| 浅成低温热液金矿床的全球背景 |
| |
| 引用本文： | 杨芳林,李之彤,朱群,吴振文. 浅成低温热液金矿床的全球背景[J]. 地质与资源, 1999, 8(4): 241-250 |
| |
| 作者姓名： | 杨芳林 李之彤 朱群 吴振文 |
| |
| 作者单位： | 中国科学院地质与地球物理研究所, 北京 100029 |
| |
| 基金项目： | 定向科研基金!（地科定96－ 08） 项目“黑龙江省大兴安岭地区松岭区古利库岩金矿地质特征及成矿规律研究”的部分内容 |
| |
| 摘 要： | 浅成低温热液金矿床分为冰长石-绢云母型和明矾石-高岭石型两类，主要分布于环太平洋地区、地中海-喜马拉雅带和蒙古-鄂霍次克带，形成了许多超大型和大型金矿床.矿床主要形成于大陆边缘和岛弧环境，与陆相火山岩和火山机构有密切的关系，已发现矿床的形成时间以中、新生代为主.矿化发生于火山作用后，火山体系脆性断裂带和深部侵入体的发育使地下水循环，具有大量成矿流体及成矿物质来源是形成浅成低温热液金矿床的重要条件.
|
| 关 键 词： | 浅成低温热液金矿床 地质特征 成矿模式 |
| 收稿时间： | 1999-05-08 |
THE DISCOVERY OF ADULAR AND ITS GEOLOGICAL SIGNIFICANCE IN GULIKU GOLD(SILVER) DEPOSIT |
| |
| YANG Fang lin,LI Zhi tong,ZHU Qun,WU Zhen wen. THE DISCOVERY OF ADULAR AND ITS GEOLOGICAL SIGNIFICANCE IN GULIKU GOLD(SILVER) DEPOSIT[J]. Geology and Resources, 1999, 8(4): 241-250 |
| |
| Authors: | YANG Fang lin LI Zhi tong ZHU Qun WU Zhen wen |
| |
| Affiliation: | Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China |
| |
| Abstract: | Adular is commonly distributed in Guliku gold(silver) deposit and can be divided into two kinds according to its occurrence One is that adular and quartz occur in vein like orebody of main mineralizing stage and altered wallrock closed to orebody with subveined or band disseminated shape,the other is that adular occurs in altered andsite and dacite with disseminated or disseminated network shape This adular is the products of altered feldspar minerals in early stage of mineralization Adular is rhombus,transparent biaxial crystal and negative character It is consisted of SiO 2(66 05%),Al 2O 3(17 53%),K 2O(16 04%) and Na 2O(0 25%) by microprobe analysis The discovery of adular has important significance in ore prospecting and metallogenic studying |
| |
| Keywords: | Guliku gold (silver) deposit adular geological significance Daxinganling |
| 本文献已被 CNKI 等数据库收录！ |
| 点击此处可从《地质与资源》浏览原始摘要信息 |
|
点击此处可从《地质与资源》下载全文 |
