地质与勘探2017，Vol.53Issue(4)：657-666,10.
青海江里沟钨多金属矿成矿控制因素及矿化富集规律
Controlling Factors and Mineralization Enrichment of the Jiangligou Tungsten Polymetallic Deposit in Qinghai Province
董想平 1陈海福 1文雪峰 1施根红 1管波1
作者信息
- 1. 青海省有色地质矿产勘查局,青海西宁 810007
- 折叠
摘要
Abstract
The Jiangligou tungsten polymetallic deposit is the largest tungsten deposit in Qinghai at present,which has reached a medium-large deposit scale.It is structurally located at the west Qinling orogenic belt of Qinling-Qilian-Kunlun composite orogenic system.This work summarized the ore-controlling factors and mineralization enrichment regularity of this deposit based on the metallogenic geological setting,geological characteristics,orebody characteristics.The orebodies are controlled by the contact zone between the Gangcha composite granite body and the surrounding rocks.The mineralization shows significant vertical zonation around the rock mass,i.e.,porphyry type molybdenum,greisen type tungsten,skarn type copper-wolfram-molybdenum,hornfels type tungsten and hydrothermal vein lead-zinc from the granite body to surrounding rocks,and the dominate type is skarn type.The genesis of deposit is multinity which related to the intrusion of late stage granite porphyry and fine-grained granite of the Jiangligou composite granite in Late Triassic and late magmatic hydrothermal solution.This work may provide basis for the next step prospecting.关键词
矽卡岩/钨多金属/控制因素/富集规律/江里沟/青海Key words
skarn/tungsten polymetallic deposit/controlling factors/enrichment regular/Jiangligou/Qinghai Province分类
天文与地球科学引用本文复制引用
董想平,陈海福,文雪峰,施根红,管波..青海江里沟钨多金属矿成矿控制因素及矿化富集规律[J].地质与勘探,2017,53(4):657-666,10.
