Results 131 to 140 of about 468 (176)

Coral geochemical response to uplift in the aftermath of the 2005 Nias-Simeulue earthquake. [PDF]

Sci Rep
Sosdian SM, Gagan MK, Natawidjaja DH, Kimbrough AK, Suwargadi BW, Rifai H, Scott-Gagan H, Prayudi D, Suprihanto I, Hantoro WS.   +9 more
europepmc   +1 more source

Ultra-low friction graphene oxide in the Atotsugawa Fault System. [PDF]

Nat Commun
Shimada T, Nagahama H, Muto J, Nakamura N, Sawa S, Ohfuji H.   +5 more
europepmc   +1 more source

Seafloor geodesy unveils seismogenesis of large subduction earthquakes in Mexico. [PDF]

Sci Adv
Cruz-Atienza VM, Tago J, Domínguez LA, Kostoglodov V, Ito Y, Ovando-Shelley E, Rodríguez-Nikl T, González R, Franco S, Solano-Rojas D, Beltrán-Gracia J, Miranda-García P, Boudin F, Rivera L, Bécel A, Villafuerte C, Real J, Kazachkina E, Ronquillo A.   +18 more
europepmc   +1 more source

Source Models of the 2016 and 2022 Menyuan Earthquakes and Their Tectonic Implications Revealed by InSAR. [PDF]

Sensors (Basel)
Bai X, Zhang B, Guo A, Yan Y, Xu H, Bian X, Zhan S, Chen J.   +7 more
europepmc   +1 more source

Rupture access to hydrous minerals controls aftershocks in subduction zones. [PDF]

Sci Rep
Gunatilake T, Gerya T, Connolly JAD, Miller SA.   +3 more
europepmc   +1 more source

Interseismic crustal deformation in and around the Japanese islands as deduced from GPS observations

, 1999
openaire   +1 more source

Bias in estimates of lithosphere viscosity from interseismic deformation [PDF]

Geophysical Research Letters, 2013
The estimation of uniform viscosities representing the lower crust and uppermost mantle from postseismic or interseismic deformation (i.e., apparent viscosities) is inherently biased with respect to a depth dependence of the viscosities within each layer.
Eric A Hetland
exaly   +3 more sources

A revised dislocation model of interseismic deformation of the Cascadia subduction zone [PDF]

Journal of Geophysical Research, 2003
CAS3D‐2, a new three‐dimensional (3‐D) dislocation model, is developed to model interseismic deformation rates at the Cascadia subduction zone. The model is considered a snapshot description of the deformation field that changes with time. The effect of northward secular motion of the central and southern Cascadia forearc sliver is subtracted to obtain
Kelin Wang, Takeshi Sagiya, Stéphane Mazzotti   +2 more
exaly   +2 more sources

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High-Pressure Creep of Serpentine, Interseismic Deformation, and Initiation of Subduction

Science, 2007
The supposed low viscosity of serpentine may strongly influence subduction-zone dynamics at all time scales, but until now its role could not be quantified because measurements relevant to intermediate-depth settings were lacking. Deformation experiments on the serpentine antigorite at high pressures and temperatures (1 to 4 gigapascals, 200° to 500°C)
Hilairet, N., Reynard, Bruno, Wang, Y., Daniel, I., Merkel, S., Nishiyama, N., Petitgirard, S.   +6 more
openaire   +6 more sources

A plate flexure approximation to postseismic and interseismic deformation

Journal of Geophysical Research: Solid Earth, 1985
The rather large postseismic deformation that is associated with two‐dimensional dip‐slip faulting in the lithosphere is related to the bending of a free plate generated by dip‐slip faulting. In the absence of gravity, asthenosphere relaxation eventually permits the faulted lithosphere to assume the dihedral configuration of a faulted free plate.
J. C. Savage, Guohua Gu
openaire   +1 more source