Pattern of apparent total strain in the bedded anhydrite cap of a folded salt wall
The dense anhydrite cap of the southern Muskox Ridge salt wall participated in the large-scale buckling of Mesozoic clastic strata at the western boundary of the Tertiary Eureka Sound fold belt on Axel Heiberg Island, Canadian Arctic. This Carboniferous anhydrite is an aggregate of strained diagenet...
Published in: | Canadian Journal of Earth Sciences |
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Language: | English |
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Canadian Science Publishing
1989
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Online Access: | http://dx.doi.org/10.1139/e89-079 http://www.nrcresearchpress.com/doi/pdf/10.1139/e89-079 |
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crcansciencepubl:10.1139/e89-079 2024-04-07T07:50:22+00:00 Pattern of apparent total strain in the bedded anhydrite cap of a folded salt wall Schwerdtner, W. M. Torrance, J. G. Berkel, J. T. van 1989 http://dx.doi.org/10.1139/e89-079 http://www.nrcresearchpress.com/doi/pdf/10.1139/e89-079 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 26, issue 5, page 983-992 ISSN 0008-4077 1480-3313 General Earth and Planetary Sciences journal-article 1989 crcansciencepubl https://doi.org/10.1139/e89-079 2024-03-08T00:37:43Z The dense anhydrite cap of the southern Muskox Ridge salt wall participated in the large-scale buckling of Mesozoic clastic strata at the western boundary of the Tertiary Eureka Sound fold belt on Axel Heiberg Island, Canadian Arctic. This Carboniferous anhydrite is an aggregate of strained diagenetic nodules and contains relict limestone beds that mark the paleohorizontal plane. The well-exposed cap provides an excellent example of fold decollement and redeformation of foliated rocks.The horizontal pattern of the nodule-shape fabric was delineated within folded and straight segments of the cap. Maps for a well-exposed folded segment show systematic variations in the intensity of apparent total strain (r) and the prolateness factor (k). If the nodule fabric pattern of adjacent straight walls represents the prefold structural state of all walls in the area, then the pattern of folding strain can be reconstructed in the southern Muskox Ridge cap. Here, the preflattened anhydrite was deformed by flexural shear in most localities, but was shortened passively near its contact with competent clastic rock. Article in Journal/Newspaper Arctic Axel Heiberg Island Eureka Sound muskox Canadian Science Publishing Arctic Eureka ENVELOPE(-85.940,-85.940,79.990,79.990) Heiberg ENVELOPE(13.964,13.964,66.424,66.424) Axel Heiberg Island ENVELOPE(-91.001,-91.001,79.752,79.752) Eureka Sound ENVELOPE(-84.999,-84.999,79.002,79.002) Canadian Journal of Earth Sciences 26 5 983 992 |
institution |
Open Polar |
collection |
Canadian Science Publishing |
op_collection_id |
crcansciencepubl |
language |
English |
topic |
General Earth and Planetary Sciences |
spellingShingle |
General Earth and Planetary Sciences Schwerdtner, W. M. Torrance, J. G. Berkel, J. T. van Pattern of apparent total strain in the bedded anhydrite cap of a folded salt wall |
topic_facet |
General Earth and Planetary Sciences |
description |
The dense anhydrite cap of the southern Muskox Ridge salt wall participated in the large-scale buckling of Mesozoic clastic strata at the western boundary of the Tertiary Eureka Sound fold belt on Axel Heiberg Island, Canadian Arctic. This Carboniferous anhydrite is an aggregate of strained diagenetic nodules and contains relict limestone beds that mark the paleohorizontal plane. The well-exposed cap provides an excellent example of fold decollement and redeformation of foliated rocks.The horizontal pattern of the nodule-shape fabric was delineated within folded and straight segments of the cap. Maps for a well-exposed folded segment show systematic variations in the intensity of apparent total strain (r) and the prolateness factor (k). If the nodule fabric pattern of adjacent straight walls represents the prefold structural state of all walls in the area, then the pattern of folding strain can be reconstructed in the southern Muskox Ridge cap. Here, the preflattened anhydrite was deformed by flexural shear in most localities, but was shortened passively near its contact with competent clastic rock. |
format |
Article in Journal/Newspaper |
author |
Schwerdtner, W. M. Torrance, J. G. Berkel, J. T. van |
author_facet |
Schwerdtner, W. M. Torrance, J. G. Berkel, J. T. van |
author_sort |
Schwerdtner, W. M. |
title |
Pattern of apparent total strain in the bedded anhydrite cap of a folded salt wall |
title_short |
Pattern of apparent total strain in the bedded anhydrite cap of a folded salt wall |
title_full |
Pattern of apparent total strain in the bedded anhydrite cap of a folded salt wall |
title_fullStr |
Pattern of apparent total strain in the bedded anhydrite cap of a folded salt wall |
title_full_unstemmed |
Pattern of apparent total strain in the bedded anhydrite cap of a folded salt wall |
title_sort |
pattern of apparent total strain in the bedded anhydrite cap of a folded salt wall |
publisher |
Canadian Science Publishing |
publishDate |
1989 |
url |
http://dx.doi.org/10.1139/e89-079 http://www.nrcresearchpress.com/doi/pdf/10.1139/e89-079 |
long_lat |
ENVELOPE(-85.940,-85.940,79.990,79.990) ENVELOPE(13.964,13.964,66.424,66.424) ENVELOPE(-91.001,-91.001,79.752,79.752) ENVELOPE(-84.999,-84.999,79.002,79.002) |
geographic |
Arctic Eureka Heiberg Axel Heiberg Island Eureka Sound |
geographic_facet |
Arctic Eureka Heiberg Axel Heiberg Island Eureka Sound |
genre |
Arctic Axel Heiberg Island Eureka Sound muskox |
genre_facet |
Arctic Axel Heiberg Island Eureka Sound muskox |
op_source |
Canadian Journal of Earth Sciences volume 26, issue 5, page 983-992 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/e89-079 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
26 |
container_issue |
5 |
container_start_page |
983 |
op_container_end_page |
992 |
_version_ |
1795665056173654016 |