摘要
阿北锡矿区位于哈萨克斯坦板块准噶尔微型板块的赛米斯台-东泉晚古生代岛弧带东段,区内已发现卡姆斯特、干梁子、贝勒库都克、黄羊山、萨惹什克和阿北6个锡矿以及苏吉泉、红土井子等锡矿点。本文主要从阿北锡矿成矿地质背景、成矿地质特征和矿床成因等进行了初步分析与总结。
The Abei tin mining area is located in the eastern part of the Semistai-Dongquan Late Paleozoic island arc belt of the Junggar micro-plate of the Kazakhstan plate,Six tin deposits, such as Kamster, Ganliangzi, Belkuduk, Huangyang Mountain, Sarayashk and Abei, as well as Sujiquan and laterite well, have been found in the area. This paper mainly analyzes and summarizes the metallogenic geological background, metallogenic geological characteristics and genesis of the Abei tin deposit.
作者
罗辉平
杨华泽
赖中伟
LUO Hui-ping;YANG Hua-ze;LAI Zhong-wei(The Ganxi Brigade of Geological Survey,Jiangxi Bureau of Geology and Mineral Resource,Nachang 330002,China)
出处
《世界有色金属》
2018年第17期114-115,共2页
World Nonferrous Metals
关键词
阿北锡矿
成矿地质特征
矿床成因
勘查启示
Abei Tin
Metallogenic geological characteristics
Genesis of ore deposits
Exploration and Revelation
