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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   +5 more sources

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   +2 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

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

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

Hydro-bio-geomechanical properties of hydrate-bearing sediments from Nankai Trough [PDF]

open access: yesMarine and Petroleum Geology, 2015
This paper is not subject to U.S. copyright. The definitive version was published in Marine and Petroleum Geology 66 (2015): 434-450, doi:10.1016/j.marpetgeo.2015.02.033.Natural hydrate-bearing sediments from the Nankai Trough, offshore Japan, were ...
J Carlos Santamarina   +2 more
exaly   +3 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

Estimation of Minimum Principal Stress from an Extended Leak-off Test Onboard the Chikyu Drilling Vessel and Suggestions for Future Test Procedures [PDF]

open access: yesScientific Drilling, 2008
To understand the physics of faulting and rupture propagation for the great M8-class Nankai earthquakes that recur approximately every 100 years, a comprehensive drilling project is underway: the Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE ...
Hideki Masago   +4 more
doaj   +1 more source

A review of shallow slow earthquakes along the Nankai Trough

open access: yesEarth, Planets and Space, 2023
Slow earthquakes occur at deep and shallow plate boundaries along the Nankai Trough. Deep slow earthquakes are continuously distributed along the 30–40 km depth contours of the upper surface of the subducted Philippine Sea Plate.
Shunsuke Takemura   +7 more
doaj   +1 more source

DONET: A Real-Time Monitoring System for Megathrust Earthquakes and Tsunamis Around Southwestern Japan [PDF]

open access: yesOceanography, 2014
DONET (Dense Ocean floor Network for Earthquakes and Tsunamis; https://www.jamstec.go.jp/donet/e/index.html) is a cabled seafloor observatory that monitors the Nankai and Tōnankai seismogenic zones, offshore southwestern Japan, in real time. In 1944, two
Yoshiyuki Kaneda
doaj   +1 more source

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