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首页 > 黄金地质

黑龙江省黑河市五道沟地区金矿化特征及矿床成因

张浩文|王可勇|马万里|孙清飞|赵晨光
作者单位：
吉林大学地球科学学院|吉林大学地球科学学院|吉林大学地球科学学院|吉林大学地球科学学院|吉林大学地球科学学院
基金项目：
东北亚矿产资源评价自然资源部重点实验室开放基金项目（DBY-ZZ-18-12）；中国地质调查局中国科学技术部项目（2017YFC0601304）
详细信息：
作者简介：
张浩文(1996—)，男，黑龙江齐齐哈尔人，硕士研究生，研究方向为矿床学；长春市建设街2199号，吉林大学地球科学学院，130061；E-mail:zhanghw19@mails.jlu.edu.cn
通讯作者：
E-mail:wangky@jlu.edu.cn，13069004095
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Characteristics and deposit genesis of gold mineralization in Wudaogou area,Heihe City,Heilongjiang Province

English Author：
College of Earth Sciences,Jilin University|College of Earth Sciences,Jilin University|College of Earth Sciences,Jilin University|College of Earth Sciences,Jilin University|College of Earth Sciences,Jilin University
Unit：

摘要
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参考文献

摘要:

五道沟地区地处中亚造山带东部，黑河—贺根山断裂西北部，构造、岩浆活动强烈，主要发育印支期侵入体和2组北东向断裂，为金矿化提供了有利的地质条件。该地区金矿化以石英脉型为主，成矿作用可分为石英-黄铁矿-自然金阶段（Ⅰ）、石英-黄铁矿-黄铜矿-闪锌矿阶段（Ⅱ）、方解石-贫硫化物阶段（Ⅲ）3个阶段，且伴随绿泥石化和绢云母化蚀变。流体包裹体研究结果表明：主要发育气液两相包裹体（L型）、含CO₂包裹体（C型）和富气相包裹体（V型）3种类型包裹体；成矿Ⅰ、Ⅱ、Ⅲ阶段由中高温、中等盐度的CO₂-NaCl-H₂O体系逐渐演化为低温、低盐度的NaCl-H₂O体系，期间压力骤降引发的流体沸腾作用是金属矿物沉淀的主要原因。氢-氧同位素测试结果表明：δDV-SMOW与δ18OH₂O分别为-128.5 ‰~-99.6 ‰和-2.3 ‰~6.5 ‰，暗示成矿流体主要来源于岩浆水，同时伴随少量的大气降水混入。

关键词:

金矿化特征；热液脉型金矿化；流体包裹体；五道沟地区；黑龙江省

Abstract:

Wudaogou area is located in the eastern section of the Central Asian orogenic belt,and the northwestern section of Heihe-Hegenshan fault.There are intense structural and magmatic activities in the area and develop Indosinian intrusions and 2 groups of NE-trending faults,which are favorable geologic conditions for gold mineralization.The gold mineralization in the area is dominated by quartz veins,and the mineralization can be pided into quartz-pyrite-gold stage (Ⅰ),quartz-pyrite-chaloopyrite-sphalerite stage (Ⅱ),and calcite-poor sulfide stage (Ⅲ);and associated with the alteration of chloritization and sericitization.Research on fluid inclusions shows that there are 3 types of fluid inclusions:gas-liquid two-phase inclusions(L-type),CO2-containing inclusions(C-type),and gas-rich inclusions(V-type).The Ⅰ,Ⅱ and Ⅲ stages of mineralization gradually evolved from the CO2-NaCl-H2O system with medium high temperature and medium salinity to the NaCl-H2O system with low temperature and low salinity.

Keywords:

characteristics of gold mineralization;hydrothermal vein type gold mineralization deposit;fluid inclusion;Wudaogou area;Heilongjiang Province

