Results 41 to 50 of about 880,168 (206)

Laboratory Hydrofractures as Analogs to Tectonic Tremors

AGU Advances
The fracture of Earth materials occurs over a wide range of time and length scales. Physical conditions, particularly the stress field and Earth material properties, may condition rupture in a specific fracture regime.
C. Yuan, T. Cochard, M. Denolle, J. Gomberg, A. Wech, L. Xiao, D. Weitz   +6 more
doaj   +1 more source

An organizational capability framework for earthquake recovery

, 2017
Engineering and construction capability affects the cost and pace of post-disaster recovery. An organizational capability framework for effective earthquake recovery was developed after studying longitudinally 15 engineering and construction ...
Chang-Richards, Alice, Seville, E, Brunsdon, D, Wilkinson, Suzanne   +3 more
core   +1 more source

Shallow Tremors Near the Nankai Trough Activated After the M 7.6 Noto Peninsula Earthquake

Geophysical Research Letters
Off the Cape Muroto near the Nankai Trough, small shallow tremor activity was observed by distributed acoustic sensing (DAS) and offshore seismic network DONET after the 2024 M7.6 Noto Peninsula earthquake approximately 600 km away.
Satoru Baba, Eiichiro Araki, Takane Hori
doaj   +1 more source

Creep-dilatancy development at a transform plate boundary

Nature Communications, 2022
This study shows a direct evidence of pore pressure changes in seabed sediments associated with slow and transient slip along the North Anatolian Fault.
Nabil Sultan, Shane Murphy, Vincent Riboulot, Louis Géli   +3 more
doaj   +1 more source

Strain waves, earthquakes, slow earthquakes, and afterslip in the framework of the Frenkel-Kontorova model [PDF]

Physical Review E, 2009
The one-dimensional Frenkel-Kontorova (FK) model, well known from the theory of dislocations in crystal materials, is applied to the simulation of the process of nonelastic stress propagation along transform faults. Dynamic parameters of plate boundary earthquakes as well as slow earthquakes and afterslip are quantitatively described, including ...
Gershenzon, Naum I., Bykov, V. G., Bambakidis, Gust   +2 more
openaire   +4 more sources

Development of a Slow Earthquake Database

Seismological Research Letters, 2018
学術論文(Ariticle)
Masayuki Kano, Naofumi Aso, Takanori Matsuzawa, Satoshi Ide, Satoshi Annoura, Ryuta Arai, Satoru Baba, Michael Bostock, Kevin Chao, Kosuke Heki, Satoshi Itaba, Yoshihiro Ito, Noriko Kamaya, Takuto Maeda, Julie Maury, Mamoru Nakamura, Takuya Nishimura, Koichiro Obana, Kazuaki Ohta, Natalia Poiata, Baptiste Rousset, Hiroko Sugioka, Ryota Takagi, Tsutomu Takahashi, Akiko Takeo, Yoko Tu, Naoki Uchida, Yusuke Yamashita, Kazushige Obara   +28 more
openaire   +1 more source

Slow Earthquakes in the Microseism Frequency Band (0.1–1.0 Hz) off Kii Peninsula, Japan

Geophysical Research Letters, 2018
It is difficult to detect the signal of slow deformation in the 0.1–1.0 Hz frequency band between tectonic tremors and very low frequency events, where microseism noise is dominant.
Lisa Kaneko, Satoshi Ide, Masaru Nakano
doaj   +1 more source

Ocean-bottom and surface seismometers reveal continuous glacial tremor and slip

Nature Communications, 2021
Anomalously slow earthquakes play a critical role in the earthquake cycle and fault sliding. Here, the authors detect continuous seismic radiation from a glacier sliding over its bed and show persistent coastal shaking to represent an addition to the ...
Evgeny A. Podolskiy, Yoshio Murai, Naoya Kanna, Shin Sugiyama   +3 more
doaj   +1 more source

Earthquakes of the Nepal Himalaya : Towards a Physical Model of the Seismic Cycle [PDF]

, 2013
Home to hundreds of millions of souls and land of excessiveness, the Himalaya is also the locus of a unique seismicity whose scope and peculiarities still remain to this day somewhat mysterious.
Ader, Thomas Joachim
core   +1 more source

Slow Slip as an Indicator of Fault Stress Criticality

Geophysical Research Letters
Fault regions inferred to be slowly slipping are interpreted to accommodate much of tectonic plate motion aseismically and potentially serve as barriers to earthquake rupture.
Valère Lambert
doaj   +1 more source