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中亚细亚矽卡岩矿床,根据其(1)构造和地质位置,(2)最主要金属以及(3)矿物和地球化学特征,可以划为六类建造。矿床类型按主要矿物划分(表1)。不同建造矽卡岩矿床地质位置的若干特征西尼村等(1957)曾在中亚细亚境内根据地质发展史、构造位置、岩浆岩性质和晚华力西期矿床等方面的不同划分了若干构造带。铁矿床分布在加里东和早海西期构造带中。某些铁矿床磁铁矿石重叠以后成绿柱石、钼、铜-金和其它矿化。一些主要的矽卡岩钨矿床和铅-锌矿床则分布在更晚期构造带中。
The Central Asia Skarn Deposit can be classified into six categories based on its (1) tectonic and geological location, (2) the most important metals, and (3) mineralogical and geochemical characteristics. The types of deposits are classified by major minerals (Table 1). Several features of the geologic location of various skarn deposits Silin et al. (1957) classified some tectonic belts in Central Asia based on their geological history, tectonic positions, magmatic rocks, and late-stage Lixi deposits . The iron deposits are distributed in the Caledonian and Early Hercynian tectonic belts. Some of the iron ore deposits in the magnetite stack are beryl, molybdenum, copper-gold and other mineralizations. Some of the major skarn tungsten and lead-zinc deposits are located in more advanced tectonic belts.