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The basic magmatism in the Famennian-Dinantian Sidi Bettache Basin (Northwest Hercynian Morocco): new facts

dc.contributor.authorLakhloufi, A.
dc.contributor.authorHamoumi, N.
dc.contributor.authorSaquaque, A.
dc.contributor.authorAarab, A.
dc.contributor.authorJermouni, A.
dc.description.abstractCommonly is held up that the Sidi Bettache Basin corresponds to the collapse of a large block of the middle Devonian carbonate platform with subsequent magmatic injections emplacement along its boundaries. Previous studies of one of us (A.L.) and those in progress show instead that this magmatism is primarily controlled by distensional activity of NNW-SSE to NW-SE faults before Middle Visean time. These faults affect throughout the 60 km wide western part of the basin which is also characterized by its Famennian-Lower Visean sedimentary evolution and by a complex variscan polyphasic structurationen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherWestern Mesetaen_US
dc.subject.otherSidi Bettache Basinen_US
dc.subject.otherBasic magmatismen_US
dc.subject.otherTournaisian-Middle Viseanen_US
dc.titleEl Magmatismo Básico en La Cuenca Fameno-Dinantiense de Sidi Bettache (Marruecos Hercínico Noroccidental): Nuevos Datosen_US
dc.titleThe basic magmatism in the Famennian-Dinantian Sidi Bettache Basin (Northwest Hercynian Morocco): new factseng

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