Mesofabric, microfabric, and submicrofabric of ice-thrust bedrock, Highvale mine, Wabamun Lake area, Alberta
The fabric of the ice-thrust argillaceous bedrock from a shear zone was studied in hand specimens, under a polarizing microscope and a scanning electron microscope. The fabric included principal displacement shears, Riedel shears, conjugate sets of particle alignments, cutans, lithorelics, and aggre...
Published in: | Canadian Journal of Earth Sciences |
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Language: | English |
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Canadian Science Publishing
1988
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Online Access: | http://dx.doi.org/10.1139/e88-136 http://www.nrcresearchpress.com/doi/pdf/10.1139/e88-136 |
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crcansciencepubl:10.1139/e88-136 2024-09-15T18:11:31+00:00 Mesofabric, microfabric, and submicrofabric of ice-thrust bedrock, Highvale mine, Wabamun Lake area, Alberta Tsui, Po C. Cruden, David M. Thomson, Stanley 1988 http://dx.doi.org/10.1139/e88-136 http://www.nrcresearchpress.com/doi/pdf/10.1139/e88-136 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 25, issue 9, page 1420-1431 ISSN 0008-4077 1480-3313 journal-article 1988 crcansciencepubl https://doi.org/10.1139/e88-136 2024-07-25T04:10:08Z The fabric of the ice-thrust argillaceous bedrock from a shear zone was studied in hand specimens, under a polarizing microscope and a scanning electron microscope. The fabric included principal displacement shears, Riedel shears, conjugate sets of particle alignments, cutans, lithorelics, and aggregations which dense cores of randomly oriented groups of clay platelets wrapped by an external layer of oriented clay particles in a turbostatic arrangement. In addition, the bedrock has been disturbed by permafrost, cycles of loading and unloading, and weathering, causing the magnitude of deformation to vary within the ice-thrust shear zone.The fabric of the ice-thrust shear zone is similar to that of shear zones formed by tectonic activity and by laboratory shear tests, suggesting that all these shear zones were formed under conditions of similar kinematic restraint. Article in Journal/Newspaper Ice permafrost Canadian Science Publishing Canadian Journal of Earth Sciences 25 9 1420 1431 |
institution |
Open Polar |
collection |
Canadian Science Publishing |
op_collection_id |
crcansciencepubl |
language |
English |
description |
The fabric of the ice-thrust argillaceous bedrock from a shear zone was studied in hand specimens, under a polarizing microscope and a scanning electron microscope. The fabric included principal displacement shears, Riedel shears, conjugate sets of particle alignments, cutans, lithorelics, and aggregations which dense cores of randomly oriented groups of clay platelets wrapped by an external layer of oriented clay particles in a turbostatic arrangement. In addition, the bedrock has been disturbed by permafrost, cycles of loading and unloading, and weathering, causing the magnitude of deformation to vary within the ice-thrust shear zone.The fabric of the ice-thrust shear zone is similar to that of shear zones formed by tectonic activity and by laboratory shear tests, suggesting that all these shear zones were formed under conditions of similar kinematic restraint. |
format |
Article in Journal/Newspaper |
author |
Tsui, Po C. Cruden, David M. Thomson, Stanley |
spellingShingle |
Tsui, Po C. Cruden, David M. Thomson, Stanley Mesofabric, microfabric, and submicrofabric of ice-thrust bedrock, Highvale mine, Wabamun Lake area, Alberta |
author_facet |
Tsui, Po C. Cruden, David M. Thomson, Stanley |
author_sort |
Tsui, Po C. |
title |
Mesofabric, microfabric, and submicrofabric of ice-thrust bedrock, Highvale mine, Wabamun Lake area, Alberta |
title_short |
Mesofabric, microfabric, and submicrofabric of ice-thrust bedrock, Highvale mine, Wabamun Lake area, Alberta |
title_full |
Mesofabric, microfabric, and submicrofabric of ice-thrust bedrock, Highvale mine, Wabamun Lake area, Alberta |
title_fullStr |
Mesofabric, microfabric, and submicrofabric of ice-thrust bedrock, Highvale mine, Wabamun Lake area, Alberta |
title_full_unstemmed |
Mesofabric, microfabric, and submicrofabric of ice-thrust bedrock, Highvale mine, Wabamun Lake area, Alberta |
title_sort |
mesofabric, microfabric, and submicrofabric of ice-thrust bedrock, highvale mine, wabamun lake area, alberta |
publisher |
Canadian Science Publishing |
publishDate |
1988 |
url |
http://dx.doi.org/10.1139/e88-136 http://www.nrcresearchpress.com/doi/pdf/10.1139/e88-136 |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
Canadian Journal of Earth Sciences volume 25, issue 9, page 1420-1431 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/e88-136 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
25 |
container_issue |
9 |
container_start_page |
1420 |
op_container_end_page |
1431 |
_version_ |
1810449109346156544 |