Výsledky vyhledávání - "Anas Abbassi"

The Numidian sand event in the Burdigalian foreland basin system of the Rif, Morocco, in a source-to-sink perspective

Autor: Mohamed El Morabet, M. N. Zaghloul, Maria Giuditta Fellin, Marcel Guillong, Domenico Cosentino, Anas Abbassi, Paola Cipollari

Publikováno v: GSA Bulletin. 134:2280-2304

During the Tertiary evolution of the Western Mediterranean subduction system, the orogenic accretion at the Maghrebian margin let the stacking of three main tectonic zones of the Rif fold-and-thrust belt: 1) the Internal Zone; 2) the “Maghrebian Fl

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bd5011091916944b76cd492ab773ee3f
https://doi.org/10.1130/b36136.1

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Provenance and sedimentary processes on Pleistocene storm deposits in Harhoura (Northern Coastal Atlantic, Morocco): New constraints from a source to sink perspective

Autor: Sofia Benamri, Pedro J.M. Costa, Mohamed Najib Zaghloul, Jean Luc Mercier, Anas Abbassi, Mohamed El Mourabet, Khadija Aboumaria

Publikováno v: Marine Geology. 457:106992

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::40b195194ba74daadd99da1cc4d14fe4
https://doi.org/10.1016/j.margeo.2023.106992

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Stratigraphy, Provenance, and Geodynamic setting of the Lower-Middle Jurassic succession in the Prerif foreland basin (Rif Chain, Morocco)

Autor: Hajar Kairouani, Anas Abbassi, Mohamed Najib Zaghloul, Mohamed El Mourabet

The Rif chain is located on the western edge of the Apennine-Maghrebian Chain. It is classically subdivided into three main superimposed tectonic domains: The Internal, Flysch Basin, and the External domains. The latter regroups three sub-domains: In

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::9b4f4349d600a28304043cebc2ed62a8
https://doi.org/10.5194/egusphere-egu22-9404

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Supplemental Material: The Numidian sand event in the Burdigalian foreland basin system of the Rif, Morocco, in a source-to-sink perspective

Autor: Anas Abbassi

Figure S1: Accumulate thickness-age diagrams of the pre- and syn-orogenic deposits of the Tanger, Ketama, Beni Ider, Tisiren, and Predorsalian units; Figure S2: Sub-Numidian calcareous nannofossils marker species; Figure S3: Quantitative analyses of

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::62073565a37bf177dc868a62412d348a
https://doi.org/10.1130/gsab.s.16926337.v1

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The Rif Chain (Northern Morocco) in the Late Tortonian‐Early Messinian Tectonics of the Western Mediterranean Orogenic Belt: Evidence From the Tanger‐Al Manzla Wedge‐Top Basin

Autor: Domenico Cosentino, Anas Abbassi, M. N. Zaghloul, Paola Cipollari

Publikováno v: Tectonics. 39

During the Neogene, the Western Mediterranean subduction-related orogen developed under differing modes and senses of subduction, resulting in the formation of the Apennines, Maghrebides, Rif, and Betics. In this work, we present the Neogene kinemati

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2424320edf09c14ac2134643225d0812
https://doi.org/10.1029/2020tc006164

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The Numidian Sandstones in northern Morocco: Evidence for early Burdigalian autochthonous deposition on top of the Tanger Unit

Autor: Anas Abbassi, M. N. Zaghloul, Domenico Cosentino, Paola Cipollari

Publikováno v: Marine and Petroleum Geology. 131:105149

The Numidian Sandstones are widespread throughout the western Mediterranean, from Spain and North Africa to southern Italy. They consist of intercalations of thick ultra-mature sandstones within brownish shale deposits. Crucial issues about the Numid

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a39295a5bf29b031e4ee012a9346000b
https://doi.org/10.1016/j.marpetgeo.2021.105149

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