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Transient stripping of subducting slabs controls periodic forearc uplift
Topography in forearc regions reflects tectonic processes along the subduction interface, from seismic cycle-related transients to long-term competition between accretion and erosion. Yet, no consensus exists about the topography drivers, especially as the contribution of deep accretion remains poor...
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| Yayımlandı: | Nat Commun |
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| Asıl Yazarlar: | , , , , , |
| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
Nature Publishing Group UK
2020
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| Konular: | |
| Online Erişim: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7156703/ https://ncbi.nlm.nih.gov/pubmed/32286304 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-020-15580-7 |
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