai subvolcanics in the southern margin of the North China Craton and their geological significance[J].Acta Geologica Sinica,2011,85(7):1134-1145.(in Chinese)
[44]Deng X H,Chen Y J,Santosh M,et al.Genesis of the 1.76 Ga Zhaiwa Mo-Cu and its link with the Xionger volcanism in the North China Craton:Implications for accretionary growth along the margin of the Columbia supercontinent[J].Precambrian Research,2013,227:337-348.
[45]Wang C M,Lu Y,He X Y,et al.The Paleoproterozoic diorite dykes in the southern margin of the North China Craton:Insight into rift-related magmatism[J].Precambrian Research,2016,277:26-46.
[46]He Y H,Zhao G C,Sun M,et al.SHRIMP and LA-ICP-MS zircon geochronology of the Xionger volcanic rocks:Implications for the PaleoMesoproterozoic evolution of the southern margin of the North China Craton[J].Precambrian Research,2009,174(3/4):213-222.
[47]赵太平,徐勇航,翟明国.华北陆块南部元古宙熊耳群火山岩的成因与构造环境:事实与争议[J].高校地质学报,2007,13(2):191-206.Zhao T P,Xu Y H,Zhai M G.Petrogenesis and tectonic setting of the Paleoproterozoic Xionger Group in the Southern part of the North China Craton:A review[J].Geological Journal of China Universities,2007,13(2):191-206.(in Chinese)
[48]杨东潮,庞绪成,宗静,等.豫西嵩县南部鸡蛋坪组岩石地球化学特征及其成因意义[J].河南理工大学学报(自然科学版),2012,31(6):679-686.Yang D C,Pang X C,Zong J,et al.Geochemistry characteristic and cause of formation of Jidanping Fm rock,south Song County of western Henan[J].Journal of Henan Polytechnic University(Natural Science),2012,31(6):679-686.(in Chinese)
[49]王卫星,邓军,龚庆杰,等.豫西熊耳山五丈山、花山、合峪花岗岩体与金成矿关系[J].黄金,2010,31(4):12-17.Wang W X,Deng J,Gong Q J,et al.Relationship of Wuzhangshan,Huashan and Heyu granite rock mass with gold mineralization,in Xiongershan area,western Henan Province[J].Gold,2010,31(4):12-17.(in Chinese)
[50]李诺,陈衍景,孙亚莉,等.河南鱼池岭钼矿床辉钼矿铼-锇同位素年龄及地质意义[J].岩石学报,2009,25(2):413-421.Li N,Chen Y J,Sun Y L,et al.Molybdenite ReOs isochron age of the Yuchiling porphyry Mo deposit,Henan Province and its geological implications[J].Acta Petrologica Sinica,2009,25(2):413-421.(in Chinese)
[51]Li N,Chen Y J,Pirajno F,et al.LA-ICP-MS zircon U-Pb dating,trace element and Hf isotope geochemistry of the Heyu granite batholith,eastern Qinling,central China:Implications for Mesozoic tectono-magmatic evolution[J].Lithos,2012,142(6):34-47.
[52]Deng J,Gong Q J,Wang C M,et al.Sequence of late Jurassic-early Cretaceous magmatichydrothermal events in the Xiongershan region,Central China:An overview with new zircon U-Pb geochronology data on quartz porphyries[J].Journal of Asian Earth Sciences,2014,79:161-172.
[53]李永峰.豫西熊耳山地区中生代花岗岩类时空演化与钼(金)成矿作用[D].北京:中国地质大学档案馆,2005.Li Y F.The Temporal-spatial Evolution of Mesozoic Granitoids in the Xiongershan Area and Their Relationships to Molybdenum-Gold Mineralization[D].Beijing:The Archive of China University of Geosciences,2005.(in Chinese)
[54]Mao J W,Xie G Q,Pirajno F,et al.Late Jurassicearly Cretaceous granitoid magmatism in Eastern Qinling,central-eastern China:SHRIMP zircon UPb ages and tectonic implications[J].Australian Journal of Earth Sciences,2010,57(1):51-78.
[55]郭波,朱赖民,李犇,等.华北陆块南缘华山和合峪花岗岩岩体锆石U-Pb年龄、Hf同位素组成与成岩动力学背景[J].岩石学报,2009,25(2):265-281.Guo B,Zhu L M,Li B,et al.Zircon U-Pb age and Hf composition of the Huashan and Heyu granite plutons at the southern margin of North China Craton:Implications for geodynamic setting[J].Acta Petrologica Sinica,2009,25(2):265-281.(in Chinese)
[56]高昕宇,赵太平,原振雷,等.华北陆块南缘中生代合峪花岗岩的地球化学特征与成因[J].岩石学报,2010,26(12):3485-3506.Gao X Y,Zhao T P,Yuan Z L,et al.Geochemistry and petrogenesis of the Heyu batholith in the southern margin of the North China Block[J].Acta Petrologica Sinica,2010,26(12):3485-3506.(in Chinese)
[57]Wang C M,Chen L,Bagas L,et al.Characterization and origin of the Taishanmiao aluminous A-type granites:Implications for early Cretaceous lithospheric thinning at the southern margin of the North China Craton[J].International Journal of Earth Sciences,2016,105(5):1563-1589.
[58]吴发富,龚庆杰,石建喜,等.熊耳山矿集区金矿控矿地质要素分析[J].地质与勘探,2012,48(5):865-875.Wu F F,Gong Q J,Shi J X,et al.Ore-controlling factors of the gold deposits in the Xiongershan gold region,western Henan Province[J].Geology and Exploration,2012,48(5):865-875.(in Chinese)
[59]Hall D L,Sterner S M,Bodnar R J.Freezing point depression of NaCl-KCl-H2O solutions[J].Economic Geology,1988,83(1):197-202.
[60]Brown P E.Flincor:A microcomputer program for the reduction and investigation of fluid inclusion data[J].American Mineralogist,1989,74:1390-1393.
[61]Brown P E,Lamb W M.P-V-T properties of fluids in the system H2O±CO2±NaCl:New graphical presentations and implications for fluid inclusion studies[J].Geochimica et Cosmochimica Acta,1989,53(6):1209-1221.
[62]孙丰月,金巍,李碧乐,等.关于脉状热液金矿床成矿深度的思考[J].长春科技大学学报,2000,30(增刊1):27-29.Sun F Y,Jin W,Li B L,et al.Considerations on the mineralizing depth of hydrothermal lode gold deposits[J].Journal of Changchun University of Science and Technology,2000,30(S1):27-29.(in Chinese)
[63]万德芳,樊天义,田世洪.用金属铬法分析微量水和有机质氢同位素组成[J].地球学报,2005,26(增刊1):35-38.Wan D F,Fan T Y,Tian S H.The Chromium analytical technique for hydrogen isotope[J].Acta Geoscientica Sinica,2005,26(S1):35-38.(in Chinese)
[64]Clayton R N,ONeil J R,Mayeda T K.Oxygen isotope exchange between quartz and water[J].Journal of Geophysical Research Atmospheres,1972,77(17):3057-3067.
[65]Touret J L R.Fluid inclusions,reviews in mineralogy[J].Geochimica et Cosmochimica Acta,1985,49(6):1491-1491.
