Výsledky vyhledávání - "Achraf Atouabat"

Akademický článek

Validating Structural Styles in the Flysch Basin Northern Rif (Morocco) by Means of Thermal Modeling

Autor: Achraf Atouabat, Sveva Corrado, Andrea Schito, Faouziya Haissen, Oriol Gimeno-Vives, Geoffroy Mohn, Dominique Frizon de Lamotte

Publikováno v: Geosciences, Vol 10, Iss 9, p 325 (2020)

Vitrinite reflectance and a micro-Raman spectroscopy parameters data set have been acquired on dispersed organic matter of the Maghrebian flysch basin and the Tangiers unit across a NE-SW section in the north-western Rif belt (North Morocco). Thermal

Externí odkaz: https://doaj.org/article/763de8e677974fad80ad51b021d7e072

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Paleogene-Neogene evolution of the central-western Rif fold-and-thrust belt (Northern Morocco) by means of thermal modeling

Autor: Achraf Atouabat, Andrea Schito, Rémi Leprêtre, Geoffroy Mohn, Sveva Corrado

The Rif belt (Northern Morocco) represents the western termination of the Maghrebides system. It is subdivided into three tectono-stratigraphic domains known as: Internal domain (i.e., Alboran domain), the Maghrebian flysch domain (i.e., the sediment

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::d0fdb5fe6984f2e7e8b179fe9c074862
https://doi.org/10.5194/egusphere-egu23-17511

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Alpine tectono-thermal evolution of the North African passive paleo-margin incorporated in the Western Rif belt (Northern Morocco)

Autor: Achraf Atouabat, Sveva corrado, Dominique Frizon de Lamotte, Remi Leprêtre, Geoffroy Mohn, Andrea Schito

Located in Northern Morocco, the Rif fold and-thrust belt is mainly made by the remnant of the north African paleo-passive margin and its sedimentary infill. We present in this contribution new field observations combined with paleo-thermal analysis

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::cb013652a4ec965127da0e08d1d62124
https://doi.org/10.5194/egusphere-egu22-11175

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The structuration of the External Rif (Rif belt: Northern Morocco). An insights from paleo-thermal and structural analyses

Autor: Andrea Schito, Faouziya Haissen, Achraf Atouabat, Sveva Corrado, Rémi Leprêtre, Geoffroy Mohn, Dominique Frizon de Lamotte

Belonging to the Maghrebides system, the Rif belt (Northern Morocco) suffered an important Cenozoic Alpine compressional deformation as a consequence of the closure of the Maghrebian Tethys and the westward translation and docking of the Alboran Doma

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::c8929e975c1e15b12769b6bf7fb01e1d
https://doi.org/10.5194/egusphere-egu21-12892

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An insight on the polyphase thermal history of the Ghomarides and Upper Sebtides in the Internal Rif (North Morocco) by means of Raman spectroscopy on organic matter

Autor: Amalia Spina, Achraf Atouabat, David Muirhead, Andrea Schito, Alessandro Pozzi, Claudia Romano, Sveva Corrado, Rocco Calcagni, Roberto Galimberti

The correct assessment of maximum temperatures experienced by rocks is an essential tool to unravel the evolution of the thermal structure of the crust during the main phases of an orogenesis. Given to broad P-T stability field of classical metamorph

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::43174b3212740ba036a7dc425c2eaa2e
https://doi.org/10.5194/egusphere-egu21-7459

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Structural styles of the External Rif and Flysch Domain (Rif belt, northern Morocco) through thermal maturity and structural data

Autor: Geoffroy Mohn, Sveva Corrado, Achraf Atouabat, Faouziya Haissen, Andrea Schito, Dominique Frizon de Lamotte

Located in northern Morocco, the Rif belt represents the western edge of the Maghrebides system. This domain underwent a significant Cenozoic alpine compressional deformation, due to the collision between the North African margin and the south-wester

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::25490c5cee2d2e36b23a5f677d4e1fba
https://doi.org/10.5194/egusphere-egu2020-19279

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The structure of the Central-Eastern Rif (Morocco) and the disregarded subduction of the North-West African paleo-margin

Autor: Oriol Gimeno, Dominique Frizon de Lamotte, Rémi Leprêtre, Faouziya Haissen, Achraf Atouabat, Geoffroy Mohn

The Rif Belt (Northern Morocco) forms the western edge of the Alpine-Himalayan orogenic system developed during the convergence between the Africa and Eurasia plates. Compared to other mountains belts, the External Rif, which preserves remnants of th

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::cd8f20eb279fa872d2346186661efccd
https://doi.org/10.5194/egusphere-egu2020-18249

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The Mesozoic Margin of the Maghrebian Tethys in the Rif Belt (Morocco): Evidence for Polyphase Rifting and Related Magmatic Activity

Autor: Faouziya Haissen, Oriol Gimeno-Vives, Dominique Frizon de Lamotte, Mohamed Najib Zaghloul, Achraf Atouabat, Geoffroy Mohn, Valérie Bosse

Publikováno v: Tectonics
Tectonics, 2019, 38, pp.2894-2918. ⟨10.1029/2019TC005508⟩

International audience; The Rif belt (northern Morocco) is a mountain chain located at the junction between the Mediterranean and Central Atlantic Domains. Although the Rif belt underwent important Cenozoic (i.e., Alpine) shortening, remnants of the

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8c05ec3a67e0ad97d4eeb17dd71c3d82
https://insu.hal.science/insu-03708952/document

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