«上一篇/Previous Article|本期目录/Table of Contents|下一篇/Next Article»

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:

第41卷

期数:

2019年第06期

页码:

691-706

栏目:

基础地质与矿产地质

出版日期:

2019-11-15

文章信息/Info

Title:

Characteristics of Ore-forming Fluids and Genesis of Kuru'er Cu-Au Deposit in West Tianshan, China

文章编号:

1672-6561(2019)06-0691-16

作者:

赵凯培¹; 顾雪祥¹; 2*; 章永梅¹; 2; 彭义伟³; 4;  王冠南⁵; 何宇¹; 郭建平⁶

(1. 中国地质大学(北京)地球科学与资源学院,北京 100083; 2. 中国地质大学(北京)地质过程与矿产资源国家重点实验室,北京 100083; 3. 成都理工大学 地球科学学院,四川 成都 610059; 4. 南京大学内生金属矿床成矿机制研究国家重点实验室,江苏 南京 210046; 5. 中国铝业集团有限公司,北京 100082; 6. 新疆维吾尔自治区有色地质勘查局七〇三队,新疆 伊宁 835000)

Author(s):

ZHAO Kai-pei¹;  GU Xue-xiang¹; 2*;  ZHANG Yong-mei¹; 2;  PENG Yi-wei³; 4;  WANG Guan-nan⁵;  HE Yu¹;  GUO Jian-ping⁶

(1. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China; 2. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China; 3. College of Earth Sciences, Chengdu University of Technology, Chengdu 610059,Sichuan, China; 4. State Key Laboratory for Mineral Deposits Research, Nanjing University, Nanjing 210046,Jiangsu, China; 5. Aluminum Corporation of China Limited, Beijing 100082, China; 6. No.703 Geological Team, Xinjiang Nonferrous Geoexploration Bureau, Yining 835000, Xinjiang, China)

关键词:

流体包裹体;  成矿流体;  流体不混溶;  矿床成因;  次浅成低温热液矿床;  铜金矿床;  西天山;  新疆

Keywords:

fluid inclusion;  ore-forming fluid;  fluid immiscibility;  genesis of deposit;  subepithermal deposit;  Cu-Au deposit;  West Tianshan;  Xinjiang

分类号:

P611; P618.2

DOI:

-

文献标志码:

A

摘要:

库茹尔铜金矿床位于新疆西天山晚古生代伊什基里克裂谷带,赋矿围岩为下石炭统大哈拉军山组安山质岩屑凝灰岩,矿体受一系列断裂构造控制。有关该矿床的成矿流体特征研究不足,限制了对矿床成因的认识。以该矿床的地质特征、流体包裹体为主要研究对象,探讨了成矿流体性质、来源及演化规律,初步查明了矿床成因类型。库茹尔铜金矿床热液成矿过程可划分为石英-黄铜矿-黄铁矿-自然金阶段、石英-黄铜矿阶段和石英-绿泥石/绿帘石-方解石阶段。流体包裹体研究表明:主成矿阶段(石英-黄铜矿-黄铁矿-自然金阶段)以气液水两相包裹体为主,含少量CO₂-H₂O三相包裹体与含石盐子晶多相包裹体,均一温度分别为184 ℃～359 ℃、250 ℃～319 ℃和229 ℃～263 ℃,盐度分别为4.1%～8.5% NaCl_eq、1.0%～6.0% NaCl_eq和32.7%～33.9% NaCl_eq; 石英-黄铜矿阶段和石英-绿泥石/绿帘石-方解石阶段均以气液水两相包裹体为主,均一温度分别为144 ℃～212 ℃和114 ℃～163 ℃,盐度分别为0.2%～6.7% NaCl_eq和0.1%～3.1% NaCl_eq。库茹尔铜金矿床的初始成矿流体具中—高温、中—低和高盐度的岩浆热液特征,流体不混溶是导致Au-Cu富集成矿的主要机制,矿床成因类型应属于与斑岩成矿系统相关的次浅成低温热液矿床。

Abstract:

