Programme annuel & rapport de suivi technique |
-
Rapport d'activités 2023
-
Programmes Techniques 2024
|
Géocatalogue |
|
Appels d'Offres |
-
ACQUISITION DES TICKETS RESTAURANT POUR LE PERSONNEL DE L’ONM
-
CHOIX D’UNE COMPAGNIE D’ASSURANCE
-
ACQUISITION ET MISE EN ŒUVRE D’UN PROGICIEL DE GESTION INTEGRE
|
Investir en Tunisie |
|
|
|
::
Documentation and Editions
>>
Research library
|
|
|
[
Search by author
]
[
Search keyword
]
[
Search by index
]
[
Search by category
]
title of the reference :
|
Tethyan margins in space and time.
|
Publication Date:
|
1991
|
Author :
|
Stampfli Gérard, Marcoux J., Baud Aymon, Channell J.E.T., Winterer, Jansa L.F.
|
Catalogue type :
|
Livre
|
Catalogue reference :
|
(NLD) Palaeogeogr., Palaeoclimatol., Palaeoecol. Tethyan margins in space and time. 28th Int. Geol. Congr. Rifting processes, leading to sea-floor spreading, are characterized by a sequence of events transtensive phase of extension with syn-rift volcanism: simple shear extension accompanied by lithospheric thinning and asthenospheric up-welling and thermal uplift of the rift shoulder and asymmetric volcanism. The simple shear model of extension leads to an asymmetric model of passive margin: a lower plate tilted block margin and an upper plate flexural, ramp-like margin. Both will be affected by thermal contraction and subsidence, staring soon after sea-floor spreading. Based on these actualistic models Tethyan margins are classified as one type of the other.
Téthys ; Marge continentale passive ; Formation rift ; Primaire ; Extension tectonique ; Asthénosphère ; Upwelling ; Modèle ; Phase transtension ; Tunisie ; Iran ; Inde ; Oman Winterer Jansa L.F. Marcoux J. Baud Aymon Channell J.E.T. Stampfli Gérard Tectonique
|
Indexation decimale :
|
Tectonique
|
Keywords :
|
Téthys ; Marge continentale passive ; Formation rift ; Primaire ; Extension tectonique ; Asthénosphère ; Upwelling ; Modèle ; Phase transtension ; Tunisie ; Iran ; Inde ; Oman
|
Summary :
|
Rifting processes, leading to sea-floor spreading, are characterized by a sequence of events transtensive phase of extension with syn-rift volcanism: simple shear extension accompanied by lithospheric thinning and asthenospheric up-welling and thermal uplift of the rift shoulder and asymmetric volcanism. The simple shear model of extension leads to an asymmetric model of passive margin: a lower plate tilted block margin and an upper plate flexural, ramp-like margin. Both will be affected by thermal contraction and subsidence, staring soon after sea-floor spreading. Based on these actualistic models Tethyan margins are classified as one type of the other.
|
Exemplaries :
|
-
|
|
|
|
|
|