Calibrating the Ediacaran-Cambrian transition in the SW Gondwana

dc.contributorUniversidade Estadual Paulista (Unesp)
dc.contributorUniversidade de São Paulo (USP)
dc.contributorVirginia Tech
dc.date.accessioned2020-12-12T01:07:26Z
dc.date.accessioned2022-12-19T20:38:39Z
dc.date.available2020-12-12T01:07:26Z
dc.date.available2022-12-19T20:38:39Z
dc.date.created2020-12-12T01:07:26Z
dc.date.issued2019-01-01
dc.identifierEstudios Geologicos, v. 75, n. 2, 2019.
dc.identifier1988-3250
dc.identifier0367-0449
dc.identifierhttp://hdl.handle.net/11449/198241
dc.identifier10.3989/EGEOL.43591.573
dc.identifier2-s2.0-85076008156
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/5378875
dc.description.abstractThe paleontological, isotopic and geochronological data summarized below support the paleogeographic and temporal correlation between Itapucumi (Paraguay) and Corumbá (Brazil) groups, suggesting a coeval sedimentary evolution of these units in the margins of the Amazon Craton and the Rio Apa Block.
dc.languageeng
dc.relationEstudios Geologicos
dc.sourceScopus
dc.subjectDetrital and volcanic zircon
dc.subjectEdiacaran-Cambrian transition
dc.subjectItapucumi Group
dc.subjectNama assemblage
dc.subjectSHRIMP ages
dc.subjectSW Gondwana
dc.titleCalibrating the Ediacaran-Cambrian transition in the SW Gondwana
dc.typeArtículos de revistas


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