世界有色金属Issue(20)：87-89,3.
新疆巩留县加满特一带银铅矿矿床特征
Characteristics of Silver Lead Ore Deposits in the Jiamante Area of Gongliu County,Xinjiang
何桂麟 1李守能 2张琼 1孙世荣 1刘发伟1
作者信息
- 1. 新疆地质矿产勘查开发局第十一地质大队,新疆 昌吉 831100
- 2. 贵州省地质矿产勘查开发局115地质大队,贵州 贵阳 551400
- 折叠
摘要
Abstract
The working area is located in the western part of the Yishikirik Late Paleozoic Rift Belt of the Yili Micro Plate.The exposed strata in the mining area are mainly the Carboniferous Dahalajunshan Formation and the Permian Wulang Formation.The ore bearing strata in the mining area are the Lower Permian Wulang Formation,with volcanic clastic rocks and lava as the main lithology.The Permian volcanic institutions and circular faults are developed in the mining area,and silver lead deposits are distributed in these structures.The Jiamante mining area has exposed the Jiazhong silver lead deposit There are three types of ore deposits in the mining area,namely the Kokbulak silver lead deposit and the Kashi silver lead deposit.The ore structure in the mining area mainly consists of semi automorphic and heteromorphic granular structures.The ore structure in the mining area is mainly disseminated and fine vein like,and the genesis of the deposit belongs to the silver lead deposit related to terrestrial volcanic hydrothermal fluids.关键词
晚古生代裂谷/乌郎组/火山机构及断裂/矿床成因Key words
Late Paleozoic Rift Valley/Ulang Formation/Volcanic institutions and faults/Genesis of mineral deposits分类
天文与地球科学引用本文复制引用
何桂麟,李守能,张琼,孙世荣,刘发伟..新疆巩留县加满特一带银铅矿矿床特征[J].世界有色金属,2023,(20):87-89,3.
