Pennsylvanian–Early Permian Carbonate Shelf to Slope Transition, Sverdrup Basin, Northwest Ellesmere Island, Arctic Canada (Nunavut)
Near continuous outcrop of Pennsylvanian to Early Permian carbonate strata were studied on northwest Ellesmere Island, in the Sverdrup Basin, Arctic Canada. Six sections were examined displaying shallow water facies of the Nansen Formation and deeper water facies of the Hare Fiord Formation. Petrogr...
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Online Access: | http://hdl.handle.net/11023/1048 https://doi.org/10.11575/PRISM/27283 |
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ftunivcalgary:oai:prism.ucalgary.ca:11023/1048 2023-08-27T04:06:35+02:00 Pennsylvanian–Early Permian Carbonate Shelf to Slope Transition, Sverdrup Basin, Northwest Ellesmere Island, Arctic Canada (Nunavut) Shultz, Candice Victoria Beauchamp, Benoit 2013 application/pdf http://hdl.handle.net/11023/1048 https://doi.org/10.11575/PRISM/27283 eng eng Graduate Studies University of Calgary Calgary Shultz, C. V. (2013). Pennsylvanian–Early Permian Carbonate Shelf to Slope Transition, Sverdrup Basin, Northwest Ellesmere Island, Arctic Canada (Nunavut) (Unpublished master's thesis). University of Calgary, Calgary, AB. doi:10.11575/PRISM/27283 http://dx.doi.org/10.11575/PRISM/27283 http://hdl.handle.net/11023/1048 University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Geology Carbonates Pennsylvanian–Early Permian Sverdrup Basin master thesis 2013 ftunivcalgary https://doi.org/10.11575/PRISM/27283 2023-08-06T06:28:24Z Near continuous outcrop of Pennsylvanian to Early Permian carbonate strata were studied on northwest Ellesmere Island, in the Sverdrup Basin, Arctic Canada. Six sections were examined displaying shallow water facies of the Nansen Formation and deeper water facies of the Hare Fiord Formation. Petrographic analysis and field observations identified 15 microfacies that represent four main depositional environments along a distally steepened ramp. The environments are: restricted shelf, shoal and patch reef, open shelf, and slope with evidence for exponential slope geometry. This is a new interpretation as the Nansen Formation studied to the north was interpreted as a rimmed shelf with a planar slope geometry. Slope morphology is influenced by: climate change, oceanography and prevailing wind direction, and tectonics. Master Thesis Arctic Arctic Climate change Ellesmere Island Nunavut sverdrup basin PRISM - University of Calgary Digital Repository Arctic Nunavut Ellesmere Island Canada Ramp The ENVELOPE(166.433,166.433,-77.633,-77.633) Hare Fiord ENVELOPE(-85.499,-85.499,81.019,81.019) |
institution |
Open Polar |
collection |
PRISM - University of Calgary Digital Repository |
op_collection_id |
ftunivcalgary |
language |
English |
topic |
Geology Carbonates Pennsylvanian–Early Permian Sverdrup Basin |
spellingShingle |
Geology Carbonates Pennsylvanian–Early Permian Sverdrup Basin Shultz, Candice Victoria Pennsylvanian–Early Permian Carbonate Shelf to Slope Transition, Sverdrup Basin, Northwest Ellesmere Island, Arctic Canada (Nunavut) |
topic_facet |
Geology Carbonates Pennsylvanian–Early Permian Sverdrup Basin |
description |
Near continuous outcrop of Pennsylvanian to Early Permian carbonate strata were studied on northwest Ellesmere Island, in the Sverdrup Basin, Arctic Canada. Six sections were examined displaying shallow water facies of the Nansen Formation and deeper water facies of the Hare Fiord Formation. Petrographic analysis and field observations identified 15 microfacies that represent four main depositional environments along a distally steepened ramp. The environments are: restricted shelf, shoal and patch reef, open shelf, and slope with evidence for exponential slope geometry. This is a new interpretation as the Nansen Formation studied to the north was interpreted as a rimmed shelf with a planar slope geometry. Slope morphology is influenced by: climate change, oceanography and prevailing wind direction, and tectonics. |
author2 |
Beauchamp, Benoit |
format |
Master Thesis |
author |
Shultz, Candice Victoria |
author_facet |
Shultz, Candice Victoria |
author_sort |
Shultz, Candice Victoria |
title |
Pennsylvanian–Early Permian Carbonate Shelf to Slope Transition, Sverdrup Basin, Northwest Ellesmere Island, Arctic Canada (Nunavut) |
title_short |
Pennsylvanian–Early Permian Carbonate Shelf to Slope Transition, Sverdrup Basin, Northwest Ellesmere Island, Arctic Canada (Nunavut) |
title_full |
Pennsylvanian–Early Permian Carbonate Shelf to Slope Transition, Sverdrup Basin, Northwest Ellesmere Island, Arctic Canada (Nunavut) |
title_fullStr |
Pennsylvanian–Early Permian Carbonate Shelf to Slope Transition, Sverdrup Basin, Northwest Ellesmere Island, Arctic Canada (Nunavut) |
title_full_unstemmed |
Pennsylvanian–Early Permian Carbonate Shelf to Slope Transition, Sverdrup Basin, Northwest Ellesmere Island, Arctic Canada (Nunavut) |
title_sort |
pennsylvanian–early permian carbonate shelf to slope transition, sverdrup basin, northwest ellesmere island, arctic canada (nunavut) |
publisher |
Graduate Studies |
publishDate |
2013 |
url |
http://hdl.handle.net/11023/1048 https://doi.org/10.11575/PRISM/27283 |
long_lat |
ENVELOPE(166.433,166.433,-77.633,-77.633) ENVELOPE(-85.499,-85.499,81.019,81.019) |
geographic |
Arctic Nunavut Ellesmere Island Canada Ramp The Hare Fiord |
geographic_facet |
Arctic Nunavut Ellesmere Island Canada Ramp The Hare Fiord |
genre |
Arctic Arctic Climate change Ellesmere Island Nunavut sverdrup basin |
genre_facet |
Arctic Arctic Climate change Ellesmere Island Nunavut sverdrup basin |
op_relation |
Shultz, C. V. (2013). Pennsylvanian–Early Permian Carbonate Shelf to Slope Transition, Sverdrup Basin, Northwest Ellesmere Island, Arctic Canada (Nunavut) (Unpublished master's thesis). University of Calgary, Calgary, AB. doi:10.11575/PRISM/27283 http://dx.doi.org/10.11575/PRISM/27283 http://hdl.handle.net/11023/1048 |
op_rights |
University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. |
op_doi |
https://doi.org/10.11575/PRISM/27283 |
_version_ |
1775347455946129408 |