Metasomatism and Mélange Development at the Conditions of Modern Deep Slow Slip: P‐T‐t Evolution of Metasomatic Rocks (Pimu'nga/Santa Catalina Island, CA)

Abstract The subduction interface hosts megathrust earthquakes and ductile creep, is fluid‐rich and chemically dynamic, and produces metasomatic rocks that may host episodic tremor and slow slip (ETS). However, determining the depths at which these metasomatic rocks form and deform remains challengi...

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Principais autores:	W. Hoover, C. B. Condit, A. Moser, S. Mulcahy, P. C. Lindquist, V. E. Guevara
Formato:	Artigo
Idioma:	Inglês
Publicado em:	Wiley 2025-10-01
Colecção:	Geochemistry, Geophysics, Geosystems
Assuntos:	subduction zone petrochronology metasomatic rock slow slip titanite rutile
Acesso em linha:	https://doi.org/10.1029/2025GC012313
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