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Direct Evidence for Fluid Pressure, Dilatancy, and Compaction Affecting Slip in Isolated Faults

Proctor, B; Lockner, DA; Kilgore, BD; Mitchell, TM; Beeler, NM; (2020) Direct Evidence for Fluid Pressure, Dilatancy, and Compaction Affecting Slip in Isolated Faults. Geophysical Research Letters , 47 (16) , Article e2019GL086767. 10.1029/2019gl086767. Green open access

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Abstract

Earthquake instability occurs as a result of strength loss during sliding on a fault. It has been known for over 50 years that fault compaction or dilatancy may cause significant weakening or strengthening by dramatically changing the fluid pressure trapped in faults. Despite this fundamental importance, we have no real understanding of the exact conditions that lead to compaction or dilation during nucleation or rupture. To date, no direct measurements of pore pressure changes during slip in hydraulically isolated faults have been reported. We show direct examples of fluid pressure variations during nucleation and rupture using a miniature pressure transducer embedded in an experimental fault. We demonstrate that fluids not only are significant in controlling fault behavior but can provide the dominant mechanism controlling fault stability. The effect of fluid pressure changes can exceed frictional variations predicted by rate‐ and state‐dependent friction laws, exerting fundamental controls on earthquake rupture initiation.

Type: Article
Title: Direct Evidence for Fluid Pressure, Dilatancy, and Compaction Affecting Slip in Isolated Faults
Open access status: An open access version is available from UCL Discovery
DOI: 10.1029/2019gl086767
Publisher version: https://doi.org/10.1029/2019gl086767
Language: English
Additional information: Copyright © 2020. The Authors. This is an open access article under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/), which permits use, distribution and reproduction in any medium, provided the original work is properly cited.
Keywords: fluid pressure, dilatancy, compaction, earthquake dynamics, instability, slow slip
UCL classification: UCL
UCL > Provost and Vice Provost Offices > UCL BEAMS
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences > Dept of Earth Sciences
URI: https://discovery.ucl.ac.uk/id/eprint/10103682
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