摘要
东昆仑热液金成矿作用较强 ,构造控制明显。作者划分出两条金成矿带 ,分别称为北昆仑金成矿带和南昆仑金成矿带 ,它们受区域地质演化控制 ,呈近EW向分布 ,各带成矿和容矿构造均呈NW向。文中论述了各成矿带的主要特征和具体差异 ,指出了成矿远景和找矿方向。
The hydrothermal gold mineralization in eastern Kunlun Mountains is strong and is closely related to tectonic-magmatic activities. This paper considers that there are two gold metallogenetic belts. They are named North Kunlun gold metallogenetic belt and south Kunlun gold metallogenitic belt respectively, are controlled by regional geological evolution and are distributed in about EW trend. The main characteristics and differences of the belts, mineralizational perspectives and prospective direction are discussed.
出处
《地质与勘探》
CAS
CSCD
北大核心
2000年第5期20-23,共4页
Geology and Exploration
关键词
金矿床
成矿带
成矿规律
找矿方向
热液矿床
gold deposit, metallogenetic belt,mineralization regular,prospective direction, eastern Kunlun Mountains.
