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胶东玲珑金矿床成矿地质特征及矿床成因

作者：
张振|于超|吴志栋|王海屹|徐增田|梁亚运
作者单位：
山东黄金矿业（玲珑）有限公司|山东黄金矿业（玲珑）有限公司|山东黄金矿业（玲珑）有限公司|北京科技大学土木与资源工程学院|山东黄金矿业（玲珑）有限公司|北京科技大学土木与资源工程学院
基金项目：
第八届中国科协青年人才托举工程项目（YESS20220661）；国家自然科学基金面上项目（42273063）
详细信息：
作者简介：
张振（1989—），男，工程师，从事矿山地质工作；E-mail:414235189@qq.com
通讯作者：
王海屹（2000—），男，硕士研究生，研究方向为岩石学与矿床学；E-mail:1434383299@qq.com
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Geological characteristics and genesis of Linglong Gold Deposit in Jiaodong

English Author：
Shandong Gold Mining (Linglong) Co.,Ltd.|Shandong Gold Mining (Linglong) Co.,Ltd.|Shandong Gold Mining (Linglong) Co.,Ltd.|School of Civil and Resource Engineering,University of Science and Technology Beijing|Shandong Gold Mining (Linglong) Co.,Ltd.|School of Civil and Resource Engineering,University of Science and Technology Beijing
Unit：

摘要
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参考文献

摘要:

玲珑金矿床位于华北克拉通东部胶东大型金矿集区西北部，是全球典型石英脉型金矿床之一，金资源总量超过1 000 t，但对于其矿床成因一直存在争议。通过系统总结玲珑金矿床地质特征、地质年代学、成矿流体特征及同位素数据，详细探讨了成矿地质特征和矿床成因。玲珑金矿床形成年龄集中在120~125 Ma，成矿流体整体属于中低温、低盐度、低密度热液流体，主要源自岩浆流体，并混有少量大气降水。C-H-O-S-Pb同位素指示，玲珑金矿床成矿流体主要来自地幔来源岩浆流体，并伴有壳源流体加入。早白垩世，华北克拉通东部岩石圈拆沉减薄引发软流圈上涌，进而不断底侵岩石圈地幔，发生部分熔融形成基性岩脉岩浆。基性岩脉岩浆上涌至地壳浅部时，温度、压力急速下降，脱气形成流体，沿着次级断裂沉淀形成金矿床，具有典型胶东型金矿床特征。

关键词:

胶东型；玲珑金矿床；石英脉型金矿床；成矿流体；矿床成因；成矿年龄

Abstract:

Linglong Gold Deposit,located in the northwestern part of the Jiaodong large-scale gold province in the eastern North China Craton,is one of the worlds typical quartz vein-type gold deposits,with total gold resources exceeding 1 000 t.However,there has been ongoing debate regarding its genesis.By systematically summarizing the geological characteristics,geochronology,characteristics of ore-forming fluids,and isotope data of Linglong Gold Deposit,this study thoroughly discusses its geological characteristics and genesis.The formation age of Linglong Gold Deposit is concentrated 120-125 Ma.The ore-forming fluids are generally medium-to-low-temperature,low-salinity,and low-density hydrothermal fluids,primarily derived from magmatic fluids with a minor contribution from meteoric water.C-H-O-S-Pb isotopes indicate that the ore-forming fluids of Linglong Gold Deposit mainly originated from mantle-derived magmatic fluids,with some contribution from crustal fluids.During the Early Cretaceous,lithospheric delamination and thinning in the eastern North China Craton triggered asthenospheric upwelling,leading to continuous underplating of the lithospheric mantle,which partially melted to form mafic dyke magma.As the mafic dyke magma ascended to the shallow crust,rapid decreases in temperature and pressure caused degassing and fluid formation,which precipitated along secondary faults to form the gold deposit,exhibiting the typical characteristics of Jiaodong-type gold deposits.

