东昆仑区域成矿规律初步研究

J4 ›› 1998, Vol. 6 ›› Issue (5-6): 6-13.

东昆仑区域成矿规律初步研究

胡正国¹,刘继庆¹,钱壮志²,李厚民¹,孙继东¹,苏春乾¹,闫臻¹

1.西安工程学院　西安　710054;
2.长春科技大学　长春　130046

收稿日期:1998-04-20 出版日期:1998-10-28 发布日期:2011-11-07
作者简介:胡正国,1938年出生,教授,主要从事金矿区域成矿规律和矿田构造研究。
基金资助:
地矿部“九五”攻关项目95-02-005资助.

A STUDY OF THE REGIONAL METALLOGENETIC REGULARITY IN EAST KUNLUN MOUNTAIN

Hu Zhengguo¹,Liu Jiqing ¹,Qian Zhuangzhi²,Li Houmin¹,Sun Jidong¹,Su Chunqian¹

1.Xi’an Engineering Uiv., Xi’an 　710054;
2.Changchun Uiv. of Science and Technology,Changchun 　130026

Received:1998-04-20 Online:1998-10-28 Published:2011-11-07

摘要/Abstract

摘要：

东昆仑依其地质构造特征的差异划分为:昆北断裂带、昆中隆起带、昆南断裂带,及其南邻的北巴颜喀拉褶皱带。它们在成矿环境,矿床类型、控矿因素和矿产分布规律上都各具特色,形成了玢岩型金矿、矽卡岩型铁、多金属伴生金矿、层控改造型金矿、低温热液型锑伴生金矿等多个典型矿床,是1条具有很大潜力的金—多金属成矿带。

关键词: 东昆仑, 金矿床, 多金属矿床, 区域成矿模型

Abstract:

On the basis of the structural characteristics,the East Kunlun Mountain can be divided into fault-fold zone in the north,upwarping zone in the middle and fault-fold zone in the south.And the north Bayankerlar fold zone is in south of the East Kunlun Mountain.According to the recent study,these zones are different in the environment of ore forming,the types of deposits,the factors controlling the ore forming and the distribution of deposits.And the porphyzite-gold deposit,the skarn-iron deposit,the gold in the multimetal ore,the layer-controlled gold deposit and companion gold ore in the stibium deposit are formed in different zones.Therefor,the East Kunlun Mountain is an important regional metallogenetic belt in gold and multimetal ore.

Key words: East Kunlun, gold deposit,multimetal deposit, model of the regional metallogenesis

中图分类号:

P618.51/P612

胡正国,刘继庆,钱壮志,李厚民,孙继东,苏春乾,闫臻. 东昆仑区域成矿规律初步研究[J]. J4, 1998, 6(5-6): 6-13.

Hu Zhengguo,Liu Jiqing ,Qian Zhuangzhi,Li Houmin,Sun Jidong,Su Chunqian. A STUDY OF THE REGIONAL METALLOGENETIC REGULARITY IN EAST KUNLUN MOUNTAIN[J]. J4, 1998, 6(5-6): 6-13.

参考文献

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[7] 胡正国.内生成矿作用时空规律性的初步探讨.地质地球化学,1988,(12).

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