| 仲麒维.贵州半坡泥盆系碎屑岩型锑矿地质特征与成矿模式探讨[J].矿产勘查,2012,3(1):23-28 |
| 贵州半坡泥盆系碎屑岩型锑矿地质特征与成矿模式探讨 |
| Geological characteristics and mineralization pattern of Banpo Devonian system detritus lithotype antimony ore,Guizhou |
| 投稿时间：2011-02-22 |
| DOI： |
| 中文关键词: 泥盆系 碎屑岩型锑矿 地质特征 成矿模式 |
| 英文关键词: Devonian system detritus lithotype antimony ore geological feature mineralization pattern |
| 基金项目: |
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| 摘要点击次数: 1994 |
| 全文下载次数: 1151 |
| 中文摘要: |
| 泥盆系是我国锑矿最重要的含矿层位。文章以独山锑矿大量的勘查与研究成果为基础,通过整理与综合分析成矿地质背景及矿床(点)地质特征,阐述了“锑”初始成生(即矿源层)的岩相古地理环境及后期改造富集成矿的因素和赋矿场所。论述了独山半坡泥盆系碎屑岩型锑矿床的地质特征、赋矿条件、锑矿床(点)类型及其规律,探讨了半坡泥盆系碎屑岩型锑矿床的成矿模式。 |
| 英文摘要: |
| In this paper, Based on a lot of Banpo antimony exploration and research reports, by finishing with a comprehensive analysis of geological background and deposits (points) geology section, a more clear explanation of the “antimony” initial into a raw (source of ore layer) of rock and post-phase transformation of the ancient geographical factors was discussed and provided enrichment mineralization of ore location. The author expounded Dushan Banpo Devonian clastic type antimony deposits geology, ore conditions, antimony deposits (point) type and its rules and so on.The Devonian rocks Banpo-type antimony mineralization model was explored. |
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