The role of water in fault lubrication

Friction plays a key role in fault slip between tectonic plates. Here, the authors demonstrate through friction experiments on calcite in brines that pressure solution at high stresses and slow sliding velocities leads to a prominent decrease in friction and therefore is a weakening mechanism in fau...

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Main Authors: Yijue Diao, Rosa M. Espinosa-Marzal
Format: Article
Language:English
Published: Nature Publishing Group 2018-06-01
Series:Nature Communications
Online Access:https://doi.org/10.1038/s41467-018-04782-9
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spelling doaj-b1f0e0fb36344c04afc52176306f64182021-05-11T10:17:33ZengNature Publishing GroupNature Communications2041-17232018-06-019111010.1038/s41467-018-04782-9The role of water in fault lubricationYijue Diao0Rosa M. Espinosa-Marzal1Civil and Environmental Engineering, University of Illinois at Urbana-ChampaignCivil and Environmental Engineering, University of Illinois at Urbana-ChampaignFriction plays a key role in fault slip between tectonic plates. Here, the authors demonstrate through friction experiments on calcite in brines that pressure solution at high stresses and slow sliding velocities leads to a prominent decrease in friction and therefore is a weakening mechanism in fault strength.https://doi.org/10.1038/s41467-018-04782-9
collection DOAJ
language English
format Article
sources DOAJ
author Yijue Diao
Rosa M. Espinosa-Marzal
spellingShingle Yijue Diao
Rosa M. Espinosa-Marzal
The role of water in fault lubrication
Nature Communications
author_facet Yijue Diao
Rosa M. Espinosa-Marzal
author_sort Yijue Diao
title The role of water in fault lubrication
title_short The role of water in fault lubrication
title_full The role of water in fault lubrication
title_fullStr The role of water in fault lubrication
title_full_unstemmed The role of water in fault lubrication
title_sort role of water in fault lubrication
publisher Nature Publishing Group
series Nature Communications
issn 2041-1723
publishDate 2018-06-01
description Friction plays a key role in fault slip between tectonic plates. Here, the authors demonstrate through friction experiments on calcite in brines that pressure solution at high stresses and slow sliding velocities leads to a prominent decrease in friction and therefore is a weakening mechanism in fault strength.
url https://doi.org/10.1038/s41467-018-04782-9
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