A Mélange of Subduction Ages: Constraints on the Timescale of Shear Zone Development and Underplating at the Subduction Interface, Catalina Schist (CA, USA)

Abstract The presence of mélange at the subduction interface influences numerous geochemical and geophysical processes. However, the relationship between the timescales of mélange development, deformation, and resultant mass transport is poorly understood. Here, we use Sm‐Nd garnet geochronology to...

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Bibliographic Details
Main Authors: K. M. Harvey, S. Walker, P. G. Starr, S. C. Penniston‐Dorland, M. J. Kohn, E. F. Baxter
Format: Article
Language:English
Published: Wiley 2021-09-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
Online Access:https://doi.org/10.1029/2021GC009790