[66]卢焕章,范宏瑞,倪培,等.流体包裹体[M].北京:科学出版社,2004.Lu H Z,Fan H R,Ni P,et al.Fluid Inclusions[M].Beijing:Science Press,2004.(in Chinese)
[67]徐九华,张国瑞,魏浩,等.脉状金矿床的成矿压力与深度:流体包裹体方法及其影响因素[J].南京大学学报(自然科学版),2012,48(3):266-277.Xu J H,Zhang G R,Wei H,et al.Ore-forming pressures and depths of vein gold deposit:Fluid inclusions studies and their influence factors[J].Journal of Nanjing University(Natural Sciences),2012,48(3):266-277.(in Chinese)
[68]Ramboz C,Pichavant M,Weisbrod A.Fluid immiscibility in natural processes:Use and misuse of fluid inclusion data:Ⅱ.Interpretation of fluid inclusion data in terms of immiscibility[J].Chemical Geology,1982,37(1):29-48.
[69]Ohmoto H.Systematics of sulfur and carbon isotopes in hydrothermal ore deposits[J].Economic Geology,1972,67(5):551-578.
[70]Ohmoto H,Goldhaber M B.Sulfur and carbon isotopes[C]//Geochemistry of Hydrothermal Ore Deposits.New York:Wiley,1997:517-611.
[71]李龚健,王庆飞,朱和平,等.青海什多龙热液脉型钼铅锌矿床流体包裹体研究及矿床成因[J].岩石学报,2013,29(4):1377-1391.Li G J,Wang Q F,Zhu H P,et al.Fluids inclusion constraints on the origin of the Shiduolong hydrothermal vein-type Mo-Pb-Zn deposit,Qinghai Province[J].Acta Petrologica Sinica,2013,29(4):1377-1391.(in Chinese)
[72]韦延光,王建国,邓军,等.山东谢家沟金矿流体包裹体研究及其地质意义[J].现代地质,2005,19(2):224-230.Wei Y G,Wang J G,Deng J,et al.Study on the fluid inclusions from Xiejiagou gold deposit in Shandong and its geological significance[J].Geoscience,2005,19(2):224-230.(in Chinese)
[73]杨立强,王中亮,吴发富,等.河南前河金矿床成矿流体特征与来源:流体包裹体地球化学与同位素约束[J].矿物学报,2009,29(增刊1):259-260.Yang L Q,Wang Z L,Wu F F,et al.Characteristics and origin of ore-forming fluids of the former Henan gold deposit:Fluid inclusion geochemistry and isotopic constraints[J].Acta Mineralogica Sinica,2009,29(S1):259-260.(in Chinese)
[74]李莉,卿敏,陈祥.河南前河金矿床地球化学特征[J].黄金地质,1999,5(3):75-80.Li L,Qing M,Chen X.Geochemical features of Qianhe gold deposit,Henan[J].Gold Geology,1999,5(3):75-80.(in Chinese)
[75]朱沛云,胡斌,赖峰,等.河南省前河金矿矿床成因及成矿模式探讨[J].地质找矿论丛,2014,29(2):199-205.Zhu P Y,Hu B,Lai F,et al.Discussion on genesis and metallogenic model of Qianhe gold deposit in Songxian county,Henan Province[J].Contributions to Geology and Mineral Resources Research,2014,29(2):199-205.(in Chinese)
[76]翟雷,刘玉刚,焦永会.河南省嵩县庙岭金矿床地质特征与成矿时代[J].吉林地质,2011,30(2):34-40.Zhai L,Liu Y G,Jiao Y H.Geological features and ore-forming age of Miaoling gold deposit in Henan[J].Jilin Geology,2011,30(2):34-40.(in Chinese)
[77]吕伟庆,刘建军.河南北岭金矿床地质特征及深部找矿远景[J].矿产勘查,2014,5(3):436-440.Lv W Q,Liu J J.Geological characteristics of the Beiling gold deposit and prospecting targets at the depth,Henan[J].Mineral Exploration,2014,5(3):436-440.(in Chinese)
[78]胡新露,何谋春,姚书振.东秦岭上宫金矿成矿流体与成矿物质来源新认识[J].地质学报,2013,87(1):91-100.Hu X L,He M C,Yao S Z.New understanding of the source of ore-forming material and fluid in the Shanggong gold deposit,east Qinling[J].Acta Geologica Sinica,2013,87(1):91-100.(in Chinese)
[79]王书来,胡拥民,李剑,等.河南店房金矿床地质特征及找矿意义[J].矿床地质,2002,21(增刊1):685-688.Wang S L,Hu Y M,Li J,et al.Characteristics of gold mine lay in near SN direction fault found at Dianfang gold mines periphery and its significances[J].Mineral Deposits,2002,21(S1):685-688.(in Chinese)
[80]张智慧,涂恩照,台本华.河南嵩县店房金矿区稳定同位素特征及其深部成矿示踪意义[J].黄金,2013,27(9):11-15.Zhang Z H,Tu E Z,Tai B H.Stable isotope characteristics of Dianfang Au deposit in Songxian,Henan and its implication for deep mineralization tracing[J].Gold,2013,27(9):11-15.(in Chinese)
[81]段存基.河南嵩县萑香洼金矿床成矿流体地球化学和矿床成因研究[D].北京:中国地质大学档案馆,2006.Duan C J.Ore-Forming Fluid Geochemistry and Genesis of the Huanxiangwa Gold Deposit in Western Henan,China[D].Beijing:The Archive of China University of Geosciences,2006.(in Chinese)
[82]王长明,邓军,张寿庭.河南萑香洼金矿床综合找矿模型[J].黄金,2006,27(7):11-14.Wang C M,Deng J,Zhang S T.Integrated ore prospecting model of the Huanxiangwa gold deposit,Henan[J].Gold,2006,27(7):11-14.(in Chinese)
[83]Mao J W,Goldfarb R J,Zhang Z W,et al.Gold deposits in the Xiaoqinling-Xiongershan region,Qinling Mountains,central China[J].Mineralium Deposita,2002,37(3):306-325.
[84]张黎.秦岭地区不同区带金矿床流体包裹体特征[D].北京:中国地质大学档案馆,2014.Zhang L.Fluid Inclusion Characters Comparison of Gold Deposits of Qinling Mountains[D].Beijing:The Archive of China University of Geosciences,2014.(in Chinese)
[85]涂光炽.论改造成矿兼评现行矿床成因分类中的弱点[C]//地球化学文集.北京:科学出版社,1986:1-7.Tu G C.On the formation of ore deposits by the process of reworking,with remarks on the weakness of the present genetic classification of ore deposits[C]//Geochemistry.Beijing:Science Press,1986:1-7.(in Chinese)
[86]Bodnar R J.Hydrothermal solutions[C]//Encyclopedia of Geochemistry.Dordrechit:Kluwer Academic Publishers,1999:333-336.
[87]Shepherd T J,Rankin A H,Alderton D H M.A Practical Guide to Fluid Inclusion Studies[M].Blackie:Chaman&Hall,1985.
[88]沈滔,陈正乐,潘家永,等.赣中良山钼矿床流体包裹体特征及其地质意义[J].现代地质,2016,30(1):17-28.Shen T,Chen Z L,Pan J Y,et al.Characteristics of fluid inclusion of the Liangshan molybdenum deposit in central Jiangxi Province and their geological implications[J].Geoscience,2016,30(1):17-28.(in Chinese)
[89]张理刚.稳定同位素在地质科学中的应用[M].西安:陕西科学技术出版社,1985.Zhang L G.The Application of Stable Isotopes in Geological Sciences[M].Xian:Shaanxi Science and Technology Press,1985.(in Chinese)
[90]卢焕章.流体不混溶性和流体包裹体[J].岩石学报,2011,27(5):1253-1261.Lu H Z.Fluids immiscibility and fluid inclusions[J].Acta Petrologica Sinica,2011,27(5):1253-1261.(in Chinese)
[91]刘斌,沈昆.流体包裹体热力学[M].北京:地质出版社,1999.Liu B,Shen K.Thermodynamics of Geologic Fluids[M].Beijing:Geological Publishing House,1999.(in Chinese)
[92]Bowers T S.The deposition of gold and other metals:Pressure-induced fluid immiscibility and associated stable isotope signatures[J].Geochimica et Cosmochimica Acta,1991,55(9):2417-2434.
