安徽省方解石矿床现状分布及类型特征分析 |
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引用本文: | 霍立新. 安徽省方解石矿床现状分布及类型特征分析[J]. 安徽地质, 2016, 26(2): 111-113. DOI: 10.3969/j.issn.1005-6157.2016.02.006 |
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作者姓名: | 霍立新 |
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作者单位: | 安徽省矿产资源储量评审中心,安徽合肥,230001 |
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摘 要: | 方解石矿为我省特色矿种,资源储量丰富,是我国方解石矿主要产地之一。通过分析,方解石矿主要分布于我省青阳县与泾县两地,占全省储量的91%;其矿床成因类型以接触变质型为主,低温热液充填型次之,两者相比,接触变质型方解石矿矿体规模较大,呈层状、似层状分布,构造简单,矿石质量较好,且稳定,便于开发利用,矿床规模以大中型矿山为主。
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关 键 词: | 方解石 接触变质型 低温热液充填型 |
DISTRIBUTION,TYPES AND FEATURES OF CALCITE DEPOSITS IN ANHUI PROVINCE |
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Abstract: | As a characteristic mineral, calcite is abundant in Anhui Province and makes it a major calcite producer in China. Analysis indicated that calcite mainly distributes in Qingyang and Jingxian Counties, taking up 91% of the total reserve of the province. The deposit was formed dominantly by contact metamorphism, secondarily by low-temperature hydrothermal filling. Comparatively, contact metamorphic calcite deposit is big in scale, lamellar, semi-lamellar, and simple in structure, good in quality, stable, easy for development and utilization. |
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Keywords: | calcite contact metamorphism low-temperature hydrothermal filling |
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