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<正>寨坪银矿位于福建省寿宁县大安银矿区域范围内。该矿床产在下白垩统南园组的火山岩中,火山岩层对银矿有较为明显的控制作用。矿区内圈定主要银矿带3条,银矿体6个。矿体呈脉状、细脉状、透镜状,受北北东和北北西向的断层及其伴生的裂隙构造控制,通过总结该类矿床的矿床特征,探讨其成因方式,为今后在闽浙粤中生代火山岩带寻找相类似的矿床具
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矿床地质
ISSN: 0258-7106
CN: 11-1965/P
Year: 2014
Issue: S1
Volume: 33
Page: 845-846
Cited Count:
WoS CC Cited Count: 0
SCOPUS Cited Count:
ESI Highly Cited Papers on the List: 0 Unfold All
WanFang Cited Count:
Chinese Cited Count:
30 Days PV: 2
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