| 福建邵武观音山钼矿床地质特征及成因探讨 |
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| 引用本文： | 赖文金. 福建邵武观音山钼矿床地质特征及成因探讨[J]. 福建地质, 2010, 29(3): 201-206 |
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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,邵武,354000 |
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| 基金项目： | 本文是根据福建省邵武市何厝坑矿区青山矿段钼矿补充勘查地质报告、童阳际矿区钼矿补充勘查地质报告以及目前矿山开采情况调查编写而成.在编写过程中得到我队林仟同教授级高级工程师的悉心指导,承蒙刘昭平高级工程师审阅,并提出了宝贵的修改意见,在此深表感谢! |
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| 摘 要： | 邵武观音山钼矿体产于早二叠世棲霞组石灰岩中,矿体呈层状、似层状,容矿岩石为透辉石石榴石矽卡岩,成矿作用在时间、空间上与燕山期岩浆活动有密切相关,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 Geological Characteristics and Genesis of the Guanyinshan Molybdenum Deposit in Shaowu, Fujian Province |
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| Lai Wenjin. On the Geological Characteristics and Genesis of the Guanyinshan Molybdenum Deposit in Shaowu, Fujian Province[J]. Geology of Fujian, 2010, 29(3): 201-206 |
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| Authors: | Lai Wenjin |
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| Affiliation: | Lai Wenjin(Northern Fujian Geologic Party of Fujian Province,Shaowu,354000) |
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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 a mineral deposit prospecting indications and guides Shaowu City |
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