Ore-Forming Characteristics of the Shangtang Village Lead And Zinc Deposit, Quanzhou County
详细信息
- 责任者：Zhou Jiejun (Guilin Research Institute of Geology and Mineral Resources ; Guilin 541004) ; Wang Liguo
- 刊名：Mineral Resources and Geology
- 出版年：2012
- 卷期：26(1)
- 关键词：铅锌矿床 ; lead-zinc deposit ; 广西 ; Guangxi
- 页码：p.62-67
- 图表：3 illus., 4 tables, 4 refs.
- 分类号：1001
- issnNo：ISSN1001-5663
- isbnNo：CN45-1174/TD
摘要
The Shangtang village lead and zinc deposit in located in northeast area of Guangxi which form part of Nanling ore belt, and the ore deposit occurs in carbonatite rock strata of the Qiziqiao Group (D2q) in Middle Devonian system while orebody occur in the side fractured zones and inter-layer fissures of tectonic composite part, characterized by multi period mineralization. Based on the comprehensive analysis on ore-forming geological condition, ore structure and texture, ore matter composition and country rock alteration, it is believed that the mineralization of the deposit is mainly characterized by underground hot fluid mineralization, magmatic hydrothermal mineralization and superimposition of magma and hot fluid mineralization. 5 ore prospecting indicators were summarized at the end for the ore prospecting in depth and periphery of the deposit.