Kuru'er Cu-Au deposit is located in Late Paleozoic Yishijilike rift belt of West Tianshan, Xinjiang. The host rock is andesite lithic tuff of Lower Carboniferous Dahalajunshan Formation, and the occurrence of orebodies is controlled by a series of fault structures. Insufficient research on the characteristics of ore-forming fluids limits the understanding of the genesis of Kuru'er Cu-Au deposit. Based on the geological characteristics and fluid inclusions, the properties, sources and evolution of ore-forming fluids were discussed, and the genetic types of deposit were initially identified. The hydrothermal mineralization process of Kuru'er Cu-Au deposit can be divided into quartz-chalcopyrite-pyrite-gold stage, quartz-chalcopyrite stage and quartz-chlorite/epidote-calcite stage. The fluid inclusion shows that the main metallogenic stage(quartz-chalcopyrite-pyrite-gold stage)is mainly composed of gas-liquid-water two-phase inclusions, containing a small amount of CO₂-H₂O three-phase inclusions and stone salt crystal multiphase inclusions, and the homogenization temperatures are 184 ℃-359 ℃, 250 ℃-319 ℃ and 229 ℃-263 ℃ with the salinities of 4.1%-8.5% NaCl_eq, 1.0%-6.0% NaCl_eq and 32.7%-33.9% NaCl_eq; quartz-chalcopyrite stage and quartz-chlorite/epidote-calcite stage are both gas-liquid-water two-phase inclusions, and the homogenization temperatures are 144 ℃-212 ℃ and 114 ℃-163 ℃, respectively, and the salinities are 0.2%-6.7% NaCl_eq and 0.1%-3.1% NaCl_eq. The initial ore-forming fluid of Kuru'er Cu-Au deposit has the characteristics of magmatic water with medium-high temperature, and medium-low and high salinities. The fluid immiscibility is the main mechanism for Au-Cu enrichment and mineralization. The genetic type of deposit belongs to the subepithermal deposit associated with the porphyry metallogenic system.

参考文献/References:

