| 东昆仑—北巴颜喀拉区域成矿规律及找矿工作思考 |
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| 引用本文： | 胡正国,刘继庆,钱壮志,李厚民,孙继东,苏春乾.东昆仑—北巴颜喀拉区域成矿规律及找矿工作思考[J].青海国土经略,1998(2). |
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| 作者姓名： | 胡正国 刘继庆 钱壮志 李厚民 孙继东 苏春乾 |
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| 作者单位： | 西安工程学院
(胡正国，刘继庆，钱壮志，李厚民，孙继东)，西安工程学院(苏春乾) |
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| 摘 要： | 东昆仑地域依据地质构造差异所划分的昆北断褶带、昆中隆起带、昆南断褶带及其南邻的北巴颜喀拉褶皱带,在金—多金属成矿地质环境、矿床类型、控矿因素和分布规律上都各具特征,但其时空演化上具密切的内在联系,构成了极有远景的金属成矿省(带),是浅成热液金—多金属矿和砂金矿的远景区。
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| 关 键 词： | 东昆仑区 区域成矿规律 金矿 多金属矿 |
REGIONAL MINEROGENIC REGULARITIES OF EAST KUNLUN-NORTH BAYAN HAR MOUNTAINS AND PROSPECTING THOUGHT |
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| Abstract: | Based on the differences of geological structure, the East Kunlun area can be di-vided into four belts, i. e.,Northern Kunlun fault-fold belt,Middle Kunlun uplift belt,South-ern Kunlun fault-fold belt,and Northern Bayan Har fold belt. Each belt has its own pecu-liarites in gold-polymetallic minerogenic geologic setting,type of ore deposits,ore-controllingfactors and distribution regularities, but these belts displayed a close internal relations inspace-time evolution. This is a metallogenic province (belt) with great prospect of hy-pabyssal hydrothermal gold-polymetallic ore and placer gold. |
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| Keywords: | East Kunlun area regional minerogenic regularities gold ore polymetallic ore |
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