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Structure kinematic and chronology of deformations in the Haouz Dorsal (Rif, Morocco)

dc.contributor.authorHlila, Rachid
dc.contributor.authorSanz de Galdeano, Carlos
dc.date.accessioned2017-07-11T10:51:44Z
dc.date.available2017-07-11T10:51:44Z
dc.date.issued1994
dc.identifier.urihttp://hdl.handle.net/10272/13923
dc.description.abstractThe complex thrust-slice structure of the Haouz Mountains was formed during the Neogene in several phases, in which we recognize: a- Paroxysmal tectonic events, occurred in the Early Miocene, responsible of the formation of the thrust slices verging towards the W and SW as well as backthrusts verging towards the E and NE. These backthrusts appeared after the blockage of the thrust slices by the Fiysch nappes situated in a more external position, and are interpreted as antiformai stack phenomena. b- Post - paroxysmal tectonic events with lesser importance, alternating as distensive and compressive phases, occurred during the Middle and Late Miocenees_ES
dc.language.isofraes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherDorsal Rifes_ES
dc.subject.otherMoroccoes_ES
dc.subject.otherNeogenees_ES
dc.subject.otherThrustses_ES
dc.titleStructure, cinématique et chronologie des déformations dans la dorsale du Haouz (Rif, Maroc)es_ES
dc.titleStructure kinematic and chronology of deformations in the Haouz Dorsal (Rif, Morocco)eng
dc.typeinfo:eu-repo/semantics/conferenceObjectes_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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