世界有色金属Issue(9):49-51,3.
四川省马边县麦子坪铅锌矿床地质特征分析及成因探讨
Geological Characteristics Analysis and Genesis Discussion of the Lead-Zinc Deposit at Maipin,Mabian County,Sichuan Province
张宁 1黄连刚 2赵伟3
作者信息
- 1. 天全县自然资源和规划局,四川 雅安 625500
- 2. 四川省马边福马磷化有限公司,四川 乐山 614600
- 3. 四川省第七地质大队,四川 乐山 614000
- 折叠
摘要
Abstract
The lead-zinc deposit at Maipin in Mabian County is located in the regional deep fault zone of the Sichuan-Guizhou-Qiangling lead-zinc metallogenic belt.The ore body is vein-like and fills the structural fractures of the Lower Cambrian Qiongzhusi Formation clayey siltstone.It develops along these fractures and intersects obliquely with surrounding rocks while being consistent with the orientation of major faults.Galena is the dominant ore mineral followed by sphalerite and closely associated with fluoritization and silicification alteration.The deposit exhibits good continuity and can reach a medium scale.Additionally,it is associated with fluorite and silver minerals which adds to its high comprehensive mining value.Based on an analysis of geological characteristics combined with controlling factors for mineralization,it is concluded that the Maipin lead-zinc deposit belongs to a medium-low temperature hydrothermal filling vein-type deposit.关键词
麦子坪/铅锌矿/筇竹寺组/矿床成因/地质特征Key words
Maipin/lead-zinc deposit/Qiongzhusi Formation/genesis of deposit/Geological characteristics分类
天文与地球科学引用本文复制引用
张宁,黄连刚,赵伟..四川省马边县麦子坪铅锌矿床地质特征分析及成因探讨[J].世界有色金属,2025,(9):49-51,3.