[93]曾国平,姚书振,何谋春,等.黑龙江省呼玛县天望台山金矿床成矿流体特征与成矿机制研究[J].矿床地质,2016,35(1):85-102.Zeng G P,Yao S Z,He M C,et al.Ore-forming fluid and metallogenic mechanism of Tianwangtaishan gold deposit,Heilongjiang Province[J].Mineral Deposits,2016,35(1):85-102.(in Chinese)
[94]Taylor H P J.Oxygen and hydrogen isotope relationships in hydrothermal mineral deposits[C]//Geochemistry of Hydrothermal Ore Deposits.New York:Wiley,1997:229-302.
[95]李永峰,毛景文,郭保健,等.豫西公峪金矿床地质地球化学特征及成因探讨[J].矿床地质,2004,23(1):61-66.Li Y F,Mao J W,Guo B J,et al.Geology,geochemistry and genesis of Gongyu altered tectonic type gold deposit in western Henan Province[J].Mineral Deposits,2004,23(1):61-66.(in Chinese)
[96]高永丰,栾文楼,魏瑞华.祁雨沟地区金矿床稳定同位素研究[J].矿床地质,1994,13(4):354-362.Gao Y F,Luan W L,Wei R H.Stable isotope studies of gold deposit in Qiyugou area,Henan Province[J].Mineral Deposit,1994,13(4):354-362.(in Chinese)
[97]陈衍景,林治家,李晶,等.东秦岭上宫金矿流体成矿作用:稳定同位素地球化学研究[J].矿物岩石,2004,24(3):13-21.Chen Y J,Lin Z J,Li J,et al.Hydrothermal metallogeny of the Shanggong gold deposit,east Qinling study on the stable isotope geochemistry[J].Journal of Mineralogy and Petrology,2004,24(3):13-21.(in Chinese)
[98]高亚龙.河南嵩县萑香洼金矿床地质地球化学特征及成因探讨[D].北京:中国地质大学档案馆,2010.Gao Y L.Geology,Geochemistry and Genesis of Huanxiangwa Gold Deposit in Dongqinling,Henan Province[D].Beijing:The Archive of China University of Geosciences,2010.(in Chinese)
[99]金伟,刘福.祁雨沟金矿田S、O、C、Pb同位素组成及成矿物质来源[J].现代地质,1994,8(2):139-145.Jin W,Liu F.S,O,C and Pb isotope composition and sources of ore-forming materials of Qiyugou gold deposits[J].Geoscience,1994,8(2):139-145.(in Chinese)
[100]任富根,赵嘉农,李双保,等.熊耳裂陷印支期磨沟正长岩体自然金的发现及其意义[J].中国学术期刊文摘(科技快报),2000,6(5):619-620.Ren F G,Zhao J N,Li S B,et al.The discovery and signification of the native gold in Mogou syenite(Indosinian Epoch),Xionger fault basin[J].Chinese Academic Journal(Science and Technology Bulletin),2000,6(5):619-620.(in Chinese)
[101]王长明,邓军,张寿庭,等.河南省华北陆块南缘铅金成矿系统[J].地质找矿论丛,2005,20(3):170-175.Wang C M,Deng J,Zhang S T,et al.Analysis of metallogenic systems of lead and gold at southern margin of North China platform in Henan[J].Contributions to Geology and Mineral Resources Research,2005,20(3):170-175.(in Chinese)
[102]陈衍景,倪培,范宏瑞,等.不同类型热液金矿系统的流体包裹体特征[J].岩石学报,2007,23(9):2085-2108.Chen Y J,Ni P,Fan H R,et al.Diagnostic fluid inclusions of different types hydrothermal gold deposits[J].Acta Petrologica Sinica,2007,23(9):2085-2108.(in Chinese)
[103]Chen Y J,Pirajno F,Sui Y H.Isotope geochemistry of the Tieluping silver-lead deposit,Henan,China:A case study of orogenic silver-dominated deposits and related tectonic setting[J].Mineralium Deposita,2004,39(5):560-575.
[104]Zhang L,Chen H,Chen Y J,et al.Geology and fluid evolution of the Wangfeng orogenic-type gold deposit,western Tian Shan,China[J].Ore Geology Reviews,2012,49(6):85-95.
[105]陈衍景,隋颖慧,Franco Pirajno.CMF模式的排他性依据和造山型银矿实例:东秦岭铁炉坪银矿同位素地球化学[J].岩石学报,2003,19(3):551-568.Chen Y J,Sui Y H,Pirajno F.Exclusive evidences for CMF model and a case of orogenic silver deposits:Isotope geochemistry of the Tieluping silver deposit,east Qinling Orogen[J].Acta Petrologica Sinica,2003,19(3):551-568.(in Chinese)
[106]陈衍景.豫西金矿成矿规律[M].北京:地震出版社,1992.Chen Y J.Metallogenic Regularity of Gold Deposits in Western Henan[M].Beijing:Seismological Press,1992.
[107]陈晶源,王长明,贺昕宇,等.河南瓦房铅锌矿床地质、流体包裹体和稳定同位素特征[J].吉林大学学报(地球科学版),2017,47(5):1383-1404.Chen J Y,Wang C M,He X Y,et al.Characteristics of geology,fluid inclusions and stable isotope of Wafang Pb-Zn deposit in Henan[J].Journal of Jilin University(Earth Science Edition),2017,47(5):1383-1404.(in Chinese)
[108]唐克非.华北克拉通南缘熊耳山地区金矿床时空演化、矿床成因及成矿构造背景[D].武汉:中国地质大学档案馆,2014.Tang K F.Characteristics,Genesis,and Geodynamic Setting of Representative Gold Deposit in the Xiongershan District,South Margin of the North China Craton[D].Wuhan:The Archive of China University of Geosciences,2014.(in Chinese)
[109]高建京,毛景文,陈懋弘,等.豫西铁炉坪银铅矿床矿脉构造解析及近矿蚀变岩绢云母40 Ar-39 Ar年龄测定[J].地质学报,2011,85(7):1172-1187.Gao J J,Mao J W,Chen M H,et al.Vein structure analysis and 40 Ar/39 Ar dating of sericite from sub-ore altered rocks in the Tieluping large-size Ag-Pb deposit of western Henan Province[J].Acta Geologica Sinica,2011,85(7):1172-1187.(in Chinese)
[110]刘军,武广,贾守民,等.豫西沙坡岭钼矿床辉钼矿Re-Os同位素年龄及其地质意义[J].矿物岩石,2011,31(1):56-62.Liu J,Wu G,Jia S M,et al.Re-Os isotopic dating of molybdenites from the Shapoling molybdenum deposit in western Henan Province and its geological significance[J].Journal of Mineralogy&Petrology,2011,31(1):56-62.(in Chinese)
[111]Goldfarb R J,Groves D I.Orogenic gold:Common or evolving fluid and metal sources through time[J].Lithos,2015,233:2-26.
[112]Zhou Z J,Chen Y J,Jiang S Y,et al.Isotope and fluid inclusion geochemistry and genesis of the Qiangma gold deposit,Xiaoqinling gold field,Qinling Orogen,China[J].Ore Geology Reviews,2015,66:47-64.