Keywords:

Jiaodong-type;Linglong Gold Deposit;quartz vein-type gold deposit;ore-forming fluids;deposit genesis;mineralization age

[1]DENGJ,WANGQF.GoldmineralizationinChina:Metallogenicprovinces,deposittypesandtectonicframework[J].GondwanaResearch,2016,36:219-274.
[2]宋明春，杨立强，范宏瑞，等.找矿突破战略行动十年胶东金矿成矿理论与深部勘查进展[J].地质通报，2022，41(6):903-935.
[3]阿卜杜萨拉木·喀迪尔，陆继龙，范玉超，等.胶东地区笏山金矿床黄铁矿微量元素特征及其成矿指示意义[J].黄金，2023，44(4):57-62.
[4]翟明国，范宏瑞，杨进辉，等.非造山带型金矿——胶东型金矿的陆内成矿作用[J].地学前缘，2004，11(1):85-98.
[5]王润生，张保涛，柳森，等.胶东牟平-乳山成矿带金青顶金矿广域电磁法探测效果分析[J].地质与勘探，2022，58(2):381-390.
[6]孙之夫，冯涛，胡跃亮，等.胶东西岭金矿床地质特征与金的赋存状态[J].地质与勘探，2022，58(1):24-36.
[7]TIANRC,LIDP,TIANJP,etal.GenesisoftheJiudiangolddeposit,JiaodongPeninsula,easternChina:FluidinclusionandC-H-O-Pbisotopeconstraints[J].OreGeologyReviews,2022，149:105086.
[8]WANGX,WANGZC,CHENGH,etal.Goldendowmentofthemetasomatizedlithosphericmantleforgiantgolddeposits:Insightsfromlamprophyredykes[J].GeochimicaetCosmochimicaActa,2022,316:21-40.
[9]李士先，刘长春，安郁宏，等.胶东金矿地质[M].北京:地质出版社，2007.
[10]SONGMC,DENGJ,YIPH,etal.ThekilotonclassJiaojiagolddepositineasternShandongProvinceanditsgenesis[J].ActaGeologicaSinica（EnglishEdition）,2014,88(3):801-824.
[11]GOLDFARBRJ,GROVESDI,GARDOLLS.Orogenicgoldandgeologictime:Aglobalsynthesis[J].OreGeologyReviews,2001,18(1/2):1-75.
[12]GROVESDI,SANTOSHM.ThegiantJiaodonggoldprovince:Thekeytoaunifiedmodelfororogenicgolddeposits?[J].GeoscienceFrontiers,2016,7(3):409-417.
[13]ZHURX,FANHR,LIJW,etal.Decratonicgolddeposits[J].ScienceChinaEarthSciences,2015,58:1523-1537.
[14]宋明春，林少一，杨立强，等.胶东金矿成矿模式[J].矿床地质,2020,39(2):215-236.
[15]程力.玲珑金矿九曲分矿通风系统优化研究[J].黄金,2023,44(10):9-12.
[16]赵泳越.?蕉×徵缃鹂罂蟠渤梢蜓芯縖D].长春：吉林大学,2012.
[17]冯岳川,邓军,于皓丞,等.胶东玲珑金矿田金的赋存状态及其对成矿过程的指示意义[J].岩石学报,2023,39(2):377-392.
[18]孙华山,韩静波,申玉科,等.胶西北玲珑、焦家金矿田锆石(U-Th)/He年龄及其对成矿后剥露程度的指示[J].地球科学,2016,41(4):644-654.
[19]WENBJ,FANHR,SANTOSHM,etal.GenesisoftwodifferenttypesofgoldmineralizationintheLinglonggoldfield,China:Constrainsfromgeology,fluidinclusionsandstableisotope[J].OreGeologyReviews,2015,65:643-658.
[20]严千豪,王翠芝,吕古贤,等.胶东玲珑金矿黄铁矿的化学成分标型特征及其矿床学意义[J].地质找矿论丛,2020,35(1):52-63.
[21]GUOLN,DENGJ,YANGLQ,etal.GolddepositionandresourcepotentialoftheLinglonggolddeposit,JiaodongPeninsula:Geochemicalcomparisonoforefluids[J].OreGeologyReviews,2020,120:103434.
[22]王志强.胶东玲珑金矿床流体包裹体特征及其成矿过程分析[D].南昌：东华理工大学,2015.
[23]李世勇,李杰,宋明春,等.胶东玲珑金矿田成矿特征和成矿作用[J].地质学报,2022,96(9):3234-3260.
