摘要
阿尔泰区因为其大陆构造主要位于西伯利亚和哈萨克斯坦——准噶尔之间,遂成为中国的重要贵重金属、稀有金属的成矿带。本文在基于对新疆阿尔泰巴斯铁列克的矿体发现,对其地质构造进行分析,主要包括断裂带、岩性构造带和含矿构造带三种,并以此将其地质划分为拉张型过渡壳型和泥盆际陆缘火山岩型。
The Altai region is mainly located between Siberia and Kazakhstan-Junggar because of its continental structure,and it has become an important metallogenic belt of precious metals and rare metals in China.In this paper,based on the discovery of the ore body of Altai Basiliek in Xinjiang,its geological structure is analyzed,which mainly includes three types of fault zone,lithologic structure zone and ore-bearing structure zone,and the geological classification is divided into tension Type transitional shell type and volcanic rock type on the continental margin of the Devonian.
作者
董雷杰
胡力升
韩永金
DONG Lei-jie;HU Li-sheng;HAN Yong-jin(Xinjiang Uygur Autonomous Region Geological and Mineral Exploration and Development Bureau Second Regional Geological Survey Brigade,Changji 831100,China)
出处
《世界有色金属》
2020年第14期118-119,共2页
World Nonferrous Metals
关键词
新疆阿尔泰巴斯铁列克
钨多金属矿
地质构造
Xinjiang Altay Basiliek
tungsten polymetallic deposit
geological structure
