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浅谈阿勒泰多金属成矿带地质特征及成矿划分

Discussion on the geological characteristics and metallogenic division of the Aletai polymetallic metallogenic belt
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摘要 阿勒泰地区板块构造位置处于西伯利亚板块与哈萨克斯坦—准噶尔板块的结合部,是我国重要的多金属成矿带之一。本文在简述阿勒泰地区金矿成矿地质背景的基础上,结合区域地质特征,对阿勒泰地区区域矿产及分带进行了详细分析,力图为该区多金属矿床的勘查和开发提供有力依据。 The location of plate tectonics in Aletai is in the conjunction part of Siberia plate and Kazakhstan Junggar plate.It is one of the most important polymetallic metallogenic belts in China.Based on the brief description of the metallogenic geological background of gold deposits in Aletai area,combined with the regional geological characteristics,the regional mineral resources and zoning in Aletai area are analyzed in detail,trying to provide a strong basis for the exploration and development of polymetallic deposits in this area.
作者 鲜小龙 XIAN Xiao-long(Fourth Geological Team of the Xinjiang Uygur Autonomous Region geological and mineral exploration and Development Bureau, Aletai 836500,China)
出处 《世界有色金属》 2018年第1期170-170,172,共2页 World Nonferrous Metals
关键词 阿勒泰地区 多金属 成矿带 地质特征 Aletai area polymetallic metallogenic belt geological characteristics
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