[24]LIANGYY,SHUL,MAPY,etal.Goldsourceandore-formingprocessoftheLinglonggolddeposit,Jiaodonggoldprovince,China:Evidencefromtextures,mineralchemicalcompositionsandsulfurisotopesofpyrite[J].OreGeologyReviews,2023,159:105523.
[25]杨进辉,周新华.胶东地区玲珑金矿矿石和载金矿物Rb-Sr等时线年龄与成矿时代[J].科学通报,2000,45(14):1547-1553.
[26]LIQL,CHENF,YANGJH,etal.SinglegrainpyriteRb-SrdatingoftheLinglonggolddeposit,easternChina[J].OreGeologyReviews,2008,34(3):263-270.
[27]王义文,朱奉三,宫润潭.胶东金矿集中区金矿成矿年代学研究[J].黄金地质,2002,8(4):48-55.
[28]YANGJH,ZHOUXH.Rb-Sr,Sm-Nd,andPbisotopesystematicsofpyrite:Implicationsfortheageandgenesisoflodegolddeposits[J].Geology,2001,29(8):711-714.
[29]DENGJ,QIUKF,WANGQF,etal.InsitudatingofhydrothermalmonaziteandimplicationsforthegeodynamiccontrolsonoreformationintheJiaodonggoldprovince,easternChina[J].EconomicGeology,2020,115(3):671-685.
[30]林祖苇.胶东玲珑金矿田石英脉型与蚀变岩型矿体黄铁矿矿物学和地球化学的对比及对成因的指示[D].武汉：中国地质大学（武汉）,2019.
[31]张栋霖.胶东玲珑九曲金矿床成矿流体特征与来源[D].北京：中国地质大学(北京),2021.
[32]卢焕章,GUHAJ,方根保.山东玲珑金矿的成矿流体特征[J].地球化学,1999,28(5):421-437.
[33]张祖青,赖勇,陈衍景.山东玲珑金矿流体包裹体地球化学特征[J].岩石学报,2007,23(9):2207-2216.
[34]王可勇,张春燕,樊岳铭,等.山东玲珑金矿床成矿流体地球化学特征[J].吉林大学学报(地球科学版),2008,38(2):194-201.
[35]李碧乐,王力,霍亮,等.胶东玲珑金矿52#脉群成矿流体特征及成因[J].自然科学进展,2009,19(1):51-60.
[36]秦丹鹤,王可勇,常亮,等.山东玲珑九曲金矿床地质特征及流体包裹体研究[J].世界地质,2013,32(3):505-514.
[37]YANGQY,SHENJF,LISR,etal.Oxygen,boron,chromiumandniobiumenrichmentinnativeAuandAggrains:AcasestudyfromtheLinglonggolddeposit,Jiaodong,easternChina[J].JournalofAsianEarthSciences,2013,62:537-546.
[38]丛智超,孙丰月,王力,等.山东招远九曲金矿床成矿流体地球化学特征[J].世界地质,2015,34(2):362-371.
[39]程韩宇.胶东玲珑金矿和焦家金矿地球化学特征对比研究[D].北京：中国地质大学(北京),2019.
[40]ZHAOSR,LIZK,LINZW,etal.MagmaticfluidsresponsibleforlodegoldmineralizationinthegiantLinglongdepositatJiaodong,NorthChinaCraton:ConstraintsfromLiOisotopes[J].ChemicalGeology,2023,638:121696.
[41]王磊.山东玲珑金矿流体包裹体及同位素特征研究[D].北京：中国地质大学（北京）,2010.
[42]陈光远，邵伟，孙岱生.胶东金矿成因矿物学与找矿[M].重庆:重庆科技出版社,1989.
[43]侯明兰,蒋少涌,姜耀辉,等.胶东蓬莱金成矿区的S-Pb同位素地球化学和Rb-Sr同位素年代学研究[J].岩石学报,2006,22(10):2525-2533.
[44]马广刚.胶东玲珑金矿成因矿物学与深部远景研究[D].北京：中国地质大学(北京),2011.
[45]LIL,SANTOSHM,LISR.The‘Jiaodongtype’golddeposits:Characteristics,originandprospecting[J].OreGeologyReviews,2015,65:589-611.
[46]杨忠芳,徐景奎,赵伦山,等.胶东两大成因系列金矿石英包裹体氢氧同位素及成矿流体组分地球化学研究[J].矿物学报,1991,11(4):363-369.
[47]卢焕章,袁万春,张国平,等.玲珑—焦家地区主要金矿床稳定同位素及同位素年代学[J].桂林工学院学报,1999,19(1):3-10.
[48]YANGLQ,DENGJ,GUOLN,etal.Originandevolutionoforefluid,andgold-depositionprocessesatthegiantTaishanggolddeposit,JiaodongPeninsula,easternChina[J].OreGeologyReviews,2016,72:585-602.
