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dc.contributor.authorOcampo Diaz, Yam Zul Ernesto
dc.contributor.authorTalavera Mendoza, Oscar
dc.contributor.authorJenchen, Uwe
dc.contributor.authorValencia, Victor A
dc.contributor.authorMedina Ferrusquia, Hugo Cesar
dc.contributor.authorGuerrero Suastegui, Martin
dc.creatorOCAMPO DIAZ, YAM ZUL ERNESTO; 162630
dc.creatorTALAVERA MENDOZA, OSCAR; 14356
dc.creatorJenchen, Uwe;#0000-0002-4998-8967
dc.creatorValencia, Victor A;#0000-0003-2508-651X
dc.creatorMEDINA FERRUSQUIA, HUGO CESAR; 231768
dc.creatorGUERRERO SUASTEGUI, MARTIN; 123318
dc.date.accessioned2020-09-09T17:01:38Z
dc.date.available2020-09-09T17:01:38Z
dc.date.issued2014-01
dc.identifier.urihttp://ri.uagro.mx/handle/uagro/1781
dc.description.abstractDuring Valanginian-Hauterivian time, La Casita Formation (Monterrey trough) and the Patula Arkose (Sabinas basin) formed sedimentary units distributed in the southeast and northeast edge of the Coahuila block. The present article discriminates the character of the different geotectonic elements that form northeastern Mexico and integrates petrographic studies of sandstone and geochronology of detrital zircons. La Casita Formation consists of volcano-plutonoclastic petrofacies with quartz-feldspathic trends, showing volcanic lithic influence with felsitic, microlitic, lathwork, and plutonic lithic fragments with myrmekitic textures, as well as metafelsitic/psammitic3y4 lithics; in contrast, the Patula Arkose is characterized by sedimentary- plutonoclastic petrofacies, with a high content of plutonic lithics with myrmekitic, metapelitic2, and metapsammitic2 textures, and a subordinate content of volcanic lithics with felsitic and lathwork textures. The detrital zircon ages vary from 2885 to 164.
dc.formatpdf
dc.language.isospa
dc.publisherRevista Mexicana De Ciencias Geológicas
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0
dc.subjectLa Casita Formation
dc.subjectPatula Arkose
dc.subjectProvenance
dc.subjectdetrital zircons
dc.subjectnortheastern Mexico
dc.subject.classificationCIENCIAS FÍSICO MATEMÁTICAS Y CIENCIAS DE LA TIERRA::CIENCIAS DE LA TIERRA Y DEL ESPACIO::OTRAS ESPECIALIDADES DE LA TIERRA, ESPACIO O ENTORNO
dc.titleProcedencia de la Formación La Casita y la Arcosa Patula: implicaciones para la evolución tectono-magmática del NE de México entre el Carbonífero y el Jurásico.
dc.typeArtículo
dc.type.conacytarticle
dc.rights.accesopenAccess
dc.audiencegeneralPublic
dc.identificator1||25||2599
dc.format.digitalOriginBorn digital
dc.thesis.degreelevelMaestría
dc.thesis.degreenameMaestría en Recursos Naturales y Ecología
dc.thesis.degreegrantorUniversidad Autónoma de Guerrero
dc.thesis.degreedepartmentFacultad de Ecología Marina
dc.thesis.degreedisciplineCiencias Físico Matemáticas Y Ciencias De La Tierra
dc.identifier.cvuagro6269


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