| 陈兴龙.黔东南火烧寨金锑(砷)矿矿床地球化学特征及矿化富集规律浅析[J].地质找矿论丛,2010,25(2):129-133 |
| 黔东南火烧寨金锑(砷)矿矿床地球化学特征及矿化富集规律浅析 |
| GEOCHEMICAL CHARACTERISTICS OF HUOSHAOZHAI Au-Sb(As) DEPOSIT IN THE SOUTHEAST GUIZHOU PROVINCE AND THE Au CONCENTRATION PATTERN |
| 投稿时间：2010-04-18 |
| DOI：10.6053/j.issn.1001-1412.2010.2. 007 |
| 中文关键词: 火烧寨金锑(砷)矿 地球化学 富集规律 黔东南 |
| 英文关键词:Huoshaozhai Au-Sb(As) deposit geochemistry the ore concentration pattern the southeast Guizhou province |
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| 中文摘要: |
| 火烧寨锑金(砷)矿位于黔东南雷公山多金属成矿带的双尧—火烧寨成矿亚带。通过对成矿地质特征和矿床地球化学特征的研究,提出矿带主要受控于深切地幔的独山—松桃深大断裂及分支断裂,成矿活动与构造-岩浆活动具有同步性,并总结了成矿富集规律。 |
| 英文摘要: |
| Huoshaozhai Au-Sb(As) deposit is situated in the Shuangyao-Huoshaozhai sub-ore belt of Leigongshan multi-metallic ore belt.This paper deals with metallogenic characteristics,summarizes geochemical characteristics and puts forward that the ore belt is mainly controlled by the mantle-cutting deep seated fracture and the branches and the ore-forming activities are synchronous with structural-magma activities,then the ore concentration pattern. |
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