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Ultralow Friction of Carbonate Faults Caused by Thermal Decomposition

Han, Raehee, Shimamoto, Toshihiko, Hirose, Takehiro, Ree, Jin-Han, Ando, Jun-ichi·2007·Science

Abstract

High-velocity weakening of faults may drive fault motion during large earthquakes. Experiments on simulated faults in Carrara marble at slip rates up to 1.3 meters per second demonstrate that thermal decomposition of calcite due to frictional heating induces pronounced fault weakening with steady-state friction coefficients as low as 0.06. Decomposition produces particles of tens of nanometers in size, and the ultralow friction appears to be associated with the flash heating on an ultrafine decomposition product. Thus, thermal decomposition may be an important process for the dynamic weakening of faults.

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Metadata

Authors
Han, R., Shimamoto, T., Hirose, T., Ree, J.-H., & Ando, J.-I.
Venue
Science
Published
2007-05-11
Volume
316
Issue
5826
Pages
878-881
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W1998037923
Cited by
430
References
0
FWCI
23.05
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Ultralow Friction of Carbonate Faults Caused by Thermal Decomposition. https://app.cochat.ai/papers/10.1126/science.1139763
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Han, R., Shimamoto, T., Hirose, T., Ree, J.-H., & Ando, J.-I. (2007). Ultralow Friction of Carbonate Faults Caused by Thermal Decomposition. Science. https://doi.org/10.1126/science.1139763

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

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