Academic literature on the topic 'Taza-Guercif Basin'

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Journal articles on the topic "Taza-Guercif Basin"

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Pratt, Jonathan R., David L. Barbeau, Tyler M. Izykowski, John I. Garver, and Anas Emran. "Sedimentary provenance of the Taza-Guercif Basin, South Rifean Corridor, Morocco: Implications for basin emergence." Geosphere 12, no. 1 (2016): 221–36. http://dx.doi.org/10.1130/ges01192.1.

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Gelati, Romano, Giovanna Moratti, and Giovanni Papani. "The Late Cenozoic sedimentary succession of the Taza-Guercif Basin, South Rifian Corridor, Morocco." Marine and Petroleum Geology 17, no. 3 (2000): 373–90. http://dx.doi.org/10.1016/s0264-8172(99)00054-9.

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Zuffetti, Chiara, Fabrizio Felletti, and Mattia Marini. "Turbidite channel-levée transitions: insights from the Tachrift system (Complex 6, Taza-Guercif Basin, NE Morocco)." Rendiconti Online della Società Geologica Italiana 59 (March 2023): 1–7. http://dx.doi.org/10.3301/rol.2023.04.

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Felletti, Fabrizio, Mattia Marini, Imad El Kati, and Hassan Tabyaoui. "The Tachrift channel-levée turbidite complexes (Tortonian) of the Taza-Guercif basin (South Rifian Corridor, NE Morocco)." Journal of Maps 16, no. 2 (2020): 902–17. http://dx.doi.org/10.1080/17445647.2020.1844088.

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Bernini, M., M. Boccaletti, G. Moratti, and G. Papani. "Structural development of the Taza-Guercif Basin as a constraint for the Middle Atlas Shear Zone tectonic evolution." Marine and Petroleum Geology 17, no. 3 (2000): 391–408. http://dx.doi.org/10.1016/s0264-8172(99)00042-2.

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Krijgsman, W., C. G. Langereis, W. J. Zachariasse, et al. "Late Neogene evolution of the Taza–Guercif Basin (Rifian Corridor, Morocco) and implications for the Messinian salinity crisis." Marine Geology 153, no. 1-4 (1999): 147–60. http://dx.doi.org/10.1016/s0025-3227(98)00084-x.

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Invernizzi, Daniele, Moreno Pizzutto, Fabrizio Felletti, George Pantopoulos, Mattia Marini, and Adam Mcarthur. "Reconstruction of the sedimentary heterogeneity in outcropping deep-water channel–levee deposits (Taza–Guercif Basin, late Tortonian, NE Morocco)." Journal of Sedimentary Research 95, no. 2 (2025): 314–41. https://doi.org/10.2110/jsr.2024.040.

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ABSTRACT In the context of subsurface modeling of deep-water sedimentary systems, it is crucial to confidently identify turbidite channel–levee architectural elements in ancient strata. This becomes particularly critical when working with data of limited resolution, such as wireline well or seismic data. Similarly, in areas with limited outcrop exposure, establishing the temporal relationships of channel–levee systems relies predominantly on inference. Moreover, the paucity of well-documented outcrops exhibiting a continuous sedimentary record between channel-fill and overbank sediments remain
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Felletti, Fabrizio, George Pantopoulos, Chiara Zuffetti, et al. "The Tachrift Project: sedimentary architecture of turbidite channel- levée deposits (Tachrift Turbidite System, Taza-Guercif Basin, Tortonian, NE Morocco)." Rendiconti Online della Società Geologica Italiana 59 (March 2023): 1–9. http://dx.doi.org/10.3301/rol.2023.13.

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Krijgsman, W., and C. G. Langereis. "Magnetostratigraphy of the Zobzit and Koudiat Zarga sections (Taza-Guercif basin, Morocco): implications for the evolution of the Rifian Corridor." Marine and Petroleum Geology 17, no. 3 (2000): 359–71. http://dx.doi.org/10.1016/s0264-8172(99)00029-x.

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Bernini, M., M. Boccaletti, R. Gelati, G. Moratti, G. Papani, and J. El Mokhtari. "TECTONICS AND SEDIMENTATION IN THE TAZA-GUERCIF BASIN, NORTHERN MOROCCO: IMPLICATIONS FOR THE NEOGENE EVOLUTION OF THE RIF-MIDDLE ATLAS OROGENIC SYSTEM." Journal of Petroleum Geology 22, no. 1 (1999): 115–28. http://dx.doi.org/10.1111/j.1747-5457.1999.tb00462.x.

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Dissertations / Theses on the topic "Taza-Guercif Basin"

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REGUZZI, SIMONE. "SEDIMENTOLOGY AND STRATIGRAPHY OF TURBIDITE SYSTEMS WITH CONTRASTING ARCHITECTURES: EXAMPLES FROM THE TERTIARY PIEDMONT BASIN (NW ITALY) AND THE TAZA-GUERCIF BASIN (NE MOROCCO)." Doctoral thesis, Università degli Studi di Milano, 2022. http://hdl.handle.net/2434/922848.

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Architectures of submarine fans and turbidite systems are endowed by a high grade of complexity, inherited by the large variability of depositional flows characterising them. This complexity is reflected upon the superimposition of depositional elements (e.g., channels, levées, splays, etc.) giving rise to contrasting sedimentary facies and geometries at different scales. Thus, the understanding and prediction of their heterogeneity over space is essential to obtain reliable depositional models, which can be applied in the field of natural resources exploration. Despite heterogeneities of fac
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