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| 东昆仑热液金成矿带及其找矿方向 | |
| 引用本文： | 袁万明 莫宣学. 东昆仑热液金成矿带及其找矿方向[J]. 地质与勘探, 2000, 36(5): 20-23 |
| 作者姓名： | 袁万明 莫宣学 |
| 作者单位： | 1. 中国科学院高能物理研究所,北京,100080 2. 中国地质大学,北京,100083 3. 青海省第八地质队,西宁,100029 |
| 摘 要： | 东昆化热液金成矿作用较强，构造控制明显。作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，各民矿和容矿构造均呈ＮＷ向。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。 |
| 关 键 词： | 金矿床 成矿带 成矿规律 找矿方向 热液矿床 |
GOLD METALLOGENIC BELTS AND PROSPECTING DIRECTION IN EASTERN KUNLUN AREAR |
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| YUAN Wan-ming,MO Xuan-xue,YU Xue-hui,LUO Zhao-hu,GAN Wei-dong. GOLD METALLOGENIC BELTS AND PROSPECTING DIRECTION IN EASTERN KUNLUN AREAR[J]. Geology and Prospecting, 2000, 36(5): 20-23 | |
| Authors: | YUAN Wan-ming MO Xuan-xue YU Xue-hui LUO Zhao-hu GAN Wei-dong |
| Abstract: | 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. |
| Keywords: | gold deposit metallogenetic belt mineralization regular prospective direction eastern Kunlun Mountains. |
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