茅排金矿床中自然金和黄铁矿的成因矿物学特征
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Minerageny of Native Gold and Pyrite in the Maopai Gold Deposit,Jiangxi Province
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    摘要:

    作者通过对新发现的茅排金矿的研究,测试了自然金、黄铁矿的物理性质、化学成分等,并论述了成因矿物学特征。文中指出自然金、黄铁矿在矿体垂向上晶体形态的分布规律,利用形态系数计算公式可判断矿体、矿带的延伸方向和剥蚀程度。并指出,明金常见,自然金成色高,矿石中贫硫化物,黄铁矿中金品位高、Sb、Hg极低、无As,Co/Ni比较稳定、晶胞参数和红外吸收峰偏大等是“茅排式”金矿床的特点。

    Abstract:

    Based on the determination of physical properties and chemical composition of native gold and pyrite from the newly-discovered Maopai gold depo-sit, the present paper deals with minerageny of native gold and pyrite. Various crystal forms of gold and pyrite could be observed along the vertical section of the orebody, and the formula for morphologic parameters might be used to judge the downward extension and the denudation degree of the orebody and the ore belt. The "Maopai-type" gold deposit has some unique cha-racteristics: ores are rich in gold. and poor in sulfides; pyrite contains high gold (>200 g/t), very low Sb and Hg and no As, and has fairly stable Co/Niratios, somewhat large cell parameter a0 and high infrared absorption peak.

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徐海江,张凤云,赖绍聪, 1993. 茅排金矿床中自然金和黄铁矿的成因矿物学特征[J]. 岩石矿物学杂志, 12(4):363~370.
Xu Haijiang, Zhang Fengyun, Lai Shaocong Hebei College of Geology, et al, 1993. Minerageny of Native Gold and Pyrite in the Maopai Gold Deposit, Jiangxi Province[J]. Acta Petrologica et Mineralogica, 12(4): 363~370.

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