Tracking the migration of the Indian continent using the carbonate clumped isotope technique on Phanerozoic soil carbonates

Approximately 140 million years ago, the Indian plate separated from Gondwana and migrated by almost 90° latitude to its current location, forming the Himalayan-Tibetan system. Large discrepancies exist in the rate of migration of Indian plate during Phanerozoic. Here we describe a new approach to p...

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Detalles Bibliográficos
Autores principales: Ghosh, Prosenjit, Vasiliev, Mikhail V., Ghosh, Parthasarathi, Sarkar, Soumen, Ghosh, Sampa, Yamada, Keita, Ueno, Yuichiro, Yoshida, Naohiro, Poulsen, Christopher J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4773985/
https://www.ncbi.nlm.nih.gov/pubmed/26931069
http://dx.doi.org/10.1038/srep22187

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4773985/
https://www.ncbi.nlm.nih.gov/pubmed/26931069
http://dx.doi.org/10.1038/srep22187

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