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...
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 |
Similar Items
-
Constraints on tectonic processes in subduction mélange: A review of insights from the Catalina Schist (CA, USA)
by: Sarah C. Penniston-Dorland, et al.
Published: (2023-08-01) -
Serpentinites and serpentinites within a fossil subduction channel: La Corea mélange, eastern Cuba
by: I.F. BLANCO QUINTERO, et al.
Published: (2011-11-01) -
Neotethyan Ankara Melange, central Turkey: Formation by accretion of seamounts and supra-subduction zone ophiolites in an oceanic fore-arc setting
by: Alastair H.F. Robertson, et al.
Published: (2023-12-01) -
Source and Migration of Fluids in a Meso-Tethyan Subduction Zone: Fluid Inclusion Study of Syn-Mélange Veins from the Mugagangri Accretionary Complex
by: Xinyu Liu, et al.
Published: (2023-09-01) -
Mélanges and chaotic rock units: Implications for exhumed subduction complexes and orogenic belts
by: Andrea Festa, et al.
Published: (2022-05-01)