Results 31 to 40 of about 6,044 (217)

Application of an inhomogeneous stress (patch) model to complex subduction zone earthquakes: A discrete interaction matrix approach [PDF]

open access: yes, 1987
In recent years it has been recognized that the level of shear and normal stress along a fault can vary; thus the stress is spatially and temporally inhomogeneous.
Kanamori, Hiroo, Rundle, John B.
core   +1 more source

In situ stress magnitude and rock strength in the Nankai accretionary complex: a novel approach using paired constraints from downhole data in two wells [PDF]

open access: yes, 2016
We present a method to simultaneously constrain both far-field horizontal stress magnitudes (S hmin and S Hmax) and in situ rock unconfined compressive strength (UCS), using geophysical logging data from two boreholes located 70 m apart that access the ...
Dugan, B., Huffman, K.A., Saffer, D.M.
core   +1 more source

Simulation of great earthquakes along the Nankai Trough: reproduction of event history, slip areas of the Showa Tonankai and Nankai earthquakes, heterogeneous slip-deficit rates, and long-term slow slip events

open access: yesEarth, Planets and Space, 2022
Great earthquakes have occurred repeatedly along the Nankai Trough, but only for recent events are details known, such as rupture areas and time lags between paired events.
Fuyuki Hirose   +3 more
doaj   +1 more source

The role of compaction contrasts in sediments in décollement initiation in an accretionary prism [PDF]

open access: yes, 2011
International audienceTo understand how décollements develop into the pristine sedimentary succession entering subduction zones, we have performed mechanical tests on samples from the sediment column entering the Nankai accretionary prism, Japan (ODP ...
Hamano, Yozo   +4 more
core   +4 more sources

Estimate of the contraction rate of central Japan through the deformation of the Philippine Sea slab

open access: yesProgress in Earth and Planetary Science, 2019
The Philippine Sea (PHS) slab is severely deformed beneath central Japan, but it is subject to little deformation before the subduction along the Nankai Trough.
Yukitoshi Fukahata
doaj   +1 more source

構造研究に基づく南海トラフ(西部)地震発生帯のプレート形状および速度構造の3次元モデル [PDF]

open access: yes, 2013
Great interplate earthquakes have repeatedly occurred in pairs along the Nankai Trough. In order to reduce a great deal of damage to coastal area from both strong ground motion and tsunami generation, it is necessary to understand rupture synchronization
KANEDA, Yoshiyuki   +23 more
core  

Anelastic strain recovery reveals extension across SW Japan subduction zone [PDF]

open access: yes, 2009
Sediment dominated convergent margins typically record substantial horizontal shortening often associated with great earthquakes. The convergent margin south of Japan is arguably one of the most extensively investigated margins and previous studies ...
Akito Tsutsumi   +35 more
core   +1 more source

Bioinspired Morphology‐Decoupled Soft Gripper with Enhanced Bidirectional Grasping Capability

open access: yesAdvanced Science, EarlyView.
Inspired by biological predation, a novel gripper decouples cross‐modal grasping via dual morphological configurations. Synergistically integrating hybrid rigid and soft coupled fingers with a metamaterial palm, the system performs active compliant grasping for static objects and passive cage capture for dynamic targets.
Yedong Huang   +4 more
wiley   +1 more source

Structural Evolution of the Eastern Nankai Trough accretionary prism, Central Japan—Subduction of Trough-Parallel Seamount Chains

open access: yesProgress in Earth and Planetary Science
The Nankai Trough, offshore of Southwest Japan, represents a plate subduction zone where a long history of devastating mega-earthquake and tsunami events has been best documented.
Philomene Vanessa Eyang Ondo Ep Ella Ndong   +6 more
doaj   +1 more source

構造研究に基づく南海トラフ地震発生帯の3次元速度構造モデル [PDF]

open access: yes, 2014
Coseismic rupture area of the great interplate earthquake concerned about its occurrence along the Nankai Trough presumed by government of Japan is now wider to the west, north and south than the former assumption. Although the new estimation is based on
KANEDA, Yoshiyuki   +13 more
core  

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