四川省拉拉铜矿田赋矿变质岩原岩恢复及其对找矿的指示  

Protolith reconstruction and its significance in the search for the ore-hosting metamorphic rock series in Hekou Group,the Lala copper orefield,Sichuan Province

作　　者：陶文[1] 薛建玲[1,2] 陈辉 程志中[1,2] 庞振山 林鲁军[1,2,3] 龚灵明 张济礼[4] TAO Wen;XUE Jianling;CHEN Hui;CHENG Zhizhong;PANG Zhenshan;LIN Lujun;GONG Lingming;ZHANG Jili(Development and Research Center,China Geological Survey,Beijing 100037,China;Technical Guidance Center for Mineral Resources Exploration,Ministry of Natural Resources,Beijing 100083,China;School of Earth Sciences and Resources,China University of Geosciences,Beijing 100083,China;No.403 Geological Party,Sichuan Bureau of Geology and Mineral Resources,Emeishan 614200,Sichuan,China)

机构地区：[1]中国地质调查局发展研究中心,北京100037 [2]自然资源部矿产勘查技术指导中心,北京100083 [3]中国地质大学(北京)地球科学与资源学院,北京100083 [4]四川省地质矿产勘查开发局四0三地质队,四川峨眉山614200

出　　处：《地质通报》2020年第8期1247-1257,共11页Geological Bulletin of China

基　　金：国家重点研发计划项目课题《深部矿产资源三维找矿预测评价示范》(编号:2017YFC0601506);中国地质调查局项目《全国重要矿集区找矿预测》(编号:DD20160052);《矿集区矿产调查及深部找矿预测》(编号:DD20190570)。

摘　　要：四川拉拉铜矿是中国著名的大型富铜矿床,其矿体均赋存于河口群变质岩系中,具有典型的层控特征,因此对这套变质岩开展原岩恢复工作能更好地限定其矿床成因,也可对区域下一步的深边部找矿提供指示。通过对赋矿变质岩开展了系统的岩相学和岩石地球化学研究,结果显示其原岩为一套泥质粉砂岩-细碧岩的岩石组合。其中,黑云石英片岩、二云石英片岩及白云石英片岩的原岩可能为泥质粉砂岩,而石英钠长岩、变火山角砾岩及变火山凝灰岩的原岩可能为细碧岩。河口群形成的构造环境可能为裂谷环境。结合矿体似层状、透镜状的层控特征及已有的成岩成矿年龄数据,认为该矿床存在早期VMS(火山成因块状硫化物矿床)型铜矿化,根据其围岩类型,可能属于“别子型”成矿亚类。本区此类矿床下一步找矿工作的方向为铁镁质火山岩与硅质碎屑岩的界面。The Lala copper deposit in Sichuan is one of the large copper-rich deposits in China.The ore bodies occur in the metamorphic rock series of the Hekou Group,and have typical stratabound characteristics.Therefore,the protolith reconstruction of this metamorphic rock can better define the genesis of the deposit and also provide directions for the next ore prospecting in this area.A series of geological and geochemical studies of its ore-bearing metamorphic rocks indicate that the original rocks are a set of argillaceous siltstone-spilite rock associations which were formed in an intracontinental rift of passive continental margin.The protoliths of biotite quartz schist,muscovite quartz schist and two-mica quartz schist are pelitic siltstone,while the original rocks of quartz albite,metavolcanic breccia and metavolcanic tuff are spilite.Based on the stratabound characteristics of stratiform as well as lenticular orebodies and diagenetic-metallogenic ages available,it is concluded that the deposit exhibits early VMS copper mineralization.Compared with the rock types of host rocks of different types of VMS deposits,Besshi type is considered to be of the early copper mineralization type.At last,the interface between mafic volcanic rocks and siliceous clastics in this region should be the direction of further prospecting work.

关 键 词：拉拉铜矿田 原岩恢复 构造环境 VMS矿床 

分 类 号：P618.41[天文地球—矿床学] P588.3[天文地球—地质学]