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Study on shear velocity structure of the crust and the uppermost mantle around Antarctic continent was started in the 1960’s by using surface waves of the earthquakes occurred around Antarctic plate (Evison et al., 1960; Kovach and Press, 1961). Permanent seismic stations have been operated from the end of 1980’s at Antarctic margins except for the South Pole (SPA) on the continental ice sheet. A majority of the stations were established as the Federation of Digital Seismographic Networks (FDSN; Butler and Anderson, 2008). The FDSN was composed of several national and governmental organizations such as the Global Seismographic Network (GSN) organized by the Incorporated Research Institutions for Seismology (IRIS), the Australian Government (AG), GEOSCOPE by French, Geo Forschungs Netz (GEOFON) by Germany, MEDNET by Italy, PACIFIC21 (Tsuboi, 1995) by Japan, and others.

Shear Wave Velocity Models Beneath Antarctic Margins Inverted by Genetic Algorithm for Teleseismic Receiver Functions