Triassic–early Liassic extensional systems and their Tertiary inversion, Essaouira Basin (Morocco)
- 1 March 2000
- journal article
- Published by Elsevier in Marine and Petroleum Geology
- Vol. 17 (3) , 409-429
- https://doi.org/10.1016/s0264-8172(98)00081-6
Abstract
No abstract availableThis publication has 34 references indexed in Scilit:
- Transtensive synsedimentary tectonics associated with ocean opening: the Essaouira–Agadir segment of the Moroccan Atlantic marginJournal of the Geological Society, 1998
- Inverse and forward numerical modeling of trishear fault‐propagation foldsTectonics, 1998
- Le volcanisme permien et mésozoïque inférieur du bassin d'Argana (Haut-Atlas occidental, Maroc): un magmatisme intraplaque associé à l'ouverture de l'Atlantique centralJournal of African Earth Sciences, 1998
- Syn- and postrift evolution of the El Jadida – Agadir basin (Morocco): constraints for the rifting models of the central AtlanticCanadian Journal of Earth Sciences, 1995
- Superimposed extensional tectonics in the Argana Triassic formations (Morocco), related to the early rifting of the Central AtlanticGeological Magazine, 1991
- Tilted-blocks pattern, paleostress orientation and amount of extension, related to triassic early rifting of the central Atlantic in the Amzri area (Argana basin, Morocco)Tectonophysics, 1988
- Role of synsedimentary strike-slip faults in the formation of Moroccan Triassic basinsGeology, 1984
- Zur Strukturgeschichte des Hohen Atlas in MarokkoInternational Journal of Earth Sciences, 1981
- Separation of Morocco and eastern North America: A Triassic-Liassic stratigraphic recordGSA Bulletin, 1978
- Major Strike-slip Fault of Late Hercynian Age in MoroccoNature, 1972