Geodetic imaging of plate motions, slip rates, and partitioning of deformation in Japan

JP Loveless, BJ Meade - Journal of Geophysical Research …, 2010 - Wiley Online Library
Interseismic deformation in Japan results from the combined effects of tectonic processes
including rotation of crustal blocks and the earthquake cycle process of elastic strain …

Development and applications of double-difference seismic tomography

H Zhang, C Thurber - pure and applied geophysics, 2006 - Springer
Double-difference (DD) tomography is a generalization of DD location; it simultaneously
solves for the three-dimensional velocity structure and seismic event locations. DD …

An episode of fault-valve behaviour during compressional inversion?—The 2004 MJ6. 8 Mid-Niigata Prefecture, Japan, earthquake sequence

RH Sibson - Earth and Planetary Science Letters, 2007 - Elsevier
Principal ruptures of the 2004 Mid-Niigata Prefecture sequence involved close-to-pure
reverse slip on a 50–60° WNW dipping fault system uplifting a Miocene rift basin on its …

[PDF][PDF] Tomography and dynamics of Western-Pacific subduction zones

D Zhao - 2012 - tohoku.repo.nii.ac.jp
We review the significant recent results of multiscale seismic tomography of the Western-
Pacific subduction zones and discuss their implications for seismotectonics, magmatism …

Simultaneous Reactivation of Two, Subparallel, Inland Normal Faults during the Mw 6.6 11 April 2011 Iwaki Earthquake Triggered by the Mw 9.0 Tohoku‐oki …

S Toda, H Tsutsumi - Bulletin of the Seismological …, 2013 - pubs.geoscienceworld.org
Abstract The gigantic M w 9.0 11 March 2011 Tohoku‐oki earthquake suddenly changed the
overriding inland area to an extensional stress regime and triggered massive seismic …

Rupture processes of the 2004 Chuetsu (mid‐Niigata prefecture) earthquake, Japan: A series of events in a complex fault system

K Hikima, K Koketsu - Geophysical research letters, 2005 - Wiley Online Library
We relocated the hypocenters of the 2004 Chuetsu earthquake sequence, Niigata, Japan,
using the double‐difference method. The distribution of aftershocks reveals a complex fault …

Seismic attenuation tomography of the source zone of the 2016 Kumamoto earthquake (M 7.3)

Z Wang, D Zhao, X Liu, X Li - Journal of Geophysical Research …, 2017 - Wiley Online Library
We study the three‐dimensional seismic attenuation (QP and QS) structure in the source
area of the 2016 Kumamoto earthquake (M 7.3) by using 18,296 and 29,668 data from 742 …

Zemmouri earthquake rupture zone (Mw 6.8, Algeria): Aftershocks sequence relocation and 3D velocity model

A Ayadi, C Dorbath, F Ousadou… - Journal of …, 2008 - Wiley Online Library
We analyze the aftershocks sequence of the Zemmouri thrust faulting earthquake (21 May
2003, Mw 6.8) located east of Algiers in the Tell Atlas. The seismic sequence located …

Determination of three-dimensional in situ stresses from anelastic strain recovery measurement of cores at great depth

W Lin, M Kwaśniewski, T Imamura, K Matsuki - Tectonophysics, 2006 - Elsevier
In order to examine whether the anelastic strain recovery (ASR) method can be applied for
determining the in situ stress in hard rocks at great depths, the anelastic strain recovery of …

Why do aftershocks occur? Relationship between mainshock rupture and aftershock sequence based on highly resolved hypocenter and focal mechanism …

Y Yukutake, Y Iio - Earth, Planets and Space, 2017 - Springer
In order to clarify the origin of aftershocks, we precisely analyze the hypocenters and focal
mechanisms of the aftershocks following the 2000 Western Tottori Earthquake, which …