Age constraint for the Moreno Hill Formation (Zuni Basin) by CA-TIMS and LA-ICP-MS detrital zircon geochronology

The “mid-Cretaceous” (~125–80 Ma) was punctuated by major plate-tectonic upheavals resulting in widespread volcanism, mountain-building, eustatic sea-level changes, and climatic shifts that together had a profound impact on terrestrial biotic assemblages. Paleontological evidence suggests terrestria...

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Detalles Bibliográficos
Autores principales: Cilliers, Charl D., Tucker, Ryan T., Crowley, James L., Zanno, Lindsay E.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: PeerJ Inc. 2021
Materias:
Evolutionary Studies
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7953880/
https://www.ncbi.nlm.nih.gov/pubmed/33854833
http://dx.doi.org/10.7717/peerj.10948

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7953880/
https://www.ncbi.nlm.nih.gov/pubmed/33854833
http://dx.doi.org/10.7717/peerj.10948

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