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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Bibliographic Details
Main Author: Shultz, Candice Victoria
Other Authors: Beauchamp, Benoit
Format: Master Thesis
Language:English
Published: Graduate Studies 2013
Subjects:
Online Access:http://hdl.handle.net/11023/1048
https://doi.org/10.11575/PRISM/27283
id ftunivcalgary:oai:prism.ucalgary.ca:11023/1048
record_format openpolar
spelling 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Permian Carbonate Shelf to Slope Transition, Sverdrup Basin, Northwest Ellesmere Island, Arctic Canada (Nunavut) (Unpublished master's thesis).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
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