Viscous strengthening followed by slip weakening during frictional melting of chert

Abstract Pelagic chert is one of the major lithologies in accretionary complexes. Thus, frictional properties of chert at seismic slip rates are important for understanding of earthquake faulting in subduction zones. Here, we conducted high-velocity friction experiments on chert collected from the J...

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Main Authors: Ginta Motohashi, Kiyokazu Oohashi, Kohtaro Ujiie
Format: Article
Language:English
Published: SpringerOpen 2019-05-01
Series:Earth, Planets and Space
Subjects:
Online Access:http://link.springer.com/article/10.1186/s40623-019-1035-5
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author Ginta Motohashi
Kiyokazu Oohashi
Kohtaro Ujiie
author_facet Ginta Motohashi
Kiyokazu Oohashi
Kohtaro Ujiie
author_sort Ginta Motohashi
collection DOAJ
description Abstract Pelagic chert is one of the major lithologies in accretionary complexes. Thus, frictional properties of chert at seismic slip rates are important for understanding of earthquake faulting in subduction zones. Here, we conducted high-velocity friction experiments on chert collected from the Jurassic accretionary complex in central Japan at a slip rate of 1.3 m/s and normal stresses of 5–13 MPa under room humidity conditions. The results show that initial slip weakening was followed by slip strengthening and subsequent second slip weakening toward a steady-state shear strength. Slip strengthening resulted from the formation of a silica-rich melt layer at lower melting temperatures than expected, which could be due to the presence of water in the illite-containing chert. The second slip weakening may be occurred due to a decrease in shear strain rate associated with the thickening of the melt layer.
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spelling doaj.art-7bd14d03644649c2878f26724a7c94e92022-12-22T00:29:14ZengSpringerOpenEarth, Planets and Space1880-59812019-05-017111710.1186/s40623-019-1035-5Viscous strengthening followed by slip weakening during frictional melting of chertGinta Motohashi0Kiyokazu Oohashi1Kohtaro Ujiie2Graduate School of Life and Environmental Sciences, University of TsukubaGraduate School of Sciences and Technology for Innovation, Yamaguchi UniversityGraduate School of Life and Environmental Sciences, University of TsukubaAbstract Pelagic chert is one of the major lithologies in accretionary complexes. Thus, frictional properties of chert at seismic slip rates are important for understanding of earthquake faulting in subduction zones. Here, we conducted high-velocity friction experiments on chert collected from the Jurassic accretionary complex in central Japan at a slip rate of 1.3 m/s and normal stresses of 5–13 MPa under room humidity conditions. The results show that initial slip weakening was followed by slip strengthening and subsequent second slip weakening toward a steady-state shear strength. Slip strengthening resulted from the formation of a silica-rich melt layer at lower melting temperatures than expected, which could be due to the presence of water in the illite-containing chert. The second slip weakening may be occurred due to a decrease in shear strain rate associated with the thickening of the melt layer.http://link.springer.com/article/10.1186/s40623-019-1035-5Frictional meltingPelagic chertViscous strengtheningSilica-rich melt
spellingShingle Ginta Motohashi
Kiyokazu Oohashi
Kohtaro Ujiie
Viscous strengthening followed by slip weakening during frictional melting of chert
Earth, Planets and Space
Frictional melting
Pelagic chert
Viscous strengthening
Silica-rich melt
title Viscous strengthening followed by slip weakening during frictional melting of chert
title_full Viscous strengthening followed by slip weakening during frictional melting of chert
title_fullStr Viscous strengthening followed by slip weakening during frictional melting of chert
title_full_unstemmed Viscous strengthening followed by slip weakening during frictional melting of chert
title_short Viscous strengthening followed by slip weakening during frictional melting of chert
title_sort viscous strengthening followed by slip weakening during frictional melting of chert
topic Frictional melting
Pelagic chert
Viscous strengthening
Silica-rich melt
url http://link.springer.com/article/10.1186/s40623-019-1035-5
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AT kohtaroujiie viscousstrengtheningfollowedbyslipweakeningduringfrictionalmeltingofchert