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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/...
Autores principales: | Wang, Fei, Shi, Wenbei, Zhang, Weibin, Wu, Lin, Yang, Liekun, Wang, Yinzhi, Zhu, Rixiang |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group
2017
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5259709/ https://www.ncbi.nlm.nih.gov/pubmed/28117351 http://dx.doi.org/10.1038/srep41164 |
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