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Contient 11 articles : Note giudicariensi III - 1) La struttura geologica attorno alla Linea delle Giudicarie. 1b) La struttura geologica a levante della linea delle Giudicarie. ; Sedimentazione e tettonica delle unità liguridi nell'Appennino N[...]Livre
Daniel J. STANLEY ; George T. Moore | TULSA : SOCIETY OF ECONOMIC PALEONTOLOGISTS AND MINERALOGISTS | 1983The shelfbreak is that point where the first major change in gradient occurs on the outermost edge of the continental shelf. Although this environment delimits the boundary between two principal and well-defined provinces, the continental shelf [...]Bulletin : Revue
Mémoires de la société géologique de France - nouvelle série, tome LXI, n°144 - Transition eaux douces-eaux salées : sédimentologie, géochimie, écologie
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* INTRODUCTION * HISTOIRE TECTONIQUE NEOGENE ET QUATERNAIRE * MORPHOLOGIE * LES FACTEURS DE LA SEDIMENTATION * LES SEDIMENTS * LES TAPHOCOENOSES * L'HISTOIRE DES RECIFS CORALLIENS QUATERNAIRES DE LA NOUVELLE CALEDONIE DEDUITE DE L'ETUDE DU FORAG[...]Thèse-Mémoire
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International association of sedimentologists | International association of sedimentologists | 1980Contents : 1. Classic sediments; 1.1 Methods; 1.2 Sedimentary structures and textures; 1.3 Depositional environments; 1.4 Tectofacies; 1.5 Weathering and diagenesis. - 2. Carbonate sediments; 2.1 Composition; 2.2 Depositional environments; 2.3 D[...]Thèse-Mémoire
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This book has been written with the aim of compiling from modern environments information that can be useful in the reconstruction of ancient environments. It is intended for all those interested in recognizing depositional environments. The stu[...]Livre
Cet ouvrage regroupe un grand nombre d'informations concernant les paléoenvironnements de dépôts sédimentaires et étudie les différents aspects des sédiments. Une importante bibliographie est proposée. Sommaire : PART 1 PRIMARY STRUCTURES AND T[...]Livre
Larry J. DOYLE ; Orrin H. Pilkey | TULSA : SOCIETY OF ECONOMIC PALEONTOLOGISTS AND MINERALOGISTS | 1979Continental slopes are the edges of continental blocks, the zones of change from continental crust to oceanic crust. They are critical links in the chain of sedimentary processes that eventually carry sediment to the true ocean basin floor. Spur[...]Thèse-Mémoire
UNIVERSITE CATHOLIQUE DE LOUVAIN ; P. PIESSENS | LOUVAIN LA NEUVE : UNIVERSITE CATHOLIQUE DE LOUVAIN | 1979* LE MILIEU PHYSIQUE * LES SEDIMENTS * COMPOSITION DE LA FRACTION SABLEUSE * INTERPRETATION * COMPARAISON AVEC D'AUTRES REGIONS * CONCLUSIONSLivre
1/ PRELIMINARY CONSIDERATIONS 2/ CLASSICAL MODELS 3/ THE OCEANIC RECORD 4/ CLASSIFICATION 5/ GEOCHRONOMETRIC DATING 6/ THE FOSSIL RECORD 7/ SEA LEVEL 8/ GLACIATION 9/ NONGLACIAL ENVIRONMENTS 10/ OVERVIEWLivre
JACQUES FLANDRIN | LYON : UNIVERSITE CLAUDE BERNARD | DOCUMENTS DES LABORATOIRES DE GEOLOGIE DE LA FACULTE DES SCIENCES DE LYON | 1978Livre jubilaire Jacques Flandrin.Livre
It has become increasingly important to better understand deep marine environments and their transitions to shoal water settings. Of importance are the processes operating in deep-water settings and the magnitude and periodicity of these process[...]Thèse-Mémoire
Etude des marques de courant par photographie sous-marine (organisation et gestion d'une phototèque)
SOMMAIRE: Liste des planches.