摘要
虎鹿夼银铅矿床是山东省第一地质矿产勘查院近年来在鲁东地区发现的一处银铅共生矿床。该矿床赋存于新太古代回龙夼单元的条带状细粒含角闪黑云英云闪长岩体内 ,矿体受构造破碎带控制 ,是一处矿体形态简单、矿化较连续且银品位较高的中低温热液矿床。
Hulukuang silver-lead deposit newly found by No.1 Exploration Institute of Geology and Mineral Resources is a syngenetic deposit of silver and lead. It occurs in banded fine-grained amphibolite-bearing biotite tonalite of Neo-archaean Huilongkuang unit, and the orebodies are controlled by structural zones. It is a low to moderate temperature hydrothermal deposit with simple orebody shapes, continuous mineralization and high grade.
出处
《山东地质》
2001年第1期30-34,共5页
Geology of Shandong
关键词
银铅共生矿床
矿床地质
山东
赋存状态
构造破碎带
围岩蚀变
Syngenetic deposit of silver and lead
deposit geology
low to moderate temperature hydrothermal
Qixia in Shandong province