[49]姚凤良.胶东西北部脉状金矿[M].长春：吉林科学技术出版社，1990.
[50]毛景文,李厚民,王义天,等.地幔流体参与胶东金矿成矿作用的氢氧碳硫同位素证据[J].地质学报,2005,79(6):839-857.
[51]HOEFSJ.Stableisotopegeochemistry[M].Berlin:Springer,1997.
[52]DENGJ,LIUXF,WANGQF,etal.OriginoftheJiaodong-typeXinligolddeposit,JiaodongPeninsula,China:ConstraintsfromfluidinclusionandC-D-O-S-Srisotopecompositions[J].OreGeo-logyReviews,2015,65:674-686.
[53]赵伦山,张本仁.地球化学[M].北京:地质出版社，1988:166-188.
[54]李兆龙,杨敏之.胶东金矿床地质地球化学[M].天津:天津科学技术出版社,1993.
[55]周新华,杨进辉,张连昌.胶东超大型金矿的形成与中生代华北大陆岩石圈深部过程[J].中国科学(D辑:地球科学),2002,32(增刊1):11-20.
[56]WANGZC,CHENGH,ZONGKQ,etal.MetasomatizedlithosphericmantleforMesozoicgiantgolddepositsintheNorthChinacraton[J].Geology,2020,48(2):169-173.
[57]LISR,SANTOSHM.Metallogenyandcratondestruction:RecordsfromtheNorthChinaCraton[J].OreGeologyReviews,2014,56:376-414.
[58]DENGJ,LIUXF,WANGQF,etal.IsotopiccharacterizationandpetrogeneticmodelingofEarlyCretaceousmaficdiking—LithosphericextensionintheNorthChinacraton,easternAsia[J].GeologicalSocietyofAmericaBulletin,2017,129(11/12):1379-1407.
[59]DONGLL,YANGZM,SONGMC,etal.PetrogenesisofMesozoicmagmaticsuitesintheJiaodongPeninsula:Implicationsforcrust-mantleinteractionsanddecratonization[J].Lithosphere,2023(1):6226908.
[60]WUFY,YANGJH,XUYG,etal.DestructionoftheNorthChinacratonintheMesozoic[J].AnnualReviewofEarthandPlanetarySciences,2019,47:173-195.
[61]王立功,李秀章,于晓卫,等.胶东大泽山、天柱山花岗岩岩石成因和构造背景:地球化学、锆石U-Pb年代学及Lu-Hf同位素约束[J].吉林大学学报(地球科学版),2022,52(3):879-898.
[62]仲米山,罗银花,刘冰,等.华北克拉通东部新房金矿床成矿规律与三维成矿预测[J].黄金,2023,44(7):48-54.
[63]王兴刚,孙涛,向胤合,等.胶西北大尹格庄金矿床与夏甸金矿床差异性研究[J].黄金,2023,44(2):67-72.
[64]LIANGYY,LIUXF,QINC,etal.PetrogenesisofearlyCretaceousmaficdikesinsoutheasternJiaolaibasin,JiaodongPeninsula,China[J].InternationalGeologyReview,2017,59(2):131-150.
[65]GOSSSC,WILDESA,WUFY,etal.Theage,isotopicsignatureandsignificanceoftheyoungestMesozoicgranitoidsintheJiaodongTerrane,ShandongProvince,NorthChinaCraton[J].Lithos,2010,120(3/4):309-326.
[66]YANQS,METCALFEI,SHIXF,etal.EarlyCretaceousgraniticrocksfromthesouthernJiaodongPeninsula,easternChina:Implicationsforlithosphericextension[J].InternationalGeologyReview,2019,61(7):821-838.
[67]邓军,王庆飞,张良,等.胶东型金矿成因模型[J].中国科学:地球科学,2023,53(10):2323-2347.

期刊导读

胶东玲珑金矿床成矿地质特征及矿床成因

基金项目：

详细信息：

Geological characteristics and genesis of Linglong Gold Deposit in Jiaodong

摘要:

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Abstract:

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