The upper crustal structure of the Soya Coast, Antarctica was estimated by a seismic refraction experiment which was carried out in January 1979. A surface thin layer with a P-wave velocity of 4-5km/s was derived from the traveltime analysis for the first time in East Antarctica by explosion seismology
A reflective lower crust' has been found in some regions of Phanerozoic orogens. In Antarctica it ha...
A seismic refraction experiment was successfully conducted along the S17-Z20 profile on the Mizuho r...
A reflective lower crust\u27 has been found in some regions in the Japanese islands as well as in th...
Two explosion seismic experiments were conducted for the investigation on the velocity structure of ...
The P-wave velocity structure of a part of the Prince Olav Coast, East Antarctica was revealed by a ...
From 1979 to 1981,explosion seismic experiments were carried out by the 20th, 21st and 22nd Japanese...
Seismic refraction experiments were carried out to investigate the crustal structure in Antarctica b...
The upper crustal structures beneath McMurdo Station, Antarctica are studied using reflected waves o...
A seismic survey with a high density network was conducted by the 41st Japanese Antarctic Research E...
The structure of the Earth’s crust and the upper mantle in East Antarctica are investigated using th...
The summer-field party of the 20th Japanese Antarctic Research Expedition (JARE-20) carried out the ...
Large seismic explosion experiments were conducted on the traverse route from Syowa to Mizuho Statio...
A refraction experiment with a 100kg charge was carried out on the ice sheet of the Prince Olav Coas...
To improve knowledge of the crustal structure, explosion seismic experiments were carried out on Mou...
Three big seismic explosion experiments were carried out by the 21st and 22nd Japanese Antarctic Res...
A reflective lower crust' has been found in some regions of Phanerozoic orogens. In Antarctica it ha...
A seismic refraction experiment was successfully conducted along the S17-Z20 profile on the Mizuho r...
A reflective lower crust\u27 has been found in some regions in the Japanese islands as well as in th...
Two explosion seismic experiments were conducted for the investigation on the velocity structure of ...
The P-wave velocity structure of a part of the Prince Olav Coast, East Antarctica was revealed by a ...
From 1979 to 1981,explosion seismic experiments were carried out by the 20th, 21st and 22nd Japanese...
Seismic refraction experiments were carried out to investigate the crustal structure in Antarctica b...
The upper crustal structures beneath McMurdo Station, Antarctica are studied using reflected waves o...
A seismic survey with a high density network was conducted by the 41st Japanese Antarctic Research E...
The structure of the Earth’s crust and the upper mantle in East Antarctica are investigated using th...
The summer-field party of the 20th Japanese Antarctic Research Expedition (JARE-20) carried out the ...
Large seismic explosion experiments were conducted on the traverse route from Syowa to Mizuho Statio...
A refraction experiment with a 100kg charge was carried out on the ice sheet of the Prince Olav Coas...
To improve knowledge of the crustal structure, explosion seismic experiments were carried out on Mou...
Three big seismic explosion experiments were carried out by the 21st and 22nd Japanese Antarctic Res...
A reflective lower crust' has been found in some regions of Phanerozoic orogens. In Antarctica it ha...
A seismic refraction experiment was successfully conducted along the S17-Z20 profile on the Mizuho r...
A reflective lower crust\u27 has been found in some regions in the Japanese islands as well as in th...