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Dislocation interactions in olivine control postseismic creep of the upper mantle

Abstract:
Changes in stress applied to mantle rocks, such as those imposed by earthquakes, commonly induce a period of transient creep, which is often modelled based on stress transfer among slip systems due to grain interactions. However, recent experiments have demonstrated that the accumulation of stresses among dislocations is the dominant cause of strain hardening in olivine at temperatures ≤600 °C, raising the question of whether the same process contributes to transient creep at higher temperatures. Here, we demonstrate that olivine samples deformed at 25 °C or 1150–1250 °C both preserve stress heterogeneities of ~1 GPa that are imparted by dislocations and have correlation lengths of ~1 μm. The similar stress distributions formed at these different temperatures indicate that accumulation of stresses among dislocations also provides a contribution to transient creep at high temperatures. The results motivate a new generation of models that capture these intragranular processes and may refine predictions of evolving mantle viscosity over the earthquake cycle.
Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1038/s41467-021-23633-8

Authors

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Role:
Author
ORCID:
0000-0001-9212-3734
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Institution:
University of Oxford
Division:
MPLS
Department:
Materials
Oxford college:
St Cross College
Role:
Author
ORCID:
0000-0002-8801-4102
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Role:
Author
ORCID:
0000-0002-3152-9105


Publisher:
Springer Nature
Journal:
Nature Communications More from this journal
Volume:
12
Issue:
1
Article number:
3496
Publication date:
2021-06-09
Acceptance date:
2021-05-05
DOI:
EISSN:
2041-1723


Language:
English
Keywords:
Pubs id:
1181560
Local pid:
pubs:1181560
Deposit date:
2021-06-13
ARK identifier:

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