摘要
澜沧县孟倮山铜矿体呈似层状、脉状产于侏罗系中统花开左组下段下亚段顶部的层间构造破碎带中,矿体分布、产出、形态均严格受构造破碎带控制,矿床成因属陆相沉积—构造—中低温热液型铜矿床。
The ore body of the Mengluoshan copper deposit in Lancang County is layered and vein-shaped,occurred in the interlayer structural fracture zone at the top of the lower sub segment of the Lower section of Middle Jurassic Huakaizuo Formation.The distribution,occurrence and shape of the ore body are strictly controlled by the structural fracture zone.The deposit was supposed to be a continental sedimentary-structural-medium to low temperature hydrothermal copper deposit.
作者
梁元钊
肖太友
谢行
刘明勇
LIANG Yuan-zhao;XIAO Tai-you;XIE Xing;LIU Ming-yong(Team 310,Yunnan Bureau of Nonferrous Geology,Dali 671000)
出处
《云南地质》
2023年第2期181-185,共5页
Yunnan Geology
关键词
地层+构造控矿
热液型矿床
找矿方向
孟倮山铜矿
云南澜沧
Stratigraphic and Structural Ore Control
Hydrothermal Deposits
Prospecting Direction
Mengluoshan Copper Deposit
Lancang,Yunnan
