峨眉山地幔柱成矿作用分析  

AN ANALYSIS OF THE MINERALIZATION CONNECTED WITH EMEISHAN MANTLE PLUME

作　　者：高振敏[1] 张乾[1] 陶琰[1] 罗泰义[1] 

机构地区：[1]中国科学院地球化学研究所矿床地球化学开放实验室,贵州贵阳550002

出　　处：《矿物学报》2004年第2期99-104,共6页Acta Mineralogica Sinica

基　　金：中国科学院知识创新工程(KZCX3 3W 125)

摘　　要：概述了峨眉山地幔柱成矿作用的基本类型和主要特点,对主要成矿类型包括地幔柱活动直接形成的岩浆矿床和地壳响应形成的间接矿床作了全面的分析介绍,初步勾画了峨眉山大火成岩省地幔柱成矿作用的基本框架。The paper gives a brief description of the metallogenic types and distinguishing features of mineralization connected with the Emeishan mantle plume. All possible kinds of ore deposits including magmatic deposits connected directly with the mantle plume and indirect deposits due to crust response have been discussed. So it has preliminarily outlined the frame work of mineralization in the large Emeishan igneous province.

关 键 词：峨眉山地幔柱 成矿作用 成矿类型 岩浆矿床 热液矿床 

分 类 号：P612[天文地球—矿床学]