The Characteristics and Origin of the Basic Dikes in Jinchuan Cu-Ni Sulfide Deposits
A dike is an important record of magmatic evolution.Jinchuan Cu-Ni sulfide deposits are hosted in the mafic - ultramafic rock.Jinchuan intrusions locate at the boundary of the fault.The main dikes types are diabase and diorite.
Yue Wu Shang-Guo Su Jian-Guang Hou Chen Song
China University of Geosciences,Beijing,100083
国际会议
贵阳
英文
182-183
2012-06-16(万方平台首次上网日期,不代表论文的发表时间)