Microfades del Cretácico medio y superior de la Sierra de Chiapas (SE México)

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dc.contributor.authorRosales, C.
dc.contributor.authorBermúdez, J.
dc.contributor.authorAguilar, M.
dc.date.accessioned2015-11-24T10:11:56Z
dc.date.available2015-11-24T10:11:56Z
dc.date.issued1996
dc.description.abstractBased on the micropaleontologic study of the carbonate rocks from the Sierra de Chiapas (SE Mexico) ten microfacies are recognized. They correspond mainly to shallow carbonates with some deeper environments toward the top of the sequence. The age of the strata ranges from Cenomanian to Maastrichtian, including some gaps such as that corresponding to subaereal exposure in Cenomanian times and that for Santonian-Early Campanian which represents a regional discontinuityen_US
dc.identifier.urihttp://hdl.handle.net/10272/11414
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherForaminiferaen_US
dc.subject.otherMicrofadesen_US
dc.subject.otherCretaceousen_US
dc.subject.otherMexicoen_US
dc.titleMicrofades del Cretácico medio y superior de la Sierra de Chiapas (SE México)en_US
dc.titleMicrofacies of the middle and upper Cretaceous from the Sierra de Chiapas (SE Mexico)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 20-1, (1996)