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In: Geologica Carpathica, vol. 54, no. 2
Mohamed Najib Zaghloul - Lisa Gioconda Gigliuto - Diego Puglisi - Abdelouahed Ouazani-Touhami - Abderrahim Belkaid

THE OLIGOCENE-MIOCENE GHOMARIDE COVER: A PETRO-SEDIMENTARY RECORD OF AN EARLY SUBSIDENT STAGE RELATED TO THE ALBORAN SEA RIFTING (NORTHERN INTERNAL RIF, MOROCCO)

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Year, pages: 2003, 93 - 105

About article:

New sedimentological, petrographic and structural data have been collected from the Oligocene-Miocene terrigenous deposits unconformably overlying the highest tectonic units of the internal Rifian Chain (Ghomaride Units). These new data show (i) the abundance of coarse- grained facies (disorganized and organized conglomerates and pebbly sandstones), (ii) a sedimentary supply from very slightly metamorphic Paleozoic sources and from Mesozoic carbonate cover and (iii) the dominance of a mainly extensional syn-sedimentary tectonic activity. Stratigraphic and petrographic characters point out a palaeogeographical al scenario where the Ghomaride Units, believed to be the sources of the analyzed successions, fed small “satellite basins” located above the fold-thrust belt by means of gravity and debris flow processes. Moreover, the low textural maturity of the analyzed sandstones seems to suggest conditions of short transports linked to a rugged topography and to a very unstable tectonic setting. Structural data acquired, in good agreement with that of literature, confirm the existence of a mainly extensional tectonic activity which lasted from the Late Oligocene up to Middle Burdigalian times during the deposition of the analysed successions. So, within a mainly extensional geodynamic context, a continuous rapid erosion of the highly elevated parts (mainly Ghomaride Units) of the folded thrust belt, progressively uplifted, produced the sedimentary supply. During this Late Oligocene-Lower Miocene rifting stage, some of these “satellite basins” evolved, in the rear of the Rifian fold-thrust belt, to more subsiding areas as \"continental trenchs\" and triggered the opening of the Alboran sea.

How to cite:

ISO 690:
Najib Zaghloul, M., Gioconda Gigliuto, L., Puglisi, D., Ouazani-Touhami, A., Belkaid, A. 2003. THE OLIGOCENE-MIOCENE GHOMARIDE COVER: A PETRO-SEDIMENTARY RECORD OF AN EARLY SUBSIDENT STAGE RELATED TO THE ALBORAN SEA RIFTING (NORTHERN INTERNAL RIF, MOROCCO). In Geologica Carpathica, vol. 54, no.2, pp. 93-105.

APA:
Najib Zaghloul, M., Gioconda Gigliuto, L., Puglisi, D., Ouazani-Touhami, A., Belkaid, A. (2003). THE OLIGOCENE-MIOCENE GHOMARIDE COVER: A PETRO-SEDIMENTARY RECORD OF AN EARLY SUBSIDENT STAGE RELATED TO THE ALBORAN SEA RIFTING (NORTHERN INTERNAL RIF, MOROCCO). Geologica Carpathica, 54(2), 93-105.