Ocean Hemisphere Research Center, Earthquake Research Institute, the University of Tokyo
Investigate the Earth's interiors from broadband ocean bottom seismology
Plate boundary is about 40 km deeper than the surrounding seafloor, which is a result of underplating of dehydrated residuals of a thermochemical mantle plume.
We constracted an age-dependent shear-wave reference model and a deviation map from the reference model.
3-D anisotropic shear wave velocity mode in and around Ontong Java Plateau
Download from DOI: 10.13140/RG.2.2.29857.94561/1
Memos for my research.