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福建邵武观音山钼矿床的地质特征及其成因探讨
作者姓名:赖文金
作者单位:福建省闽北地质大队,福建,邵武,354000
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。

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
Authors:LAI Wen-Jin
Institution:LAI Wen-Jin (Northern Fujian Geologic Party of Fujian Province,Fujian Shaowu 354000,China)
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.
Keywords:molybdenum deposit  geological characteristics  genesis of mineral deposit  prospecting indications and guides  Shaowu city  
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