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An Exhumation Pulse From the Nascent Franciscan Subduction Zone (California, USA)

Rutte, DanielORCIDiD
Garber, JoshuaORCIDiD
Kylander-Clark, AndrewORCIDiD
Renne, Paul R.ORCIDiD
DOI: https://doi.org/10.1029/2020TC006305
Persistent URL: http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/9493
Rutte, Daniel; Garber, Joshua; Kylander-Clark, Andrew; Renne, Paul R., 2020: An Exhumation Pulse From the Nascent Franciscan Subduction Zone (California, USA). In: Tectonics, Band 39, 10, DOI: 10.1029/2020TC006305.
 
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  • Abstract
We investigated a suite of metabasite blocks from serpentinite matrix and shale matrix mélanges of the California Coast Ranges. Our new data set consists of 40Ar/39Ar dates of amphibole and phengite and U-Pb dates of metamorphic zircon. Combined with published geochronology, including prograde Lu-Hf garnet ages from the same blocks, we can reconstruct the timing and time scales of prograde and retrograde metamorphism of individual blocks. In particular we find that exhumation from amphibole-eclogite facies conditions occurred as a single episode at 165–157 Ma, with an apparent southward younging trend. The rate and timing of exhumation were initially uniform (when comparing individual blocks) and fast (with cooling rates up to ~140°C/Ma). In the cooler and shallower blueschist facies, exhumation slowed and became less uniform among blocks. Considering the subduction zone system, the high-grade exhumation temporally correlates with a magmatic arc pulse (Sierra Nevada) and the termination of forearc spreading (Coast Range Ophiolite). Our findings suggest that a geodynamic one-time event led to exhumation of amphibole-eclogite facies rocks. We propose that interaction of the Franciscan subduction zone with a spreading ridge led to extraction of the forearc mantle wedge from its position between forearc crust and subducting crust. The extraction led to fast and uniform exhumation of subducted rocks into the blueschist facies. We also show that the Franciscan subduction zone did not undergo significant cooling over time and that its initiation was not coeval with blueschist-facies metamorphism of the Red Ant schist of the Sierra Nevada foothills.
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  • Geologie [755]
Subjects:
subduction zone
eclogite exhumation
mantle extraction
block-in-matrix mélange
Franciscan Complex
petrochronology
This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.

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