摘要
石缸河锡矿床在空间上、时间上和成因上与志本山花岗岩演化分异晚期形成的浅色细粒白云母花岗岩有着密切联系。
The Shiganghe tin deposit is closely related to the light coloured fine grained muscovite granite formed in the late stage of evolution and differentiation of the Zhibenshan granite even in time, space and origin. It belongs to the post magmatic hydrothermal deposit.
出处
《矿产与地质》
1996年第3期159-164,共6页
Mineral Resources and Geology
关键词
锡矿床
矿床成因论
热液矿床
岩浆演化
Tin deposit, Genesis of ore deposit, Western Yunnan Province, Shiganghe
