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Genetic Analogy Between Sediment-Hosted Gold Deposits and Sediment-Hosted Copper Deposits in Southwest China

机译:中国西南地区沉积物金矿床与沉积物铜矿床的成因类比

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摘要

The sediment-hosted copper deposits, according to the authors' study, were formed from connate formation water during the post-sedimentary or diagenetic stage while the sediment-hosted disseminated gold deposits are unanimously considered to be of post-sedimentary hydrothermal origin. Therefore, apart from their own individualities, these two types of deposits must share some characters in common. Comparisons are attempted, in this paper! between the sediment-hosted copper deposits in southwest China and the Triassic sediment-hosted disseminated gold deposits in the Yunnan-Guizhou-Guangxi Triangle in terms of geological'and geochemical features.
机译:根据作者的研究,沉积物承载的铜矿床是在沉积后或成岩阶段由原生地层水形成的,而沉积物承载的散布型金矿床则被认为是沉积后的热液源。因此,除了它们自己的个性之外,这两种类型的存款必须具有某些共同点。本文尝试进行比较!从地质和地球化学特征看,中国西南部的沉积物沉积铜矿床与云南-贵州-广西三角地区的三叠纪沉积物沉积金矿床之间的关系。

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