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Seismic imaging of subduction zone metamorphism

Rondenay, Stéphane, Abers, Geoffrey A., van Keken, Peter E.·2008·Geology

Abstract

Combined analysis of high-resolution seismic images of the Alaska and Cascadia subduction zones reveals where metamorphic fl uids are released. Both images show the subducted oceanic crust as a dipping low-velocity layer with a clear termination depth. However, in Alaska the crust is thicker (15-20 km compared to 8 km) and terminates at greater depth (120 km com- pared to 40 km) than in Cascadia. Based on metamorphic reaction estimates and geodynamic models, we demonstrate that the termination depth corresponds to eclogitization of the crust triggered by dehydration of water-bearing minerals, and that the location of this reaction is dependent on the thermal structure of the subducted slab.

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Metadata

Authors
Rondenay, S., Abers, G. A., & van Keken, P. E.
Venue
Geology
Published
2008
Volume
36
Issue
4
Pages
275
ISSN
0091-7613 (ISSN-L)
OpenAlex
W2009367373
Cited by
219
References
1
FWCI
15.74
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Seismic imaging of subduction zone metamorphism. https://app.cochat.ai/papers/10.1130/g24112a.1
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Rondenay, S., Abers, G. A., & van Keken, P. E. (2008). Seismic imaging of subduction zone metamorphism. Geology. https://doi.org/10.1130/g24112a.1

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