福建邵武观音山钼矿床的地质特征及其成因探讨 |
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作者姓名: | 赖文金 |
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作者单位: | 福建省闽北地质大队,福建,邵武,354000 |
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摘 要: | 邵武观音山钼矿体产于早二叠世栖霞组(P1q)中,矿体呈层状、似层状,容矿岩石为透辉石石榴子石矽卡岩,成矿作用在时间、空间上与燕山期岩浆活动密切相关,属热液交代矽卡岩型钼矿床。
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关 键 词: | 钼矿床 地质特征 矿床成因 找矿标志 邵武观音山 |
On the Geologcal Characteristics and Genesis of the Guanyinshan Molybdenum deposit in Shaowu,Fujian Province |
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Authors: | LAI Wen-Jin |
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Institution: | LAI Wen-Jin (Northern Fujian Geologic Party of Fujian Province,Fujian Shaowu 354000,China) |
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Abstract: | The Guanyinshan molybdenum deposit in Shaowu,Fujian Province exists in the limestone of Early Permian Qixia Formation. The orebody is in a stratiform and parabedded occurrence.The host rock is the diopside garnet skarn.The ore-forming process has a close relation with the Yanshanian magmatic activity in time and space.It belongs to the molybdenum deposit of the hydrothermal metasomatic skarn type. |
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Keywords: | molybdenum deposit geological characteristics genesis of mineral deposit prospecting indications and guides Shaowu city |
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