Stratigraphic evolution of a spectacularly exposed turbidite channel belt from the Tachrift System (late Tortonian, north‐East Morocco)

Author:

Reguzzi Simone1ORCID,Marini Mattia1ORCID,Felletti Fabrizio1ORCID,El Kati Imad2ORCID,Zuffetti Chiara1ORCID,Tabyaoui Hassan2ORCID

Affiliation:

1. Dipartimento di Scienze della Terra ‘A. Desio’ Università degli Studi di Milano Via Mangiagalli 34 Milan 20133 Italy

2. Natural Resources and Environment Laboratory, Polydisciplinary Faculty of Taza Sidi Mohamed Ben Abdellah University P.B. 1223 Taza Morocco

Publisher

Wiley

Subject

Stratigraphy,Geology,General Medicine

Reference102 articles.

1. Lateral accretion packages (LAPs): an important reservoir element in deep water sinuous channels;Abreu V.;Mar. Pet. Geol.,2003

2. Bedforms, primary structures and grain fabric in the presence of suspended sediment rain;Arnott R.W.C.;J. Sediment. Res.,1989

3. Laterally accreting sinuous channels and their deposits: the goldilocks of deep‐water slope systems;Arnott R.W.C.;J. Sediment. Res.,2021

4. Sedimentary architecture in meanders of a Submarine Channel: detailed study of the present Congo Turbidite Channel (Zaiango project);Babonneau N.;J. Sediment. Res.,2010

5. Deep‐water leveed‐channel complexes of the Cerro Toro formation, upper cretaceous, southern Chile;Beaubouef R.T.;Am. Assoc. Pet. Geol. Bull.,2004

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