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Mantle wedge diapirs detected by a dense seismic array in Northern Taiwan
It is conventionally believed that magma generation beneath the volcanic arc is triggered by the infiltration of fluids or melts derived from the subducted slab. However, recently geochemical analyses argue the arc magma may be formed by mélange diapirs that are physically mixed by sediment, altered...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2021
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7810894/ https://www.ncbi.nlm.nih.gov/pubmed/33452469 http://dx.doi.org/10.1038/s41598-021-81357-7 |