Structure and Strain in the Burwash Formation, Northwest Territories.
The Burwash Formation is an extensive package of Archean volcanic-turbidite sedimentary units in the Slave Province, Northwest Territories. The turbidites are metamorphosed to greenschist facies, and have undergone two episodes of deformation. The F1 generation folds were refolded forming a fold int...
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ftdalhouse:oai:DalSpace.library.dal.ca:10222/78989 2023-05-15T17:46:29+02:00 Structure and Strain in the Burwash Formation, Northwest Territories. Cuthbert, Robert 2020-04-29T11:37:58Z http://hdl.handle.net/10222/78989 unknown http://hdl.handle.net/10222/78989 Report 2020 ftdalhouse 2021-12-29T18:19:54Z The Burwash Formation is an extensive package of Archean volcanic-turbidite sedimentary units in the Slave Province, Northwest Territories. The turbidites are metamorphosed to greenschist facies, and have undergone two episodes of deformation. The F1 generation folds were refolded forming a fold interference pattern, intermediate between dome, and mushroom shape. Cleavage is axial planar to F2 fold hinges. Rare volcanic tuff sequences provide good markers for stratigraphic correlation and strain analysis. Bulk strain was determined by two different methods, the Fry, and Rf/Phi. In both cases a prolate ellipsoid is found, with the long axis steeply plunging. The prolate shape is consistent with two episodes of plain strain. Keywords: Burwash, volcanic-turbidite, sedimentary, folds, dome, strucrural. Pages: 105 Supervisors: John Waldron Report Northwest Territories Dalhousie University: DalSpace Institutional Repository Northwest Territories Waldron ENVELOPE(115.083,115.083,-66.500,-66.500) |
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Open Polar |
collection |
Dalhousie University: DalSpace Institutional Repository |
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ftdalhouse |
language |
unknown |
description |
The Burwash Formation is an extensive package of Archean volcanic-turbidite sedimentary units in the Slave Province, Northwest Territories. The turbidites are metamorphosed to greenschist facies, and have undergone two episodes of deformation. The F1 generation folds were refolded forming a fold interference pattern, intermediate between dome, and mushroom shape. Cleavage is axial planar to F2 fold hinges. Rare volcanic tuff sequences provide good markers for stratigraphic correlation and strain analysis. Bulk strain was determined by two different methods, the Fry, and Rf/Phi. In both cases a prolate ellipsoid is found, with the long axis steeply plunging. The prolate shape is consistent with two episodes of plain strain. Keywords: Burwash, volcanic-turbidite, sedimentary, folds, dome, strucrural. Pages: 105 Supervisors: John Waldron |
format |
Report |
author |
Cuthbert, Robert |
spellingShingle |
Cuthbert, Robert Structure and Strain in the Burwash Formation, Northwest Territories. |
author_facet |
Cuthbert, Robert |
author_sort |
Cuthbert, Robert |
title |
Structure and Strain in the Burwash Formation, Northwest Territories. |
title_short |
Structure and Strain in the Burwash Formation, Northwest Territories. |
title_full |
Structure and Strain in the Burwash Formation, Northwest Territories. |
title_fullStr |
Structure and Strain in the Burwash Formation, Northwest Territories. |
title_full_unstemmed |
Structure and Strain in the Burwash Formation, Northwest Territories. |
title_sort |
structure and strain in the burwash formation, northwest territories. |
publishDate |
2020 |
url |
http://hdl.handle.net/10222/78989 |
long_lat |
ENVELOPE(115.083,115.083,-66.500,-66.500) |
geographic |
Northwest Territories Waldron |
geographic_facet |
Northwest Territories Waldron |
genre |
Northwest Territories |
genre_facet |
Northwest Territories |
op_relation |
http://hdl.handle.net/10222/78989 |
_version_ |
1766150165522022400 |