[1] 肖 龙,王方正,BEGG G,等.新疆京希—伊尔曼德金矿床矿化类型:热液蚀变及流体包裹体证据[J].矿床地质,2002,21(1):58-63.
XIAO Long,WANG Fang-zheng,BEGG G,et al.Gold Mineralization Styles of Jingxi-Yelmend Deposit:Evidence from Hydrothermal Alteration and Fluid Inclusion Data[J].Mineral Deposits,2002,21(1):58-63.
[2] XIAO L,HAYWARD N,GRAHAM B,et al.The Jingxi-Yelmand High-sulfidation Epithermal Gold Deposit,Western Tianshan,Xinjiang Province,P.R.China[J].Ore Geology Reviews,2005,26(1/2):27-30.
[3] 顾雪祥,董连慧,彭义伟,等.新疆西天山吐拉苏火山岩盆地浅成低温热液-斑岩型金多金属成矿系统的形成与演化[J].岩石学报,2016,32(5):1283-1300.
GU Xue-xiang,DONG Lian-hui,PENG Yi-wei,et al.Formation and Evolution of the Epithermal-porphyry Au Polymetallic Mineralization System in the Tulasu Volcanic Basin of the West Tianshan,Xinjiang[J].Acta Petrologica Sinica,2016,32(5):1283-1300.
[4] 王 敏,吴艳爽,汪立今,等.新疆加曼特金矿与阿希金矿的成矿条件及矿物学特征对比研究[J].中国矿业,2015,24(2):86-88.
WANG Min,WU Yan-shuang,WANG Li-jin,et al.Comparative Study on the Minerogenetic Conditions and Mineralogical Characteristics of Jiamante and Axi Gold Deposit in Xinjiang[J].China Mining Magazine,2015,24(2):86-88.
[5] 顾雪祥,章永梅,彭义伟,等.西天山博罗科努成矿带与侵入岩有关的铁铜钼多金属成矿系统:成岩成矿地球化学与构造-岩浆演化[J].地学前缘,2014,21(5):156-175.
GU Xue-xiang,ZHANG Yong-mei,PENG Yi-wei,et al.The Fe-Cu-Mo Polymetallic Mineralization System Related to Intermediate-acid Intrusions in the Boluokenu Me-tallogenic Belt of the West Tianshan,Xinjiang:Rock- and Ore-forming Geochemistry and Tectonomagmatic Evolution[J].Earth Science Frontiers,2014,21(5):156-175.
[6] 刘文臣.新疆巩留县库茹尔金铜矿地质特征及成矿分析[J].新疆有色金属,2012(2):1-4.
LIU Wen-chen.Geological Characteristics and Metallogenic Analysis of the Kuru'er Copper-gold Deposit in Gongliu County,Xinjiang[J].Xinjiang Nonferrous Metals,2012(2):1-4.
[7] 郭建平.新疆巩留县库茹尔铜金矿地质特征浅析[J].新疆有色金属,2016(1):31-33.
GUO Jian-ping.Analysis on the Geological Characteristics of the Kuru'er Copper-gold Deposit in Gongliu County,Xinjiang[J].Xinjiang Nonferrous Metals,2016(1):31-33.
[8] 刘 飞.新疆巩留县库茹尔铜金矿地质特征及找矿远景[J].新疆有色金属,2013(3):42-44,46.
LIU Fei.Geological Characteristics and Prospecting Potential of the Kuru'er Copper-gold Deposit in Gongliu County,Xinjiang[J].Xinjiang Nonferrous Metals,2013(3):42-44,46.
[9] YU J,LI N,SHU S P,et al.Geology,Fluid Inclusion and H-O-S Isotopes of the Kuru'er Cu-Au Deposit in Western Tianshan,Xinjiang,China[J].Ore Geology Reviews,2018,100:237-249.
[10] YU J,LI N,QI N,et al.Carboniferous-Permian Tectonic Transition Envisaged in Two Magmatic Episodes at the Kuru'er Cu-Au Deposit,Western Tian-shan(NW China)[J].Journal of Asian Earth Sciences,2018,153:395-411.
[11] GAO J,LONG L L,KLEMD R,et al.Tectonic Evolution of the South Tianshan Orogen and Adjacent Regions,NW China:Geochemical and Age Constraints of Granitoid Rocks[J].International Journal of Earth Sciences,2009,98(6):1221-1238.
