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Paleocene latitude of the Kohistan–Ladakh arc indicates multistage India–Eurasia collision
We report paleomagnetic data showing that an intraoceanic Trans-Tethyan subduction zone existed south of the Eurasian continent and north of the Indian subcontinent until at least Paleocene time. This system was active between 66 and 62 Ma at a paleolatitude of 8.1 ± 5.6 °N, placing it 600–2,300 km...
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| Publicat a: | Proc Natl Acad Sci U S A |
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| Autors principals: | , , , , , , , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
National Academy of Sciences
2020
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7703637/ https://ncbi.nlm.nih.gov/pubmed/33148806 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.2009039117 |
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