新疆西昆仑—喀喇昆仑地区锂多金属成矿带地质特征及资源潜力  

Eological Characteristics and Resource Potential of the Lithium-Polymetallic Metallogenic Belt in the Western Kunlun-Karakoram Region of Xinjiang

作　　者：蒋炜[1] 李伟[1] 杜斌 裴森龙 杜杰 JIANG Wei;LIWei;DU Bin;PEI Seng-long;DU Jie(Nonferrous Metals Resource Geological Survey of China,Beijing 100012,China)

机构地区：[1]有色金属矿产地质调查中心,北京100012

出　　处：《西部探矿工程》2024年第7期78-81,共4页West-China Exploration Engineering

摘　　要：通过对新疆西昆仑—喀喇昆仑地区的地质背景、矿床类型及资源现状进行综合分析,揭示了其作为我国重要战略资源基地的潜力。该地区地质构造复杂,受特提斯构造域北缘的影响,历经多期构造活动,形成了丰富的锂多金属矿产资源。矿床类型主要为花岗伟晶岩型。目前,该区域的锂资源开发正处于起步阶段,大多数矿区仍未被充分开发。鉴于全球对清洁能源和新能源汽车的需求持续增长,该地区的锂多金属资源有望成为未来重要的供应基地。This article conducts a comprehensive analysis of the geological background,deposit types,and the current status of resources in the Xinjiang West Kunlun-Karakoram region,revealing its potential as an important strategic resource base in China.The region's geological structure is complex,influenced by the northern edge of the Tethys tectonic domain,and has undergone multiple phases of tectonic activity,resulting in abundant lithium polymetallic mineral resources.The main type of deposit is the granite pegmatite type.Currently,the development of lithium resources in this area is in its initial stages,with most mining areas still not fully developed.Given the global demand for clean energy and new energy vehicles continues to grow,the lithium polymetallic resources of this region are expected to become an important supply base in the future.

关 键 词：新疆西昆仑—喀喇昆仑 锂多金属 地质特征 矿床类型 资源开发 

分 类 号：P542.3[天文地球—构造地质学]