摘要
通过阐述黄柏峪铜钼矿床的地质特征及地球化学特征,来探讨其成矿地质条件,认为该区不仅存在矽卡岩型矿床,而且也有斑岩型及热液型矿床存在的可能。
By the study on the geological and geochemical characteristics of the Cu-Mo deposit in Huangbaiyu area,it's ore-forming condition is discussed.Therefore,it is consider that they are not only SK type deposit , but also porphyry and mesothermal type deposit in the area.
出处
《有色矿冶》
2005年第3期7-8,11,共3页
Non-Ferrous Mining and Metallurgy
关键词
本溪黄柏峪
铜钼矿床
成矿地质条件
Huangbaiyu area of Benxi
Cu-Mo deposit
ore-forming condition
