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dc.contributor.authorArmstrong-Altrin, John
dc.contributor.authorNagarajan, Ramasamy
dc.contributor.authorMadhavaraju, Jayagopal
dc.contributor.authorRosalez-Hoz, Leticia
dc.contributor.authorLee, Yong
dc.contributor.authorBalaram, Vysetti
dc.contributor.authorCruz-Martinez, Adriana
dc.contributor.authorAvila-Ramirez, Gladis
dc.date.accessioned2017-01-30T11:32:03Z
dc.date.available2017-01-30T11:32:03Z
dc.date.created2014-03-16T20:01:13Z
dc.date.issued2013
dc.identifier.citationArmstrong-Altrin, John and Nagarajan, Ramasamy and Madhavaraju, Jayagopal and Rosalez-Hoz, Leticia and Lee, Yong and Balaram, Vysetti and Cruz-Martinez, Adriana and Avila-Ramirez, Gladis. 2013. Geochemistry of the Jurassic and Upper Cretaceous shales from the Molango Region, Hidalgo, eastern Mexico: Implications for source-area weathering, provenance, and tectonic setting. Comptes Rendus Geoscience. 345 (4): pp. 185-202.
dc.identifier.urihttp://hdl.handle.net/20.500.11937/12655
dc.identifier.doi10.1016/j.crte.2013.03.004
dc.description.abstract

This study focuses on the Jurassic (Huayacocotla and Pimienta Formations) and Upper Cretaceous (Mendez Formation) shales from the Molango Region, Hidalgo, Mexico. In this article, we discuss the mineralogy, major, and trace element geochemistry of the Mesozoic shales of Mexico. The goal of this study is to constrain the provenance of the shales, which belong to two different periods of the Mesozoic Era and to understand the weathering conditions and tectonic environments of the source region.

dc.publisherElsevier
dc.subjectTrace elements - Rare earth elements - Huayacocotla anticlinorium - Pimienta and Me´ndez Formations - ANOVA - Eastern Mexico
dc.titleGeochemistry of the Jurassic and Upper Cretaceous shales from the Molango Region, Hidalgo, eastern Mexico: Implications for source-area weathering, provenance, and tectonic setting
dc.typeJournal Article
dcterms.source.volume345
dcterms.source.number4
dcterms.source.startPage185
dcterms.source.endPage202
dcterms.source.issn16310713
dcterms.source.titleComptes Rendus Geoscience
curtin.note

NOTICE: this is the author’s version of a work that was accepted for publication in Comptes Rendus Geoscience. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Comptes Rendus Geoscience, Vol. 345, No. 4 (2013). DOI: 10.1016/j.crte.2013.03.004

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curtin.accessStatusOpen access


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