摘要
广西佛子冲铅锌矿田位于桂东南博白-岑溪多金属成矿带的NE端,区内发育燕山期花岗岩、花岗闪长岩、二长花岗斑岩和英安质凝灰熔岩等;其中花岗闪长岩和二长花岗斑岩与铅锌成矿关系密切,成矿岩体形成时代分别为156M a和127M a。
The Fuzichong mine field is located compound spot of the many kinds of structural system in northmost part of the Neocathaysian Liangjiang - Cenxi fault zone in the southeast the Guangxi, in the area constructs the shape mark to be extremely complex, acidic magmatic rock growth. Granite -diorite and two long granite - porphyries and is close relations with the lead zinc mineralization. The mineralization rock mass forms the time respectively is 156Ma and 127Ma.
出处
《华南地质与矿产》
CAS
2008年第3期46-49,共4页
Geology and Mineral Resources of South China
基金
危机矿山"广西壮族自治区岑溪市佛子冲铅锌矿山矿产预测"项目(200545050)资助
关键词
岩浆岩
成岩时代
铅锌矿
佛子冲矿田
Magmatic rock
Age of rock - forming
Lead - zinc mine
Fuzichong ore field
