Deformation microfabric development in chalcopyrite in fault zones, Mt. Lyell, Tasmania

S. F. Cox; MA ETHERIDGE

doi:10.1016/0191-8141(85)90058-6

Deformation microfabric development in chalcopyrite in fault zones, Mt. Lyell, Tasmania

S. F. Cox, MA ETHERIDGE

Research output: Contribution to journal › Meeting abstract › peer-review

Abstract

Deformation of chalcopyrite (CuFeS2) under low-grade metamorphic
conditions within fault zones in the Mt. Lyell area of western
Tasmania (Australia) has occurred dominantly by a dislocation flow
process. Elongate grain fabrics and well-developed crystallographic
preferred orientations have developed by { 112} (110)/(20l) dislocation
glide. However, the presence of recovered dislocation substructures
indicates that dislocation climb has also been important.

Original language	English
Pages (from-to)	490-490
Number of pages	1
Journal	Journal of Structural Geology
Volume	7
Issue number	3-4
DOIs	https://doi.org/10.1016/0191-8141(85)90058-6
Publication status	Published - 1985
Externally published	Yes

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@article{16c4fbd862c14949887072cd75550ff3,

title = "Deformation microfabric development in chalcopyrite in fault zones, Mt. Lyell, Tasmania",

abstract = "Deformation of chalcopyrite (CuFeS2) under low-grade metamorphic conditions within fault zones in the Mt. Lyell area of western Tasmania (Australia) has occurred dominantly by a dislocation flow process. Elongate grain fabrics and well-developed crystallographic preferred orientations have developed by \{ 112\} (110)/(20l) dislocation glide. However, the presence of recovered dislocation substructures indicates that dislocation climb has also been important. ",

author = "Cox, \{S. F.\} and MA ETHERIDGE",

year = "1985",

doi = "10.1016/0191-8141(85)90058-6",

language = "English",

volume = "7",

pages = "490--490",

journal = "Journal of Structural Geology",

issn = "0191-8141",

publisher = "Elsevier",

number = "3-4",

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TY - JOUR

T1 - Deformation microfabric development in chalcopyrite in fault zones, Mt. Lyell, Tasmania

AU - Cox, S. F.

AU - ETHERIDGE, MA

PY - 1985

Y1 - 1985

N2 - Deformation of chalcopyrite (CuFeS2) under low-grade metamorphic conditions within fault zones in the Mt. Lyell area of western Tasmania (Australia) has occurred dominantly by a dislocation flow process. Elongate grain fabrics and well-developed crystallographic preferred orientations have developed by { 112} (110)/(20l) dislocation glide. However, the presence of recovered dislocation substructures indicates that dislocation climb has also been important.

AB - Deformation of chalcopyrite (CuFeS2) under low-grade metamorphic conditions within fault zones in the Mt. Lyell area of western Tasmania (Australia) has occurred dominantly by a dislocation flow process. Elongate grain fabrics and well-developed crystallographic preferred orientations have developed by { 112} (110)/(20l) dislocation glide. However, the presence of recovered dislocation substructures indicates that dislocation climb has also been important.

U2 - 10.1016/0191-8141(85)90058-6

DO - 10.1016/0191-8141(85)90058-6

M3 - Meeting abstract

SN - 0191-8141

VL - 7

SP - 490

EP - 490

JO - Journal of Structural Geology

JF - Journal of Structural Geology

IS - 3-4

ER -

Deformation microfabric development in chalcopyrite in fault zones, Mt. Lyell, Tasmania

Abstract

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