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Compressive and tensile failure at hith fluid pressure where preexisting fractures have cohesive strength, with application to the San Andreas Fault

Author
FOURNIER, R. O1
[1] U.S. Geological Survey, Menlo Park, California, United States
Source

Journal of geophysical research. 1996, Vol 101, Num B11, pp 25499-25509 ; ref : 66 ref

ISSN
0148-0227
Scientific domain
Astronomy earth cosmic environment; Geology; Geophysics; Climatology, meteorology; Oceanography
Publisher
American Geophysical Union, Washington, DC
Publication country
United States
Document type
Article
Language
English
Keyword (fr)
Cicatrisation Cisaillement Distribution contrainte Faille active Faille chevauchement Faille décrochement Fracturation hydraulique Liquide interstitiel Pression charge Pression fluide Pression pores Propagation fissure Résistance mécanique Ténacité Faille San Andreas
Keyword (en)
Cicatrization Shear Stress distribution active faults thrust fault strike-slip faults Hydraulic fracturing Interstitial fluid load pressure fluid pressure Pore pressure Crack propagation Strength Fracture toughness San Andreas Fault
Keyword (es)
Cicatrización Cizalladura Campo restricción Falla activa Cabalgamiento Falla horizontal Fracturación hidraúlica Líquido intersticial Presión carga Presión fluido Presión poros Propagación fisura Resistencia mecánica Tenacidad
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01M Internal geophysics / 001E01M02 Solid-earth geophysics, tectonophysics, gravimetry

Discipline
Earth sciences
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
2500012

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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