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首页> 外文期刊>Transactions of Nonferrous Metals Society of China >ANALYSIS OF GEOLOGICAL CONSTRAINT FACTOR ON COPPER POLYMETAL METALLOGENIC ZONES IN NORTH REGION OF CHIFENG
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ANALYSIS OF GEOLOGICAL CONSTRAINT FACTOR ON COPPER POLYMETAL METALLOGENIC ZONES IN NORTH REGION OF CHIFENG

机译:七峰市北部铜多金属成矿带的地质制约因素分析

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摘要

The controlling of ore-forming processes of the copper-polymetal metallogenic zones in north region of Chifeng, Inner Mongolia has been investigated via the regional tectonics, the strata and paleogeographical setting and mineralization, and the regional magmatism and mineralization. The following results were pointed out that due to the differential effect of the above three geological factors the mineralizations are mainly related with Yanshanian magamatism, at the early stage of the Yanshani-an magmatism the mineralization (in weet Chifeng) is mainly represented by Cu, Au deposit resulted from anatexis, and at the late stage (in east Chifeng) is dominated by Sn, W polymetal deposit resulted from the dissemination of upper crust materials.
机译:通过区域构造,地层和古地理背景及成矿作用,区域岩浆作用和成矿作用,研究了内蒙古赤峰北部地区铜多金属成矿带的成矿过程控制。下列结果指出,由于上述三个地质因素的不同作用,成矿作用主要与燕山岩浆作用有关,在燕山一安岩浆作用的早期,矿化作用(湿赤峰)主要以铜为代表,沉积物是由食盐动物引起的,在后期(赤峰以东)以锡,钨为主,多金属沉积物是由于上地壳物质的传播所致。

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