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Differential growth of the northern Tibetan margin: evidence for oblique stepwise rise of the Tibetan Plateau
Models of how high elevations formed across Tibet predict: (a) the continuous thickening of a “viscous sheet”; (b) time-dependent, oblique stepwise growth; and (c) synchronous deformation across Tibet that accompanied collision. Our new observations may shed light on this issue. Here, we use (40)Ar/...
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| Pubblicato in: | Sci Rep |
|---|---|
| Autori principali: | , , , , , , |
| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
Nature Publishing Group
2017
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| Soggetti: | |
| Accesso online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5259709/ https://ncbi.nlm.nih.gov/pubmed/28117351 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep41164 |
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