摘要
层控接触变质型硅灰石矿床的形成,取决于成矿原岩、岩体侵入形成的面型热变质及一定的构造裂隙系统.
The formation of the stratabound-contact metamorphic type wollastonite deposits is related to the
original ore-forming rocks, the surfacial thermo-metamorphism formed during the intrusion of rock
masses and a particular structural fissure system.
出处
《地质与勘探》
CAS
CSCD
北大核心
1990年第6期21-25,共5页
Geology and Exploration