摘要
Mafic dike swarms are well-developed within the Tethyan Himalaya,southern Tibet,in response to the breakup of Gondwana supercontinent,seafloor spreading of the Tethyan Ocean,and forearc hyperextension during the
基金
supported by National Science Foundation of China (Grant No. 41425010, 41503023 &41273034)
China Geological Survey (Grant No. 12120114022701 & 12120115027101)