Résultats de la recherche (8 résultats)
- > VELLA, P., (Editeur scientifique) (supprimer)
Affinez votre recherche
Par Collection Par Auteur- CRESSWELL, M. M., (Editeur scientifique) (8)
- VELLA, P., (Editeur scientifique) (8)
- ADAMS, C. J. (1)
- ANDREWS, P. B. (1)
- GLEADOW, A. J. W. (1)
- GREGORY, M. R. (1)
- HEMING, R. F. (1)
- LOVERING, J. F. (1)
- MUSACCHIO, E. (1)
- SAMESHIMA, T. (1)
- SHRIVASTAVA, B. B. P. (1)
- VOLKHEIMER, W. (1)
- BALLANCE, P. F. (1)
- BASU, T. N. (1)
- BRADSHAW, J. D. (1)
- MORLEY, M. E. (1)
- ROSENFELD, U. (1)
- SPORLI, K. B. (1)
- VOLKHEIMER, W. (1)
- WOPFNER, H. (1)
- 1981 (8)
- Geography of Oceania (4)
- Geography of America (2)
- Andes ; Argentine ; Gondwana ; Géographie de l'Amérique ; Micropaléontologie ; Mésozoïque ; Palynologie ; Paléobiogéographie ; Paléogéographie (1)
- Apatite ; Australie ; Cristallin ; Datation ; Flux de chaleur ; Granite ; Géographie physique ; Mésozoïque ; Paléozoïque ; Rifting ; Tectonique globale ; Trace de fission (1)
- Argentine ; Bassin sédimentaire ; Géographie de l'Amérique ; Jurassique ; Mésozoïque ; Neuquén ; Paléogéographie ; Turbidite (1)
- Australie ; Bassin intracratonique ; Bassin sédimentaire ; Géographie de l'Océanie ; Géomorphologie structurale ; Paléogéographie ; Paléozoïque ; Permien (1)
- Bassin sédimentaire ; Gondwana ; Géographie de l'Asie ; Inde ; Mésozoïque ; Paléozoïque ; Permo-Trias ; Structure ; Tectonique (1)
- Calcaire à fusulinidés ; Gondwana ; Géographie de l'Océanie ; Nouvelle-Zélande ; Paléogéographie ; Paléozoïque ; Permien ; Tethys (1)
- Crétacé ; Gondwana ; Géographie de l'Océanie ; Géomorphogenèse ; Mésozoïque ; Nouvelle-Zélande ; Orogenèse ; Orogène de Rangitata ; Paléogéographie ; Paléozoïque ; Rangitata orogen ; Tectonique globale (1)
- Geography of Asia (1)
- Gondwana ; Géographie de l'Océanie ; Huriwai Group ; Jurassique supérieur ; Mésozoïque ; Nouvelle-Zélande ; Paléogéographie ; Paléozoïque ; Pétrographie ; Volcanisme (1)
- Physical geography (1)
- Carboniferous to Cretaceous on the Pacific margin of Gondwana: the Rangitata Phase of New-Zealand in Gondwana Five. Selected papers and abstracts of papers. (1)
- Development of Permian intracratonic basins in Australia in Gondwana Five. Selected papers and abstracts of papers. (1)
- Evolution of the Tasman rift: apatite fission track dating evidence from the southeastern Australian continental margin in Gondwana Five. Selected papers and abstracts of papers. (1)
- Jurassic turbidites in central western Argentina (Neuquén Basin) in Gondwana Five. Selected papers and abstracts of papers. (1)
- Petrography of the youngest known Murihiku Supergroup, New Zealand: latest Jurassic arc volcanism on the southern margin of Gondwana in Gondwana Five. Selected papers and abstracts of papers. (1)
- Significance of Tethyan fusulinid limestones of New Zealand in Gondwana Five. Selected papers and abstracts of papers. (1)
- Structure and tectonics of Gondwana basins of peninsular India in Gondwana Five. Selected papers and abstracts of papers. (1)
- The continental margin of Gondwana, principally in central western Argentina: Jurassic and Lower Cretaceous palynomorphs and calcareous microfossils in Gondwana Five. Selected papers and abstracts of papers. (1)
- Carboniferous to Cretaceous on the Pacific margin of Gondwana: the Rangitata Phase of New-Zealand in Gondwana Five. Selected papers and abstracts of papers.
- Petrography of the youngest known Murihiku Supergroup, New Zealand: latest Jurassic arc volcanism on the southern margin of Gondwana in Gondwana Five. Selected papers and abstracts of papers.
- The continental margin of Gondwana, principally in central western Argentina: Jurassic and Lower Cretaceous palynomorphs and calcareous microfossils in Gondwana Five. Selected papers and abstracts of papers.
- Evolution of the Tasman rift: apatite fission track dating evidence from the southeastern Australian continental margin in Gondwana Five. Selected papers and abstracts of papers.
- The fusulinid limestones were deposited in an equatorial belt of open ocean, distant from the New Zealand Gondwana margin, where climate contrasted markedly with the cold environment of continental New Zealand represented by the Parapara Peak
- Carboniferous or early Permian and were intermittently active until the end of the Permian. The structures resulted from compression generated mainly by plate convergence on the eastern craton margin (Tasman Fold Belt) and to a lesser extent by taphrogenesis
- of the sediments are clearly related to the margin of the basin and indicate its rapid subsidence. Tuffites in the sequence indicate volcanic activities in the hinterland. The development of the Argentine Neuquén Basin in the early Jurassique, shown
- The intracratonic Gondwana basins of peninsular India occur in long, narrow, well-defined belts on the Precambrian platform, corresponding to rivervalleys of Damodar-Son, Mahanadi and Godavari. The basins are half grabens or grabens, with margin