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甘肃武山温泉钼矿床地质特征
引用本文:梁亚忠.甘肃武山温泉钼矿床地质特征[J].甘肃地质学报,2008(2):40-49.
作者姓名:梁亚忠
作者单位:甘肃省有色地质勘查局天水总队 甘肃天水741025
基金项目:中国地质调查局地质大调查项目《甘肃省北秦岭温泉外围铜钼矿调查评价》(1212010631006)资助
摘    要:武山温泉钼矿床位于西秦岭东段多金属矿区,近年来勘查成为一个较大而且有一定找矿潜力的中一大型钼矿床。岩体呈巨大岩基状产出的中浅成杂岩体,出露面积253.68km^2。印支晚期超浅成细粒黑云母二长花岗岩(γ5^1-10)(岩株)对钼矿床的最终形成及矿化富集有明显的活化作用。矿区以近NNW向主干断裂为导矿构造,次级裂隙(节理)为容矿构造,尤其以向东倾的一组裂隙(节理)为主要的含矿构造。控矿因素主要为“岩相”+构造的二元模式。

关 键 词:武山钼矿床  “岩相”+构造  矿床特征  活化作用

GEOLOGICAL CHARACTERISTICS OF WENQUAN MOLYBDENUM DEPOSIT IN WUSHAN COUNTY OF GANSU PROVINCE
LIANG Ya-zhong.GEOLOGICAL CHARACTERISTICS OF WENQUAN MOLYBDENUM DEPOSIT IN WUSHAN COUNTY OF GANSU PROVINCE[J].Acta Geologica Gansu,2008(2):40-49.
Authors:LIANG Ya-zhong
Institution:LIANG Ya-zhong(Tianshui Team,Gansu Provincial Bureau of Non-ferrous Metals Geology and Exploration,Tianshui 741025,China)
Abstract:Wenquan Molybdenum deposit in Wushan County is situated in the multi-metal mineral district within the eastern section of west Qinling,which is believed to be a potential middle-large scale molybdenum deposit through a series of recent explorations.Rock mass is a middle shallow complex,the occurrence of huge batholith with the exposed area of 253.68km2.The super shallow fine granular biotite adamellite,formed at late Indo-Chinese epoch,acted as a role of obvious activation on the formation of molybdenum deposit and mineralization enrichment.NNW-striking main fault in the mineral district is the main ore transmitting structure,secondary fissures(joints) is the host structures,among which a series of fissures dipping east towards is main host structure.Factors of ore controlling is the model of lithofacies and structures.
Keywords:Wenquan molybdenum deposit in Wushan County  lithofacies  structures  geological characteristics  activation
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