龙王庙隐爆角砾岩型金多金属矿床地质特征及其成因
Modern Mining(2013)
Abstract
详细介绍了龙王庙隐爆角砾岩型金多金属矿床的地质特征,分别从成矿时期、控矿因素、矿化分带等方面对其矿床成因进行了探讨,认为这些隐爆角砾岩体主要产于石英正长斑岩体内南东侧边缘部位,矿体主要受断裂控制,产于隐爆角砾岩与石英正长斑岩接触带中,并总结了隐爆角砾岩型金多金属矿床的成矿模式.
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