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铜陵地区海底喷流沉积(SEDEX)块状硫化物矿床成矿流体研究 被引量:6

Study on Fluids of SEDEX Massive Sulfide Deposits in Tongling District, Anhui Province
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摘要 安徽铜陵地区的铜-金矿床是海底喷流沉积的块状硫化物矿床,经过燕山期岩浆热液的叠加改造而成的产物。本文主要从两方面(海底喷流期以及燕山期)来探讨该区块状硫化物矿床的流体特征。结果表明,该区喷流沉积期流体可与世界上大多数SEDEX块状硫化物矿床流体对比,而燕山期的热液流体却呈多阶段并常伴随沸腾特征。这同样也表明,该区矿床成矿机制、流体作用的复杂性。
出处 《矿床地质》 CAS CSCD 北大核心 2002年第S1期491-494,共4页 Mineral Deposits
基金 国家自然科学基金(No.49733120 No.49773194) 地质矿产部九五攻关项目(No.9501102-04-01)资助
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