摘要
Abstract
The Yangjianlangzi lead-zinc ore body occurs in the marble near the contact zone between the granite body and the Silurian Middle-Upper Series(S2+3),sand and shale,and the mineralization is strictly controlled by lithology,structure,magmatic rock,etc.,and the mineralization is relatively concentrated on the lithological difference surface.The ore body is stratiform-like output,which is more continuous and stable in strike and tendency,and is almost consistent with the occurrence of the surrounding rock.The genesis of the deposit is a skarn-type lead-zinc deposit,and the key areas for the next work in the mining area are the deep and eastern regions of the mining area.关键词
成矿地质体/成矿构造和成矿结构面/成矿作用特征标志/矿床成因Key words
Ore-forming geological body/Metallogenic structure and metallogenic structural plane/Characteristic signs of mineralization/genesis of deposit分类
天文与地球科学