[113]Groves D I,Goldfarb R J,Gebre-Mariam M,et al.Orogenic gold deposits-A proposed classification in the context of their crustal distribution and relationship to other gold deposit types[J].Ore Geology Reviews,1998,13:7-27.
[114]Lang J R,Baker T.Intrusion-related gold systems:The present level of understanding[J].Mineralium Deposita,2001,36:477-489.
[2]王义天,毛景文,卢欣祥.嵩县祁雨沟金矿成矿时代的40 Ar-39 Ar年代学证据[J].地质论评,2001,47(5):551-555.Wang Y T,Mao J W,Lu X X.40 Ar-39 Ar and geochronological constraints on the ore-forming epoch of the Qiyugou gold deposit in Songxian County,Henan Province[J].Geological Review,2001,47(5):551-555.(in Chinese)
[3]Chen Y J,Pirajno F,Qi J P,et al.Ore geology,fluid geochemistry and genesis of the Shanggong gold deposit,Eastern Qinling Orogen,China[J].Resource Geology,2006,56(2):99-116.
[4]周珂,叶会寿,毛景文,等.豫西鱼池岭斑岩型钼矿床地质特征及其辉钼矿铼-锇同位素年龄[J].矿床地质,2009,28(2):170-184.Zhou K,Ye H S,Mao J W,et al.Geological characteristics and molybdenite Re-Os isotopic dating of Yuchiling porphyry Mo deposit in western Henan Province[J].Mineral Deposits,2009,28(2):170-184.(in Chinese)
[5]毛景文,郑榕芬,叶会寿,等.豫西熊耳山地区沙沟银铅锌矿床成矿的40 Ar-39 Ar年龄及其地质意义[J].矿床地质,2006,25(4):359-368.Mao J W,Zheng R F,Ye H S,et al.40 Ar-39 Ar dating of fuchsite and sericite from altered rocks close to ore veins in Shagou large-size Ag-Pb-Zn deposit of Xiongershan area,western Henan Province,and its significance[J].Mineral Deposits,2006,25(4):359-368.(in Chinese)
[6]叶会寿.华北陆块南缘中生代构造演化与铅锌银成矿作用[D].北京:中国地质科学院,2006.Ye H S.The Mesozoic Tectonic Evolution and PbZn-Ag Mineralization in South Margin of North China Craton[D].Beijing:Chinese Academy of Geological Sciences,2006.(in Chinese)
[7]Cao M P,Yao J M,Deng X H,et al.Diverse and multistage Mo,Au,Ag-Pb-Zn and Cu deposits in the Xionger Terrane,East Qinling:From Triassic Cu mineralization[J].Ore Geology Reviews,2017,81(2):565-574.
[8]范宏瑞,谢奕汉,王英兰.豫西花山花岗岩岩浆热液的性质及与金成矿的关系[J].岩石学报,1993,9(2):136-145.Fan H R,Xie Y H,Wang Y L.The properties of magmatic hydrothermal fluid of Huashan granitic batholith in western Henan Province and their relationship to gold mineralization[J].Acta Petrologica Sinica,1993,9(2):136-145.(in Chinese)
[9]范宏瑞,谢奕汉.豫西熊耳山地区岩石和金矿床稳定同位素地球化学研究[J].地质找矿论丛,1994,9(1):54-64.Fan H R,Xie Y H.Stable isotope geochemistry of rocks and gold deposit in the Xiongershan area,western Henan Province[J].Contributions to Geology and Mineral Resources Research,1994,9(1):54-64.(in Chinese)
[10]付治国,瓮纪昌,卢欣祥.小秦岭-熊耳山地区金矿硫同位素地球化学特征[J].物探与化探,2009,33(5):507-514.Fu Z G,Weng J C,Lu X X.Sulfur isotope geochemical characteristics of gold deposit in Xiaoqinling-Xionger Mountain area[J].Geophysical and Geochemical Exploration,2009,33(5):507-514.(in Chinese)
[11]王团华,谢桂青,叶安旺,等.豫西小秦岭-熊耳山地区金矿成矿物质来源研究——兼论中基性岩墙与金成矿作用关系[J].地球学报,2009,30(1):27-38.Wang T H,Xie G Q,Ye A W,et al.Material sources of gold deposits in Xiaoqinling-Xiongershan area of western Henan Province as well as the relationship between gold deposits and intermediatebasic dyke[J].Acta Geosicientia Sinica,2009,30(1):27-38.(in Chinese)
[12]卢欣祥,尉向东,于在平,等.小秦岭-熊耳山地区金矿的成矿流体特征[J].矿床地质,2003,22(4):377Lu X X,Yu X D,Yu Z P,et al.Characteristics of ore-forming fluids in gold deposits of XiaoqinlingXiongershan area[J].Mineral Deposits,2003,22(4):377-385.(in Chinese)
[13]卢欣祥.小秦岭-熊耳山地区金矿特征与地幔流体[M].北京:地质出版社,2004.Lu X X.The Characteristics of Gold Deposits and Mantle Fluid in Xiaoqinling-Xiongershan Area[M].Beijing:Geological Publishing House,2004.(in Chinese)
[14]Deng J,Yuan W M,Carranza E J M,et al.Geochronology and thermochronometry of the Jiapigou gold belt,northeastern China:New evidence for multiple episodes of mineralization[J].Journal of Asian Earth Sciences,2014,89(3):10-27.
[15]Wang C M,Bagas L,Lu Y J,et al.Terrane boundary and spatio-temporal distribution of ore deposits in the Sanjiang Tethyan Orogen:Insights from zircon Hf-isotopic mapping[J].Earth-Science Reviews,2016,156:39-65.
[16]廖诗进,宁勇.河南磨沟金矿床地质特征及找矿方向[J].地质调查与研究,2010,33(2):142-148.Liao S J,Ning Y.Geological characteristics and ore prospecting of the Mogou gold deposit,Henan Province[J].Geological Survey and Research,2010,33(2):142-148.(in Chinese)
[17]卢焕章,郭迪江.流体包裹体研究的进展和方向[J].地质论评,2000,46(4):385-392.Lu H Z,Guo D J.Progress and trends of researches on fluid inclusions[J].Geological Review,2000,46(4):385-392.(in Chinese)
[18]倪培,蒋少涌,凌鸿飞,等.流体包裹体面的研究背景、现状及发展前景[J].地质论评,2001,47(4):398-404.Ni P,Jiang S Y,Ling H F,et al.The background,application and development of fluid inclusion planes research[J].Geological Review,2001,47(4):398-404.(in Chinese)
[19]池国祥,周义明,卢焕章.当前流体包裹体研究和应用概况[J].岩石学报,2003,19(2):201-212.Chi G X,Zhou Y M,Lu H Z.An overview on current fluid-inclusion research and application[J].Acta Petrologica Sinica,2003,19(2):201-212.(in Chinese)
[20]周慧,郗爱华,熊益学,等.流体包裹体的研究进展[J].矿物学报,2013,33(1):92-100.Zhou H,Xi A H,Xiong Y X,et al.Progress in the research on fluid inclusions[J].Acta Mineralogica Sinica,2013,33(1):92-100.(in Chinese)
[21]Farber K,Dziggel A,Meyer F M,et al.Fluid inclusion analysis of silicified Paleoarchean oceanic crust-A record of Archaean seawater[J].Precambrian Research,2015,266:150-164.
[22]Terrence M.A review of fluid inclusions in diagenetic systems[J].Acta Geologica Sinica,2015,89(3):697-714.
