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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...
| Autores principales: | , , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group
2016
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| Materias: | |
| 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 |