Man

Masataka Kinoshita

Professor, Ph.D.

The University of Tokyo

Tokyo, Japón

Líneas de Investigación


Marine Geophysic , Heat Flow, Natural Resources, Geofluids

Educación

  •  Geofisica, UNIVERSITY OF TOKYO. Japón, 1990

Experiencia Académica

  •   Professor Full Time

    UNIVERSITY OF TOKYO

    Tokyo, Japón

    2015 - A la fecha

  •   Deputy Director Full Time

    Japan Agency for Marine-Earth Sci. Tech.

    Tokyo, Japón

    2015 - 2016


 

Article (20)

Geometrical dependence on the stress and slip tendency acting on the subduction megathrust of the Nankai seismogenic zone off Kumano
Thermal maturity structures in an accretionary wedge by a numerical simulation
Constraints on the fluid supply rate into and through gas hydrate reservoir systems as inferred from pore-water chloride and in situ temperature profiles, Krishna-Godavari Basin, India
Equivalent formation strength as a proxy tool for exploring for the location and distribution of gas hydrates
Examination of gas hydrate-bearing deep ocean sediments by X-ray Computed Tomography and verification of physical property measurements of sediments
In-situ mechanical weakness of subducting sediments beneath a plate boundary décollement in the Nankai Trough
Origin of low-chloride fluid in sediments from the eastern continental margin of India, results from the National Gas Hydrate Program Expedition 02
Porosity, permeability, and grain size of sediment cores from gas-hydrate-bearing sites and their implication for overpressure in shallow argillaceous formations: Results from the national gas hydrate program expedition 02, Krishna-Godavari Basin, India
Repeated large-scale mass-transport deposits and consequent rapid sedimentation in the western part of the Bay of Bengal, India
Strength characteristics of sediments from a gas hydrate deposit in the Krishna–Godavari Basin on the eastern margin of India
The vertical chloride ion profile at the IODP Site C0002, Kumano Basin, off coast of Japan
Distribution of stress state in the Nankai subduction zone, southwest Japan and a comparison with Japan Trench
Near-trench slip potential of megaquakes evaluated from fault properties and conditions
In situ thermal excursions detected in the Nankai Trough forearc slope sediment at IODP NanTroSEIZE Site C0008
Q(P) structure of the accretionary wedge in the Kumano Basin, Nankai Trough, Japan, revealed by long-offset walk-away VSP
Gas hydrate saturation at Site C0002, IODP Expeditions 314 and 315, in the Kumano Basin, Nankai trough
Geological structure of the offshore Sumatra forearc region estimated from high-resolution MCS reflection survey
Re-evaluation of temperature at the updip limit of locked portion of Nankai megasplay inferred from IODP Site C0002 temperature observatory
Thermal conductivities, thermal diffusivities, and volumetric heat capacities of core samples obtained from the Japan Trench Fast Drilling Project (JFAST)
Tracing geologically constrained fluid flow pathways using a combination of heat flow measurements, pore water chemistry, and acoustic imaging near the deformation front of the Nankai Trough off the Muroto Peninsula, Japan

BookSection (2)

Thermal conductivity changes in subducting basalt, Nankai subduction zone, SW Japan: An estimation from laboratory measurements under separate high-pressure and high-temperature conditions
Seismogenic processes revealed through the Nankai Trough Seismogenic Zone Experiments; core, log, geophysics, and observatory measurements
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Masataka Kinoshita

Professor, Ph.D.

Earthquake Research Institute

The University of Tokyo

Tokyo, Japón