[23]郑永飞.稳定同位素体系理论模式及其矿床地球化学应用[J].矿床地质,2001,20(1):57-70.Zheng Y F.Theoretical modeling of stable isotope systems and its applications to geochemistry of hydrothermal ore deposits[J].Mineral Deposits,2001,20(1):57-70.(in Chinese)
[24]Tang K F,Li J W,Selby D,et al.Geology,mineralization,and geochronology of the Qianhe gold deposit,Xiongershan area,southern North China Craton[J].Mineralium Deposita,2013,48(6):729-747.
[25]Dong Y P,Santosh M.Tectonic architecture and multiple orogeny of the Qinling Orogenic Belt,Central China[J].Gondwana Research,2016,29(1):1-40.
[26]Wang C M,Deng J,Bagas L,et al.Zircon Hfisotopic mapping for understanding crustal architecture and metallogenesis in the Eastern Qinling Orogen[J].Gondwana Research,2017,50:293-310.
[27]张国伟,张本仁,袁学诚,等.秦岭造山带与大陆动力学[M].北京:科学出版社,2001.Zhang G W,Zhang B R,Yuan X C,et al.Qinling Orogenic Belt and Continental Dynamics[M].Beijing:Science Press,2001.(in Chinese)
[28]刘红樱,胡受奚,周顺之.豫西马超营断裂带的控岩控矿作用研究[J].矿床地质,1998,17(1):70-81.Liu H Y,Hu S X,Zhou S Z.A study of rockcontrolling and ore-controlling role of the Machaoying fault in western Henan[J].Mineral Deposits,1998,17(1):70-81.(in Chinese)
[29]张元厚,张世红,韩以贵,等.华熊地块马超营断裂走滑特征及演化[J].吉林大学学报(地球科学版),2006,36(2):169-176.Zhang Y H,Zhang S H,Han Y G,et al.Strik-slip features of the Machaoying fault zone and its evolution in the Huaxiong terrane,southern North China Craton[J].Journal of Jilin University(Earth Science Edition),2006,36(2):169-176.(in Chinese)
[30]卿敏,陈祥,关连绪.金矿与花岗岩类关系的“同源说”——以豫西外方山地区为例[J].黄金地质,1997,3(3):30-35.Qing M,Chen X,Guan L X.The theory of“cognate genesis”about relationships between granitoids and gold deposits:Taking example of Waifangshan area,western Henan Province[J].Gold Geology,1997,3(3):30-35.(in Chinese)
[31]卢仁,梁涛,白凤军,等.豫西磨沟正长岩LA-ICPMS锆石U-Pb年代学及Hf同位素[J].地质论评,2013,59(2):355-368.Lu R,Liang T,Bai F J,et al.LA-ICP-MS zircon age and Hf isotope composition of Mogou syenite,western Henan Province[J].Geological Review,2013,59(2):355-368.(in Chinese)
[32]郭保健,李永峰,王志光,等.熊耳山Au-Ag-Pb-Mo矿集区成矿模式与找矿方向[J].地质与勘探,2005,41(5):43-47.Guo B J,Li Y F,Wang Z G,et al.Type metallogenetic regularities mineralization and prospecting proposal in the Xiongershan district[J].Geology and Prospecting,2005,41(5):43-47.(in Chinese)
[33]Kr9ner A,Compston W,Zhang G W,et al.Age and tectonic setting of late Archean greenstonegneiss terrain in Henan Province,China,as revealed by single-grain zircon dating[J].Geology,1988,16:211-215.
[34]薛良伟,原振雷,张荫树,等.鲁山太华群Sm-Nd同位素年龄及其意义[J].地球化学,1995,24(增刊1):92-97.Xue L W,Yuan Z L,Zhang Y S,et al.The Sm-Nd isotope age of Taihua Group in Lushan area and their implications[J].Geochimica,1995,24(S1):92-97.(in Chinese)
[35]倪志耀,王仁民,童英,等.河南洛宁太华岩群斜长角闪岩的锆石207 Pb/206 Pb和角闪石40 Ar/39 Ar年龄[J].地质论评,2003,49(4):361-366.Ni Z Y,Wang R M,Tong Y,et al.207Pb/206Pb age of zircon and 40 Ar/39 Ar of amphibole from plagioclase amphibolite in the Taihua Group,Luoning,Henan,China[J].Geological Review,2003,49(4):361-366.(in Chinese)
[36]杨长秀.河南鲁山地区早前寒武纪变质岩系的锆石SHRIMP U-Pb年龄、地球化学特征及环境演化[J].地质通报,2008,27(4):517-533.Yang C X.Zircon SHRIMP U-Pb ages,geochemical characteristics and environmental evolution of the early Precambrian metamorphic series in the Lushan area,Henan,China[J].Geological Bulletin of China,2008,27(4):517-533.(in Chinese)
[37]侯万荣,肖荣阁,张汉成,等.熊耳裂谷火山岩系金-多金属矿床成矿模式[J].黄金地质,2003,9(2):22Hou W R,Xiao R G,Zhang H C,et al.The genesis model of the gold-polymetal deposit from the volcanic rocks in the Xionger rift[J].Gold Geology,2003,9(2):22-27.(in Chinese)
[38]任富根,丁士应,李增慧,等.豫西元古宙盆岭构造及其形成机制[J].中国区域地质,1996(3):239-243.Ren F G,Ding S Y,Li Z H,et al.The Proterozoic basin-range structure and its formation mechanism,western Henan[J].Regional Geology of China,1996(3):239-243.(in Chinese)
[39]赵太平,周美夫,金成伟,等.华北陆块南缘熊耳群形成时代讨论[J].地质科学,2001,36(3):326-334.Zhao T P,Zhou M F,Jin C W,et al.Discussion on age of the Xionger Group in southern margin of Northern China Craton[J].Chinese Journal of Geology,2001,36(3):326-334.(in Chinese)
[40]赵太平,翟明国,夏斌,等.熊耳群火山岩锆石SHRIMP年代学研究:对华北克拉通盖层发育初始时间的制约[J].科学通报,2004,49(22):2342-2349.Zhao T P,Zhai M G,Xia B,et al.The study of Zircon SHRIMP geochronology about the Precambrian volcano rock:Constraints on the overlying strata developmental initial time,North China Craton[J].Chinese Science Bulletin,2004,49(22):2342-2349.(in Chinese)
[41]王长明,邓军,张寿庭.河南熊耳山地区花山花岗岩与金矿化的关系[J].现代地质,2006,20(2):315-321.Wang C M,Deng J,Zhang S T.Relationship between Huashan granite and gold mineralization in Xiongershan area,Henan[J].Geoscience,2006,20(2):315-321.(in Chinese)
[42]Peng P,Zhai M G,Ernst R E,et al.A 1.78Ga large igneous province in the North China Craton:The Xionger volcanic province and the North China dyke swarm[J].Lithos,2008,101(3/4):260-280.
[43]柳晓艳,蔡剑辉,阎国翰.华北克拉通南缘熊耳群眼窑寨组次火山岩岩石地球化学与年代学研究及其意义[J].地质学报,2011,85(7):1134-1145.Liu X Y,Cai J H,Yan G H.Lithogeochemistry and geochronology of Xionger Group Yanyaozhai subvolcanics in the southern margin of the North China Craton and their geological significance[J].Acta Geologica Sinica,2011,85(7):1134-1145.(in Chinese)
[44]Deng X H,Chen Y J,Santosh M,et al.Genesis of the 1.76 Ga Zhaiwa Mo-Cu and its link with the Xionger volcanism in the North China Craton:Implications for accretionary growth along the margin of the Columbia supercontinent[J].Precambrian Research,2013,227:337-348.