[12] XIAO W J,WINDLEY B F,ALLEN M B,et al.Paleo-zoic Multiple Accretionary and Collisional Tectonics of the Chinese Tianshan Orogenic Collage[J].Gondwana Research,2013,23(4):1316-1341.
[13] 左国朝,张作衡,王志良,等.新疆西天山地区构造单元划分、地层系统及其构造演化[J].地质论评,2008,54(6):748-767.
ZUO Guo-chao,ZHANG Zuo-heng,WANG Zhi-liang,et al.Tectonic Division,Stratigraphical Stystem and the Evolution of Western Tianshan Mountains,Xinjiang[J].Geological Review,2008,54(6):748-767.
[14] 朱志新,董连慧,王克卓,等.西天山造山带构造单元划分与构造演化[J].地质通报,2013,32(增1):297-306.
ZHU Zhi-xin,DONG Lian-hui,WANG Ke-zhuo,et al.Tectonic Division and Regional Tectonic Evolution of West Tianshan Organic Belt[J].Geological Bulletin of China,2013,32(S1):297-306.
[15] 薛春纪.西天山巨型金铜铅锌成矿带构造成矿演化和找矿方向[J].地质学报,2014,88(12):2490-2531.
XUE Chun-ji.Tectonic-metallogenic Evolution of Western Tianshan Giant Au-Cu-Zn-Pb Metallogenic Belt and Prospecting Orientation[J].Acta Geologica Sinica,2014,88(12):2490-2531.
[16] 新疆维吾尔自治区有色地质勘查局七〇三队.新疆巩留县库勒金矿详查设计[R].伊宁:新疆维吾尔自治区有色地质勘查局,2016.
No.703 Geological Team,Xinjiang Nonferrous Geoexploration Bureau.Detailed Design of the Kule Gold Mine in Gongliu County,Xinjiang[R].Yining:Xinjiang Nonferrous Geoexploration Bureau,2016.
[17] XIAO W J,HAN C M,YUAN C,et al.Middle Cambrian to Permian Subduction-related Accretionary Orogenesis of Northern Xinjiang,NW China:Implications for the Tectonic Evolution of Central Asia[J].Journal of Asian Earth Sciences,2008,32(2/3/4):102-117.
[18] 孙升升,薛春纪,陶剑丰,等.西天山博故图金矿床H-O-S-Pb同位素示踪和Re-Os法测年[J].岩石学报,2016,32(5):1346-1360.
SUN Sheng-sheng,XUE Chun-ji,TAO Jian-feng,et al.H-O-S-Pb Isotopic Tracing and Re-Os Dating of Bogutu Gold Deposit,Western Tianshan,Xinjiang[J].Acta Petrologica Sinica,2016,32(5):1346-1360.
[19] 魏 虎,张英宁.新疆伊什基里克西段铜多金属成矿地质条件及找矿方向[J].新疆地质,2013,31(2):172-178.
WEI Hu,ZHANG Ying-ning.Ore-forming Conditions and Exploration Direction of Copper-polymetallic Deposits in the West Yishijilike Region,Xinjiang[J].Xinjiang Geology,2013,31(2):172-178.
[20] 高丽晔,章永梅,顾雪祥,等.内蒙古敖汉旗金路金矿床地质特征及成矿流体研究[J].现代地质,2019,33(1):137-151.
GAO Li-ye,ZHANG Yong-mei,GU Xue-xiang,et al.Geological Characteristics and Ore-forming Fluids of the Jinlu Gold Deposit in Aohan Banne,Inner Mongolia[J].Geoscience,2019,33(1):137-151.
[21] 陈思尧,顾雪祥,程文斌,等.云南羊拉铜矿床成矿流体特征及成矿过程[J].地学前缘,2013,20(1):82-91.
CHEN Si-yao,GU Xue-xiang,CHENG Wen-bin,et al.Characteristics of Ore-forming Fluid and Mineralization Process of the Yangla Copper Deposit,Yunnan[J].Earth Science Frontiers,2013,20(1):82-91.
[22] POTTER R W I,CLYNNE M A,BROWN D L.Freezing Point Depression of Aqueous Sodium Chloride Solutions[J].Economic Geology,1978,73(2):284-285.
