摘要
受红河右旋走滑深大断裂构造控制,铁矿床主要赋存于华力西期侵入基性-超基性岩杂岩体内,成矿专属性明显,矿床属晚期岩浆结晶分异型磁铁矿矿床。
The Fe ore deposit is controlled mainly by Honghe right lateral strike slipfault.It is in the basic-ultrabasic complex of Variscan intrusion,with the evident metallogenetic specialization.It belongs to the magnetite deposit of late magmatic crystal differentiate type.
出处
《云南地质》
2012年第2期208-210,共3页
Yunnan Geology
关键词
岩体控矿
基性分异体
磁铁矿
外围找矿远景
云南金平太平桥
Ore Control of Rock Body
Basic Differentiate
Magnetite
Surrounding Prospecting Potentiality
Taipingqiao,Jinping,Yunnan
