Provenance and source-to-sink of lower-middle Jurassic sediments from hinterland mounts to NW-Gondwana hyper-extended passive margin (Prerif sub-domain, External Rif, Morocco): First evidence from sedimentary petrology and detrital Zircon geochronology

Petrographic and geochemical study of Precambrian and Paleozoic rocks in the western Anti-Atlas belt, Morocco: Facies, weathering, provenance and economic exploitation

“…The geological history of the Ifni Buttonhole begins in the Paleoproterozoic and continues through the Middle Neoproterozoic, Late Neoproterozoic, Paleozoic, Mesozoic, and Cenozoic [ 18 , [23] , [24] , [25] , 37 , [47] , [48] , [49] , [50] , [51] , [52] , [53] ]. The geodynamic evolution of the Ifni Buttonhole is probably subdivided into six stages ( Fig.…”