江西安远园岭寨矿区钼矿床地质特征及矿床成因探讨
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中国地质调查局地质大调查项目(199910200233)资助。


Geological characteristics and genesis of the Yuanlingzhai molybdenum deposit in Anyuan, Jiangxi Province
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    摘要:

    提要:园岭寨矿区泥竹塘区段钼矿床是江西境内发现的最大斑岩型钼矿,现探明储量属超大型。矿体赋存于花岗斑岩体内外接触带中,呈大透镜状、似层状。矿体厚度巨大,最大达456.57 m, 最薄52 m,平均227.8 m,矿床平均品位0.067%。本文重点阐述矿床的地质特征及矿床成因探讨,并对矿区的构造及成矿机制进行分析,提出深部具有隐伏爆破角砾岩筒。而北东向及北西西向断裂是矿区的控岩构造,控制了隐爆角砾岩筒及花岗斑岩体的侵入、就位,且导致花岗斑岩体周边50~450 m内不同方向的成矿节理极为发育,为本区钼矿床提供了良好的储矿空间。

    Abstract:

    Abstract:The Nizhutang molybdenum ore block in the Yuanlingzhai ore district is the largest molybdenum deposit of porphyry type in Jiangxi Province, with very huge ore reserves. The ore bodies in lenticular and bedded forms occur in the internal and external contact zones of the granite, and their thicknesses are from 52 to 456.57 m, with the mean thickness being 227.8 m. The average grade of the ore deposit is 0.067%. In this paper, the authors summarized geological characteristics and genesis of the ore deposit, analyzed the structure and the formation mechanism of the ore deposit, and pointed out that a concealed blasting breccia pipe might exist in the depth. The NE- and NW-trending faults were rock-controlling structures, which controlled the cryptoexplosive breccia and the granite porphyry. The ore-related joints in different directions 50-450 m around the granite porphyry were very well developed, which provided favorable ore storage space for the molybdenum deposit.

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梁景时 漆富勇 胡论元 丁 勇. 江西安远园岭寨矿区钼矿床地质特征及矿床成因探讨[J]. 中国地质, 2012, 39(5): 1327-1338.
LIANG Jing-shi, QI Fu-yong, HU Lun-yuan, DING Yong. Geological characteristics and genesis of the Yuanlingzhai molybdenum deposit in Anyuan, Jiangxi Province[J]. Geology in China, 2012, 39(5): 1327-1338(in Chinese with English abstract).

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  • 在线发布日期: 2012-12-04
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