Stratigraphy, sedimentology and resource assessment of the Lower Cretaceous Isachsen Formation: Sverdrup Basin, Ellef Ringnes Island, Nunavut, Arctic Canada ...

The Isachsen Formation is a Barremian to Aptian-aged fluvio-deltaic succession ranging in thickness from tens of meters to over 1400 m within the Sverdrup Basin of the Canadian Arctic Archipelago. The formation exhibits a variety of lithologies including coarse-grained quartz-arenite sandstones, fin...

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Main Author: Tullius, Dylan Neill
Format: Master Thesis
Language:English
Published: Graduate Studies 2014
Subjects:
Online Access:https://dx.doi.org/10.11575/prism/27890
https://prism.ucalgary.ca/handle/11023/1690
id ftdatacite:10.11575/prism/27890
record_format openpolar
spelling ftdatacite:10.11575/prism/27890 2023-11-05T03:37:56+01:00 Stratigraphy, sedimentology and resource assessment of the Lower Cretaceous Isachsen Formation: Sverdrup Basin, Ellef Ringnes Island, Nunavut, Arctic Canada ... Tullius, Dylan Neill 2014 https://dx.doi.org/10.11575/prism/27890 https://prism.ucalgary.ca/handle/11023/1690 en eng Graduate Studies 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 FOS Earth and related environmental sciences Mineralogy Palynology Isachsen Sverdrup Cretaceous article master thesis CreativeWork Other 2014 ftdatacite https://doi.org/10.11575/prism/27890 2023-10-09T10:53:51Z The Isachsen Formation is a Barremian to Aptian-aged fluvio-deltaic succession ranging in thickness from tens of meters to over 1400 m within the Sverdrup Basin of the Canadian Arctic Archipelago. The formation exhibits a variety of lithologies including coarse-grained quartz-arenite sandstones, fine-grained ripple laminated sandstones and siltstones, marine mudstones and coal deposits that were deposited in meandering, braided stream, coastal plain and shallow marine shelf depositional environments. This study classifies the Isachsen Formation as a mixture of recycled and craton derived sediments prograding northwest through the Sverdrup Basin with both source and reservoir potential in previously overlooked areas. Sedimentation during this time period was affected by active diapirism in some locations on Ellef Ringnes Island. Interpretations are based on observations from over 6,000 m of measured stratigraphic sections, local mapping of facies contacts, palynology, sandstone petrography and field sample ... Master Thesis Arctic Archipelago Arctic Canadian Arctic Archipelago Ellef Ringnes Island Isachsen Nunavut sverdrup basin DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Geology
FOS Earth and related environmental sciences
Mineralogy
Palynology
Isachsen
Sverdrup
Cretaceous
spellingShingle Geology
FOS Earth and related environmental sciences
Mineralogy
Palynology
Isachsen
Sverdrup
Cretaceous
Tullius, Dylan Neill
Stratigraphy, sedimentology and resource assessment of the Lower Cretaceous Isachsen Formation: Sverdrup Basin, Ellef Ringnes Island, Nunavut, Arctic Canada ...
topic_facet Geology
FOS Earth and related environmental sciences
Mineralogy
Palynology
Isachsen
Sverdrup
Cretaceous
description The Isachsen Formation is a Barremian to Aptian-aged fluvio-deltaic succession ranging in thickness from tens of meters to over 1400 m within the Sverdrup Basin of the Canadian Arctic Archipelago. The formation exhibits a variety of lithologies including coarse-grained quartz-arenite sandstones, fine-grained ripple laminated sandstones and siltstones, marine mudstones and coal deposits that were deposited in meandering, braided stream, coastal plain and shallow marine shelf depositional environments. This study classifies the Isachsen Formation as a mixture of recycled and craton derived sediments prograding northwest through the Sverdrup Basin with both source and reservoir potential in previously overlooked areas. Sedimentation during this time period was affected by active diapirism in some locations on Ellef Ringnes Island. Interpretations are based on observations from over 6,000 m of measured stratigraphic sections, local mapping of facies contacts, palynology, sandstone petrography and field sample ...
format Master Thesis
author Tullius, Dylan Neill
author_facet Tullius, Dylan Neill
author_sort Tullius, Dylan Neill
title Stratigraphy, sedimentology and resource assessment of the Lower Cretaceous Isachsen Formation: Sverdrup Basin, Ellef Ringnes Island, Nunavut, Arctic Canada ...
title_short Stratigraphy, sedimentology and resource assessment of the Lower Cretaceous Isachsen Formation: Sverdrup Basin, Ellef Ringnes Island, Nunavut, Arctic Canada ...
title_full Stratigraphy, sedimentology and resource assessment of the Lower Cretaceous Isachsen Formation: Sverdrup Basin, Ellef Ringnes Island, Nunavut, Arctic Canada ...
title_fullStr Stratigraphy, sedimentology and resource assessment of the Lower Cretaceous Isachsen Formation: Sverdrup Basin, Ellef Ringnes Island, Nunavut, Arctic Canada ...
title_full_unstemmed Stratigraphy, sedimentology and resource assessment of the Lower Cretaceous Isachsen Formation: Sverdrup Basin, Ellef Ringnes Island, Nunavut, Arctic Canada ...
title_sort stratigraphy, sedimentology and resource assessment of the lower cretaceous isachsen formation: sverdrup basin, ellef ringnes island, nunavut, arctic canada ...
publisher Graduate Studies
publishDate 2014
url https://dx.doi.org/10.11575/prism/27890
https://prism.ucalgary.ca/handle/11023/1690
genre Arctic Archipelago
Arctic
Canadian Arctic Archipelago
Ellef Ringnes Island
Isachsen
Nunavut
sverdrup basin
genre_facet Arctic Archipelago
Arctic
Canadian Arctic Archipelago
Ellef Ringnes Island
Isachsen
Nunavut
sverdrup basin
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/27890
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