摘要
银场型硫-多金属矿体顺层贮存于船山-棲霞石灰岩中,为晚石炭-早二叠世闽西南海盆地沉积形成"矿源层"的基础上,经印支期、燕山期构造变动,受多次岩浆热液作用富集成的层控矽卡岩型矿床。
The sulphur-polymetallic orebody of the silver field type bed-parallel stored in the Chuanshan-Qixia limestone,it is on the basis of the source bed which is formed by being deposited on the basin of the southwest sea of late carboniferous-early permian in Fujian province,after tectonism of the Indo-chiness and Yanshanian.It is the stratabound Skarn type ore deposit becouse of the action of the magmatic hydrothermalism.
出处
《福建地质》
2011年第1期29-37,共9页
Geology of Fujian
关键词
矿源层
层控矽卡岩型
硫-多金属矿床
福建大田
source bed
the stratabound skarn type
sulphur-polymetallic orebody
Datian County Fujian Province
