Campus Units

Geological and Atmospheric Sciences

Document Type

Article

Publication Version

Published Version

Publication Date

5-28-2014

Journal or Book Title

Geophysical Research Letters

Volume

41

Issue

10

First Page

3471

Last Page

3477

DOI

10.1002/2014GL059832

Abstract

Crustal deformation can occur via stick-slip events, viscous creep, or strain transients at variable rates. Here we explore such strain transients with physical experiments comprising a quasi-two-dimensional shear zone with elastic, acrylic discs and interstitial viscous silicone. Experiments of solely elastic discs produce stick-slip events and an overall (constant volume) strengthening. The addition of the viscous silicone enhances localization but does not greatly change the overall pattern of strengthening. It does, however, damp the stick-slip events, leading to transient, creep-like behavior that approaches the behavior of a Maxwell body. There is no gradual transition from frictional to viscous deformation with increasing amounts of silicone, suggesting that the mixed rheology is in effect as soon as an interstitial fluid is present. Our experiments support the hypothesis that a possible cause for strain transients in nature is an interstitial viscous phase in shear zones.

Comments

This article is published as Reber, Jacqueline E., Nicholas W. Hayman, and Luc L. Lavier. "Stick‐slip and creep behavior in lubricated granular material: Insights into the brittle‐ductile transition." Geophysical Research Letters 41, no. 10 (2014): 3471-3477. DOI:10.1002/2014GL059832. Posted with permission.

Copyright Owner

American Geophysical Union

Language

en

File Format

application/pdf

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