Consolidation state and strength of underthrust sediments and evolution of the décollement at the Nankai accretionary margin: Results of uniaxial reconsolidation experiments
- 9 March 2004
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 109 (B3)
- https://doi.org/10.1029/2002jb002335
Abstract
No abstract availableKeywords
This publication has 67 references indexed in Scilit:
- 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
- New insights into deformation and fluid flow processes in the Nankai Trough accretionary prism: Results of Ocean Drilling Program Leg 190Geochemistry, Geophysics, Geosystems, 2001
- Mechanical tests on claystone from Ocean Drilling Program Hole 1070A (Leg 173) — implications for elevatedpore-fluid pressure in sediments within the ocean–continent transition zone, West IberiaMarine Geology, 2001
- Episodic fluid flow in the Nankai accretionary complex: Timescale, geochemistry, flow rates, and fluid budgetJournal of Geophysical Research, 1998
- Kinematics and a balanced and restored cross-section across the toe of the eastern Nankai accretionary prismJournal of Structural Geology, 1995
- Velocity and inferred porosity model of the Oregon accretionary prism from multichannel seismic reflection data: Implications on sediment dewatering and overpressureJournal of Geophysical Research, 1994
- Fluids in accretionary prismsReviews of Geophysics, 1992
- Tectonics and hydrogeology of accretionary prisms: role of the décollement zoneJournal of Structural Geology, 1989
- The application of stress path and critical state analysis to sediment deformationJournal of Structural Geology, 1986
- A Comparison of Marine Clays from Ariake Bay, Japan and the South Nation River Landslide Site, CanadaSoils and Foundations, 1984