摘要
矿床属与中三叠统中酸性火山岩有关的喷流型(或火山沉积改造型)铁铅锌多金属矿,并受地层构造双重控制。
The Fe deposit belongs to the effusion type （or volcanic deposition reformation type） related with Middle Triassic intermediate- acid volcanic rock in genesis. The Pb-Zn multimetallic deposit is related to Shanglan Formation slate, silty slate with intercalation of limestone, marl and Sanhedong Formation limestone in genesis, which is a Cu -Pb -Zn multimetallic deposit of hydrothermal type controlled by both strata and structure.
出处
《云南地质》
2013年第4期429-432,442,共5页
Yunnan Geology
关键词
铁铅锌多金属
双重控制地层
热液喷流型
云南维西娃渣
Fe - Pb - Zn Multimetallic
Dual Control
Hydrothermal Effusion Type
Wazha, Weixi, Yunnan
