Results 131 to 140 of about 444 (185)
Seismic loading of fault-controlled fluid seepage systems by great subduction earthquakes. [PDF]
Sci Rep, 2019 Bonini M.
europepmc +1 more source
Subsurface architecture of the tuina prospect and its relationship to fluid migration in mineral deposit formation. [PDF]
Sci RepJaque-Reyes J +8 more
europepmc +1 more source
Rupture access to hydrous minerals controls aftershocks in subduction zones. [PDF]
Sci RepGunatilake T +3 more
europepmc +1 more source
Can restoring tidal wetlands reduce estuarine nuisance flooding of coasts under future sea-level rise? [PDF]
Earths FutureBrand MW +9 more
europepmc +1 more source
Physics-informed deep learning quantifies propagated uncertainty in seismic structure and hypocenter determination. [PDF]
Sci RepAgata R, Shiraishi K, Fujie G.
europepmc +1 more source
Structure and hydrogeology of the Nankai accretionary prism
Structure and hydrogeology of the Nankai accretionary prismopenaire
Some of the next articles are maybe not open access.
Related searches:
Related searches:
Reviews of Geophysics, 1992
Accretionary prisms are composed of initially saturated sediments caught in subduction zone tectonism. As sediments deform, fluid pressures rise and fluid is expelled, resembling a saturated sponge being tectonically squeezed. Fluid flow from the accretionary prism feeds surface biological cases, precipitates and dissolves minerals, and causes ...
J. Casey Moore, Peter Vrolijk
openaire +3 more sources
Accretionary prisms are composed of initially saturated sediments caught in subduction zone tectonism. As sediments deform, fluid pressures rise and fluid is expelled, resembling a saturated sponge being tectonically squeezed. Fluid flow from the accretionary prism feeds surface biological cases, precipitates and dissolves minerals, and causes ...
J. Casey Moore, Peter Vrolijk
openaire +3 more sources
2018
Geodetic observations are commonly used to make inferences about the rheology of the lower crust and mantle, frictional properties of faults, and the structure of the Earth following an earthquake. On 24 September 2013, an Mw 7.7 earthquake ruptured a 200 km segment of the Hoshab fault in southern Pakistan.
Katherine Elizabeth Peterson +3 more
openaire +1 more source
Geodetic observations are commonly used to make inferences about the rheology of the lower crust and mantle, frictional properties of faults, and the structure of the Earth following an earthquake. On 24 September 2013, an Mw 7.7 earthquake ruptured a 200 km segment of the Hoshab fault in southern Pakistan.
Katherine Elizabeth Peterson +3 more
openaire +1 more source
Sediment dewatering in the Makran accretionary prism
Earth and Planetary Science Letters, 1985Abstract Sediments within the Makran accretionary prism are considerably more compacted than the material entering the subduction zone due to the additional tectonic stresses resulting from plate convergence and accretionary processes. Tectonic compaction of the offscraped sediments has been documented by deriving in-situ porosities in the upper 4 km
Susan R. Fowler +2 more
openaire +1 more source
Mineralogically mature sandstones in accretionary prisms
Journal of Sedimentary Research, 1985Abstract Plate-tectonic interpretations of sandstone composition are made in the hope that "detrital framework modes of sandstone suites provide information about the tectonic setting of basins of deposition and associated provenances" (Dickinson et al. 1983).
openaire +1 more source