Results 141 to 150 of about 141,827 (166)

Tracing Marine Algal and Terrestrial Plant Inputs During Cenozoic Marine Incursions in the Northern Central Myanmar Basin: A Biomarker Perspective. [PDF]

Biology (Basel)
Zhou Z, Shi Y, Yan T, Wang X.
europepmc   +1 more source

Soft-sediment deformation structures in Holocene coastal gravel deposits reveal two 1.8-2.0 ka old M_w > 7.0 earthquakes in southern-central Hispaniola. [PDF]

Sci Rep
Fernández FJ, Pérez Valera F, Escuder-Viruete J.   +2 more
europepmc   +1 more source

Subsurface architecture of the tuina prospect and its relationship to fluid migration in mineral deposit formation. [PDF]

Sci Rep
Jaque-Reyes J, Reyes-Wagner V, Comte D, Peña M, Calle-Gardella D, Leon-Rios S, Roecker SW, Jiménez F, Pichott S.   +8 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

Can restoring tidal wetlands reduce estuarine nuisance flooding of coasts under future sea-level rise? [PDF]

Earths Future
Brand MW, Diefenderfer HL, Cornu C, McKeon M, Janousek CN, Borde AB, Souza T, Keogh M, Brown CA, Bridgham SD.   +9 more
europepmc   +1 more source

Assessing the state of deep-sea biological knowledge and charting a path for scientific research in Barbados. [PDF]

PeerJ
Foster K, Rabone M, Palacios-Abrantes J, Gobin J, Kanhai DK, Vallès H, Amon D.   +6 more
europepmc   +1 more source

The structure and fault activity of the Makran accretionary prism

Journal of Geophysical Research: Solid Earth, 2012
The Makran Subduction Zone has the highest incoming sediment thickness (up to 7.5 km) of any subduction zone. These sediments have formed a wide accretionary prism (~400 km). Seismicity in the Makran is generally low; however the margin experienced an Mw
Timothy Henstock, Lisa C McNeill
exaly   +2 more sources

Identification of the static backstop and its influence on the evolution of the accretionary prism in the Nankai Trough [PDF]

Earth and Planetary Science Letters, 2015
To reveal the origin of a backstop and its influence on the evolution of the accretionary prism, we analyzed reflection seismic data acquired in the Nankai Trough off the Kii Peninsula. The deformation features of the forearc basin sequence show that the
Juichiro Ashi, Gaku Kimura, Takeshi Tsuji   +2 more
exaly   +2 more sources

Deformation of the Nankai Trough inner accretionary prism: The role of inherited structures [PDF]

Geochemistry, Geophysics, Geosystems, 2016
Accretionary prisms commonly grow seaward, with the strata of the inner prism consisting of older, previously accreted outer prism rocks overlain by thick fore-arc basin strata.
Hiroki Sone, María José Jurado, Brian Boston   +2 more
exaly   +2 more sources

Sequence stratigraphy, structural style, and age of deformation of the Malaita accretionary prism (Solomon arc–Ontong Java Plateau convergent zone)

Tectonophysics, 2004
Possibilities for the fate of oceanic plateaus at subduction zones range from complete subduction of the plateau beneath the arc to complete plateau–arc accretion and resulting collisional orogenesis.
Thomas H Shipley
exaly   +2 more sources