A seismic refraction survey was conducted along a profile from Ajimu, Oita Prefecture, to Tano, Miyazaki Prefecture, on November 14, 1996. This profile is almost the same as the profile of the survey conducted in 1994. The total length of the Ajimu-Tano Profile was about 230km, and three shots and 236 temporary observation sites were arranged along the profile. Charge size of all shots was 500kg. Record signals of the observation sites in a distance range of less than 120km were of good quality. Travel times of first arrivals indicated the complex velocity structure of the shallow part of the crust. Reflected waves from the deeper part of the crust or the upper mantle were also clearly observed. Analysis of the high-quality data sets obtain...
To study a detailed structure of the upper crust in Izu Peninsula, Central Japan, explosion seismic ...
In the summer of 1999, we conducted a highly dense, onshore-offshore integrated seismic experiment i...
An extensive onshore-offshore seismic refraction/wide-angle reflection experiment was undertaken in ...
A seismic refraction survey was conducted along a profile from Shonai, Oita Prefecture to Kushima, M...
A seismic refraction survey was conducted along a profile from Ajimu, Oita Prefecture, to Tano, Miya...
A seismic refraction survey was conducted along a profile from Shonai, Oita Prefecture to Kushima, M...
A seismic refraction survey was conducted along a profile from Fujihashi, Gifu Prefecture, to Kamigo...
On November 11,1993, seismic refraction experiments were carried out in the northern part of the Kan...
To study a detailed structure of the upper crust in Izu Peninsula, Central Japan, explosion seismic ...
In the summer of 1999, we conducted a highly dense, onshore-offshore integrated seismic experiment i...
The tectonic structure of Hokkaido is interpreted as forming by plate motions and associated seconda...
A seismic refraction experiment with 75 seismometers and 4 explosions (J-1 to J-4) was carried out i...
A seismic refraction survey was conducted along a profile from Fujihashi, Gifu Prefecture, to Kamigo...
Seismic surveys of the crust and the upper mantle structure have been conducted under the Special Pr...
The Hinagu fault system, Kyushu, Japan, is located in the westernmost part of the Beppu-Shimabara gr...
To study a detailed structure of the upper crust in Izu Peninsula, Central Japan, explosion seismic ...
In the summer of 1999, we conducted a highly dense, onshore-offshore integrated seismic experiment i...
An extensive onshore-offshore seismic refraction/wide-angle reflection experiment was undertaken in ...
A seismic refraction survey was conducted along a profile from Shonai, Oita Prefecture to Kushima, M...
A seismic refraction survey was conducted along a profile from Ajimu, Oita Prefecture, to Tano, Miya...
A seismic refraction survey was conducted along a profile from Shonai, Oita Prefecture to Kushima, M...
A seismic refraction survey was conducted along a profile from Fujihashi, Gifu Prefecture, to Kamigo...
On November 11,1993, seismic refraction experiments were carried out in the northern part of the Kan...
To study a detailed structure of the upper crust in Izu Peninsula, Central Japan, explosion seismic ...
In the summer of 1999, we conducted a highly dense, onshore-offshore integrated seismic experiment i...
The tectonic structure of Hokkaido is interpreted as forming by plate motions and associated seconda...
A seismic refraction experiment with 75 seismometers and 4 explosions (J-1 to J-4) was carried out i...
A seismic refraction survey was conducted along a profile from Fujihashi, Gifu Prefecture, to Kamigo...
Seismic surveys of the crust and the upper mantle structure have been conducted under the Special Pr...
The Hinagu fault system, Kyushu, Japan, is located in the westernmost part of the Beppu-Shimabara gr...
To study a detailed structure of the upper crust in Izu Peninsula, Central Japan, explosion seismic ...
In the summer of 1999, we conducted a highly dense, onshore-offshore integrated seismic experiment i...
An extensive onshore-offshore seismic refraction/wide-angle reflection experiment was undertaken in ...