[23] HALL D L,STEMER S M,BODNAR R J.Freezing Point Depression of NaCl-KCl-H₂O Solutions[J].Economic Geology,1988,83(1):197-202.
[24] BOZZO A T,CHEN H S,KASS J R,et al.The Pro-perties of the Hydrates of Chlorine and Carbon Dio-xide[J].Desalination,1975,16(3):303-320.
[25] 吴程赟,顾雪祥,刘 丽,等.贵州丫他卡林型金矿床流体包裹体特征及其成矿意义[J].现代地质,2012,26(2):277-285.
WU Cheng-yun,GU Xue-xiang,LIU Li,et al.Fluid Inclusion Characteristics of Yata Carlin-type Gold Deposit,Guizhou Province and Its Metallogenic Significance[J].Geoscience,2012,26(2):277-285.
[26] 刘 斌.利用不混溶流体包裹体作为地质温度计和压力计[J].科学通报,1986,31(18):1432-1436.
LIU Bin.Using Immiscible Fluid Inclusions as Geological Thermometers and Pressure Gauges[J].Chinese Science Bulletin,1986,31(18):1432-1436.
[27] 刘 斌,段光贤.NaCl-H₂O溶液包裹体的密度式和等容式及其应用[J].矿物学报,1987,7(4):345-352.
LIU Bin,DUAN Guang-xian.The Density and Isochoric Formulae for NaCl-H₂O Fluid Inclusions and Their Applications[J].Acta Mineralogica Sinica,1987,7(4):345-352.
[28] 邵洁涟,梅建明.浙江火山岩区金矿床的矿物包裹体标型特征研究及其成因找矿意义[J].矿物岩石,1986,6(3):103-111.
SHAO Jie-lian,MEI Jian-ming.Study on the Characterization of Mineral Inclusions in Gold Deposits in Volcanic Rocks of Zhejiang Province and Its Genesis and Prospecting Significance[J].Journal of Mineralogy and Petrology,1986,6(3):103-111.
[29] 吕鹏瑞,顾雪祥,李德荣,等.黑龙江嫩江地区三矿沟矽卡岩型铜-铁-钼多金属矿床的成矿流体特征与成矿机制[J].地质通报,2011,30(10):1563-1574.
LU Peng-rui,GU Xue-xiang,LI De-rong,et al.Ore-forming Fluid Characteristics and Mineralization Mechanism of the Sankuanggou Skarn-type Cu-Fe-Mo Polymetallic Deposit in Nenjiang Area of Heilongjiang Province[J].Geological Bulletin of China,2011,30(10):1563-1574.
[30] 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].吉林大学学报(地球科学版),2000,30(增):27-30.
SUN Feng-yue,JIN Wei,LI Bi-le,et al.Thoughts on the Metallogenic Depth of Vein Hydrothermal Gold Deposit[J].Journal of Jilin University(Earth Science Edition),2000,30(S):27-30.
[31] BODNAR R J.A Method of Calculating Fluid Inclusion Volumes Based on Vapor Bubble Diameters and P-V-T-X Properties of Inclusion Fluids[J].Economic Geology,1983,78(3):538-542.
[32] 吕鹏瑞,程文斌,吴程赟,等.西藏拉屋铜多金属矿床的成矿流体特征与成矿机制研究[J].现代地质,2013,27(1):24-36.
LU Peng-rui,CHENG Wen-bin,WU Cheng-yun,et al.Studies on Ore-forming Fluid Characteristics and Mineralization Mechanisms of the Lawu Copper Polymetallic Deposit,Tibet[J].Geoscience,2013,27(1):24-36.
[33] GIGGENBACH W F.The Origin and Evolution of Fluids in Magmatic-hydrothermal Systems[M]∥BARNES H L.Geochemistry of Hydrothermal Ore Deposits.New York:John Wiley and Sons,1997:737-796.
[34] 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 Yan-jing,NI Pei,FAN Hong-rui,et al.Diagnostic Fluid Inclusions of Different Types Hydrothermal Gold Deposits[J].Acta Petrologica Sinica,2007,23(9):2085-2108.
