Results 11 to 20 of about 4,021 (150)

Errata to "Characteristic activities of slow earthquakes in Japan". [PDF]

Proc Jpn Acad Ser B Phys Biol Sci, 2020
Obara K.
europepmc   +4 more sources

Spontaneous complexity in the dynamics of slow laboratory earthquakes

Nature Communications
Rock deformation experiments play a key role in our understanding of earthquake physics and friction constitutive laws. These laws commonly describe the response of analogue laboratory faults as a simple and homogeneous system, without accounting for the
G. Pozzi, G. Volpe, J. Taddeucci, M. Cocco, C. Marone, C. Collettini   +5 more
doaj   +3 more sources

Fast and Slow Earthquakes in Alaska: Implications from a Three-Dimensional Thermal Regime and Slab Metamorphism

Applied Sciences, 2022
Fast and slow earthquakes are predominantly generated along faults constituting active plate boundaries. Characterized by repeated devastating earthquakes and frequent slow slip events and tremors, the Alaska megathrust presents a chance to understand ...
Rui Qu, Yingfeng Ji, Weiling Zhu, Youjia Zhao, Ye Zhu   +4 more
doaj   +1 more source

A review on slow earthquakes in the Japan Trench

Progress in Earth and Planetary Science, 2023
Slow earthquakes are episodic slow fault slips. They form a fundamental component of interplate deformation processes, along with fast, regular earthquakes.
Tomoaki Nishikawa, Satoshi Ide, Takuya Nishimura   +2 more
doaj   +1 more source

Frictional and Lithological Controls on Shallow Slow Slip at the Northern Hikurangi Margin

Geochemistry, Geophysics, Geosystems, 2022
Slow slip events (SSEs) have been identified at subduction zones globally as an important link in the continuum between elastodynamic ruptures and stable creep.
Srisharan Shreedharan, Matt Ikari, Clay Wood, Demian Saffer, Laura Wallace, Chris Marone   +5 more
doaj   +1 more source

A review of shallow slow earthquakes along the Nankai Trough

Earth, Planets and Space, 2023
Slow earthquakes occur at deep and shallow plate boundaries along the Nankai Trough. Deep slow earthquakes are continuously distributed along the 30–40 km depth contours of the upper surface of the subducted Philippine Sea Plate.
Shunsuke Takemura, Yohei Hamada, Hanaya Okuda, Yutaro Okada, Kurama Okubo, Takeshi Akuhara, Akemi Noda, Takashi Tonegawa   +7 more
doaj   +1 more source

A review of tidal triggering of global earthquakes

Geodesy and Geodynamics, 2023
Earthquake prediction remains a challenging and difficult task for scientists all over the world. The tidal triggering of earthquakes is being proven by an increasing number of investigations, most of which have shown that earthquakes are positively ...
Ruyu Yan, Xiaodong Chen, Heping Sun, Jianqiao Xu, Jiangcun Zhou   +4 more
doaj   +1 more source

A combination of tides and nontidal variations in ocean bottom pressure may generate interannual slip fluctuations in the transition zone along a subduction plate interface

Geodesy and Geodynamics, 2023
The tidal triggering of earthquakes has been studied for many years. The discovery of slow earthquakes in the early 2000s, including slow slip, has urged scientists to investigate the tidal responses of these earthquakes due to their sensitivity to weak ...
Yoshiyuki Tanaka, Hiromu Sakaue, Masayuki Kano, Suguru Yabe   +3 more
doaj   +1 more source

Observation of Shallow Slow Earthquakes by Distributed Acoustic Sensing Using Offshore Fiber‐Optic Cable in the Nankai Trough, Southwest Japan

Geophysical Research Letters, 2023
Off Cape Muroto area, along the Nankai Trough in southwest Japan, is a typical area with adjacent occurrences of slow and megathrust earthquakes. High‐resolution monitoring of slow earthquakes is necessary to understand tectonic conditions.
Satoru Baba, Eiichiro Araki, Yojiro Yamamoto, Takane Hori, Gou Fujie, Yasuyuki Nakamura, Takashi Yokobiki, Hiroyuki Matsumoto   +7 more
doaj   +1 more source

Slow Slip Events in the Kanto and Tokai Regions of Central Japan Detected Using Global Navigation Satellite System Data During 1994–2020

Geochemistry, Geophysics, Geosystems, 2021
Slow slip events (SSEs) along subduction zones play an important role in accommodating relative plate motion. SSEs interplay with large megathrust earthquakes and other slow earthquakes, including low frequency and very low frequency earthquakes.
Takuya Nishimura
doaj   +1 more source