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Kinematics and paleostresses in the Jebha-Chrafate transcurrent fault (northern Rif, Morocco)

dc.contributor.authorBen Makhlouf, Mohamed
dc.contributor.authorGalindo Zaldívar, Jesús
dc.contributor.authorChalouan, Ahmed
dc.contributor.authorSanz de Galdeano, Carlos
dc.contributor.authorAhmamou, M’Fedal
dc.contributor.authorLópez Garrido, Ángel Carlos
dc.description.abstractThe Jebha-Chrafate is an ENE-WSW sinistral major transcurrent fault of the Rif Cordillera, formed during the southwestwards emplacement of the Internal Zones on the Flysch units and the External Zones. The analysis of minor structures along the Jebha area indicates the activity of top to the SW low and high angle normal faults during the tectonic wedge emplacement. In addition, most of the kinematic indicators along the transcurrent fault zone point to a reactivation as dextral fault during the recent NW-SE Eurasia-Africa convergence and a final overprinting of normal faults during the late stages of relief upliften_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.subject.otherInternal Rifen_US
dc.subject.otherTransfer faulten_US
dc.subject.otherLow angle normal faultsen_US
dc.subject.otherPaleostress evolutionen_US
dc.titleCinemática y paleoesfuerzos en la zona de falla transcurrente de Jebha-Chrafate (Rif septentrional, Marruecos)en_US
dc.titleKinematics and paleostresses in the Jebha-Chrafate transcurrent fault (northern Rif, Morocco)eng

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Atribución-NoComercial-SinDerivadas 3.0 España
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