[35] 陈衍景,李 诺.大陆内部浆控高温热液矿床成矿流体性质及其与岛弧区同类矿床的差异[J].岩石学报,2009,25(10):2477-2508.
CHEN Yan-Jing,LI Nuo.Nature of Ore-fluids of Intracontinental Intrusion-related Hypothermal Deposits and Its Difference from Those in Island Arcs[J].Acta Petrologica Sinica,2009,25(10):2477-2508.
[36] PENG Y W,GU X X,CHENG W B,et al.Metallogenesis of the Late Palaeozoic Axi-Tawu'erbieke Au-Pb-Zn District in the Tulasu Basin,Western Tian-shan,China:Constraints from Geological Characteristics and Isotope Geochemistry[J].Geological Journal,2018,53(6):3030-3050.
[37] 翟 伟,孙晓明,贺小平,等.新疆阿希低硫型金矿床流体地球化学特征与成矿机制[J].地质学报,2007,81(5):663-665.
ZHAI Wei,SUN Xiao-ming,HE Xiao-ping,et al.Geo-chemistry of Ore Forming Fluid and Metallogenic Mechanism of Axi Low-sulfidation Gold Deposit in Xinjiang,China[J].Acta Geologica Sinica,2007,81(5):663-665.
[38] 彭义伟,顾雪祥,程文斌,等.西天山吐拉苏盆地塔吾尔别克金矿床成因探讨:来自同位素年代学和稳定同位素证据[J].岩石学报,2016,32(5):1370-1373.
PENG Yi-wei,GU Xue-xiang,CHENG Wen-bin,et al.Genesis of the Tawu'erbieke Gold Deposit in the Tulasu Basin,Western Tianshan:Evidence from Geochronology and Stable Isotopes[J].Acta Petrologica Sinica,2016,32(5):1370-1373.
[39] 贾 斌,毋瑞身,田昌烈,等.塔吾尔别克—阿庇因迪斑岩型金矿特征[J].地质与资源,2001,10(3):139-145.
JIA Bin,WU Rui-shen,TIAN Chang-lie,et al.The Characteristics of Tawu'erbieke-Abiyindi Porphyry Type of Gold Deposit[J].Geology and Resources,2001,10(3):139-145.
[40] 沙德铭,金成洙,董连慧,等.西天山阿希金矿成矿地球化学特征研究[J].地质与资源,2005,14(2):121-124.
SHA De-ming,JIN Cheng-zhu,DONG Lian-hui,et al.Study on the Metallogenic Geochemical Characteristics of Axi Gold Deposit in West Tianshan Mountains[J].Geology and Resources,2005,14(2):121-124.
[41] 肖 龙,王 方,付民禄,等.伊犁京希—伊尔曼德金矿床的热液蚀变及成矿流体演化特征[J].地质学报,2001,75(4):518-524.
XIAO Long,WANG Fang,FU Min-lu,et al.Hydrothermal Alteration and Ore-forming Fluids Evolution of the Jingxi-Yelmend Gold Deposit,Xinjiang,China[J].Acta Geologica Sinica,2001,75(4):518-524.
[42] 顾雪祥,刘 丽,董树义,等.山东沂南金铜铁矿床中的液态不混溶作用与成矿:流体包裹体和氢氧同位素证据[J].矿床地质,2010,29(1):43-57.
GU Xue-xiang,LIU Li,DONG Shu-yi,et al.Immiscibility During Mineralization of Yinan Au-Cu-Fe Deposit,Shandong Province:Evidence from Fluid Inclusions and H-O Isotopes[J].Mineral Deposits,2010,29(1):43-57.
[43] 卢焕章,毕献武,王 蝶,等.斑岩铜(钼-金)矿床的成矿流体[J].矿床地质,2016,35(5):940-947.
LU Huan-zhang,BI Xian-wu,WANG Die,et al.Ore-forming Fluids of Porphyry Copper(Molybdenum-gold)Deposits[J].Mineral Deposits,2016,35(5):940-947.
[44] 张文淮,张志坚,伍 刚.成矿流体及成矿机制[J].地学前缘,1996,3(4):245-252.
ZHANG Wen-huai,ZHANG Zhi-jian,WU Gang.Ore-forming Fluids and Metallogenic Mechanisms[J].Earth Science Frontiers,1996,3(4):245-252.
[45] 张德会.成矿流体中金属沉淀机制研究综述[J].地质科技情报,1997,16(3):53-58.
ZHANG De-hui.Summary of Metal Precipitation Mechanism in Ore-forming Fluids[J].Geological Science and Technology Information,1997,16(3):53-58.
