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The effect of metamorphism on the aggregate properties of gabbroic rocks

Urueña, Cindy LU orcid ; Möller, Charlotte LU ; Andersson, Jenny ; Lindqvist, Jan Erik and Göransson, Mattias (2022) In Bulletin of Engineering Geology and the Environment 81(5).
Abstract

Granitic rocks are durable materials sought after for the production of road and railroad aggregates. Granitic bedrock commonly, however, includes gabbroic components, which may enhance or decrease the aggregate performance. This study evaluates the variation in resistance to fragmentation (Los Angeles value, LA) and wear/abrasion (micro-Deval value, MDE) for the fraction 10/14 mm of gabbro in different metamorphic states. Samples were collected along a 150-km profile where metamorphic conditions grade from epidote–amphibolite to high-pressure granulite-facies, and the degree of metamorphic recrystallization varies with the amount of hydrous fluid. Rocks with no or incipient metamorphic recrystallization preserving their... (More)

Granitic rocks are durable materials sought after for the production of road and railroad aggregates. Granitic bedrock commonly, however, includes gabbroic components, which may enhance or decrease the aggregate performance. This study evaluates the variation in resistance to fragmentation (Los Angeles value, LA) and wear/abrasion (micro-Deval value, MDE) for the fraction 10/14 mm of gabbro in different metamorphic states. Samples were collected along a 150-km profile where metamorphic conditions grade from epidote–amphibolite to high-pressure granulite-facies, and the degree of metamorphic recrystallization varies with the amount of hydrous fluid. Rocks with no or incipient metamorphic recrystallization preserving their primary igneous fabric and interlocking texture meet the criteria for both asphalt base course and track ballast in railroad, with LA and MDE values below 25% and 14%, respectively. Mafic granulite and fine-grained amphibolite have LA values below 25% and can be used in unbound layers. Mafic granulites crystallize at high temperatures but commonly preserve a relict igneous texture due to limited hydration. Coarse-grained amphibolite and migmatitic amphibolite have the poorest performance. They recrystallized at hydrous conditions, leading to complete recrystallization, grain coarsening, and loss of interlocking igneous texture. This study shows that both temperature and infiltration of hydrous fluids significantly affect the technical properties. Even at high metamorphic temperatures, gabbroic rocks may yield aggregates of high technical performance. At hydrous conditions, however, recrystallization results in rock aggregates suitable for unbound layers only. The variation in metamorphic grade and hydration is easily assessed by the geologist in the field and by using standard petrographic microscopy.

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Please use this url to cite or link to this publication:
author
; ; ; and
organization
publishing date
type
Contribution to journal
publication status
published
subject
keywords
Crushed rock aggregates, Gabbroic rocks, Los Angeles, Metamorphic recrystallization, Micro-Deval
in
Bulletin of Engineering Geology and the Environment
volume
81
issue
5
article number
213
publisher
Springer
external identifiers
  • scopus:85128970039
ISSN
1435-9529
DOI
10.1007/s10064-022-02718-8
language
English
LU publication?
yes
id
fb5deed5-f2d1-49bb-a2c5-c4b9140636c3
date added to LUP
2022-06-30 14:40:30
date last changed
2023-04-05 17:58:07
@article{fb5deed5-f2d1-49bb-a2c5-c4b9140636c3,
  abstract     = {{<p>Granitic rocks are durable materials sought after for the production of road and railroad aggregates. Granitic bedrock commonly, however, includes gabbroic components, which may enhance or decrease the aggregate performance. This study evaluates the variation in resistance to fragmentation (Los Angeles value, LA) and wear/abrasion (micro-Deval value, M<sub>DE</sub>) for the fraction 10/14 mm of gabbro in different metamorphic states. Samples were collected along a 150-km profile where metamorphic conditions grade from epidote–amphibolite to high-pressure granulite-facies, and the degree of metamorphic recrystallization varies with the amount of hydrous fluid. Rocks with no or incipient metamorphic recrystallization preserving their primary igneous fabric and interlocking texture meet the criteria for both asphalt base course and track ballast in railroad, with LA and M<sub>DE</sub> values below 25% and 14%, respectively. Mafic granulite and fine-grained amphibolite have LA values below 25% and can be used in unbound layers. Mafic granulites crystallize at high temperatures but commonly preserve a relict igneous texture due to limited hydration. Coarse-grained amphibolite and migmatitic amphibolite have the poorest performance. They recrystallized at hydrous conditions, leading to complete recrystallization, grain coarsening, and loss of interlocking igneous texture. This study shows that both temperature and infiltration of hydrous fluids significantly affect the technical properties. Even at high metamorphic temperatures, gabbroic rocks may yield aggregates of high technical performance. At hydrous conditions, however, recrystallization results in rock aggregates suitable for unbound layers only. The variation in metamorphic grade and hydration is easily assessed by the geologist in the field and by using standard petrographic microscopy.</p>}},
  author       = {{Urueña, Cindy and Möller, Charlotte and Andersson, Jenny and Lindqvist, Jan Erik and Göransson, Mattias}},
  issn         = {{1435-9529}},
  keywords     = {{Crushed rock aggregates; Gabbroic rocks; Los Angeles; Metamorphic recrystallization; Micro-Deval}},
  language     = {{eng}},
  number       = {{5}},
  publisher    = {{Springer}},
  series       = {{Bulletin of Engineering Geology and the Environment}},
  title        = {{The effect of metamorphism on the aggregate properties of gabbroic rocks}},
  url          = {{http://dx.doi.org/10.1007/s10064-022-02718-8}},
  doi          = {{10.1007/s10064-022-02718-8}},
  volume       = {{81}},
  year         = {{2022}},
}