Results 81 to 90 of about 1,202,006 (199)
Pore‐Pressure Cycles and Slow Slip Generation on Mildly Velocity‐Weakening Faults
Abstract Recent observations have revealed pore‐fluid pressure fluctuations correlated with the occurrence of slow slip events (SSEs) in several subduction zones. These fluctuations, caused by fluid accumulation and migration before and during SSEs, may modulate the timing and characteristics of these events.
Andrea Perez‐Silva +2 more
wiley +1 more source
<p>EarthByte DCO-commissioned project, Spatio-temporal modelling of deep time atmospheric carbon flux from subduction zone interactions, specifically addresses this goal by using plate reconstructions and cutting-edge, open-source ...
Sabin Zahirovic +7 more
core +1 more source
Precise tilt measurement by seafloor borehole tiltmeters at the Nankai Trough subduction zone
In this study, geodetic and seismic phenomena occurring in the subduction zone were observed with two tiltmeters that were installed in seafloor boreholes drilled in the Kumano Basin in the Nankai Trough, southwest Japan.
Shuhei Tsuji +6 more
doaj +1 more source
P wave anisotropic tomography of the Nankai subduction zone in Southwest Japan
The active subduction of the young Philippine Sea (PHS) plate and the old Pacific plate has resulted in significant seismic heterogeneity and anisotropy in Southwest (SW) Japan. In this work we determined a detailed 3‐D P wave anisotropic tomography of the crust and upper mantle beneath SW Japan using ∼540,000 P wave arrival times from 5,249 local ...
Jian Wang, Dapeng Zhao
openaire +1 more source
Abstract Recurring slow slip events (SSEs) with moment magnitudes in the mid‐6 range have occurred every few years since the 1990s offshore the Boso Peninsula, Japan. These events occur near the source area of ∼M8 megathrust earthquakes beneath the Tokyo metropolitan area and are accompanied by earthquake swarms.
Riko Arai, Shiori Watanabe, Yuta Mitsui
wiley +1 more source
The southeast offshore Mie earthquake occurred on April 1, 2016 near the rupture area of the 1944 Tonankai earthquake, where seismicity around the interface of the Philippine Sea plate had been very low until this earthquake.
Shunsuke Takemura +4 more
doaj +1 more source
Abstract Serpentinite plays a major role in the geodynamics of subduction zones. However, the processes by which serpentinite is incorporated into accretionary complexes, and the extent to which it interacts chemically and physically with accretionary lithologies, remain unclear.
Yusuke Shimura +5 more
wiley +1 more source
The physical and chemical processes that occur during the subduction of two converging tectonic plates have significant consequences, contributing to both the growth of the continental crust and the chemical and thermal evolution of the Earth's interior.
Eggins, S., Tatsumi, Y.
core
Abstract Exhumed metamorphic rocks yield critical insights into the mechanical, chemical, and thermal structure of the plate interface that can be used to infer exhumation pathways and their evolution throughout a subduction zone's lifetime. Metamorphosed oceanic rocks often record exhumation and underplating over relatively punctuated time periods ...
Valeria Turino +4 more
wiley +1 more source
Various stress-releasing phenomena, such as episodic tremor and slip (ETS) and low-frequency earthquakes, occur at the downdip seismogenic zone in southwest Japan.
Shaoyang Li, Ling Chen
doaj +1 more source

