Results 151 to 160 of about 1,202,006 (199)

Frictional instabilities in clay illuminate the origin of slow earthquakes. [PDF]

Sci Adv
Volpe G, Collettini C, Taddeucci J, Marone C, Pozzi G.   +4 more
europepmc   +1 more source

Geochemical and Isotopic Evidence for Fluid Flow in the Western Nankai Subduction Zone, Japan

, 1993
M. Kastner, H. Elderfield, W.J. Jenkins, J.M. Gieskes, T. Gamo   +4 more
openaire   +1 more source

A pressure solution flow law for the seismogenic zone: Application to Cascadia. [PDF]

Sci Adv
Fisher DM, Hirth G.
europepmc   +1 more source

Subducting plate structure and megathrust morphology from deep seismic imaging linked to earthquake rupture segmentation at Cascadia. [PDF]

Sci Adv
Carbotte SM, Boston B, Han S, Shuck B, Beeson J, Canales JP, Tobin H, Miller N, Nedimovic M, Tréhu A, Lee M, Lucas MC, Jian H, Jiang D, Moser L, Anderson C, Judd D, Fernandez J, Campbell C, Goswami A, Gahlawat R.   +20 more
europepmc   +1 more source

Multimodal Non-Extensive Frequency-Magnitude Distributions and Their Relationship to Multi-Source Seismicity. [PDF]

Entropy (Basel)
de la Barra E, Vega-Jorquera P, da Silva SLEF.   +2 more
europepmc   +1 more source

Gravity-induced seismicity modulation on planetary bodies and their natural satellites. [PDF]

Sci Rep
Senapati B, Kundu B, Jha B, Jin S.
europepmc   +1 more source

Perturbation-induced granular fluidization as a model for remote earthquake triggering. [PDF]

Sci Adv
Farain K, Bonn D.
europepmc   +1 more source

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Geological characteristics of the Nankai Trough subduction zone and their tectonic significances

Acta Oceanologica Sinica, 2020
The Nankai Trough subduction zone is a typical subduction system characterized by subduction of multiple geological units of the Philippine Sea Plate (the Kyushu-Palau Ridge, the Shikoku Basin, the Kinan Seamount Chain, and the Izu-Bonin Arc) beneath the Eurasian Plate in the southwest of Japan.
limei Tang
exaly   +2 more sources

Origin of a zone of anomalously high porosity in the subduction inputs to Nankai Trough

Marine Geology, 2015
Abstract One poorly understood feature of the subduction inputs to the Nankai Trough subduction zone (SW Japan) is a stratigraphic interval with an anomalously high porosity zone (HPZ), which is up to 240 m thick and located within the clay- and volcanic ash-rich Shikoku Basin facies.
Brandon Dugan, M B Underwood
exaly   +2 more sources