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Par Collection Par Auteur- GILL, D., (Editeur scientifique) (4)
- MERRIAM, D. F., (Editeur scientifique) (4)
- DENEKAMP, S. A. (1)
- MERRIAM, D. F. (1)
- ARNON, B. (1)
- NISHIWAKI, N. (1)
- RIBEIRO, J. C. (1)
- TSUR-LAVIE, Y. (1)
- 1979 (4)
- Physical geography (4)
- Analyse de régression multiple ; Analyse multivariée ; Brésil ; Crétacé ; Ere tertiaire ; Géographie physique ; Reconcavo, bassin ; Stratigraphie ; Surfaces de tendance ; Tectonique (1)
- Analyse quantitative ; Donnée informatique ; Géographie physique ; Lithologie ; Mathématique ; Milieu de dépôt ; Programme FORTRAN ; Stratification ; Structure sédimentaire ; Sédimentaire ; Sédimentologie (1)
- Diapirisme ; Géographie physique ; Géomorphologie structurale ; Halocinèse ; Modèle ; Méthode de déplacement des limites ; Simulation ; Stratigraphie ; Tectonique (1)
- Géographie physique ; Loi de Poisson ; Modèle ; Modèle stochastique ; Méthode Monte Carlo ; Statistique ; Sédimentation ; Sédimentologie ; Taux de sédimentation ; Turbidité (1)
- Analysis of stress and deformation around a diapiric intrusion in Geomathematical and petrophysical studies in Sedimentology. An international Symposium. (1)
- Quantitative analysis of depositional environments (Aratu Unit, Reconcavo Series, Lower Cretaceous) in the Reconcavo Basin, Bahia, Brazil in Geomathematical and petrophysical studies in Sedimentology. An international Symposium. (1)
- Recognizing terrigenous depositional environments with the aid of the computer in Geomathematical and petrophysical studies in Sedimentology. An international Symposium. (1)
- Simulation of bed-thickness distribution based ou waiting time in the Poisson process in Geomathematical and petrophysical studies in Sedimentology. An international Symposium. (1)
- A numerical model for the evaluation of deformation and stress associated with geological structures is presented. The method is based on a fundamental solution of stress and deformation around a single rectangular indentation at the boundary
- of an infinite, elastic half-plane. Groups of indentation of different shape, define displacement boundary conditions representing forms of geological structures. The method is demonstrated by a solution of deformation and stress around a nonpiercing diapiric
- A FORTRAN program designed to simplify and duplicate the mental processes which lead to an interpretation of a depositional setting is presented. In order to simplify the geologic interpretation of clastic depositional environments, seven general
- Regression and trend surface analyses were used to facilitate interpretation of geological history of a stratigraphic interval of the Aratu Unit, Reconcavo Series (Lower Cretaceous) in the Reconcavo Basin, Bahia State, Brazil. The relation between
- simulation models, incorporating additional geological parameters, are required.