Mantle wedge diapirs detected by a dense seismic array in Northern Taiwan

Abstract 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...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Cheng-Horng Lin, Min-Hung Shih, Ya-Chuan Lai
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2021
Materias:
R
Q
Acceso en línea:https://doaj.org/article/e431e17415d84967a86915e01369968e
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!