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安徽省方解石矿床现状分布及类型特征分析
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
作者姓名:霍立新
作者单位:安徽省矿产资源储量评审中心,安徽合肥,230001
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。

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
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.
Keywords:calcite  contact metamorphism  low-temperature hydrothermal filling
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