Tectono-sedimentary evolution of the Miocene Oued Dayr Formation (Ghomaride Complex, Internal Domain of the Maghrebian Rif Belt, Morocco)

• Published in: Arabian journal of geosciences 2016-10, Vol.9 (15), p.1-28, Article 660
• Main Authors: El Ouaragli, Bilal, Zaghloul, Mohamed Najib, El Talibi, Hajar, Somma, Roberta
• Format: Article
• Language: English
• Subjects: Alpine environments; Basins; Chains; Cobblestone; Conglomerates; Deformation; Ductile-brittle transition; Earth and Environmental Science; Earth science; Earth Sciences; Erosion; Geological faults; Geological time; Marginal basins; Marine environment; Mesozoic; Metamorphic rocks; Miocene; Nappes; Original Paper; Paleozoic; Pebbles; Provenance; Quartzite; Rock; Rocks; Sandstone; Sedimentary facies; Sedimentary rocks; Shales; Structural analysis
• ISSN: 1866-7511; 1866-7538
• DOI: 10.1007/s12517-016-2663-8

This work deals with sedimentological, petrographic, and structural analyses of a middle Miocene late-orogenic sedimentary cycle, denoted Oued Dayr Formation, recognized in the Rifian sector of the Maghrebian Chain (Morocco). The analyzed Formation (75 m thick) starts with 15–20 m of light colored polymict conglomerates, with minor sandstone beds, lying on the Paleozoic basement and Mesozoic cover of the Ghomaride Nappe. Facies analysis indicates a fining-upward deposition in a marine environment characterized by increasing deepening, reflecting a subsidence rate that exceeds sedimentary supply. Petrographic analysis points out that sandstones are represented by litharenites originated by erosion of recycled orogen. The conglomerates pebbles and cobbles consist of Alpine low- to high-grade metamorphic rocks as metarenites, phyllites, mylonitic quartzites, micaschists, augen gneisses deriving from the exhumed deep metamorphic basement, the overlying metasedimentary of the Sebtide Nappes and of sedimentary rocks as sandstones, jaspes, limestones, and shales deriving from the Ghomaride Nappes and their sedimentary cover. Data reveal mixed provenance indicating that the Oued Dayr Formation was fed by the Internal Nappes stack of the Maghrebian Chain. Structural analysis shows that the Oued Dayr Formation accumulated in a Thrust-Top basin, during an early extension (D 0 phase), recorded by synsedimentary normal faults within middle Langhian deposits on the rear of the Internal Nappes stack. Subsequent ductile and brittle compressional (D 1 , D 2 , D 3 ) and extensional (D 4 ) deformation phases occurred during and/or after the stacking, exhumation, and early unroofing of Sebtide Complex coeval with the opening of the western Mediterranean back-arc basins since middle Miocene time.