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South-American plate advance and forced Andean trench retreat as drivers for transient flat subduction episodes
At two trench segments below the Andes, the Nazca Plate is subducting sub-horizontally over ∼200–300 km, thought to result from a combination of buoyant oceanic-plateau subduction and hydrodynamic mantle-wedge suction. Whether the actual conditions for both processes to work in concert existed is un...
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| 出版年: | Nat Commun |
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| 主要な著者: | , , , , , |
| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
Nature Publishing Group
2017
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| 主題: | |
| オンライン･アクセス: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5440808/ https://ncbi.nlm.nih.gov/pubmed/28508893 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms15249 |
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