Palaeogeographic evolution of the late Miocene Rifian Corridor (Morocco):Reconstructions from surface and subsurface data

Autor: Capella, W., Barhoun, N., Flecker, R., Hilgen, F. J., Kouwenhoven, T., Matenco, L. C., Sierro, Francisco J., Tulbure, M. A., Yousfi, Mohamed Zakaria, Krijgsman, W., Paleomagnetism, Stratigraphy and paleontology, Tectonics, Stratigraphy & paleontology

Publikováno v: Capella, W, Barhoun, N, Flecker, R, Hilgen, F J, Kouwenhoven, T, Matenco, L C, Sierro, F J, Tulbure, M A, Yousfi, M Z & Krijgsman, W 2018, ' Palaeogeographic evolution of the late Miocene Rifian Corridor (Morocco) : Reconstructions from surface and subsurface data ', Earth-Science Reviews, vol. 180, pp. 37-59 . https://doi.org/10.1016/j.earscirev.2018.02.017
Earth-Science Reviews, 180, 37. Elsevier

The Rifian Corridor was one of the Mediterranean–Atlantic seaways that progressively restricted and caused the Messinian Salinity Crisis (MSC). Many key questions concerning the controls on the onset, progression and termination of the MSC remain u

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7ca5be784df29c005011ffcb699cee13
https://research-information.bris.ac.uk/ws/files/186032171/Full_text_PDF_accepted_author_manuscript_.pdf

Gateway to a vanishing ocean: the tectono-sedimentary evolution of the Rifian Corridor (Morocco) and the Late Miocene isolation of the Mediterranean

The Mediterranean Sea needs a connection to the world ocean otherwise it would evaporate. If the Gibraltar Straits were closed, the Mediterranean would desiccate in about 3000 to 8000 years. Because the volume of water lost by evaporation exceeds the

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dris___00893::186c4d14947c291a75758cc9514d7ed6
https://hdl.handle.net/1874/350723

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