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Source and Enrichment of Toxic Elements in Coal Seams around Mafic Intrusions: Constraints from Pyrites in the Yuandian Coal Mine in Anhui, Eastern China

机译:镁铁质侵入体周围煤层中有毒元素的来源和富集:来自中国东部安徽元店煤矿的黄铁矿的约束

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Pyrite, a mineral that can cause potential environmental issues in coal mining, is commonly found in coal seams around intrusions. In this paper, pyrites from the Yuandian Coal Mine (Huaibei Coalfield, Anhui, Eastern China) were studied using SEM, Raman and LA-ICP-MS. The pyrite morphologic and geochemical data suggest that (1) four pyrite generations are present (framboidal sedimentary pyrites (Py I) in the original coal, coarse-grained magmatic pyrites (Py II) in the intruding diabase, fine-grained metamorphic pyrites (Py III) in the intrusive contact aureole, and spheroid/vein hydrothermal pyrites (Py IV) in the cokeite); and (2) concentrations of cobalt, nickel, arsenic, selenium, lead and copper in the metamorphic pyrites are much higher than the other pyrite generations. We propose that mafic magmatism is the main contributor of the toxic elements to the intrusion-related cokeite at Yuandian.
机译:黄铁矿是一种可能在煤矿开采中引起潜在环境问题的矿物,通常在侵入岩周围的煤层中发现。本文利用扫描电镜,拉曼光谱和LA-ICP-MS技术对元店煤矿(淮北煤田,中国东部)的黄铁矿进行了研究。黄铁矿的形态学和地球化学数据表明(1)存在四个黄铁矿世代(原始煤中有黄腐沉积黄铁矿(Py I),侵入辉绿岩中有粗粒岩浆黄铁矿(Py II),细粒变质黄铁矿(Py III)在侵入性接触的金针和球状/静脉热液黄铁矿(Py IV)中; (2)变质黄铁矿中钴,镍,砷,硒,铅和铜的浓度远高于其他黄铁矿世代。我们认为,镁铁质岩浆作用是元店侵入性白云母中有毒元素的主要来源。

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