摘要
广西象州县妙皇矿区铜多金属矿床位于广西大瑶山西侧多金属成矿带中部,该矿床主要受断裂构造控制,为热液充填型脉状矿床,文章主要从矿体特征、构造控矿作用等方面探讨,提出该矿床的成矿模式,以利于在广西大瑶山西侧多金属成矿带上进一步发现该类型矿床。
Miaohuang polymetallic Cu deposit is located in the central part of the western polymetallic metallogenic belt of Dayaoshan in Xiangzhou County of Guangxi.The deposit is mainly controlled by the fault structure,which is a vein deposit of hydrothermal fluid filling type.The paper mainly discusses the ore body characteristics and ore-controlling function of structure,and proposes the metallogenic model of the deposit in order to further find out the same type deposit in the western polymetallic metallogenic belt of Dayaoshan in Guangxi.
出处
《矿产与地质》
2017年第2期331-334,共4页
Mineral Resources and Geology
基金
国家自然科学基金项目(编号:41273040)
中国地质调查局项目(编号:12120113067600)联合资助
关键词
妙皇铜矿
热液充填型
矿体特征
构造控矿
成矿模式
广西大瑶山
Miaohuang polymetallic Cu deposit
hydrothermal fluid filling type
orebody characteristics
ore controlling structure
metallogenic model
Dayaoshan in Guangxi
