成矿过程流体地球化学模拟及其矿床学意义——以江西银山矿床为例

被引：8

作者：

陈繁荣

机构：

[1] 中国科学院地质新技术研究所广州

来源：

地质论评 | 1995年 / 01期

关键词：

流体地球化学; 元素地球化学; 计算机模拟; 江西银山矿床;

D O I：

10.16509/j.georeview.1995.01.007

中图分类号：

P59 [地球化学];

学科分类号：

070902 ;

摘要：

本文将银山成矿体系作为富含H2S、CO2的NaCl体系,对Cu、Pb、Zn、Ag和Au等金属元素在该体系降温过程中的地球化学行为和银山矿床的成矿过程进行了计算机数字模拟,并与沸腾降温体系进行对比,证明了成矿体系地球化学演化对金属元素的迁移与沉淀具有重要影响,成矿流体地球化学摸拟在矿床成因、深部成矿预测和区域成矿规律研究中具有重要意义。

引用

页码：42 / 47

页数：6

共 10 条

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