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首页> 外文期刊>Ore Geology Reviews: Journal for Comprehensive Studies of Ore Genesis and Ore Exploration >Mineral chemistry and geothermometry of chlorites in relation to physico-chemical conditions of uranium mineralization in the central part of the Singhbhum Shear Zone, eastern India
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Mineral chemistry and geothermometry of chlorites in relation to physico-chemical conditions of uranium mineralization in the central part of the Singhbhum Shear Zone, eastern India

机译:煤矿化学与地质植物与印度东部Syshhum剪切区中央部分铀矿化物理化学条件相关

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摘要

The Singhbhum Shear Zone (SSZ) in eastern India is one of the major uranium repositories of the country. Some of the important uranium deposits viz., Bagjata, Jaduguda, Bhatin, Narwapahar and Banadungri-Singridungri are juxtaposed in the central part of SSZ. The uranium mineralization in central SSZ is mainly hosted by tourmaline-apatite-magnetite bearing sericite quartz chlorite schist with uraninite being the main radioactive mineral phase. A close spatial relationship exists between uraniferous minerals and chlorite occurrences in central SSZ. Three different types of chlorite assemblages were recognized and their relationship with uranium mineralization was studied in detail to unravel the physico-chemical conditions for precipitation of uranium vis-avis chlorite geothermometry and constrains on the chlorite chemistry.
机译:印度东部的Singhhum剪切区(SSZ)是该国主要铀储存库之一。 一些重要的铀矿床,巴拉贾,Jadududa,Bhatin,Narwapahar和Banadungri-Singridungri在SSZ的中部并置。 中央SSZ中的铀矿化主要是由含有纤维素石英氯化物片段的Tourmaline-磷灰石 - 磁铁矿,其具有铀矿是主要的放射性矿物相。 中央SSZ中铀矿物质和氯酸盐发生之间存在紧密的空间关系。 认识到三种不同类型的氯酸盐组合,详细研究了与铀矿化的关系,以解开铀Vis-Avis氯酸盐地质测量沉淀的物理化学条件,并在氯酸盐化学上约束。

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