首页 | 本学科首页   官方微博 | 高级检索  
     检索      

西秦岭礼岷金矿带李坝群含金浊积岩建造地球化学特征
引用本文:孙省利,武安斌.西秦岭礼岷金矿带李坝群含金浊积岩建造地球化学特征[J].沉积学报,1995,13(4):145-152.
作者姓名:孙省利  武安斌
作者单位:1 甘肃有色地质研究所 兰州 730000;
摘    要:本文通过对李坝群含金浊积岩建造中金及其它微量元素的分布、地球化学特征及与金矿成因的关系研究,结果表明,李坝群含金浊积岩建造明显富集Au、As、Sb、Bi和铁族元素Co、Ni、Cr、V,且具有较高的AU/Ag比值。李坝群含金浊积岩建造是衍生含金建造,对于金成矿来说,并非是主要的矿源层,而是赋矿岩系。

关 键 词:含金浊积岩建造    地球化学特征    衍生含金建造    矿源层
收稿时间:1994-12-02

Geochemical Characteristics of Liba Group Gold-Bearing Turbidite Formation in Lixian-Minxian Gold Mineralized Zone,West Qinling,Gansu Province
Institution:1 Gansu Institute of Geology for Nonferrous Metals;2 Department of Geology, Lanzhou University
Abstract:The distribution of gold, geochemical features of trace elements in the Liba group goldbearing turbidite formation and their relationship with gold metalisation have been studied in detail. The results show that Liba group gold-bearing turbidite formation is rich in An, As,Sb, Bi and Cr, Ni, Co and V, and has high ratios of An/Ag and An/As, but it is depleted in Hg, Sr and Ba. Contents of As, Bi, Ni, Mn, Ti, Cr, V and ratios of Au/Ag, Au/ As and As/Sb gradually increase from D2Lb1 to D2Lb3, on the contrary, contents of Sb, Sb+Bi+Hg and ratios of Co/Ni and Cr/Ni reduce by degrees. R-type cluster analysis of trace elements in Liziyuan group, gold-bearing turbidite formation and Liba ore-bearing faults indicates that they have common elements association which are Ni, Co, Cr and V, and ore-forming elements in the Liba gold mine inherit obviously components in the Liba gold-bearing turbidite formation and Liziyuan group. The Liziyuan group is the primary gold-bearing formation which consists mainly of basic volcanic rocks with high gold abaundance. The Liba group goldbearing turbidite formation is a derivative gold-bearing formation. The Liba group gold-bearing formation is not main gold source rocks, but gold host rocks.
Keywords:
本文献已被 CNKI 维普 等数据库收录!
点击此处可从《沉积学报》浏览原始摘要信息
点击此处可从《沉积学报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号