作者: Yan Liang , Alan Schiemenz , Marc A. Hesse , E. M. Parmentier
DOI: 10.1029/2011GL049034
关键词: Shock wave 、 Basalt 、 Mantle wedge 、 Melt flow index 、 Petrology 、 Geophysics 、 Geology 、 Mantle (geology) 、 Porosity 、 Compaction 、 Transition zone
摘要: The style of melt migration in the mantle is important to the interpretation of basalts erupted on the surface. Both grain‐scale diffuse porous flow and channelized melt migration have …