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The effect of metastable pyroxene on the slab dynamics

Agrusta, R.; van Hunen, J.; Goes, S.

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Authors

R. Agrusta

S. Goes



Abstract

Seismic studies show that some subducting slabs penetrate straight into the lower mantle, whereas others seem to flatten near the base of the mantle transition zone. Slab stagnation is often attributed to an increase in viscosity and phase transformations in the olivine system. However, recent mineral physics studies showed that due to extremely low transformational diffusion rates, low-density metastable pyroxene may persist into the transition zone in cool slabs. Here we use a dynamically fully self-consistent subduction model to investigate the influence of metastable pyroxene on the dynamics of subducting oceanic lithosphere. Our results show that metastable pyroxene affects slab buoyancy at least as much as olivine metastability. However, unlike metastable olivine, which can inhibit slab penetration in the lower mantle only for cold, old, and fast slabs, metastable pyroxene is likely to also affect sinking of relatively young and slow slabs.

Citation

Agrusta, R., van Hunen, J., & Goes, S. (2014). The effect of metastable pyroxene on the slab dynamics. Geophysical Research Letters, 41(24), 8800-8808. https://doi.org/10.1002/2014gl062159

Journal Article Type Article
Acceptance Date Dec 6, 2014
Online Publication Date Dec 20, 2014
Publication Date Dec 28, 2014
Deposit Date Jan 4, 2015
Publicly Available Date Jan 22, 2015
Journal Geophysical Research Letters
Print ISSN 0094-8276
Electronic ISSN 1944-8007
Publisher Wiley
Peer Reviewed Peer Reviewed
Volume 41
Issue 24
Pages 8800-8808
DOI https://doi.org/10.1002/2014gl062159
Keywords Subduction, Metastable pyroxene, Phase transition.

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Published Journal Article (Advance online version) (503 Kb)
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Publisher Licence URL
http://creativecommons.org/licenses/by/4.0/

Copyright Statement
Advance online version ©2015. The authors. 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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