摘要
贵州赋存于沉积岩中的微细浸染型金矿床为低温开放体系中经复杂地质地球化学作用形成。在综合研究该类矿床地质地球化学、矿床组合和元素组合的基础上，拟定实验方案，总结出元素迁移富集的规律。
The sedimentary rock-hosted micrograined and disseminated gold deposits in Guizhou were formed by complex geological and geochemical processes in low temperature and open system. The rules of migration and enrichment of elements in low temperature and open system have been probed on the basis of comprehensive researches of these gold deposits andsimulat ing experiments.
出处
《地质与勘探》
CAS
CSCD
北大核心
1996年第5期37-41,共5页
Geology and Exploration
基金
国家自然科学基金
中国科学院矿床地球化学开放研究室基金
关键词
低温
开放体系
元素迁移
富集
金矿床
矿化
low temperature and open system,migration and enrichment of elements, disseminated gold deposit
