The evolution of the Suez rift: a combination of stretching and secondary convection

Tectonophysics

Volumn 133, Issue 3-4, 1987, Pages 229-234

  Moretti, I ^a   Chenet P Y ^a  

^a IFP ENERGIES NOUVELLES   (France)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0023503734     PISSN: 00401951     EISSN: None     Source Type: Journal    
DOI: 10.1016/0040-1951(87)90266-6     Document Type: Article

References (16)

1. Some remarks on subsidence study of sedimentary basins Application to the Gulf of Lions margin (Western Mediterranean)
2. Tectonique de la zone comprise entre Abu Durha et Gebel mezzazat (Sinaï, Egypte) dans le contexte de l'évolution du rift de Suez
3. The tectonic development of the Western margin of the Gulf of Elat (Aqaba) rift
4. Steady-state, secondary convection beneath lithospheric plates with temperature and pressure dependent viscosity
5. The tectonics of the Suez rift
6. Dynamical extension of the lithosphere during rifting: some numerical model results
7. History of uplift of the crystalline basement of Sinaï and its relation to opening of the Red Sea
8. Structural trends in the northerns Red Sea
9. Some remarks on the development of sedimentary basins
10. Physical models of extensional tectonics
11. Lithospheric boudinage and stretching instability
12. Rifting process and thermal evolution of the continental margin of eastern Canada determined from subsidence curves
13. Uplift and extension at the Gulf of Suez—indications of induced mantle convection
14. Geodynamic evolution of the Suez rift, Egypt. Application to the modelling of oil genesis
15. Thinning of the lithosphere by small-scale convective destabilization