摘要
Gold ores of the Qiyugou deposit in the easternpart of the Xiong’ershan region are hosted in brecciapipes within a Mesozoic granitic porphyry.Threestages of alteration-hydrothermal activity are recog-nized within the Qiyugou breccias.
出处
《矿物学报》
CAS
CSCD
北大核心
2009年第S1期212-212,共1页
Acta Mineralogica Sinica