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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Váldodahkkit:	W. Hoover, C. B. Condit, A. Moser, S. Mulcahy, P. C. Lindquist, V. E. Guevara
Materiálatiipa:	Artigo
Giella:	Inglês
Almmustuhtton:	Wiley 2025-10-01
Ráidu:	Geochemistry, Geophysics, Geosystems
Fáttát:	subduction zone petrochronology metasomatic rock slow slip titanite rutile
Liŋkkat:	https://doi.org/10.1029/2025GC012313
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