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• W3183770145 abstract "Despite the critical role of subduction in plate tectonics, the dynamics of its initiation remains unclear. High-temperature low-pressure metamorphic soles are vestiges of subduction initiation, providing records of the pressure and temperature conditions along the subducting slab surface during subduction initiation that can possibly differentiate the two end-member subduction initiation modes: spontaneous and induced. Here, using numerical models, we show that the slab surface temperature reaches 800-900 °C at ~1 GPa over a wide range of parameter values for spontaneous subduction initiation whereas for induced subduction initiation, such conditions can be reached only if the age of the overriding plate is <5 Ma. These modeling results indicate that spontaneous subduction initiation would be more favorable for creating high-temperature conditions. However, the synthesis of our modeling results and geological observations indicate that the majority of the metamorphic soles likely formed during induced subduction initiation that involved a young overriding plate." @default.
• W3183770145 created "2021-08-02" @default.
• W3183770145 creator A5018469520 @default.
• W3183770145 creator A5055260143 @default.
• W3183770145 date "2021-07-30" @default.
• W3183770145 modified "2023-10-14" @default.
• W3183770145 title "Differentiating induced versus spontaneous subduction initiation using thermomechanical models and metamorphic soles" @default.
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• W3183770145 doi "https://doi.org/10.1038/s41467-021-24896-x" @default.
• W3183770145 hasPubMedCentralId "https://www.ncbi.nlm.nih.gov/pmc/articles/8324860" @default.
• W3183770145 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/34330929" @default.
• W3183770145 hasPublicationYear "2021" @default.
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• W3183770145 hasAuthorship W3183770145A5018469520 @default.

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