首页> 外文会议>International Conference on Measurement and Control of Granular Materials(MCGM 2006) >GEOCHEMISTRY OF LATE TRIASSIC COAL IN CHANGHEBIAN COALFIELD, CHONGQING, CHINA
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GEOCHEMISTRY OF LATE TRIASSIC COAL IN CHANGHEBIAN COALFIELD, CHONGQING, CHINA

机译:重庆长庚碧煤田晚三叠世煤的地球化学

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摘要

Research of trace element in coals mainly places on three aspects. Well understanding concentration, migration, transformation and occurrence of trace element in coal utilization offers basic formation for researches on environmental effect of coals. In addition, trace elements in coal are the indicator for geologic condition in coal-forming. What's more, some high enrichment trace element in coal could be exploited as mining resource, such as Ge, Ga and U. Xujiahe Formation are the main coal bearing strata in Chongqing, but previous research have less report on these coals. In this paper, we discuss the chemistry of coals, petrographic compositon of coals, the abundance of trace element and the element-enriching factor for Changhebian coal in ChongQing.
机译:煤中微量元素的研究主要集中在三个方面。对煤炭利用中微量元素的浓度,迁移,转化和发生的认识,为研究煤炭的环境效应提供了基础。另外,煤中的微量元素是成煤地质条件的指标。此外,可以将一些高浓的微量元素作为采矿资源,例如锗,镓和铀。徐家河组是重庆的主要含煤地层,但先前的研究报道较少。本文讨论了重庆长河边煤的化学特征,煤的岩石学组成,微量元素的丰度和元素富集因子。

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