湘西北下寒武统黑色岩系钒镍钼矿微量元素地球化学  

Trace element geochemistry of V-Ni-Mo deposits from the Lower Cambrian black rock series of Northwestern Hunan

作　　者：贾亮亮[1] 戴塔根[1] 游先军[1] 刘尧[1] 付松武[1] 欧阳黎明[1] 

机构地区：[1]中南大学地学与环境工程学院,湖南长沙410083

出　　处：《地学前缘》2012年第4期260-265,共6页Earth Science Frontiers

基　　金：湘西自治州矿产资源整体规划项目

摘　　要：湘西北下寒武统黑色岩系是中国南方下寒武统黑色岩系的重要组成部分,富含钒镍钼等多金属元素。文中对湘西北下寒武统黑色岩系钒镍钼矿进行了微量元素研究,研究区内Ni、Cd、Mo、Sb、V、Zn、W、Ba等元素特别富集,高含量的Sb和Ba表明其为热水沉积;Mo含量极高说明其为缺氧的还原环境;高的V/(V+Ni)、V/Cr、Ni/Co以及δU值表明其沉积环境为缺氧环境;高的U/Th表明本区有热水沉积作用;稀土元素配分模式、Ce和Eu异常及La/Yb-Ce/La和La/Yb-ΣREE图解投点表明其沉积环境为还原环境,并有热水沉积作用。可见黑色岩系形成于缺氧环境,热液活动为其提供了丰富的热液来源。The lower Cambrian black rock series in northwestern Hunan,rich in V-Ni-Mo polymetal elements,are an important part of lower Cambrian black rock series in South China.The present paper is aimed at the study of trace elements in this rock series.In the studied area some elements,including Ni,Cd,Mo,Sb,V,Zn,W,Ba,are heavily enriched.The high content of Sb and Ba and high U/Th in the black rock series reflects hydrothermal sedimentary environment.The high content of Mo and high V/（V＋Ni）,V/Cr,Ni/Co and δU indicate an anoxic sedimentary environment for these rocks.The REE patterns,Ce and Eu anomalies,La/Yb-Ce/La and La/Yb-ΣREE diagrams suggest that V-Ni-Mo deposit was formed in an anoxic sedimentary environment together with hydrothermal sedimentary processes.All the trace element geochemical characteristics of the black rock series indicate that the V-Ni-Mo deposit from Lower Cambrian black rock series in Northwestern Hunan was deposited in an anoxic sea environment.The seafloor hydrothermal activity provides the source for the abundant metallic elements.

关 键 词：下寒武统 黑色岩系 微量元素地区化学 缺氧环境 热水沉积 

分 类 号：P618.6[天文地球—矿床学] P591[天文地球—地质学]