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西昆仑地区成矿远景
引用本文:董永观,郭坤一 肖惠良 张传林 王爱国 赵 宇.西昆仑地区成矿远景[J].中国地质,2003,30(2):173-178.
作者姓名:董永观  郭坤一 肖惠良 张传林 王爱国 赵 宇
作者单位:1. 中国地质大学地球科学院,湖北,武汉,430074;南京地质矿产研究所,江苏,南京,210016
2. 南京地质矿产研究所,江苏,南京,210016
基金项目:国土资源部地质大调查项目(199910200247)
摘    要:西昆仑地区位于青藏高原西北缘和塔里木盆地西南缘的结合部,构造上处于古亚洲构造域和特提斯构造域的结合部,是横豆于中国中部巨型纬向构造带(昆仑一祁连一秦岭构造带)的重要组成部分。地层、构造、岩浆活动等多种成矿地质条件非常优越,区内已经发现的矿床种类、类型繁多,矿种较全,在空间上分带规律明显,矿化相对集中。多种成矿信息表明,研究区是寻找大型、超大型矿床的有利远景区之一。

关 键 词:西昆仑地区  成矿远景  青藏高原  地层  构造  岩浆活动  成矿地质条件  成矿信息
文章编号:1000-3657(2003)02-0173-06

Ore prospects of the West Kunlun area in western China
DONG Yong-guan,GUO Kun-yi,XIAO Hui-liang,ZHANG Chuan-lin,Wang Ai-guo,ZHAO Yu.Ore prospects of the West Kunlun area in western China[J].Chinese Geology,2003,30(2):173-178.
Authors:DONG Yong-guan  GUO Kun-yi  XIAO Hui-liang  ZHANG Chuan-lin  Wang Ai-guo  ZHAO Yu
Institution:DONGYong-guan1,2,GUOKun-yi2,XIAOHui-liang2,ZHANGChuan-lin2,WangAi-guo2,ZHAOYu2
Abstract:The West Kunlun area is geographically located at the junction between the northwestern margin of the Qinghai-Tibet Plateau and the southwestern margin of the Tarim basin and tectonically at the junction be-tween the Paleo-Asiatic tectonic domain and the Tethys-Himalaya tectonic dom ain.It is an important compo-nent of the gigantic latitudinal tectonic belt(Kunlun-Qilian-Qinling tectoni c belt)across central China.This area has excellent metallogenic conditions in t erms of stratigraphy,structure,magmatism etc.The kinds and types of mineral depo sit found in the area are highly varied and there is a full range of minerals.In space the minerals show distinct zoning and mineralizations are relatively conc entrated.Many kinds of information regarding mineral-ization indicate that the study area is one of the favorable ore prospect ar eas for looking for large and superlarge mineral deposits.
Keywords:deposit type  metallogeny  ore prospects  West Kunlun area
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