Low palaeoelevation of the northern Lhasa terrane during late Eocene: Fossil foraminifera and stable isotope evidence from the Gerze Basin

The Lhasa terrane is a key region for understanding the paleoelevation of the southern Tibetan Plateau after India-Asia collision. The Gerze Basin, located in the northern part of the Lhasa terrane, is a shortening-related basin. We discovered Lagena laevis (Bandy) fossils in upper Eocene strata of...

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Detalles Bibliográficos
Autores principales: Wei, Yi, Zhang, Kexin, Garzione, Carmala N., Xu, Yadong, Song, Bowen, Ji, Junliang
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4897749/
https://www.ncbi.nlm.nih.gov/pubmed/27272610
http://dx.doi.org/10.1038/srep27508

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4897749/
https://www.ncbi.nlm.nih.gov/pubmed/27272610
http://dx.doi.org/10.1038/srep27508

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