摘要
东秦岭(河南段)钼矿床类型可分为斑岩型、斑岩-矽卡岩型、斑岩-角砾岩型,以斑岩型钼矿床为主,近几年又相继发现石英脉型及剪切带型钼矿。通过对东秦岭(河南段)钼异常、矿床空间分布特征及成矿区带综合研究,并对东秦岭(河南段)钼成矿区带进行了划分,为该区进一步开展钼矿地质勘查工作具有重要意义。
The Mo deposits of East Qinling （Henan Section） could be classified into porphyry type, porphyry- skarn type and porphyry-breccia type, of which porphyry type is the major one. Recently, quartz-vein type deposits and the Mo deposits in sheared zone have been discovered one by one. After a comprehensive study on Mo anomalies, spacial distribution of deposits and metallogenic belts in East Qinling （Henan Section）, it has partitioned the Mo metallogenic provinces and belts in East Qinling （Henan Section）, which will be very important for guiding further geological exploration of Mo deposits in this area.
出处
《矿产与地质》
2008年第3期216-220,共5页
Mineral Resources and Geology
关键词
钼矿床
地质特征
异常特征
东秦岭
河南段
Mo deposit, geological characteristics, characteristics of anomalies, East Qinling, Henan section
作者简介
刘国庆（1969-），男，工程师，主要从事矿产普查与勘探工作。