[45]Wang C M,Lu Y,He X Y,et al.The Paleoproterozoic diorite dykes in the southern margin of the North China Craton:Insight into rift-related magmatism[J].Precambrian Research,2016,277:26-46.
[46]He Y H,Zhao G C,Sun M,et al.SHRIMP and LA-ICP-MS zircon geochronology of the Xionger volcanic rocks:Implications for the PaleoMesoproterozoic evolution of the southern margin of the North China Craton[J].Precambrian Research,2009,174(3/4):213-222.
[47]赵太平,徐勇航,翟明国.华北陆块南部元古宙熊耳群火山岩的成因与构造环境:事实与争议[J].高校地质学报,2007,13(2):191-206.Zhao T P,Xu Y H,Zhai M G.Petrogenesis and tectonic setting of the Paleoproterozoic Xionger Group in the Southern part of the North China Craton:A review[J].Geological Journal of China Universities,2007,13(2):191-206.(in Chinese)
[48]杨东潮,庞绪成,宗静,等.豫西嵩县南部鸡蛋坪组岩石地球化学特征及其成因意义[J].河南理工大学学报(自然科学版),2012,31(6):679-686.Yang D C,Pang X C,Zong J,et al.Geochemistry characteristic and cause of formation of Jidanping Fm rock,south Song County of western Henan[J].Journal of Henan Polytechnic University(Natural Science),2012,31(6):679-686.(in Chinese)
[49]王卫星,邓军,龚庆杰,等.豫西熊耳山五丈山、花山、合峪花岗岩体与金成矿关系[J].黄金,2010,31(4):12-17.Wang W X,Deng J,Gong Q J,et al.Relationship of Wuzhangshan,Huashan and Heyu granite rock mass with gold mineralization,in Xiongershan area,western Henan Province[J].Gold,2010,31(4):12-17.(in Chinese)
[50]李诺,陈衍景,孙亚莉,等.河南鱼池岭钼矿床辉钼矿铼-锇同位素年龄及地质意义[J].岩石学报,2009,25(2):413-421.Li N,Chen Y J,Sun Y L,et al.Molybdenite ReOs isochron age of the Yuchiling porphyry Mo deposit,Henan Province and its geological implications[J].Acta Petrologica Sinica,2009,25(2):413-421.(in Chinese)
[51]Li N,Chen Y J,Pirajno F,et al.LA-ICP-MS zircon U-Pb dating,trace element and Hf isotope geochemistry of the Heyu granite batholith,eastern Qinling,central China:Implications for Mesozoic tectono-magmatic evolution[J].Lithos,2012,142(6):34-47.
[52]Deng J,Gong Q J,Wang C M,et al.Sequence of late Jurassic-early Cretaceous magmatichydrothermal events in the Xiongershan region,Central China:An overview with new zircon U-Pb geochronology data on quartz porphyries[J].Journal of Asian Earth Sciences,2014,79:161-172.
[53]李永峰.豫西熊耳山地区中生代花岗岩类时空演化与钼(金)成矿作用[D].北京:中国地质大学档案馆,2005.Li Y F.The Temporal-spatial Evolution of Mesozoic Granitoids in the Xiongershan Area and Their Relationships to Molybdenum-Gold Mineralization[D].Beijing:The Archive of China University of Geosciences,2005.(in Chinese)
[54]Mao J W,Xie G Q,Pirajno F,et al.Late Jurassicearly Cretaceous granitoid magmatism in Eastern Qinling,central-eastern China:SHRIMP zircon UPb ages and tectonic implications[J].Australian Journal of Earth Sciences,2010,57(1):51-78.
[55]郭波,朱赖民,李犇,等.华北陆块南缘华山和合峪花岗岩岩体锆石U-Pb年龄、Hf同位素组成与成岩动力学背景[J].岩石学报,2009,25(2):265-281.Guo B,Zhu L M,Li B,et al.Zircon U-Pb age and Hf composition of the Huashan and Heyu granite plutons at the southern margin of North China Craton:Implications for geodynamic setting[J].Acta Petrologica Sinica,2009,25(2):265-281.(in Chinese)
[56]高昕宇,赵太平,原振雷,等.华北陆块南缘中生代合峪花岗岩的地球化学特征与成因[J].岩石学报,2010,26(12):3485-3506.Gao X Y,Zhao T P,Yuan Z L,et al.Geochemistry and petrogenesis of the Heyu batholith in the southern margin of the North China Block[J].Acta Petrologica Sinica,2010,26(12):3485-3506.(in Chinese)
[57]Wang C M,Chen L,Bagas L,et al.Characterization and origin of the Taishanmiao aluminous A-type granites:Implications for early Cretaceous lithospheric thinning at the southern margin of the North China Craton[J].International Journal of Earth Sciences,2016,105(5):1563-1589.
[58]吴发富,龚庆杰,石建喜,等.熊耳山矿集区金矿控矿地质要素分析[J].地质与勘探,2012,48(5):865-875.Wu F F,Gong Q J,Shi J X,et al.Ore-controlling factors of the gold deposits in the Xiongershan gold region,western Henan Province[J].Geology and Exploration,2012,48(5):865-875.(in Chinese)
[59]Hall D L,Sterner S M,Bodnar R J.Freezing point depression of NaCl-KCl-H2O solutions[J].Economic Geology,1988,83(1):197-202.
[60]Brown P E.Flincor:A microcomputer program for the reduction and investigation of fluid inclusion data[J].American Mineralogist,1989,74:1390-1393.
[61]Brown P E,Lamb W M.P-V-T properties of fluids in the system H2O±CO2±NaCl:New graphical presentations and implications for fluid inclusion studies[J].Geochimica et Cosmochimica Acta,1989,53(6):1209-1221.
[62]孙丰月,金巍,李碧乐,等.关于脉状热液金矿床成矿深度的思考[J].长春科技大学学报,2000,30(增刊1):27-29.Sun F Y,Jin W,Li B L,et al.Considerations on the mineralizing depth of hydrothermal lode gold deposits[J].Journal of Changchun University of Science and Technology,2000,30(S1):27-29.(in Chinese)
[63]万德芳,樊天义,田世洪.用金属铬法分析微量水和有机质氢同位素组成[J].地球学报,2005,26(增刊1):35-38.Wan D F,Fan T Y,Tian S H.The Chromium analytical technique for hydrogen isotope[J].Acta Geoscientica Sinica,2005,26(S1):35-38.(in Chinese)
[64]Clayton R N,ONeil J R,Mayeda T K.Oxygen isotope exchange between quartz and water[J].Journal of Geophysical Research Atmospheres,1972,77(17):3057-3067.
[65]Touret J L R.Fluid inclusions,reviews in mineralogy[J].Geochimica et Cosmochimica Acta,1985,49(6):1491-1491.
[66]卢焕章,范宏瑞,倪培,等.流体包裹体[M].北京:科学出版社,2004.Lu H Z,Fan H R,Ni P,et al.Fluid Inclusions[M].Beijing:Science Press,2004.(in Chinese)
[67]徐九华,张国瑞,魏浩,等.脉状金矿床的成矿压力与深度:流体包裹体方法及其影响因素[J].南京大学学报(自然科学版),2012,48(3):266-277.Xu J H,Zhang G R,Wei H,et al.Ore-forming pressures and depths of vein gold deposit:Fluid inclusions studies and their influence factors[J].Journal of Nanjing University(Natural Sciences),2012,48(3):266-277.(in Chinese)
[68]Ramboz C,Pichavant M,Weisbrod A.Fluid immiscibility in natural processes:Use and misuse of fluid inclusion data:Ⅱ.Interpretation of fluid inclusion data in terms of immiscibility[J].Chemical Geology,1982,37(1):29-48.
