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Browsing by Author "Maaté, Ali"
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Conodontos del Paleozoico Gomáride (Rif Septentrional, Marruecos). Nota preliminar
Rodríguez Cañero, Rosario; Maaté, Ali; Martín Algarra, Agustín (Sociedad Geológica de España, 1989)A moderately tectonised stratigraphic section pertaining to the Ghomarides, NW of Tetuan, Morocco, is formed by platy limestones and slates, and contains interesting associations of conodonts of uppermost Silurian to upper ... -
La serie paleógena de la unidad superior del Gomáride en Talembote (Rif Interno, Marruecos)
Hlila, Rachid; Maaté, Ali; Sanz de Galdeano, Carlos; Serra Kiel, Josep; Serrano Lozano, Francisco; El Kadiri, Khalil (2007)The lower Paleogene stratigraphic successions of the Talembote upper Ghomaride Unit represent an interval of age going from the (middle?) Ilerdian to the early Bartonian, showing a transgressive sequence interrupted by ... -
New structural data on the Tertiary of the External Tánger Unit (Intrarif, Morocco)
Maaté, Soufian; Guerrera, Francesco; Hlila, Rachid; Maaté, Ali; Martín Martín, Manuel; Tramontana, Mario (Sociedad Geológica de España, 2018)A tectonic study has been carried out in the Cenozoic of the External Tanger Unit. This parauthocthonous unit, characterized by open SW-vergent folds, overrides by mean of a thrusting the Intrarif Loukkos Unit and it is ... -
Nuevos datos sobre la estratigrafía de las escamas de la Hafa el Banat y de Fahs Dohor (Hauz interno, Rif Septentrional, Marruecos)
Maaté, Ali; Martín Algarra, Agustín (Sociedad Geológica de España, 1992)The stratigraphic succesions of the Hafa el Banat and of the Fahs Dohor slices (Internal Hauz, Northern Rif) are described. Both slices show stratigraphic features and a tectonic position similar to that of the Uestia II ... -
El Terciario de la unidad de Saaden ("Dorsal" externa, Rif Septentrional, Marruecos)
Martín Algarra, Agustín; Serrano Lozano, Francisco; Maaté, Ali (Sociedad Geológica de España, 1993)In the Saaden unit (External "Limestone Chain", northern Internal Rif), the uppermost Eocene and the Oligocene have been dated by planktonic foraminifera. It confirms that an important transgression accounted during the ...