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- W2113132295 abstract "The integrated analysis of thrust structures and facies allows us to interpret the Carboniferous volcano-sedimentary complex of Tazekka massif as a compressive sub-basin controlled mainly by the Hajra Sbaa–Merja Caï’d northwest-verging thrust-propagation fold. The tectono-sedimentary sequence (conglomerates, greywacke and shale) is associated with an extrusive magmatism comprising basalts, andesites and rhyolites, under effusive and volcanoclastic facies (or rhyolites with exotic blocks), of orogenic calk-alkaline nature, which is consistent with a context of continental subduction. These results, and the comparison of regional contraction ages in the Moroccan Meseta, integrate the Carboniferous volcano-sedimentary depocentre of Tazekka massif in the wedgetop depozone of a foreland basin system generated by two north-west thrusted piggy-back sequences (aged from Fameno-Tournaisian to upper Visean-lower Westphalian) from the eastern Meseta to the western Meseta of Morocco." @default.
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- W2113132295 date "2004-06-01" @default.
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- W2113132295 title "The Carboniferous volcano-sedimentary depocentre of Tazekka Massif (Middle-Atlas, Morocco): new observations and geodynamic implications" @default.
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- W2113132295 doi "https://doi.org/10.1016/j.jafrearsci.2004.07.032" @default.
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