摘要
万古金矿位于扬子准地台南缘之江南地轴中部,赋存在新元古界冷家溪群中,受北西西向构造控制.Ⅷ号矿脉是万古金矿的主矿脉之一,在总结万古金矿Ⅷ号矿脉地质特征、矿石特征的基础上,分析了其成矿富集规律,并指出找矿方向.
The Wangu gold deposit is located in the middle of the Jiangnan Earth axis on the southern margin of the Yangtze platform,and occurs in the Neoproterozoic Lengjianxi Group,controlled by the NWW trending structure.Ⅷvein is one of the main vein of the Wangu gold deposit.On the basis of summarizing the geological and ore characteristics ofⅧvein of the Wangu gold deposit,the regularities of mineralization and enrichment are analyzed,and the prospecting direction is pointed out.
作者
息朝庄
吴圣刚
陈吉华
Xi Chaozhuang;Wu Shenggang;Chen Jihua(School of Civil Engineering,Hunan City University,Yiyang Hunan 413000;Hunan Huangjindong mining Co.LTD,Pingjiang Hunan 410400;Hunan gold mining Co.LTD,Changsha Hunan 410007)
出处
《国土资源导刊》
2022年第3期11-15,共5页
Land & Resources Herald
基金
湖南省自然科学基金联合基金项目(2022JJ50277)
湖南省教育厅科学研究一般项目(20C0381)
益阳市社科联项目(2021YS133,2022YS154)
关键词
地质特征
矿脉
万古金矿
平江
geological characteristics
ore vein
Wangu gold deposit
Pingjiang
作者简介
第一作者:息朝庄(1979—),男,高级工程师,研究方向:矿床地质、安全工程,E-mail:xczcsummmmmm@126.com。
