摘要
本文以华南MS花岗岩铀矿床为例。研究了构造作用所引起的蚀变(即构造蚀变)作用和构造蚀变岩的地球化学特征,指出该铀矿床是构造蚀变作用促使铀的活化转移并富集形成的,从而揭示了构造控矿的本质方面。
Taking a uranium deposit in South China as an example, the authors study tectonic alteraion (which is caused by tectonic process)and geochemistry of teetonically altered rocks in the region, and suggests that tectonic alteration made uranium mobilize, transport and concentrate to form the deposit. This brings to light the essence of tectonic control on ores.
出处
《大地构造与成矿学》
EI
CAS
CSCD
1989年第2期168-175,共8页
Geotectonica et Metallogenia