[1]PIRAJNOF.Intracontinentalstrike-slipfaults,associatedmagmatism,mineralsystemsandmantledynamics:examplesfromNWChinaandAltay-Sayan(Siberia)[J].JournalofGeodynamics,2010,50(3/4):325-346.
[2]SENGORAMC,NATALINBA,BURTMANVS.EvolutionoftheAltaidtectoniccollageandPalaeozoiccrustalgrowthinEurasia[J].Nature,1993,364:299-307.
[3]XIAOWJ,WINDLEYBF,ALLENMB,etal.PaleozoicmultipleaccretionaryandcollisionaltectonicsoftheChineseTianshanorogeniccollage[J].GondwanaResearch,2013,23(4):1316-1341.
[4]GOLDFARBRJ,TAYLORRD,COLLINSGS,etal.PhanerozoiccontinentalgrowthandgoldmetallogenyofAsia[J].GondwanaResearch,2014,25(1):48-102.
[5]MAOJW,PIRAJNOF,LEHMANNB,etal.DistributionofporphyrydepositsintheEurasiancontinentandtheircorrespondingtectonicsettings[J].JournalofAsianEarthSciences,2014,79:576-584.
[6]SELTMANNR,PORTERTM,PIRAJNOF.Geodynamicsandmetal-logenyofthecentralEurasianporphyryandrelatedepithermalmineralsystems:areview[J].JournalofAsianEarthSciences,2014,79:810-841.
[7]ZHANGFF,WANGYH,LIUJJ,etal.OriginoftheWunugetushanporphyryCu-Modeposit,InnerMongolia,NEChina:constraintsfromgeology,geochronology,geochemistry,andisotopiccompositions[J].JournalofAsianEarthSciences,2016,117:208-224.
[8]ZHAOYY,WANGJP,ZHAOGJ,etal.MetallogenicregularityandprospectingdirectionofDuobaoshanorefield,HeilongjiangProvince,China[J].JournalofJilinUniversity(EarthScienceEdition),2011,41(6):1676-1688.
[9]崔根,王金益,张景仙,等.黑龙江多宝山花岗闪长岩的锆石SHRIMPU-Pb年龄及其地质意义[J].世界地质,2008,27(4):387-394.
[10]CHENYJ,ZHANGC,LIN,etal.GeologyoftheModepositsinnortheastChina[J].JournalofJilinUniversity(EarthScienceEdition),2012,42(5):1223-1268.
[11]LIUJ,WUG,HONGW,etal.FluidinclusionstudyoftheDuobao-shanporphyryCu(Mo)deposit,HeilongjiangProvince,China[J].ActaPetrologicaSinica,2010,26(5):1450-1464.
[12]杜琦.多宝山斑岩铜矿床蚀变与矿化特征[J].地质学报,1980,54(4):310-323.
[13]XIAOWJ,WINDLEYB,HAOJJ,etal.AccretionleadingtocollisionandthePermianSolonkersuture,InnerMongolia,China:terminationoftheCentralAsianOragenicBelt[J].Tectonics,2003,22(6):8-1-8-20.
[14]蔡文艳.黑龙江省多宝山矿集区铜—钼—金多金属成矿作用研究[D].长春：吉林大学,2020.
[15]SONGGX,QINKZ,WANGL,etal.Type,zirconU-PbageandPaleo-volcanoedificeofZhengguanggolddepositinDuobaoshanorefieldinHeilongjiangProvince,NE-China[J].ActaPetrologicaSinica,2015,31(8):2402-2416.
[16]QUH,LICL,ZHAOZH,etal.ZirconU-PbagesandgeochemicalcharacteristicsofthegranitesinDuobaoshanarea,NortheastDaHingganMountains[J].GeologyinChina,2011,38(2):292-300.
[17]ZENGH,ZHAOYY,FUJJ,etal.FeaturesofsulfideandplumbumisotopesoftheCopperdepositsinDuobaoshanDepositClusterinHeilongjiangProvince,China[J].ActaGeologicaSinica,2014,88(S2):643-644.
[18]HAOYJ,RENYS,DUANMX,etal.MetallogeniceventsandtectonicsettingoftheDuobaoshanorefieldinHeilongjiangPro-vince,NEChina[J].JournalofAsianEarthSciences,2015,97:442-458.
[19]韩振新,徐衍强,郑庆道.黑龙江省重要金属和非金属矿产的矿床成矿系列及其演化[M].哈尔滨：黑龙江人民出版社,2004.
[20]李之彤,王希今,王宏博,等.黑龙江省嫩江县三矿沟含金铁铜矿床地质特征[J].地质与资源,2008，17(3):170-174.
[21]GAORZ,XUECJ,L XB,etal.GenesisoftheZhengguanggolddepositintheDuobaoshanorefield,HeilongjiangProvince,NEChina:constraintsfromgeology,geochronologyandS-Pbisotopiccompositions[J].OreGeologyReviews,2017,84:202-217.
[22]ZHAOC,QINKZ,SONGGX,etal.EarlyPalaeozoichigh-Mgbasalt-andesitesuiteintheDuobaoshanPorphyryCudeposit,NEChina:constraintsonpetrogenesis,mineralization,andtectonicsetting[J].GondwanaResearch,2019,71:91-116.
[23]POTTERⅡRW,CLYNNEMA.Solubilityofhighlysolublesaltsinaqueousmedia.Part1.NaCl,KCl,CaCl2,Na2SO4,andK2SO4solubilitiesto100℃[J].JournalResearchofUnitedStatesGeologicalSurvey,1978,6(6):701-705.
[24]张文淮,陈紫英.流体包裹体地质学[M].武汉：中国地质大学出版社,1993：83-92.
[25]卢焕章.流体包裹体[M].北京:科学出版社,2004:487.
[26]CLAYTONRN,O’NEILJR,MAYEDATK.Oxygenisotopeexchangebetweenquartzandwater[J].JournalofGeophysicalResearch,1972,77(17):3057-3067.
[27]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.
[28]O’NEILJR.Stableisotopesinmineralogy[J].PhysicsandChemistryofMinerals,1977,2(1/2):105-123.
[29]EVANSAM.Oregeologyandindustrialminerals[M].Oxford:BlackwellScientificPublications,1993.
[30]刘斌.利用流体包裹体及其主矿物共生平衡的热力学方程计算形成温度和压力[J].中国科学(B辑),1987(3):303-310.
[31]HAOYJ,RENYS,DUANMX,etal.TectonicsettingofTriassicmagmaticandmetallogeniceventintheDuobaoshanmineralizationareaofHeilongjiangProvince,NEChina[J].GeologicalJournal,2015,52(1):67-91.
[32]马万里.黑龙江省黑河市五道沟地区Au-Mo矿化特征及成因研究[D].长春：吉林大学,2020.

期刊导读

黑龙江省黑河市五道沟地区金矿化特征及矿床成因

基金项目：

详细信息：

Characteristics and deposit genesis of gold mineralization in Wudaogou area,Heihe City,Heilongjiang Province

摘要:

关键词:

Abstract:

Keywords:

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