摘要
会东县麦地铅锌矿矿体呈层状、似层状赋存于层间构造破碎带中,近矿围岩为寒武系麦地坪段,矿体产状与岩层产状基本一致。矿体明显受地层和构造的双重控制,属于热液-层控型(MVT型)矿床。
The orebody of Maidi Pb-Zn deposit in Huidong is bedded,stratoid in the interbedded structure fracture zone. The wall rock near orebody is Cambrian Maidiping Member. The occurrence of orebody is consistent basically with that of the rock bed. The orebody is controlled clear by both rock bed and structure,belonging to hydrothermal stratabound（ MVT） deposit.
作者
冀盘龙
杨斌
龙训荣
JI Pan-long;YANG Bin;LONG Xun-rong(College of Geosciences,Chengdu University of Science ＆ Technology,Chengdu 610059;Chengdu Institute of Geology ＆ Mineral Resources,Chengdu 610081)
出处
《云南地质》
2018年第2期195-199,共5页
Yunnan Geology
基金
乌蒙山区地质矿产综合调查(编号:121201010000150002)
关键词
构造控矿
地层控矿
热液-层控型型矿床
四川会东县麦地
Ore Control of Structure
Ore Control of Strata
Hydrothermal Stratabound Deposit
Maidi
Huidong
Sichuan
