摘要
贵州省开阳地区矿产资源丰富,尤以磷矿最为著名。其中“平安磷矿二矿(扩界)”主要产于震旦系下统陡山沱组中,属中型磷块岩矿床。矿石中的矿物主要以碳氟磷灰石居多,其矿床的成因类型为浅-滨海相沉积的磷块岩矿床类型亚种。本文通过对矿区的成矿地质条件(矿区地层、构造)进行探讨,分析了平安磷矿二矿(扩界)的矿床地质特征(含矿岩系、矿石组构、矿物成分、矿石类型等),不仅为该地区磷矿资源勘查提供相对可靠的参考依据,还可以服务于矿区周边的有利找矿靶区。
Guizhou Kaiyang area is rich in mineral resources,especially phosphate rock.Among them,"Ping'an Phosphate Mine No.2(Extension)"mainly occurs in Doushantuo Formation of Lower Sinian System,which is a medium-sized phosphorite deposit.The minerals in the ore are mainly fluorocarbon apatite,and the genetic type of the deposit is a subspecies of phosphorite deposit type deposited in shallow-coastal facies.This paper discusses the metallogenic geological conditions(strata and structure of the mining area),and analyzes the geological characteristics(ore-bearing rock series,ore fabric,mineral composition,ore type,etc.)of Ping'an Phosphate Mine No.2(extension),which not only provides a relatively reliable reference for the exploration of phosphate resources in this area,but also serves the favorable prospecting target areas around the mining area.
作者
杨光亮
YANG Guangliang(Guizhou Geological Exploration Institute,China Chemical Geology and Mine Bureau,Guiyang 550002,China)
出处
《四川有色金属》
2022年第1期26-29,共4页
Sichuan Nonferrous Metals
关键词
开阳
金中镇
磷矿
震旦系
地质特征
Kaiyang
Jinzhong town
phosphate rock
Sinian system
geologic feature