Consolidation state and strength of underthrust sediments and evolution of the décollement at the Nankai accretionary margin: Results of uniaxial reconsolidation experiments-Reference-Cited by-同舟云学术

Consolidation state and strength of underthrust sediments and evolution of the décollement at the Nankai accretionary margin: Results of uniaxial reconsolidation experiments

Published:2004 Issue:B3 Volume:109 Page:
ISSN:0148-0227
Container-title:Journal of Geophysical Research
language:en
Short-container-title:J. Geophys. Res.

Author:

Morgan Julia K.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference83 articles.

1. Mechanical tests on claystone from Ocean Drilling Program Hole 1070A (Leg 173): Implications for elevated pore-fluid pressure in sediments within the ocean-continent transition zone, West Iberia;Ask;Mar. Geol.,2001

2. Density, porosity, and compaction of sedimentary rocks;Athy;Am. Assoc. Pet. Geol. Bull.,1930

3. Evolution of the décollement from the trench into the seismogenic zone inferred from mapping Nankai Trough décollement seismic reflections in 3-D, Muroto Transect;Bangs;Geology

4. A simplified analysis of parameters controlling dewatering in accretionary prisms;Bekins;Earth Planet. Sci. Lett.,1992

5. Porosity of sediments in accretionary prisms and some implications for dewatering processes;Bray;J. Geophys. Res.,1985

Cited by 41 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Subduction Zone Interface Structure Within the Southern M _W 9.2 1964 Great Alaska Earthquake Asperity: Constraints From Receiver Functions Across a Spatially Dense Node Array;Geophysical Research Letters;2022-08-12

2. Subduction Zone Interface Structure within the Southern MW9.2 1964 Great Alaska Earthquake Asperity: Constraints from Receiver Functions Across a Spatially Dense Node Array;2022-02-25

3. Pore Pressure Regime and Fluid Flow Processes in the Shallow Nankai Trough Subduction Zone Based on Experimental and Modeling Results from IODP Site C0023;Journal of Geophysical Research: Solid Earth;2021-02

4. Pore Fluid Pressures and Strength Contrasts Maintain Frontal Fault Activity, Northern Hikurangi Margin, New Zealand;Geophysical Research Letters;2020-11-05

5. Conceptual consideration and outcrop interpretation on early stage deformation of sand and mud in accretionary prisms for chaotic deposit formation;Gondwana Research;2019-10