[69]Ohmoto H.Systematics of sulfur and carbon isotopes in hydrothermal ore deposits[J].Economic Geology,1972,67(5):551-578.
[70]Ohmoto H,Goldhaber M B.Sulfur and carbon isotopes[C]//Geochemistry of Hydrothermal Ore Deposits.New York:Wiley,1997:517-611.
[71]李龚健,王庆飞,朱和平,等.青海什多龙热液脉型钼铅锌矿床流体包裹体研究及矿床成因[J].岩石学报,2013,29(4):1377-1391.Li G J,Wang Q F,Zhu H P,et al.Fluids inclusion constraints on the origin of the Shiduolong hydrothermal vein-type Mo-Pb-Zn deposit,Qinghai Province[J].Acta Petrologica Sinica,2013,29(4):1377-1391.(in Chinese)
[72]韦延光,王建国,邓军,等.山东谢家沟金矿流体包裹体研究及其地质意义[J].现代地质,2005,19(2):224-230.Wei Y G,Wang J G,Deng J,et al.Study on the fluid inclusions from Xiejiagou gold deposit in Shandong and its geological significance[J].Geoscience,2005,19(2):224-230.(in Chinese)
[73]杨立强,王中亮,吴发富,等.河南前河金矿床成矿流体特征与来源:流体包裹体地球化学与同位素约束[J].矿物学报,2009,29(增刊1):259-260.Yang L Q,Wang Z L,Wu F F,et al.Characteristics and origin of ore-forming fluids of the former Henan gold deposit:Fluid inclusion geochemistry and isotopic constraints[J].Acta Mineralogica Sinica,2009,29(S1):259-260.(in Chinese)
[74]李莉,卿敏,陈祥.河南前河金矿床地球化学特征[J].黄金地质,1999,5(3):75-80.Li L,Qing M,Chen X.Geochemical features of Qianhe gold deposit,Henan[J].Gold Geology,1999,5(3):75-80.(in Chinese)
[75]朱沛云,胡斌,赖峰,等.河南省前河金矿矿床成因及成矿模式探讨[J].地质找矿论丛,2014,29(2):199-205.Zhu P Y,Hu B,Lai F,et al.Discussion on genesis and metallogenic model of Qianhe gold deposit in Songxian county,Henan Province[J].Contributions to Geology and Mineral Resources Research,2014,29(2):199-205.(in Chinese)
[76]翟雷,刘玉刚,焦永会.河南省嵩县庙岭金矿床地质特征与成矿时代[J].吉林地质,2011,30(2):34-40.Zhai L,Liu Y G,Jiao Y H.Geological features and ore-forming age of Miaoling gold deposit in Henan[J].Jilin Geology,2011,30(2):34-40.(in Chinese)
[77]吕伟庆,刘建军.河南北岭金矿床地质特征及深部找矿远景[J].矿产勘查,2014,5(3):436-440.Lv W Q,Liu J J.Geological characteristics of the Beiling gold deposit and prospecting targets at the depth,Henan[J].Mineral Exploration,2014,5(3):436-440.(in Chinese)
[78]胡新露,何谋春,姚书振.东秦岭上宫金矿成矿流体与成矿物质来源新认识[J].地质学报,2013,87(1):91-100.Hu X L,He M C,Yao S Z.New understanding of the source of ore-forming material and fluid in the Shanggong gold deposit,east Qinling[J].Acta Geologica Sinica,2013,87(1):91-100.(in Chinese)
[79]王书来,胡拥民,李剑,等.河南店房金矿床地质特征及找矿意义[J].矿床地质,2002,21(增刊1):685-688.Wang S L,Hu Y M,Li J,et al.Characteristics of gold mine lay in near SN direction fault found at Dianfang gold mines periphery and its significances[J].Mineral Deposits,2002,21(S1):685-688.(in Chinese)
[80]张智慧,涂恩照,台本华.河南嵩县店房金矿区稳定同位素特征及其深部成矿示踪意义[J].黄金,2013,27(9):11-15.Zhang Z H,Tu E Z,Tai B H.Stable isotope characteristics of Dianfang Au deposit in Songxian,Henan and its implication for deep mineralization tracing[J].Gold,2013,27(9):11-15.(in Chinese)
[81]段存基.河南嵩县萑香洼金矿床成矿流体地球化学和矿床成因研究[D].北京:中国地质大学档案馆,2006.Duan C J.Ore-Forming Fluid Geochemistry and Genesis of the Huanxiangwa Gold Deposit in Western Henan,China[D].Beijing:The Archive of China University of Geosciences,2006.(in Chinese)
[82]王长明,邓军,张寿庭.河南萑香洼金矿床综合找矿模型[J].黄金,2006,27(7):11-14.Wang C M,Deng J,Zhang S T.Integrated ore prospecting model of the Huanxiangwa gold deposit,Henan[J].Gold,2006,27(7):11-14.(in Chinese)
[83]Mao J W,Goldfarb R J,Zhang Z W,et al.Gold deposits in the Xiaoqinling-Xiongershan region,Qinling Mountains,central China[J].Mineralium Deposita,2002,37(3):306-325.
[84]张黎.秦岭地区不同区带金矿床流体包裹体特征[D].北京:中国地质大学档案馆,2014.Zhang L.Fluid Inclusion Characters Comparison of Gold Deposits of Qinling Mountains[D].Beijing:The Archive of China University of Geosciences,2014.(in Chinese)
[85]涂光炽.论改造成矿兼评现行矿床成因分类中的弱点[C]//地球化学文集.北京:科学出版社,1986:1-7.Tu G C.On the formation of ore deposits by the process of reworking,with remarks on the weakness of the present genetic classification of ore deposits[C]//Geochemistry.Beijing:Science Press,1986:1-7.(in Chinese)
[86]Bodnar R J.Hydrothermal solutions[C]//Encyclopedia of Geochemistry.Dordrechit:Kluwer Academic Publishers,1999:333-336.
[87]Shepherd T J,Rankin A H,Alderton D H M.A Practical Guide to Fluid Inclusion Studies[M].Blackie:Chaman&Hall,1985.
[88]沈滔,陈正乐,潘家永,等.赣中良山钼矿床流体包裹体特征及其地质意义[J].现代地质,2016,30(1):17-28.Shen T,Chen Z L,Pan J Y,et al.Characteristics of fluid inclusion of the Liangshan molybdenum deposit in central Jiangxi Province and their geological implications[J].Geoscience,2016,30(1):17-28.(in Chinese)
[89]张理刚.稳定同位素在地质科学中的应用[M].西安:陕西科学技术出版社,1985.Zhang L G.The Application of Stable Isotopes in Geological Sciences[M].Xian:Shaanxi Science and Technology Press,1985.(in Chinese)
[90]卢焕章.流体不混溶性和流体包裹体[J].岩石学报,2011,27(5):1253-1261.Lu H Z.Fluids immiscibility and fluid inclusions[J].Acta Petrologica Sinica,2011,27(5):1253-1261.(in Chinese)
[91]刘斌,沈昆.流体包裹体热力学[M].北京:地质出版社,1999.Liu B,Shen K.Thermodynamics of Geologic Fluids[M].Beijing:Geological Publishing House,1999.(in Chinese)
[92]Bowers T S.The deposition of gold and other metals:Pressure-induced fluid immiscibility and associated stable isotope signatures[J].Geochimica et Cosmochimica Acta,1991,55(9):2417-2434.
