Projection of mechanical properties from shallow to greater depths seaward of the Nankai accretionary prism

Author:

Ask Maria V.S.,Morgan Julia K.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference46 articles.

1. A fault model of the 1946 Nankaido earthquake derived from tsunami data;Ando;Physics of the Earth and Planetary Interiors,1982

2. The Mechanics of Soils, an Introduction to Critical State Soil Mechanics;Atkinson,1978

3. Physical properties along the developing decollement in the Nankai Trough; inferences from 3-D seismic reflection data inversion and Leg 190 and 196 drilling data. [online];Bangs,2005

4. Work as a criterion for determining in situ and yield stresses in clays;Becker;Canadian Geotechnical Journal,1987

5. Hydration-phase diagrams and friction of montmorillonite under laboratory and geologic conditions, with implications for shale compaction, slope stability, and strength of fault gouge;Bird;Tectonophysics,1984

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2. 10.14379/iodp.sp.362.2016;International Ocean Discovery Program Scientific Prospectus;2016-04-14

3. Geotechnical behavior of mudstones from the Shimanto and Boso accretionary complexes, and implications for the Nankai accretionary prism;Earth, Planets and Space;2014

4. Subduction Zones;Earth and Life Processes Discovered from Subseafloor Environments - A Decade of Science Achieved by the Integrated Ocean Drilling Program (IODP);2014

5. Mechanical and hydraulic properties of Nankai accretionary prism sediments: Effect of stress path;Geochemistry, Geophysics, Geosystems;2012-10

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