[46] HEDENQUIST J W,ARRIBAS A,REYNOLDS T J.Evolution of an Intrusion-centered Hydrothermal System:Far Southeast Lepanto Porphyry and Epithermal Cu-Au Deposits,Philippines[J].Economic Geology,1998,93(4):374-404.
[47] SEWARD T M,BARNES H L.Metal Transport by Hydrothermal Ore Fluids[M]∥BARNES H L.Geochemistry of Hydrothermal Ore Deposits.New York:John Wiley and Sons,1997:435-486.
[48] LANDTWING M R,PETTKE T,HALTER W E,et al.Copper Deposition During Quartz Dissolution by Cooling Magmatic-hydrothermal Fluids:The Bingham Porphyry[J].Earth and Planetary Science Letters,2005,235(1/2):229-243.
[49] PUDACK C,HALTER W E,HEINRICH C A,et al.Evolution of Magmatic Vapor to Gold-rich Epithermal Liquid:The Porphyry to Epithermal Transition at Nevados de Famatina,Northwest Argentina[J].Economic Geology,2009,104(4):449-477.
[50] 蔡逸涛,倪 培,沈 昆,等.江西东乡铜矿流体包裹体研究[J].岩石学报,2011,27(5):1375-1386.
CAI Yi-tao,NI Pei,SHEN Kun,et al.Study on the Fluid Inclusion from Dongxiang Copper Deposit,Jiangxi Province,China[J].Acta Petrologica Sinica,2011,27(5):1375-1386.
[51] HEDENQUIST J W,ARRIBAS A,GONZALEZ-URIEN E.Exploration for Epithermal Gold Deposits[M]∥HAGEMANN S G,BROWN P E.Gold in 2000:Reviews in Economic Geology.Littleton:Society of Economic Geologist,2000:245-277.
[52] 陈 辉,倪 培,陈仁义,等.浙江建德铜矿流体包裹体研究[J].高校地质学报,2016,22(1):1-11.
CHEN Hui,NI Pei,CHEN Ren-yi,et al.Fluid Inclusion Studies of the Jiande Copper Deposit,Zhejiang Province,China[J].Geological Journal of China Universities,2016,22(1):1-11.
[53] 卢焕章,范宏瑞,倪 培,等.流体包裹体[M].北京:科学出版社,2004.
LU Huan-zhang,FAN Hong-rui,NI Pei,et al.Fluid Inclusions[M].Beijing:Science Press,2004.
[54] SILLITOE R H.Enargite-bearing Massive Sulfide Deposits High in Porphyry Copper Systems[J].Economic Geology,1983,78(2):348-352.
[55] SILLITOE R H.Porphyry Copper Systems[J].Economic Geology,2010,105(1):3-41.
[56] LEFORT D,HANLEY J,GUILLONG M.Subepithermal Au-Pd Mineralization Associated with an Alka-lic Porphyry Cu-Au Deposit,Mount Milligan,Quesnel Terrane,British Columbia,Canada[J].Economic Geo-logy,2011,106(5):781-808.
[57] REYES M.The Andacollo Strata-bound Gold Deposit,Chile,and Its Position in a Porphyry Copper-gold System[J].Economic Geology,1991,86(6):1301-1316.
[58] CATCHPOLE H,KOUZMANOV K.Zoned Base Metal Mineralization in a Porphyry System:Origin and Evolution of Mineralizing Fluids in the Morococha District,Peru[J].Economic Geology,2015,110(1):29-71.
[59] MAYDAGAN L,FRANCHINI M,RUSK B,et al.Porphyry to Epithermal Transition in the Altar Cu-(Au-Mo)Deposit,Argentina,Studied by Cathodoluminescence,LA-ICP-MS,and Fluid Inclusion Analysis[J].Economic Geology,2015,110(4):889-923.

