摘要
A number of E-W trending subparallel mafic dikes of diabase composition occurred in Gyangze-Kangma area,eastern Tethyan Himalaya,southern Tibet.They intruded into the Tethyan Himalaya sedimentary sequence.Whether they belong to the;32 Ma Comei LIP(Zhu et al.,2009)or
基金
supported by National Science Foundation of China (Grant No. 41425010 & 41503023)
China Geological Survey (Grant No. 12120114022701 & 12120115027101)