In order to find a practical method to assess forthcoming activity of aftershocks, an attempt was made to predict a plausible range of the number of major aftershocks of the 1999 Chi-Chi, Taiwan earthquake of September 20 (UTC;Ms=7.7). Although a method of predicting the probability of aftershocks had been proposed, assuming that parameters in the modified Omori formula would not change during the period of prediction, such an assumption might sometimes be invalid at the time of the especially large aftershocks. For this reason, a range of the number of aftershocks was experimentally discussed between September 22 and November 21 based on the 5-95% or the 0-90% points of the Poisson distribution. As a result, 11 cases were successful among ...
金沢大学理工研究域物質化学系This study was performed to examine the possibility of the X-ray stress measurement by...
The slab intersection of the Northeast Honshu and Izu-Bonin Arcs beneath Central Japan is modeled fr...
笠岡湾干拓地海底ヘドロを充テンしたライシメーターを用いて,地表排水開始(干陸)後8年を経過した乾燥風化土について各種土壌物理試験を行ない、その結果を干陸後2年の未風化土の結果とも比較しつつ検討し考察を...
Impedance tensor elements were determined for periods between 20 and 240 min from the magnetic and t...
Late in the fall of 1987, as a part of the Japanese National Research Program (DELP/Dynamics and Evo...
The present author established the table of diagrammatic calendar ages of the housefly females, Musc...
Steady-state convection currents of an incompressible Newtonian fluid of very high viscosity in a no...
The interference of the fundamental and higher modes of Love waves is an important subject to be sol...
The magnetic-compass-deviation in the small fishing-training boat built from block system "Nansei-ma...
B-type, explosion and N-type earthquakes recorded by short period seismographs at Asama volcano, cen...
In Section II, we discuss from a viewpoint of ray theory the frequency equations of the spheroidal o...
The tsunamis which were generated at E Luzon I. on Aug. 1, 1968 and off NE Celebes I. on Aug. 10, 19...
The tectonic relief on the focal regions of great shallow earthquakes in the circum-Pacific belt and...
During explosion seismic studies in the Matsushiro Earthquake Swarm Area the seismic waves from shot...
In forensic science, age estimation is an important step in identifying unidentified cadavers. As te...
金沢大学理工研究域物質化学系This study was performed to examine the possibility of the X-ray stress measurement by...
The slab intersection of the Northeast Honshu and Izu-Bonin Arcs beneath Central Japan is modeled fr...
笠岡湾干拓地海底ヘドロを充テンしたライシメーターを用いて,地表排水開始(干陸)後8年を経過した乾燥風化土について各種土壌物理試験を行ない、その結果を干陸後2年の未風化土の結果とも比較しつつ検討し考察を...
Impedance tensor elements were determined for periods between 20 and 240 min from the magnetic and t...
Late in the fall of 1987, as a part of the Japanese National Research Program (DELP/Dynamics and Evo...
The present author established the table of diagrammatic calendar ages of the housefly females, Musc...
Steady-state convection currents of an incompressible Newtonian fluid of very high viscosity in a no...
The interference of the fundamental and higher modes of Love waves is an important subject to be sol...
The magnetic-compass-deviation in the small fishing-training boat built from block system "Nansei-ma...
B-type, explosion and N-type earthquakes recorded by short period seismographs at Asama volcano, cen...
In Section II, we discuss from a viewpoint of ray theory the frequency equations of the spheroidal o...
The tsunamis which were generated at E Luzon I. on Aug. 1, 1968 and off NE Celebes I. on Aug. 10, 19...
The tectonic relief on the focal regions of great shallow earthquakes in the circum-Pacific belt and...
During explosion seismic studies in the Matsushiro Earthquake Swarm Area the seismic waves from shot...
In forensic science, age estimation is an important step in identifying unidentified cadavers. As te...
金沢大学理工研究域物質化学系This study was performed to examine the possibility of the X-ray stress measurement by...
The slab intersection of the Northeast Honshu and Izu-Bonin Arcs beneath Central Japan is modeled fr...
笠岡湾干拓地海底ヘドロを充テンしたライシメーターを用いて,地表排水開始(干陸)後8年を経過した乾燥風化土について各種土壌物理試験を行ない、その結果を干陸後2年の未風化土の結果とも比較しつつ検討し考察を...