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Morgan, Julia K. (2004) Consolidation state and strength of underthrust sediments and evolution of the décollement at the Nankai accretionary margin: Results of uniaxial reconsolidation experiments. Journal of Geophysical Research, 109. doi:10.1029/2002jb002335

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Reference TypeJournal (article/letter/editorial)
TitleConsolidation state and strength of underthrust sediments and evolution of the décollement at the Nankai accretionary margin: Results of uniaxial reconsolidation experiments
JournalJournal of Geophysical Research
AuthorsMorgan, Julia K.Author
Year2004Volume109
PublisherAmerican Geophysical Union (AGU)
DOIdoi:10.1029/2002jb002335Search in ResearchGate
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Mindat Ref. ID858488Long-form Identifiermindat:1:5:858488:9
GUID0
Full ReferenceMorgan, Julia K. (2004) Consolidation state and strength of underthrust sediments and evolution of the décollement at the Nankai accretionary margin: Results of uniaxial reconsolidation experiments. Journal of Geophysical Research, 109. doi:10.1029/2002jb002335
Plain TextMorgan, Julia K. (2004) Consolidation state and strength of underthrust sediments and evolution of the décollement at the Nankai accretionary margin: Results of uniaxial reconsolidation experiments. Journal of Geophysical Research, 109. doi:10.1029/2002jb002335
In(2004) Journal of Geophysical Research Vol. 109. American Geophysical Union (AGU)

See Also

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Morgan, Julia K., Karig, Daniel E. (1995) Décollement processes at the Nankai accretionary margin, southeast Japan: Propagation, deformation, and dewatering. Journal of Geophysical Research: Solid Earth, 100. 15221-15231 doi:10.1029/95jb00675
Saffer, Demian M. (2003) Pore pressure development and progressive dewatering in underthrust sediments at the Costa Rican subduction margin: Comparison with northern Barbados and Nankai. Journal of Geophysical Research: Solid Earth, 108. doi:10.1029/2002jb001787
Ujiie, Kohtaro (2003) Deformation and fluid pressure variation during initiation and evolution of the plate boundary décollement zone in the Nankai accretionary prism. Journal of Geophysical Research, 108. doi:10.1029/2002jb002314
Morgan, Julia K., Karig, Daniel E., Maniatty, Antoinette (1994) The estimation of diffuse strains in the toe of the western Nankai accretionary prism: A kinematic solution. Journal of Geophysical Research, 99. 7019 doi:10.1029/93jb03367
Hüpers, A., Kopf, A.J. (2009) The thermal influence on the consolidation state of underthrust sediments from the Nankai margin and its implications for excess pore pressure. Earth and Planetary Science Letters, 286 (1) 324-332 doi:10.1016/j.epsl.2009.05.047
Guo, Yonggui, Morgan, Julia K. (2007) Fault gouge evolution and its dependence on normal stress and rock strength—Results of discrete element simulations: Gouge zone properties. Journal of Geophysical Research, 112. doi:10.1029/2006jb004524
Skarbek, Robert M., Saffer, Demian M. (2009) Pore pressure development beneath the décollement at the Nankai subduction zone: Implications for plate boundary fault strength and sediment dewatering. Journal of Geophysical Research, 114. doi:10.1029/2008jb006205
Guo, Yonggui, Morgan, Julia K. (2008) Fault gouge evolution and its dependence on normal stress and rock strength-Results of discrete element simulations: Gouge zone micromechanics. Journal of Geophysical Research: Solid Earth, 113. doi:10.1029/2006jb004525
Gamage, K., Screaton, E. (2006) Characterization of excess pore pressures at the toe of the Nankai accretionary complex, Ocean Drilling Program sites 1173, 1174, and 808: Results of one-dimensional modeling. Journal of Geophysical Research, 111. doi:10.1029/2004jb003572
French, Melodie E., Morgan, Julia K. (2020) Pore Fluid Pressures and Strength Contrasts Maintain Frontal Fault Activity, Northern Hikurangi Margin, New Zealand. Geophysical Research Letters, 47 (21) doi:10.1029/2020gl089209
Yuan, T., Spence, G. D., Hyndman, R. D. (1994) Seismic velocities and inferred porosities in the accretionary wedge sediments at the Cascadia margin. Journal of Geophysical Research: Solid Earth, 99. 4413-4427 doi:10.1029/93jb03203
 
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