相似文献/References:

[1]杨富全,刘锋,柴凤梅,等.新疆阿尔泰铁矿成矿流体及成矿过程[J].地球科学与环境学报,2012,34(03):17.
　YANG Fu-quan,LIU Feng,CHAI Feng-mei,et al.Ore-forming Fluid and Metallogenic Process of Iron Deposit in Altay of Xinjiang[J].Journal of Earth Sciences and Environment,2012,34(06):17.
[2]张海,何明友,李方林,等.陕西凤县二里河喷流沉积型铅锌矿床的地质地球化学证据[J].地球科学与环境学报,2011,33(01):64.
　ZHANG Hai,HE Ming-you,LI Fang-lin,et al.Geological and Geochemical Evidence of the Erlihe SEDEX Pb-Zn Deposit in Fengxian, Shaanxi[J].Journal of Earth Sciences and Environment,2011,33(06):64.
[3]旷理雄,郭建华,童小兰,等.准噶尔盆地南缘东段油气成藏条件及成藏模式[J].地球科学与环境学报,2007,29(01):34.
　KUANG Li-xiong,GUO Jian-hua,TONG Xiao-lan,et al.Forming Conditions and Patterns of Hydrocarbon Reservoirs in East of Southern Fringe of Junggar Basin[J].Journal of Earth Sciences and Environment,2007,29(06):34.
[4]朱华平,孙丰月,李碧乐,等.青海驼路沟钴矿床流体 包裹体及成矿物理化学条件[J].地球科学与环境学报,2007,29(04):351.
　ZHU Hua-ping,SUN Feng-yue,LI Bi-le,et al.Fluid Inclusions Characteristics and Physicochemical Condition of Tuolugou Cobalt Deposit,Qinghai[J].Journal of Earth Sciences and Environment,2007,29(06):351.
[5]高晓理,彭明兴,胡长安,等.新疆彩霞山铅锌矿床流体包裹体研究[J].地球科学与环境学报,2006,28(02):25.
　GAO Xiao-li,PENG Ming-xing,HU Chang-an,et al.Fluid Inclusions of Caixiashan Pb-Zn Deposit in Xinjiang[J].Journal of Earth Sciences and Environment,2006,28(06):25.
[6]国殿斌,万涛,李继东,等.东濮凹陷方里集构造带油气来源及成藏期[J].地球科学与环境学报,2017,39(04):530.
　GUO Dian-bin,WAN Tao,LI Ji-dong,et al.Hydrocarbon Sources and Reservoir Forming Stages in Fangliji Tectonic Belt of Dongpu Depression, China[J].Journal of Earth Sciences and Environment,2017,39(06):530.
[7]彭军,林攀,夏青松,等.塔北地区寒武系白云岩储层裂缝充填特征与有效性[J].地球科学与环境学报,2019,41(01):40.
　PENG Jun,LIN Pan,XIA Qing-song,et al.Effectiveness and Filling Characteristics of the Fractures of Cambrian Dolomite Reservoir in the Northern Tarim Basin, China[J].Journal of Earth Sciences and Environment,2019,41(06):40.
[8]王敏芳,尚晓雨,魏克涛,等.鄂东南矿集区铜绿山矽卡岩型铜铁金矿床元素地球化学特征及其地质意义[J].地球科学与环境学报,2019,41(04):431.
　WANG Min-fang,SHANG Xiao-yu,WEI Ke-tao,et al.Elemental Geochemical Characteristics of Tonglushan Skarn-type Cu-Fe-Au Deposit in the Southeastern Hubei, China and Their Geological Implications[J].Journal of Earth Sciences and Environment,2019,41(06):431.
[9]毛光周,何铁良,许庆林,等.山东胶东地区盘子涧金矿成矿流体He-Ar同位素地球化学特征[J].地球科学与环境学报,2020,42(02):188.[doi:10.19814/j.jese.2019.10042]
　MAO Guang-zhou,HE Tie-liang,XU Qing-lin,et al.He-Ar Isotope Geochemical Characteristics of Ore-forming Fluids for Panzijian Gold Deposit in Jiaodong Area of Shandong, China[J].Journal of Earth Sciences and Environment,2020,42(06):188.[doi:10.19814/j.jese.2019.10042]
[10]吴夏涛,周家喜*,张 浩,等.川滇黔接壤地区铅锌矿床成矿物质来源:方铅矿原位Pb同位素制约[J].地球科学与环境学报,2023,45(02):266.[doi:10.19814/j.jese.2022.11027]
　WU Xia-tao,ZHOU Jia-xi*,ZHANG Hao,et al.Source of Ore-forming Materials for the Carbonate-hosted Pb-Zn Deposits in Sichuan-Yunnan-Guizhou Adjacent Area, SW China: Constraints of Galena In-situ Pb Isotopes[J].Journal of Earth Sciences and Environment,2023,45(06):266.[doi:10.19814/j.jese.2022.11027]
[11]李铁刚,武 广,陈公正,等.华北克拉通南缘小秦岭矿集区灵湖金矿床成因:流体包裹体和H-O、S-Pb同位素证据[J].地球科学与环境学报,2020,42(05):569.[doi:10.19814/j.jese.2020.06031]
　LI Tie-gang,WU Guang,CHEN Gong-zheng,et al.Genesis of Linghu Gold Deposit in Xiaoqinling Ore District, the Southern Margin of North China Craton, China: Evidence from Fluid Inclusions, H-O and S-Pb Isotopic Compositions[J].Journal of Earth Sciences and Environment,2020,42(06):569.[doi:10.19814/j.jese.2020.06031]

备注/Memo

备注/Memo:

收稿日期:2019-04-17; 修回日期:2019-07-08投稿网址:http:∥jese.chd.edu.cn/
基金项目:国家自然科学基金项目(41572062,41702081); 国家重点研发计划项目(2018YFC0604003); 南京大学内生金属矿床成矿机制研究国家重点实验室开放研究基金项目(2018-LAMD-K07); 中央高校基本科研业务费专项资金项目(2652017226)
作者简介:赵凯培(1994-),男,河北石家庄人,理学硕士研究生,E-mail:1185327300@qq.com。
*通讯作者:顾雪祥(1963-),男,江苏海门人,教授,博士研究生导师,理学博士,E-mail:xuexiang_gu@cugb.edu.cn。

常用功能

更新日期/Last Update: 2019-11-19