Mechanical characterization of slope sediments: Constraints on in situ stress and pore pressure near the tip of the megasplay fault in the Nankai accretionary complex
- 25 August 2011
- journal article
- research article
- Published by American Geophysical Union (AGU) in Geochemistry, Geophysics, Geosystems
- Vol. 12 (8)
- https://doi.org/10.1029/2011gc003556
Abstract
No abstract availableKeywords
This publication has 56 references indexed in Scilit:
- Structural restoration of thrusts at the toe of the Nankai Trough accretionary prism off Shikoku Island, Japan: Implications for dewatering processesGeochemistry, Geophysics, Geosystems, 2011
- Slumping and mass transport deposition in the Nankai fore arc: Evidence from IODP drilling and 3‐D reflection seismic dataGeochemistry, Geophysics, Geosystems, 2011
- Interpretation of porosity and LWD resistivity from the Nankai accretionary wedge in light of clay physicochemical properties: Evidence for erosion and local overpressuringGeochemistry, Geophysics, Geosystems, 2011
- In situ stress state in the Nankai accretionary wedge estimated from borehole wall failuresGeochemistry, Geophysics, Geosystems, 2010
- Anelastic strain recovery reveals extension across SW Japan subduction zoneGeophysical Research Letters, 2009
- Consolidation state and strength of underthrust sediments and evolution of the décollement at the Nankai accretionary margin: Results of uniaxial reconsolidation experimentsJournal of Geophysical Research, 2004
- Anisotropy of electrical conductivity record of initial strain at the toe of the Nankai accretionary wedgeJournal of Geophysical Research, 2003
- Pore pressure development and progressive dewatering in underthrust sediments at the Costa Rican subduction margin: Comparison with northern Barbados and NankaiJournal of Geophysical Research, 2003
- Crustal velocity field of southwest Japan: Subduction and arc‐arc collisionJournal of Geophysical Research, 2001
- Mechanics of low‐stress forearcs: Nankai and CascadiaJournal of Geophysical Research, 1999