摘要
工作区大地构造位置隶属华南褶皱系右江褶皱带册亨—望谟构造变形区,其位于右江褶皱带北缘凸起端(赖子山背斜近北端),与扬子准地台西南缘相毗邻。本区金矿成因为构造热液成矿,属浅成低温热液矿床。本文通过对区域地质背景、矿区地质特征以及地球化学特征、矿床地质特征进行了分析,并结合前人资料,将塘新寨金矿初步定为卡林型金矿。
The geotectonic position of work area belongs to Ceheng to Wangmo tectonic deformation zones in Youjiang fold belt,South of China.It's located in the convex part in the northern margin of Youjiang fold belt(the north of Laizi Mountain anticline),and near to the southwest of Yangzi quasi platform.This gold deposits' genesis is tectonic and hydrothemal mineralization and it's a shallow hydrothermal deposit.This thesis preliminarily discusses the genetic types of this deposit on the base of having found out the ore-forming geological background,ore deposits' geological characteristics and understanding its ore controlling factors,ore prospecting markers and referring to previous datas.And the conclusion is,Tangxinzhai gold deposit is considered preliminarily as Carlin type.
出处
《世界有色金属》
2016年第9S期126-,128,共2页
World Nonferrous Metals
关键词
卡林型金矿
地质特征
成因浅析
红旗坡塘新寨金矿
贵州
Carlin-Type Gold Deposit
geological characteristics
preliminary discussion about genesis
Tangxinzhai gold deposit at Hongqipo
Guizhou province
