Photointerpretation of Tertiary structures in platform cover strata of interior Oscar II Land, Spitsbergen
A structural map of Oscar II Land compiled using black and white, stereo-pair air photos and other available information sources suggests the existence of three structural zones within the deformed platform cover strata. The western zone consists of basement involved overthrusts of complex geometry...
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Norwegian Polar Institute
1998
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Online Access: | https://polarresearch.net/index.php/polar/article/view/2429 https://doi.org/10.3402/polar.v6i2.6857 |
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ftjpolarres:oai:journals.openacademia.net:article/2429 2023-05-15T17:54:07+02:00 Photointerpretation of Tertiary structures in platform cover strata of interior Oscar II Land, Spitsbergen Maher Jr., Harmon D. 1998-01-12 application/pdf https://polarresearch.net/index.php/polar/article/view/2429 https://doi.org/10.3402/polar.v6i2.6857 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/2429/5679 https://polarresearch.net/index.php/polar/article/view/2429 doi:10.3402/polar.v6i2.6857 Copyright (c) 2018 Polar Research Polar Research; Vol. 6 No. 2 (1988); 155-172 1751-8369 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 1998 ftjpolarres https://doi.org/10.3402/polar.v6i2.6857 2021-11-11T19:12:43Z A structural map of Oscar II Land compiled using black and white, stereo-pair air photos and other available information sources suggests the existence of three structural zones within the deformed platform cover strata. The western zone consists of basement involved overthrusts of complex geometry in the north large-scale folds of platform cover strata with a stepped, down to the east profile in the south. The central zone consists primarily of folds within Kapp Starostin Fm. and overlying Triassic strata that likely formed above a subhorizontal décollement within Gipshuken Fm. strata. Farther to the east thrusts emplace Permian Kapp Starostin Fm. strata over Triassic strata. This zone probably represents stratigraphic climb of the basal decollement. Conservative estimates of shortening for the central and eastern zones are in the 15-25% range. The contribution of the western zone structures to overall Tertiary shortening depends on the geometry of faults underlying the stepped folds and is uncertain at present. Changes along strike are in part due to differential levels of erosion and changes in transport direction, but also probably important was variable thickness of the platform cover strata involved (less to the north) and the availability of incompetent horizons along which thrust-fiats could form. Two areas with anomalous structural trends may represent oblique ramps. Article in Journal/Newspaper Oscar II Land Polar Research Spitsbergen Polar Research (E-Journal) Oscar II ENVELOPE(-62.500,-62.500,-65.750,-65.750) Oscar II Land ENVELOPE(13.299,13.299,78.441,78.441) Kapp Starostin ENVELOPE(13.828,13.828,78.093,78.093) Gipshuken ENVELOPE(16.470,16.470,78.458,78.458) Polar Research 6 2 155 172 |
institution |
Open Polar |
collection |
Polar Research (E-Journal) |
op_collection_id |
ftjpolarres |
language |
English |
description |
A structural map of Oscar II Land compiled using black and white, stereo-pair air photos and other available information sources suggests the existence of three structural zones within the deformed platform cover strata. The western zone consists of basement involved overthrusts of complex geometry in the north large-scale folds of platform cover strata with a stepped, down to the east profile in the south. The central zone consists primarily of folds within Kapp Starostin Fm. and overlying Triassic strata that likely formed above a subhorizontal décollement within Gipshuken Fm. strata. Farther to the east thrusts emplace Permian Kapp Starostin Fm. strata over Triassic strata. This zone probably represents stratigraphic climb of the basal decollement. Conservative estimates of shortening for the central and eastern zones are in the 15-25% range. The contribution of the western zone structures to overall Tertiary shortening depends on the geometry of faults underlying the stepped folds and is uncertain at present. Changes along strike are in part due to differential levels of erosion and changes in transport direction, but also probably important was variable thickness of the platform cover strata involved (less to the north) and the availability of incompetent horizons along which thrust-fiats could form. Two areas with anomalous structural trends may represent oblique ramps. |
format |
Article in Journal/Newspaper |
author |
Maher Jr., Harmon D. |
spellingShingle |
Maher Jr., Harmon D. Photointerpretation of Tertiary structures in platform cover strata of interior Oscar II Land, Spitsbergen |
author_facet |
Maher Jr., Harmon D. |
author_sort |
Maher Jr., Harmon D. |
title |
Photointerpretation of Tertiary structures in platform cover strata of interior Oscar II Land, Spitsbergen |
title_short |
Photointerpretation of Tertiary structures in platform cover strata of interior Oscar II Land, Spitsbergen |
title_full |
Photointerpretation of Tertiary structures in platform cover strata of interior Oscar II Land, Spitsbergen |
title_fullStr |
Photointerpretation of Tertiary structures in platform cover strata of interior Oscar II Land, Spitsbergen |
title_full_unstemmed |
Photointerpretation of Tertiary structures in platform cover strata of interior Oscar II Land, Spitsbergen |
title_sort |
photointerpretation of tertiary structures in platform cover strata of interior oscar ii land, spitsbergen |
publisher |
Norwegian Polar Institute |
publishDate |
1998 |
url |
https://polarresearch.net/index.php/polar/article/view/2429 https://doi.org/10.3402/polar.v6i2.6857 |
long_lat |
ENVELOPE(-62.500,-62.500,-65.750,-65.750) ENVELOPE(13.299,13.299,78.441,78.441) ENVELOPE(13.828,13.828,78.093,78.093) ENVELOPE(16.470,16.470,78.458,78.458) |
geographic |
Oscar II Oscar II Land Kapp Starostin Gipshuken |
geographic_facet |
Oscar II Oscar II Land Kapp Starostin Gipshuken |
genre |
Oscar II Land Polar Research Spitsbergen |
genre_facet |
Oscar II Land Polar Research Spitsbergen |
op_source |
Polar Research; Vol. 6 No. 2 (1988); 155-172 1751-8369 |
op_relation |
https://polarresearch.net/index.php/polar/article/view/2429/5679 https://polarresearch.net/index.php/polar/article/view/2429 doi:10.3402/polar.v6i2.6857 |
op_rights |
Copyright (c) 2018 Polar Research |
op_doi |
https://doi.org/10.3402/polar.v6i2.6857 |
container_title |
Polar Research |
container_volume |
6 |
container_issue |
2 |
container_start_page |
155 |
op_container_end_page |
172 |
_version_ |
1766161837717454848 |