Observation of fault gouge development in laboratory see-through experiments

Kerry Haggert, Simon J.D. Cox, Mark W. Jessell

Research output: Contribution to journalArticle

7 Citations (Scopus)

Abstract

We describe the results of a set of brittle sliding and wear experiments on thin sheets of polycrystalline sodium nitrate. We have built a new brittle deformation apparatus that allowed us to simultaneously observe the microstructural evolution under the microscope, and measure the mechanical response of the material. The microstructural history was recorded using a video microscopy technique and selected frames were then digitized and analysed. Fault gouge in these experiments was the direct product of frictional wear and was produced dominantly by intense intergranular fracturing and accompanying grain surface erosion. Although an increase in displacement was accompanied by an increase in gouge zone width, the development of a gouge zone is not a constant process either with respect to displacement, or with respect to the spatial distribution along the fault zone.

Original languageEnglish
Pages (from-to)123-136
Number of pages14
JournalTectonophysics
Volume204
Issue number1-2
DOIs
Publication statusPublished - 30 Mar 1992
Externally publishedYes

Fingerprint

fault gouge
sodium nitrates
brittle deformation
fracturing
erosion
sliding
fault zone
microscopy
spatial distribution
experiment
microscopes
sodium
histories
nitrate
products
history
laboratory
video
material
product

Cite this

Haggert, Kerry ; Cox, Simon J.D. ; Jessell, Mark W. / Observation of fault gouge development in laboratory see-through experiments. In: Tectonophysics. 1992 ; Vol. 204, No. 1-2. pp. 123-136.
@article{afaa7951d571442a9deb7d65c03f0539,
title = "Observation of fault gouge development in laboratory see-through experiments",
abstract = "We describe the results of a set of brittle sliding and wear experiments on thin sheets of polycrystalline sodium nitrate. We have built a new brittle deformation apparatus that allowed us to simultaneously observe the microstructural evolution under the microscope, and measure the mechanical response of the material. The microstructural history was recorded using a video microscopy technique and selected frames were then digitized and analysed. Fault gouge in these experiments was the direct product of frictional wear and was produced dominantly by intense intergranular fracturing and accompanying grain surface erosion. Although an increase in displacement was accompanied by an increase in gouge zone width, the development of a gouge zone is not a constant process either with respect to displacement, or with respect to the spatial distribution along the fault zone.",
author = "Kerry Haggert and Cox, {Simon J.D.} and Jessell, {Mark W.}",
year = "1992",
month = "3",
day = "30",
doi = "10.1016/0040-1951(92)90274-A",
language = "English",
volume = "204",
pages = "123--136",
journal = "Tectonophysics",
issn = "0040-1951",
publisher = "Elsevier",
number = "1-2",

}

Observation of fault gouge development in laboratory see-through experiments. / Haggert, Kerry; Cox, Simon J.D.; Jessell, Mark W.

In: Tectonophysics, Vol. 204, No. 1-2, 30.03.1992, p. 123-136.

Research output: Contribution to journalArticle

TY - JOUR

T1 - Observation of fault gouge development in laboratory see-through experiments

AU - Haggert, Kerry

AU - Cox, Simon J.D.

AU - Jessell, Mark W.

PY - 1992/3/30

Y1 - 1992/3/30

N2 - We describe the results of a set of brittle sliding and wear experiments on thin sheets of polycrystalline sodium nitrate. We have built a new brittle deformation apparatus that allowed us to simultaneously observe the microstructural evolution under the microscope, and measure the mechanical response of the material. The microstructural history was recorded using a video microscopy technique and selected frames were then digitized and analysed. Fault gouge in these experiments was the direct product of frictional wear and was produced dominantly by intense intergranular fracturing and accompanying grain surface erosion. Although an increase in displacement was accompanied by an increase in gouge zone width, the development of a gouge zone is not a constant process either with respect to displacement, or with respect to the spatial distribution along the fault zone.

AB - We describe the results of a set of brittle sliding and wear experiments on thin sheets of polycrystalline sodium nitrate. We have built a new brittle deformation apparatus that allowed us to simultaneously observe the microstructural evolution under the microscope, and measure the mechanical response of the material. The microstructural history was recorded using a video microscopy technique and selected frames were then digitized and analysed. Fault gouge in these experiments was the direct product of frictional wear and was produced dominantly by intense intergranular fracturing and accompanying grain surface erosion. Although an increase in displacement was accompanied by an increase in gouge zone width, the development of a gouge zone is not a constant process either with respect to displacement, or with respect to the spatial distribution along the fault zone.

UR - http://www.scopus.com/inward/record.url?scp=0026460777&partnerID=8YFLogxK

U2 - 10.1016/0040-1951(92)90274-A

DO - 10.1016/0040-1951(92)90274-A

M3 - Article

VL - 204

SP - 123

EP - 136

JO - Tectonophysics

JF - Tectonophysics

SN - 0040-1951

IS - 1-2

ER -