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Sedimentary and tectonic processes in the Upper Lias-Dogger transition of the Sierra de Reclot (External Subbetic, Alicante province)

dc.contributor.authorNieto, Luis M.
dc.contributor.authorMolina, José Miguel
dc.contributor.authorRuiz Ortiz, Pedro Alejandro
dc.date.accessioned2017-03-09T11:56:27Z
dc.date.available2017-03-09T11:56:27Z
dc.date.issued1995
dc.identifier.urihttp://hdl.handle.net/10272/13435
dc.description.abstractThe stratigraphy and biostratigraphy of the Upper Lias-Dogger transition in the Sierra de Reclot is analysed. These stratigraphic levels in the boundary between the Zegri and Upper Ammonitico Rosso formations show condensed deposits and an important stratigraphic lacuna as a minimum of Middle Toarcian-Upper Aalenian age. During Upper Lias-Aalenian the sedimentary processes were controlled by synsedimentary faults, after fossilized by an Upper Aalenian stromatolitic crusten_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherToarcianen_US
dc.subject.otherAalenianen_US
dc.subject.otherStromatolitic crusten_US
dc.subject.otherMacrooncoidsen_US
dc.subject.otherCalcarenitesen_US
dc.subject.otherSynsedimentary normal faulten_US
dc.subject.otherStratigraphic lacunaen_US
dc.titleProcesos sedimentarios y tectónicos en el tránsito Lías Superior-Dogger de la Sª de Reclot (Subbético externo, prov. Alicante)en_US
dc.titleSedimentary and tectonic processes in the Upper Lias-Dogger transition of the Sierra de Reclot (External Subbetic, Alicante province)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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