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dc.contributor.advisorBasu, Asish R
dc.creatorChakrabarty, Puloma
dc.date.accessioned2021-06-03T19:57:48Z
dc.date.available2021-06-03T19:57:48Z
dc.date.created2019-05
dc.date.issued2019-05-07
dc.date.submittedMay 2019
dc.identifier.urihttp://hdl.handle.net/10106/29884
dc.description.abstractThe Cretaceous Period (145-66 Ma), with no magnetic reversal for ~79 Ma, is generally termed as the Cretaceous Normal Superchron or the Magnetic Quiet Zone. There is evidence of at least two major large scale, global volcanisms in this long period synchronous with mass extinctions, during the Late Cretaceous and at the end of the Cretaceous. This study focusses on the effect of these two global volcanisms on 1. The Ocean: Eagle Ford, South Texas at the beginning of the Late Cretaceous, 93.9 Ma, probably caused by Cretaceous mafic volcanism from the Ontong Java Plateau and/or Caribbean Large Igneous Province volcanism (LIP), and 2. The Land: Deccan Traps, end-Cretaceous, 66 Ma, LIP volcanism.
dc.format.mimetypeapplication/pdf
dc.language.isoen_US
dc.subjectEagle Ford Shale
dc.subjectAcid volcanism deccan
dc.titleTWO CRETACEOUS TALES OF THE LAND AND THE SEA
dc.typeThesis
dc.degree.departmentEarth and Environmental Sciences
dc.degree.nameDoctor of Philosophy in Earth and Environmental Science
dc.date.updated2021-06-03T19:57:49Z
thesis.degree.departmentEarth and Environmental Sciences
thesis.degree.grantorThe University of Texas at Arlington
thesis.degree.levelDoctoral
thesis.degree.nameDoctor of Philosophy in Earth and Environmental Science
dc.type.materialtext
dc.creator.orcid0000-0001-9181-5157


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