| 徐顺国.江西蔡家坪铅锌(银)矿床特征[J].矿产勘查,2011,2(1):54-60 |
| 江西蔡家坪铅锌(银)矿床特征 |
| The characteristics of Caijiaping lead-zinc (silver) ore deposit, Jiangxi |
| 投稿时间：2010-04-22 |
| DOI： |
| 中文关键词: 铅锌(银)矿床 次火山热液矿床 蔡家坪 |
| 英文关键词: lead-zinc (silver) ore deposit subvolcanic hydrothermal ore deposit Caijiaping |
| 基金项目:江西永平地区矿产远景调查项目(编号:矿调[2005]13－10号)资助。 |
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| 中文摘要: |
| 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。 |
| 英文摘要: |
| Caijiaping lead-zinc (silver) ore deposit is located in northern Wuyi lead-zinc silver metallogenic belt. On the basis 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 hydrothermal filling, and the ore deposit, belonging to the subvolcanic hydrothermal one, is related closely with sub-volcanic body (rhyolitic porpyry). |
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