[93]曾国平,姚书振,何谋春,等.黑龙江省呼玛县天望台山金矿床成矿流体特征与成矿机制研究[J].矿床地质,2016,35(1):85-102.Zeng G P,Yao S Z,He M C,et al.Ore-forming fluid and metallogenic mechanism of Tianwangtaishan gold deposit,Heilongjiang Province[J].Mineral Deposits,2016,35(1):85-102.(in Chinese)
[94]Taylor H P J.Oxygen and hydrogen isotope relationships in hydrothermal mineral deposits[C]//Geochemistry of Hydrothermal Ore Deposits.New York:Wiley,1997:229-302.
[95]李永峰,毛景文,郭保健,等.豫西公峪金矿床地质地球化学特征及成因探讨[J].矿床地质,2004,23(1):61-66.Li Y F,Mao J W,Guo B J,et al.Geology,geochemistry and genesis of Gongyu altered tectonic type gold deposit in western Henan Province[J].Mineral Deposits,2004,23(1):61-66.(in Chinese)
[96]高永丰,栾文楼,魏瑞华.祁雨沟地区金矿床稳定同位素研究[J].矿床地质,1994,13(4):354-362.Gao Y F,Luan W L,Wei R H.Stable isotope studies of gold deposit in Qiyugou area,Henan Province[J].Mineral Deposit,1994,13(4):354-362.(in Chinese)
[97]陈衍景,林治家,李晶,等.东秦岭上宫金矿流体成矿作用:稳定同位素地球化学研究[J].矿物岩石,2004,24(3):13-21.Chen Y J,Lin Z J,Li J,et al.Hydrothermal metallogeny of the Shanggong gold deposit,east Qinling study on the stable isotope geochemistry[J].Journal of Mineralogy and Petrology,2004,24(3):13-21.(in Chinese)
[98]高亚龙.河南嵩县萑香洼金矿床地质地球化学特征及成因探讨[D].北京:中国地质大学档案馆,2010.Gao Y L.Geology,Geochemistry and Genesis of Huanxiangwa Gold Deposit in Dongqinling,Henan Province[D].Beijing:The Archive of China University of Geosciences,2010.(in Chinese)
[99]金伟,刘福.祁雨沟金矿田S、O、C、Pb同位素组成及成矿物质来源[J].现代地质,1994,8(2):139-145.Jin W,Liu F.S,O,C and Pb isotope composition and sources of ore-forming materials of Qiyugou gold deposits[J].Geoscience,1994,8(2):139-145.(in Chinese)
[100]任富根,赵嘉农,李双保,等.熊耳裂陷印支期磨沟正长岩体自然金的发现及其意义[J].中国学术期刊文摘(科技快报),2000,6(5):619-620.Ren F G,Zhao J N,Li S B,et al.The discovery and signification of the native gold in Mogou syenite(Indosinian Epoch),Xionger fault basin[J].Chinese Academic Journal(Science and Technology Bulletin),2000,6(5):619-620.(in Chinese)
[101]王长明,邓军,张寿庭,等.河南省华北陆块南缘铅金成矿系统[J].地质找矿论丛,2005,20(3):170-175.Wang C M,Deng J,Zhang S T,et al.Analysis of metallogenic systems of lead and gold at southern margin of North China platform in Henan[J].Contributions to Geology and Mineral Resources Research,2005,20(3):170-175.(in Chinese)
[102]陈衍景,倪培,范宏瑞,等.不同类型热液金矿系统的流体包裹体特征[J].岩石学报,2007,23(9):2085-2108.Chen Y J,Ni P,Fan H R,et al.Diagnostic fluid inclusions of different types hydrothermal gold deposits[J].Acta Petrologica Sinica,2007,23(9):2085-2108.(in Chinese)
[103]Chen Y J,Pirajno F,Sui Y H.Isotope geochemistry of the Tieluping silver-lead deposit,Henan,China:A case study of orogenic silver-dominated deposits and related tectonic setting[J].Mineralium Deposita,2004,39(5):560-575.
[104]Zhang L,Chen H,Chen Y J,et al.Geology and fluid evolution of the Wangfeng orogenic-type gold deposit,western Tian Shan,China[J].Ore Geology Reviews,2012,49(6):85-95.
[105]陈衍景,隋颖慧,Franco Pirajno.CMF模式的排他性依据和造山型银矿实例:东秦岭铁炉坪银矿同位素地球化学[J].岩石学报,2003,19(3):551-568.Chen Y J,Sui Y H,Pirajno F.Exclusive evidences for CMF model and a case of orogenic silver deposits:Isotope geochemistry of the Tieluping silver deposit,east Qinling Orogen[J].Acta Petrologica Sinica,2003,19(3):551-568.(in Chinese)
[106]陈衍景.豫西金矿成矿规律[M].北京:地震出版社,1992.Chen Y J.Metallogenic Regularity of Gold Deposits in Western Henan[M].Beijing:Seismological Press,1992.
[107]陈晶源,王长明,贺昕宇,等.河南瓦房铅锌矿床地质、流体包裹体和稳定同位素特征[J].吉林大学学报(地球科学版),2017,47(5):1383-1404.Chen J Y,Wang C M,He X Y,et al.Characteristics of geology,fluid inclusions and stable isotope of Wafang Pb-Zn deposit in Henan[J].Journal of Jilin University(Earth Science Edition),2017,47(5):1383-1404.(in Chinese)
[108]唐克非.华北克拉通南缘熊耳山地区金矿床时空演化、矿床成因及成矿构造背景[D].武汉:中国地质大学档案馆,2014.Tang K F.Characteristics,Genesis,and Geodynamic Setting of Representative Gold Deposit in the Xiongershan District,South Margin of the North China Craton[D].Wuhan:The Archive of China University of Geosciences,2014.(in Chinese)
[109]高建京,毛景文,陈懋弘,等.豫西铁炉坪银铅矿床矿脉构造解析及近矿蚀变岩绢云母40 Ar-39 Ar年龄测定[J].地质学报,2011,85(7):1172-1187.Gao J J,Mao J W,Chen M H,et al.Vein structure analysis and 40 Ar/39 Ar dating of sericite from sub-ore altered rocks in the Tieluping large-size Ag-Pb deposit of western Henan Province[J].Acta Geologica Sinica,2011,85(7):1172-1187.(in Chinese)
[110]刘军,武广,贾守民,等.豫西沙坡岭钼矿床辉钼矿Re-Os同位素年龄及其地质意义[J].矿物岩石,2011,31(1):56-62.Liu J,Wu G,Jia S M,et al.Re-Os isotopic dating of molybdenites from the Shapoling molybdenum deposit in western Henan Province and its geological significance[J].Journal of Mineralogy&Petrology,2011,31(1):56-62.(in Chinese)
[111]Goldfarb R J,Groves D I.Orogenic gold:Common or evolving fluid and metal sources through time[J].Lithos,2015,233:2-26.
[112]Zhou Z J,Chen Y J,Jiang S Y,et al.Isotope and fluid inclusion geochemistry and genesis of the Qiangma gold deposit,Xiaoqinling gold field,Qinling Orogen,China[J].Ore Geology Reviews,2015,66:47-64.
[113]Groves D I,Goldfarb R J,Gebre-Mariam M,et al.Orogenic gold deposits-A proposed classification in the context of their crustal distribution and relationship to other gold deposit types[J].Ore Geology Reviews,1998,13:7-27.
[114]Lang J R,Baker T.Intrusion-related gold systems:The present level of understanding[J].Mineralium Deposita,2001,36:477-489.