期刊文献+

江西蔡家坪铅锌(银)矿床特征

The characteristics of Caijiaping lead-zinc(silver) ore deposit,Jiangxi
下载PDF
导出
摘要 蔡家坪铅锌(银)矿区位于北武夷铅锌银成矿带内,文章系统阐述了矿区地质和矿床特征,并对矿床的成因进行了探讨。认为本区铅锌(银)矿床,经历了火山喷发沉积和后期热液充填两大成矿期,与次火山岩体(流纹斑岩)有密切的关系,属次火山热液矿床。 Caijiaping lead - zinc (silver) ore deposit is located in northern Wuyi lead - zinc silver metallogenic belt. On the ba- sis of illustrating the characteristics of geology and mineral deposit, studying the genesis of the ore deposit, the author proposed that the lead - zinc - (silver) ore deposit formed during two ore - forming period, i. e. , the early volcanic eruption and deposition and late hy- drothermal filling, and the ore deposit, belonging to the subvolcanic hydrothermal one, is related closely with sub - volcanic body (rhyolitic porpyry).
作者 徐顺国
出处 《矿产勘查》 2011年第1期54-60,共7页 Mineral Exploration
基金 江西永平地区矿产远景调查项目(编号:矿调[2005]13-10号)资助
关键词 铅锌(银)矿床 次火山热液矿床 蔡家坪 lead- zinc (silver) ore deposit subvolcanic hydrothermal ore deposit Caijiaping
  • 相关文献

参考文献10

二级参考文献25

共引文献61

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部