scholarly journals 3D Seismic Velocity Structure Around Plate Boundaries and Active Fault Zones

10.5772/65512 ◽  
2017 ◽  
Author(s):  
Mohamed K. Salah
Keyword(s):  
Active Fault ◽  
Velocity Structure ◽  
Seismic Velocity ◽  
Fault Zones ◽  
Plate Boundaries ◽  
3D Seismic ◽  
Seismic Velocity Structure

scholarly journals 3D Seismic Velocity Structure in and around the Source Region of the 2001 M6.7 Geiyo Intraslab Earthquake, SW Japan

2006 ◽  
Vol 59 (2) ◽  
pp. 87-105
Author(s):  
Junichi SUGANOMATA ◽  
Tomomi OKADA ◽  
Akira HASEGAWA ◽  
Haijiang ZHANG ◽  
Clifford THURBER
Keyword(s):  
Velocity Structure ◽  
Seismic Velocity ◽  
Source Region ◽  
3D Seismic ◽  
Seismic Velocity Structure ◽  
Intraslab Earthquake ◽  
Sw Japan

scholarly journals 3D Seismic Velocity Structure below Mounds and Pockmarks in the Deep Water Southwest of the Sado Island

2009 ◽  
Vol 118 (1) ◽  
pp. 93-110 ◽  
Author(s):  
Tatsuo SAEKI ◽  
Takao INAMORI ◽  
Sadao NAGAKUBO ◽  
Peter WARD ◽  
Eiichi ASAKAWA
Keyword(s):  
Deep Water ◽  
Velocity Structure ◽  
Seismic Velocity ◽  
3D Seismic ◽  
Seismic Velocity Structure

scholarly journals Seismic velocity structure at the southern termination of the 2016 Kumamoto Earthquake rupture, Japan

2020 ◽  
Vol 72 (1) ◽  
Author(s):  
Yasuhira Aoyagi ◽  
Haruo Kimura ◽  
Kazuo Mizoguchi
Keyword(s):  
Fault Zone ◽  
Velocity Structure ◽  
Seismic Velocity ◽  
Earthquake Rupture ◽  
2016 Kumamoto Earthquake ◽  
Seismic Velocity Structure ◽  
Kumamoto Earthquake ◽  
Seismogenic Layer ◽  
The 2016 Kumamoto Earthquake ◽  
Tectonic Line

Abstract The earthquake rupture termination mechanism and size of the ruptured area are crucial parameters for earthquake magnitude estimations and seismic hazard assessments. The 2016 Mw 7.0 Kumamoto Earthquake, central Kyushu, Japan, ruptured a 34-km-long area along previously recognized active faults, eastern part of the Futagawa fault zone and northernmost part of the Hinagu fault zone. Many researchers have suggested that a magma chamber under Aso Volcano terminated the eastward rupture. However, the termination mechanism of the southward rupture has remained unclear. Here, we conduct a local seismic tomographic inversion using a dense temporary seismic network to detail the seismic velocity structure around the southern termination of the rupture. The compressional-wave velocity (Vp) results and compressional- to shear-wave velocity (Vp/Vs) structure indicate several E–W- and ENE–WSW-trending zonal anomalies in the upper to middle crust. These zonal anomalies may reflect regional geological structures that follow the same trends as the Oita–Kumamoto Tectonic Line and Usuki–Yatsushiro Tectonic Line. While the 2016 Kumamoto Earthquake rupture mainly propagated through a low-Vp/Vs area (1.62–1.74) along the Hinagu fault zone, the southern termination of the earthquake at the focal depth of the mainshock is adjacent to a 3-km-diameter high-Vp/Vs body. There is a rapid 5-km step in the depth of the seismogenic layer across the E–W-trending velocity boundary between the low- and high-Vp/Vs areas that corresponds well with the Rokkoku Tectonic Line; this geological boundary is the likely cause of the dislocation of the seismogenic layer because it is intruded by serpentinite veins. A possible factor in the southern rupture termination of the 2016 Kumamoto Earthquake is the existence of a high-Vp/Vs body in the direction of southern rupture propagation. The provided details of this inhomogeneous barrier, which are inferred from the seismic velocity structures, may improve future seismic hazard assessments for a complex fault system composed of multiple segments.

Seismic velocity structure and gravity anomalies: a comparison

1987 ◽  
Vol 140 (1) ◽  
pp. 115-120
Author(s):  
Yoshibumi Tomoda ◽  
Hiromi Fujimoto
Keyword(s):  
Velocity Structure ◽  
Seismic Velocity ◽  
Gravity Anomalies ◽  
Seismic Velocity Structure
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