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Rare-Earth Elements and the Genesis of Ore Mineralization at the Kalgutinskoe Tungsten Ore Field,Gornyi Altai

机译:戈尔尼·阿尔泰的卡尔古丁斯科钨矿田中的稀土元素和矿化成因

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摘要

Rare-earth elements (REE)are widely used as indicators of the conditions under which rocks and minerals were produced [1,2].This paper reports the results of our study of REE in granites and minerals from quartz zones with ore mineralization and the principal parameters under which these minerals were formed at the Kalgutinskoe ore field,which is located in the southeastern part of the Gornyi Altai Range,within the Charysh-Terekta tectono-stratigraphic zone.
机译:稀土元素(REE)被广泛用作岩石和矿物产生条件的指示剂[1,2]。本文报道了我们对矿石矿化和石英成因的石英区花岗岩和矿物中REE的研究结果。这些矿物的主要参数是在位于Charysh-Terekta构造地层带内的Gornyi Altai山脉东南部的Kalgutinskoe矿田中形成的。

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