Early Cretaceous methane seepage system and associated carbonates, biota and geochemistry, Sverdrup Basin, Ellef Ringnes Island, Nunavut ...

Over one hundred carbonate deposits, interpreted as having formed at methane seepage sites in the Sverdrup Basin have been discovered on Ellef Ringnes Island, Canadian Arctic. The deposits, up to 2.7 metres tall and 60 metres wide, are found within the lower member of the Lower Cretaceous Christophe...

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Main Author: Williscroft, Krista
Format: Master Thesis
Language:English
Published: Graduate Studies 2013
Subjects:
Online Access:https://dx.doi.org/10.11575/prism/25767
https://prism.ucalgary.ca/handle/11023/1102
id ftdatacite:10.11575/prism/25767
record_format openpolar
spelling ftdatacite:10.11575/prism/25767 2023-11-05T03:38:06+01:00 Early Cretaceous methane seepage system and associated carbonates, biota and geochemistry, Sverdrup Basin, Ellef Ringnes Island, Nunavut ... Williscroft, Krista 2013 https://dx.doi.org/10.11575/prism/25767 https://prism.ucalgary.ca/handle/11023/1102 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. Biogeochemistry Geochemistry FOS Earth and related environmental sciences Geology Arctic Methane Seep Carbonate Ellef Ringnes article master thesis CreativeWork Other 2013 ftdatacite https://doi.org/10.11575/prism/25767 2023-10-09T10:52:52Z Over one hundred carbonate deposits, interpreted as having formed at methane seepage sites in the Sverdrup Basin have been discovered on Ellef Ringnes Island, Canadian Arctic. The deposits, up to 2.7 metres tall and 60 metres wide, are found within the lower member of the Lower Cretaceous Christopher Formation, a silty marine shale. The carbonates have complex and heterogeneous structures typical of seep carbonates, including banded botryoidal and clotted textures as well as void filling sparite. Stable carbon isotopes show highly 13C-depleted values, as low as δ13CVPDB = -53‰, indicative of authigenic carbonate precipitation via the anaerobic oxidation of biogenic methane. Abundant and well-preserved fauna include multiple species of bivalves, worm tubes, ammonites and gastropods. Methane seepage is calculated to have lasted ~500,000 years and was brought about by a tensional stress regime as well as salt diapirism related faulting. ... Master Thesis arctic methane Arctic Ellef Ringnes Island 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 Biogeochemistry
Geochemistry
FOS Earth and related environmental sciences
Geology
Arctic
Methane
Seep
Carbonate
Ellef
Ringnes
spellingShingle Biogeochemistry
Geochemistry
FOS Earth and related environmental sciences
Geology
Arctic
Methane
Seep
Carbonate
Ellef
Ringnes
Williscroft, Krista
Early Cretaceous methane seepage system and associated carbonates, biota and geochemistry, Sverdrup Basin, Ellef Ringnes Island, Nunavut ...
topic_facet Biogeochemistry
Geochemistry
FOS Earth and related environmental sciences
Geology
Arctic
Methane
Seep
Carbonate
Ellef
Ringnes
description Over one hundred carbonate deposits, interpreted as having formed at methane seepage sites in the Sverdrup Basin have been discovered on Ellef Ringnes Island, Canadian Arctic. The deposits, up to 2.7 metres tall and 60 metres wide, are found within the lower member of the Lower Cretaceous Christopher Formation, a silty marine shale. The carbonates have complex and heterogeneous structures typical of seep carbonates, including banded botryoidal and clotted textures as well as void filling sparite. Stable carbon isotopes show highly 13C-depleted values, as low as δ13CVPDB = -53‰, indicative of authigenic carbonate precipitation via the anaerobic oxidation of biogenic methane. Abundant and well-preserved fauna include multiple species of bivalves, worm tubes, ammonites and gastropods. Methane seepage is calculated to have lasted ~500,000 years and was brought about by a tensional stress regime as well as salt diapirism related faulting. ...
format Master Thesis
author Williscroft, Krista
author_facet Williscroft, Krista
author_sort Williscroft, Krista
title Early Cretaceous methane seepage system and associated carbonates, biota and geochemistry, Sverdrup Basin, Ellef Ringnes Island, Nunavut ...
title_short Early Cretaceous methane seepage system and associated carbonates, biota and geochemistry, Sverdrup Basin, Ellef Ringnes Island, Nunavut ...
title_full Early Cretaceous methane seepage system and associated carbonates, biota and geochemistry, Sverdrup Basin, Ellef Ringnes Island, Nunavut ...
title_fullStr Early Cretaceous methane seepage system and associated carbonates, biota and geochemistry, Sverdrup Basin, Ellef Ringnes Island, Nunavut ...
title_full_unstemmed Early Cretaceous methane seepage system and associated carbonates, biota and geochemistry, Sverdrup Basin, Ellef Ringnes Island, Nunavut ...
title_sort early cretaceous methane seepage system and associated carbonates, biota and geochemistry, sverdrup basin, ellef ringnes island, nunavut ...
publisher Graduate Studies
publishDate 2013
url https://dx.doi.org/10.11575/prism/25767
https://prism.ucalgary.ca/handle/11023/1102
genre arctic methane
Arctic
Ellef Ringnes Island
Nunavut
sverdrup basin
genre_facet arctic methane
Arctic
Ellef Ringnes Island
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/25767
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