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Time-dependent deformation of shale gas reservoir rocks and its long-term effect on the in situ state of stress

Author
SONE, Hiroki1 ; ZOBACK, Mark D2
[1] CFZ German Research Centre for Geosciences, Telegrafenberg, Potsdam 14473, Germany
[2] Department of Geophysics, Stanford University, Stanford, CA 94305, United States
Source

International journal of rock mechanics and mining sciences (1997). 2014, Vol 69, pp 120-132, 13 p ; ref : 28 ref

ISSN
1365-1609
Scientific domain
Civil engineering; Geology; Geophysics
Publisher
Elsevier, Oxford
Publication country
United Kingdom
Document type
Article
Language
English
Author keyword
Creep Gas Shale Viscoelasticity in situ stress
Keyword (fr)
Contrainte in situ Déformation Dépendance du temps Equation constitutive Essai laboratoire Etude expérimentale Evaluation performance Fluage Long terme Mécanique roche Roche magasin Shale Viscoélasticité
Keyword (en)
In situ stress Deformation Time dependence Constitutive equation Laboratory test Experimental study Performance evaluation Creep Long term Rock mechanics Reservoir rock Shale Viscoelasticity
Keyword (es)
Tensión in situ Deformación Dependencia del tiempo Ecuación constitutiva Ensayo laboratorio Estudio experimental Evaluación prestación Fluencia Largo plazo Mecánica roca Roca reservorio Pizarra no metamórfica Viscoelasticidad
Classification
Pascal
001 Exact sciences and technology / 001D Applied sciences / 001D14 Buildings. Public works / 001D14F Geotechnics / 001D14F02 Soil mechanics. Rocks mechanics

Discipline
Building. Public works. Transport. Civil engineering
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
28472505

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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