摘要
旌德岩体位于江南地块的东段,本文对旌德岩体及其中发现的捕虏体的地质特征以及捕虏体的含矿情况进行了介绍,并认为其成因和岩浆热液作用有关,为矽卡型矿床;并对捕虏体发现的找矿意义进行了说明。
The Jingde rock mass is located in the eastern part of the Jiangnan Massif.This paper introduces the Jingde rock mass,geological features and ore-bearing conditions of xenolith found in it,argues that it is genetically related to magmatic hydrothermalism and is a skarn ore deposit,and then describes the significance of xenolith discovery to ore prospecting.
作者
丁希国
王克友
李伟
许卫
DING Xi-guo;WANG Ke-you;LI Wei;XU Wei(Institute of Geological Survey of Anhui Province,Hefei,Anhui 230001,China;Bureau of Geology and Mineral Exploration of Anhui Province,Hefei,Anhui 230001,China)
出处
《安徽地质》
2018年第1期23-26,共4页
Geology of Anhui
关键词
旌德岩体
捕虏体
钨矿
地质特征
矿床成因
找矿意义
Jingde rock mass
xenolith
tungsten
geologic features
origin of ore deposit
prospecting significance
