Brief Analysis for Geological Features and Ore Deposit Origin of Weibao Lead-Zinc Deposit in Ruoqiang County, Xinjiang
详细信息
- 责任者：Hu Huawei (Geophysical and Geochemical Party ; Xinjiang Bareau of Geology and Mineral Resource Exploration and Development ; Changji 831100 ; China) ; Jing Baosheng
- 刊名：Northwestern Geology
- 出版年：2010
- 卷期：43(4)
- 关键词：铅锌矿床 ; lead-zinc deposit ; 新疆 ; Xinjiang
- 页码：p.73-80
- 图表：3 illus., 2 tables, 11 refs.
- 分类号：1001
- issnNo：ISSN1009-6248
- isbnNo：CN61-1149/P
摘要
The Weibao mining area, located at the Qimantage Paleozoic Era compound trench-arc belt in the Qaidam micro tectonic plate of Tarimu-North China tectonic plate, belongs to the east Kunlun Mountains Fe-Pb-Zn-Cu-Co-Au-W-Sn-asbestos-salts mineralization belt-Qimantage W-Sn-Pb-Zn-Fe-Cu multi-metalliferous ore belt, the Qin-Qi-Kun mountains mineralization territory-Kunlun mountains mineralization province. The ore is mainly with half idiomorphic-xenomorphic-granular metacryst texture and contaminated structure, partially with block structure. Genetic type of the ore deposit is classified into the deposition-magmatic gas fluid superimposition and stratabouned.