Contact metamorphism of Palaeozoic shale in southern Sweden: influences on clay mineralogy and implications for railway construction material properties
(2003) In GFF 125(2). p.63-68- Abstract
- Abundant shale fragments were observed in dolerite material used for railway construction in western Skane, due to quarrying of Permo-Carboniferous dolerite in contact with Silurian shale (the Colonus Shale) in the Ronnarp Quarry, western Skane. Shale fragments were particularly enriched in the finest fractions of the crushed rock material. We analysed the clay mineralogy of shale from the railway material and at different distances from the dolerite in the quarry, in order to better understand the properties of the delivered rock material. The illite and chlorite dominated Colonus Shale in Skane typically shows background illite crystallinity in the uppermost diagenetic realm. In the Ronnarp Quarry, fissile shale a few meters away from... (More)
- Abundant shale fragments were observed in dolerite material used for railway construction in western Skane, due to quarrying of Permo-Carboniferous dolerite in contact with Silurian shale (the Colonus Shale) in the Ronnarp Quarry, western Skane. Shale fragments were particularly enriched in the finest fractions of the crushed rock material. We analysed the clay mineralogy of shale from the railway material and at different distances from the dolerite in the quarry, in order to better understand the properties of the delivered rock material. The illite and chlorite dominated Colonus Shale in Skane typically shows background illite crystallinity in the uppermost diagenetic realm. In the Ronnarp Quarry, fissile shale a few meters away from the dolerite intrusion shows illite crystallinity in the anchimetamorphic stage. In massive shale less than I m from the shale-dolerite contact, swelling clay minerals have formed at the expense of illite. Therefore, despite the massive appearance of the contact metamorphosed shale, it is suggested that such rocks should be avoided during construction material production. A tentative model for post-intrusion hydrothermal clay mineral transformation is suggested. (Less)
Please use this url to cite or link to this publication:
https://lup.lub.lu.se/record/303534
- author
- Olsson, Ingela LU and Ahlberg, Anders LU
- organization
- publishing date
- 2003
- type
- Contribution to journal
- publication status
- published
- subject
- keywords
- clay minerals, contact metamorphism, dolerite, Colonus Shale
- in
- GFF
- volume
- 125
- issue
- 2
- pages
- 63 - 68
- publisher
- Taylor & Francis
- external identifiers
-
- wos:000184805100003
- scopus:3843093025
- ISSN
- 2000-0863
- DOI
- 10.1080/11035890301252063
- language
- English
- LU publication?
- yes
- id
- 13d65280-f896-4fed-aca3-e75e9a170e76 (old id 303534)
- date added to LUP
- 2016-04-01 12:15:15
- date last changed
- 2022-01-27 01:06:23
@article{13d65280-f896-4fed-aca3-e75e9a170e76,
abstract = {{Abundant shale fragments were observed in dolerite material used for railway construction in western Skane, due to quarrying of Permo-Carboniferous dolerite in contact with Silurian shale (the Colonus Shale) in the Ronnarp Quarry, western Skane. Shale fragments were particularly enriched in the finest fractions of the crushed rock material. We analysed the clay mineralogy of shale from the railway material and at different distances from the dolerite in the quarry, in order to better understand the properties of the delivered rock material. The illite and chlorite dominated Colonus Shale in Skane typically shows background illite crystallinity in the uppermost diagenetic realm. In the Ronnarp Quarry, fissile shale a few meters away from the dolerite intrusion shows illite crystallinity in the anchimetamorphic stage. In massive shale less than I m from the shale-dolerite contact, swelling clay minerals have formed at the expense of illite. Therefore, despite the massive appearance of the contact metamorphosed shale, it is suggested that such rocks should be avoided during construction material production. A tentative model for post-intrusion hydrothermal clay mineral transformation is suggested.}},
author = {{Olsson, Ingela and Ahlberg, Anders}},
issn = {{2000-0863}},
keywords = {{clay minerals; contact metamorphism; dolerite; Colonus Shale}},
language = {{eng}},
number = {{2}},
pages = {{63--68}},
publisher = {{Taylor & Francis}},
series = {{GFF}},
title = {{Contact metamorphism of Palaeozoic shale in southern Sweden: influences on clay mineralogy and implications for railway construction material properties}},
url = {{http://dx.doi.org/10.1080/11035890301252063}},
doi = {{10.1080/11035890301252063}},
volume = {{125}},
year = {{2003}},
}