Results 1 to 10 of about 95,452 (164)

A b map implying the first eastern rupture of the Nankai Trough earthquakes [PDF]

open access: yesNature Communications, 2018
Earthquakes generated from the Nankai Trough have caused much devastation over the years. Here, the authors present a b-value map for the Nankai Trough zone, where the Eastern part of the trough has lower b-values than the West, which may help to explain
K. Z. Nanjo, A. Yoshida
doaj   +3 more sources

Topography of the subducting basement throughout the entire Nankai Trough [PDF]

open access: yesScientific Reports
The heterogeneous distributions of large and slow earthquakes in subduction zones are caused by multiple uncertain conditions in the source regions, and the basement topography is considered one of the major controlling factors.
Kazuya Shiraishi   +9 more
doaj   +2 more sources

IODP Expedition 333: Return to Nankai Trough Subduction Inputs Sites and Coring of Mass Transport Deposits [PDF]

open access: yesScientific Drilling, 2012
Integrated Ocean Drilling Program (IODP) Expedition 333 returned to two sites drilled during IODP Expedition 322 on the ocean side of the Nankai Trough to pursue the characterization of the inputs to the Nankai subduction and seismogenic zone, as part of
Michael Strasser   +4 more
doaj   +4 more sources

Numerical modeling of subduction and evaluation of Philippine Sea Plate tectonic history along the Nankai Trough [PDF]

open access: yesScientific Reports, 2023
The subduction of the Philippine Sea (PHS) plate along the Nankai Trough in in southwest Japan is a relatively recent process compared with subduction along the Japan Trench in northeast Japan.
E. J. Moreno   +5 more
doaj   +2 more sources

Biological surveys reveal unexpectedly high faunal diversity at Nankai Trough methane seeps

open access: yesEcosphere
Cold seeps are chemosynthesis‐based ecosystems powered by microbial primary production that support diverse and specialized faunal assemblages in the deep sea. Despite Nankai Trough in Japan being a geologically active margin hosting numerous seeps, much
Chong Chen   +6 more
doaj   +2 more sources

Thick slab crust with rough basement weakens interplate coupling in the western Nankai Trough

open access: yesEarth, Planets and Space
The westernmost Nankai Trough, southwest Japan, exhibits a rapid along-strike reduction in plate coupling in the proximity to the subducting Kyushu-Palau ridge. Yet how and to what extent the ridge subduction impacts physical properties at the megathrust
Ryuta Arai   +14 more
doaj   +2 more sources

Detailed Shallow Shear Velocity Structure in the Nankai Trough From Ambient Noise Differential Adjoint Tomography: Implications for Earthquake Generation Mechanisms

open access: yesGeophysical Research Letters
Seismic and aseismic slip has been reported in the Nankai Trough. In this study we apply ambient noise differential adjoint tomography to obtain a high‐resolution S‐wave velocity (Vs) model in the Nankai Trough.
Lina Gao   +6 more
doaj   +2 more sources

Link between the Nankai underthrust turbidites and shallow slow earthquakes [PDF]

open access: yesScientific Reports, 2023
Trench sediments such as pelagic clay or terrigenous turbidites have long been invoked to explain the seismogenic behavior of the megathrust fault (i.e., décollement).
Jin-Oh Park, Ehsan Jamali Hondori
doaj   +2 more sources

Thermogenic methane and hydrogen generation in subducted sediments of the Nankai Trough

open access: yesCommunications Earth & Environment
Active and widespread CH4 accumulations and emissions in the Nankai Trough subduction zone are attested by numerous mud volcanoes, gas plumes, and gas hydrates containing biogenic and thermogenic CH4.
Noriyuki Suzuki   +3 more
doaj   +2 more sources

Muroto Project: Scientifi c Drilling of the Late Pliocene Forearc Basin Deposit on the West Coast of Muroto Peninsula, Shikoku, Japan [PDF]

open access: yesScientific Drilling, 2006
The Muroto Peninsula on the Pacifi c margin of southwest Japan (Fig.1) formed as a result of tectonic events associated with oblique subduction along the Nankai Trough (Sugiyama, 1992, 1994). Late Pliocene forearc basin deposits of the Tonohama Group are
Kazuto Kodama, Masao Iwai, Yasuo Kondo
doaj   +1 more source

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