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The impact of megasplay faulting and permeability contrasts on Nankai Trough subduction zone pore pressures

Author
SCREATON, Elizabeth J1 ; GE, Shemin2
[1] Department of Geology, University of Florida, Gainesville, Florida, United States
[2] Department of Geological Sciences, University of Colorado Boulder, Boulder, Colorado, United States
Source

Geophysical research letters. 2012, Vol 39, Num 22 ; L22301.1-L22301.6 ; ref : 3/4 p

CODEN
GPRLAJ
ISSN
0094-8276
Scientific domain
Astronomy earth cosmic environment; Geophysics; Climatology, meteorology; Oceanography
Publisher
American Geophysical Union, Washington, DC
Publication country
United States
Document type
Article
Language
English
Keyword (fr)
Argile Compartiment supérieur Compression Déformation Ecoulement Faille Glissement Modèle Perméabilité Pression interstitielle Prisme accrétion Simulation Surrection Turbidites Vitesse Zone faillée Zone subduction Fosse Nankai Roche clastique Roche sédimentaire Océan Pacifique Nord Ouest Océan Pacifique Nord Océan Pacifique
Keyword (en)
clay hanging wall compression deformation Flow(fluid) faults slip models permeability pore pressure accretionary wedges simulation uplifts turbidites velocity fault zones subduction zones Nankai Trough clastic rocks sedimentary rocks Northwest Pacific North Pacific Pacific Ocean
Keyword (es)
Arcilla Compresión Flujo Quebrado Modelo Permeabilidad Presión poros Simulación Turbidita Velocidad Zona falla Zona subducto Roca clástica Roca sedimentaria Océano Pacífico
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences

Discipline
Earth sciences
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
26755429

Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS

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