Laboratory observations of the effect of geologic discontinuities on hydrofracture propagation
- Other title
- Observations en laboratoire de l'effet des discontinuités géologiques sur la propagation de la fracturation hydraulique (fr)
- Author
- BLAIR, S.C; THORPE, R.K; HEUZE, F.E; SHAFFER, R.J
Livermore national lab., United States - Conference title
- U.S. symposium on rock mechanics : Rock mechanics as a guide for efficient utilization of natural resources. 30
- Conference name
- U.S. symposium on rock mechanics : Rock mechanics as a guide for efficient utilization of natural resources. 30 (1989-06-19)
- Source
U.S. symposium on rock mechanics : Rock mechanics as a guide for efficient utilization of natural resources. 30. 1989, pp 443-450, 8 p ; Illustration ; ref : 3 ref
- Publisher
- A.A. Balkema, Rotterdam
- Publication country
- Netherlands
- Document type
- Conference Paper
- Language
- English
- Keyword (fr)
- Discontinuité Essai laboratoire Fracturation hydraulique Interface Modèle physique Méthode élément fini Propagation
- Keyword (en)
- Discontinuities Discontinuity Laboratory studies Laboratory test Hydraulic fracturing Interfaces Interface Physical models Physical model Finite element analysis Finite element method Propagation
- Keyword (es)
- Discontinuidad Ensayo laboratorio Fracturación hidraúlica Interfase Modelo físico Método elemento finito Propagación
- Classification
- Pascal
- 001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01O Engineering and environment geology. Geothermics / 001E01O01 Engineering geology
- Discipline
- Earth sciences
- Origin
- BRGM
- Database
- PASCAL
- INIST identifier
- 19574405
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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