• 责任者：Li Hongpu (Institue of Geology Chinese Academy of Geological Sciences ; Beijing 10086 ; China) ; Cheng Xueming
• 刊名：Northwestern Geology
• 出版年：2012
• 卷期：45(1)
• 关键词：火山活动 ; volcanicity ; 多金属矿 ; polymetallic ores ; 唐古拉山 ; Tanggula Mountains
• 页码：p.71-78
• 图表：4 illus., 2 tables, 16 refs.
• 分类号：1001
• issnNo：ISSN1009-6248
• isbnNo：CN61-1149/P

Based on field geological observation and indoor analysis, the authors reclassified the stratum in Kaxinling polymetallic mining deposit, and discussed the metallogenic geological features mineralization mechanism of the deposit. There are 4 sections of ore that have circled 15 ore bodies including 8 concealed ore bodies. 10 of them are Fe-orebody and 5 are Zn-orebody. All of the orebodies are grown in volcanic rocks of Early Permain Gadekao Formation. The volcanism formed six rhythmic layers in three effusive period according to the rock association. The genesis of the deposit is a volcanic plume (VMS) zinc polymetallic deposit, and volcanic rocks are the most important regional prospecting criteria.