中国钼业Issue(5)：23-26,4.DOI:10.13384/j.cnki.cmi.1006-2602.2014.05.005
八渡钼矿地质特征及找矿潜力分析
GEOLOGICAL CHARACTERISTICS AND ORE POTENTIAL ANALYSIS OF BADU MOLYBDENUM DEPOSIT
翟义存 1张选固1
作者信息
- 1. 西北有色地质勘查局七一七总队，陕西 宝鸡721015
- 折叠
摘要
Abstract
Badu molybdenum deposit is located in Caledonian folding belt of North Qinling, the ore body occurs mainly in the Middle Proterozoic Qinling group stratum,and ore body shape,occurrence is controlled obviously by S-N trending fault or concentrated fissure zone in structure,the ore body shows low thickness,veins set and high grade. Main metal mineral in the body are molybdenite and chalcopyrite . The genesis of the deposit belongs to the porphyry type deposits in broad sense. The research shows that there is great prospecting potential in the deep ore-body hidden part,extending part of known ore belt as well as the contact zone of granite and gneissic rock.关键词
钼矿床/地质特征/找矿潜力Key words
molybdenum deposit/geological characteristics/exploration potential分类
矿业与冶金引用本文复制引用
翟义存,张选固..八渡钼矿地质特征及找矿潜力分析[J].中国钼业,2014,(5):23-26,4.
