| 福建安溪霞春硫铁矿床地质特征及成因探讨 |
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| 引用本文： | 李彦斌.福建安溪霞春硫铁矿床地质特征及成因探讨[J].福建地质,2010,29(1):17-21. |
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| 作者姓名： | 李彦斌 |
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| 作者单位： | 安溪县国土资源局,安溪,362400 |
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| 摘 要： | 霞春硫铁矿体在空间分布上具有一定层位,主要呈透镜状产于与棲霞组石灰岩有关的矽卡岩内,硫铁矿形成经历矽卡岩阶段→磁铁矿阶段→硫化物阶段,为矽卡岩型矿床。
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| 关 键 词： | 硫铁矿 地质特征 矿床成因 安溪霞春 |
On the Geologic Characteristics and Genesis of the Xiachun Pyrite Deposit in Anxi County, Fujian Province |
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| Li Yanbin.On the Geologic Characteristics and Genesis of the Xiachun Pyrite Deposit in Anxi County, Fujian Province[J].Geology of Fujian,2010,29(1):17-21. |
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| Authors: | Li Yanbin |
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| Institution: | Li Yanbin (Anxi Bureau of Land and Mineral Resources, Anxi, 362400) |
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| Abstract: | The Xiachun pyrite ores with a lenticular shape exist in one stratigraphic position in space and are discovered in the skarn which is related to the limestone of Lower Permain Qixia Formation and take shapes by three metallogenetic stages, namely, the skarn stage, the magnetite stage and the sulfidic stage. The Xiachun pyrite deposit belongs to the ore deposit of the high and moderate temperature hydrothermal pyrometasomatie skarn type. |
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| Keywords: | pyrite geologic characteristics the genesis of a mineral deposit Anxi County |
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