西秦岭地区脉岩成因与金成矿关系——来自李坝金矿年代学、地球化学及Nd-Hf-S同位素的约束  

Petrogenesis of dykes and its relationship to gold mineralization in the western Qinling belt: Constraints from zircon U-Pb age,geochemistry and Nd-Hf-S isotopes of Liba gold deposit

作　　者：柯昌辉[1] 王晓霞[1] 杨阳[2] 田永飞 李金宝[2] 聂政融 吕星球 王顺安 龚明权 KE ChangHui;WANG XiaoXia;YANG Yang;TIAN YongFei;LI JinBao;NIE ZhengRong;LÜXingQiu;WANG ShunAn;GONG MingQuan(MNR Key Laboratory of Metallogeny and Mineral Assessment,Institute of Mineral Resources,CAGS,Beijing 100037,China;Collega of Earth Science and Resources,Chang'an University,Xi'an 710054,Shaanxi,China;Henan New Road&Bridge Group Motorway Management Co.,Ltd.,Zhengzhou 450000,Henan,China;No.214 Geological Party,Hunan Geological&Mining Organization for Non-Ferrous Metals,Zhuzhou 412007,Hunan,China;CCCC-FHDI Engineering Co.,Ltd.,Guangzhou 510230,Guangdong,China;School of History and Tourism,Shanxi Datong University,Datong 037009,Shanxi,China)

机构地区：[1]中国地质科学院矿产资源研究所自然资源部成矿作用与资源评价重点实验室,北京100037 [2]长安大学地球科学与资源学院,陕西西安710054 [3]河南新路桥集团高速公路管理有限公司,河南郑州450000 [4]湖南省有色地质勘查局二一四队,湖南株洲412007 [5]中交第四航务工程勘察设计院有限公司,广东广州510230 [6]山西大同大学历史与旅游文化学院,山西大同037009

出　　处：《矿床地质》2020年第1期42-62,共21页Mineral Deposits

基　　金：国家重点研发计划项目(编号:2017YFC0601403);国家自然科学基金项目(编号:41502075、41572052);中国地质科学院矿产资源研究所基本科研业务费专项经费资助(项目编号:KK1406、KK1916)联合资助

摘　　要：甘肃李坝金矿位于西秦岭北成矿亚带礼岷金矿带东部,矿区内脉岩主要包括斜闪煌斑岩、云斜煌斑岩、闪长(玢)岩、细晶闪长岩、石英闪长岩、花岗(斑)岩、花岗细晶岩等。根据各脉岩与金矿的产出关系可划分为成矿前脉岩、成矿期脉岩和成矿后脉岩3类。不同种类、不同期次脉岩的成因及其对金成矿作用的制约存在不同认识。LA-ICP-MS锆石U-Pb定年结果显示,李坝金矿区花岗斑岩脉的年龄为(210±1)Ma(MSWD=0.15),与中川岩体同属晚三叠世构造岩浆活动的产物。成矿期花岗(斑)岩脉富碱、高钾,属于过铝质、高钾钙碱性系列,与成矿密切相关的煌斑岩脉同属高钾钙碱性系列。Nd-Hf同位素结果显示,李坝金矿区花岗斑岩脉的143Nd/144Nd比值为0.512084±0.000007,147Sm/143Nd比值为0.0903,εNd(t)为-7.98,Nd同位素亏损地幔模式年龄TDM2为1.64Ga;锆石εHf(t)=-6.30^+1.47,TDMC为1.65~1.15 Ga,显示花岗斑岩脉的源区以古老的壳源物质为主,并有年轻物质的加入。硫同位素和矿床地球化学结果显示,黄铁矿的δ34S值变化于4.3‰~11.6‰,平均值为8.45‰,表明其成矿硫源具有深源特点,金矿成矿物质来源于与脉岩有关的深部岩浆。综上,笔者认为矿区内脉岩与金矿化具有深部同源性,成矿同期的煌斑岩可能为金矿化提供部分成矿物质或成矿流体。The Liba gold deposit is located in the Lixian-Minxian gold belt,western Qinling.Geological characteristics show that dykes are widely developed in the mining area and are composed of camptovogesite,mica-plagioclase lamprophyre,diorite aplite,diorite porphyry,fine diorite,quartz diorite,granite porphyry and fine-grained granite.According to their cross-cutting relationship,they can be divided into premetallogenic,mineralization and postmetallogenic dykes.The granite porphyry from the Liba gold deposit yielded an age of 210±1Ma(MSWD=0.15)by using LA-ICPMS zircon U-Pb.Granite porphyry is alkali-rich and potassium-rich,and belongs to peraluminous and high-K calc-alkaline series,whereas lamprophyre belongs to high-K calc-alkaline series.In terms of Nd-Hf-S isotopes,the granite-porphyry dykes have the data 143Nd/144Nd=0.512084±0.000007,147Sm/143Nd=0.0903,εNd(t)=-7.98,TDM2=1.64Ga,andεHf(t)=-6.30^+1.47,and TDMC=1.65~1.15Ga,suggesting that granitoid was derived mainly from an ancient continental crust,with involvement of juvenile components.Theδ34SV-CDT values of sulfides from the Liba gold deposit vary from 4.3‰to 11.6‰,with a mean of-8.45‰,which indicates that the sulfur in the orefield mainly came from mantle source.Au was mainly derived from deep magma related to granite dykes.According to these data,the authors have reached the conclusion that dykes and gold orebodies exist together spatially and temporally and have the features of the same source and successive evolution.In some degree,the dyke rocks probably provided a channel for upward movement of ore-forming materials and dykes probably provided a small amount of ore-forming materials for gold deposits.

关 键 词：地球化学 锆石U-PB测年 Nd-Hf-S同位素 李坝金矿 西秦岭 

分 类 号：P618.31[天文地球—矿床学]