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Indian plate paleogeography, subduction and horizontal underthrusting below Tibet: paradoxes, controversies and opportunities
The India–Asia collision zone is the archetype to calibrate geological responses to continent–continent collision, but hosts a paradox: there is no orogen-wide geological record of oceanic subduction after initial collision around 60–55 Ma, yet thousands of kilometers of post-collisional subduction...
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Oxford University Press
2022
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9385461/ https://www.ncbi.nlm.nih.gov/pubmed/35992242 http://dx.doi.org/10.1093/nsr/nwac074 |