摘要
湖北省随州市红石地区是河南省破山—银洞坡金银成矿带的东延部分,成矿地质条件十分优越。燕山期形成了一些金银矿床(点),研究表明,成矿流体来自岩浆期后热液,有大量大气降水参与,属浅成、中低温热液矿床成因。
As eastern branch of gold-silver metallogenic zone of Poshan-Yindongpo in Henan Province,the Hongshi area in Suizhou City,Hubei Province has superior metallogenic geological conditions, and some gold-silver deposits （points） has been formed iu Yanshannian. According to the research,the authors believe that metallogenic fluid comes from post magmatic hydrothermal fluid with a large quantity of precipitation,it belongs to hypabyssal and medium-low temperature Hydrothermal deposit.
出处
《资源环境与工程》
2008年第3期302-309,共8页
Resources Environment & Engineering
关键词
红石地区
银金矿
矿床成因
Hongshi area
silver-gold deposit
deposit genesis
