GIG OpenIR  > 中国科学院矿物学与成矿学重点实验室  > 会议论文
海南抱伦金矿区岩浆演化及其与成矿关系研究
赵朝霞; 朱昱桦; 单强; 吴传军; 侯茂洲; 陈根文; 蔡建新; 许德如
Source Publication第八届全国成矿理论与找矿方法学术讨论会论文摘要文集
2017-12-09
Conference Date2017-12-09
Conference Place中国江西南昌
Country中国
Indexed By其他
Language中文
Keyword抱伦金矿 细晶岩 花岗闪长岩 陀烈组
Abstract抱伦金矿床位于海南西南部乐东县抱伦农场内,是20世纪90年代发现的高品位大型金矿床。区域构造上,该矿床处于海南岛东西向尖峰—吊罗与九所—陵水深大断裂之间的西端,乐东盆地南西边缘地带(舒斌等,2006)。赋矿围岩和其内矿体主要受豪岗岭背斜、NNW向断裂带及NNE铁湾岭断裂(F1)及矿区中部断层F2的控制(陈柏林等,2001)。矿区及外围侵入岩包括海西晚期黑云母二长花岗岩、花岗闪长岩、
Document Type会议论文
Identifierhttp://ir.gig.ac.cn/handle/344008/35629
Collection中国科学院矿物学与成矿学重点实验室_会议论文
Recommended Citation
GB/T 7714
赵朝霞,朱昱桦,单强,等. 海南抱伦金矿区岩浆演化及其与成矿关系研究[C],2017.
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