Upper Triassic Mid-Latitude Cool-Water Carbonate Deposit: Sedimentology and Stratigraphy of the Gore Point Member, Roche Point Formation, Arctic Islands, Canada ...
The Gore Point Member is a mixed carbonate-siliciclastic unit deposited in the Sverdup Basin (Canadian Arctic Islands) during the Carnian (Late Triassic). While mixed carbonate-siliciclastic deposits are not rare within the global rock record, the Gore Point Member is unique in that it is the only u...
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Online Access: | https://dx.doi.org/10.11575/prism/38630 https://prism.ucalgary.ca/handle/1880/113068 |
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ftdatacite:10.11575/prism/38630 2023-08-27T04:07:34+02:00 Upper Triassic Mid-Latitude Cool-Water Carbonate Deposit: Sedimentology and Stratigraphy of the Gore Point Member, Roche Point Formation, Arctic Islands, Canada ... Hay, Chelsey 2021 https://dx.doi.org/10.11575/prism/38630 https://prism.ucalgary.ca/handle/1880/113068 unknown Science 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. Education--Sciences Geology FOS Earth and related environmental sciences CreativeWork article 2021 ftdatacite https://doi.org/10.11575/prism/38630 2023-08-07T14:24:23Z The Gore Point Member is a mixed carbonate-siliciclastic unit deposited in the Sverdup Basin (Canadian Arctic Islands) during the Carnian (Late Triassic). While mixed carbonate-siliciclastic deposits are not rare within the global rock record, the Gore Point Member is unique in that it is the only unit with meaningful amounts of carbonate material within the Mesozoic succession of the Sverdrup Basin. However, as detailed sedimentological or sequence stratigraphic studies of the Gore Point Member have been yet to be undertaken, the existence of this anomalous unit remains unexplained. This study applies thin section microscopy and microfacies analysis of 285 samples from 12 sites across western Ellesmere Island, and lithofacies analysis of one core on Mackenzie King Island, to interpret the depositional setting of the Gore Point Member. These observations reveal fine-grained quartz-dominated siliciclastics and heterozoan carbonate material deposited in a ramp setting in an arid, cool-temperate environment. ... Article in Journal/Newspaper Arctic Ellesmere Island sverdrup basin DataCite Metadata Store (German National Library of Science and Technology) Arctic Ellesmere Island Canada King Island ENVELOPE(-58.100,-58.100,-62.000,-62.000) Mackenzie King Island ENVELOPE(-111.989,-111.989,77.768,77.768) Roche Point ENVELOPE(-109.464,-109.464,76.726,76.726) |
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DataCite Metadata Store (German National Library of Science and Technology) |
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topic |
Education--Sciences Geology FOS Earth and related environmental sciences |
spellingShingle |
Education--Sciences Geology FOS Earth and related environmental sciences Hay, Chelsey Upper Triassic Mid-Latitude Cool-Water Carbonate Deposit: Sedimentology and Stratigraphy of the Gore Point Member, Roche Point Formation, Arctic Islands, Canada ... |
topic_facet |
Education--Sciences Geology FOS Earth and related environmental sciences |
description |
The Gore Point Member is a mixed carbonate-siliciclastic unit deposited in the Sverdup Basin (Canadian Arctic Islands) during the Carnian (Late Triassic). While mixed carbonate-siliciclastic deposits are not rare within the global rock record, the Gore Point Member is unique in that it is the only unit with meaningful amounts of carbonate material within the Mesozoic succession of the Sverdrup Basin. However, as detailed sedimentological or sequence stratigraphic studies of the Gore Point Member have been yet to be undertaken, the existence of this anomalous unit remains unexplained. This study applies thin section microscopy and microfacies analysis of 285 samples from 12 sites across western Ellesmere Island, and lithofacies analysis of one core on Mackenzie King Island, to interpret the depositional setting of the Gore Point Member. These observations reveal fine-grained quartz-dominated siliciclastics and heterozoan carbonate material deposited in a ramp setting in an arid, cool-temperate environment. ... |
format |
Article in Journal/Newspaper |
author |
Hay, Chelsey |
author_facet |
Hay, Chelsey |
author_sort |
Hay, Chelsey |
title |
Upper Triassic Mid-Latitude Cool-Water Carbonate Deposit: Sedimentology and Stratigraphy of the Gore Point Member, Roche Point Formation, Arctic Islands, Canada ... |
title_short |
Upper Triassic Mid-Latitude Cool-Water Carbonate Deposit: Sedimentology and Stratigraphy of the Gore Point Member, Roche Point Formation, Arctic Islands, Canada ... |
title_full |
Upper Triassic Mid-Latitude Cool-Water Carbonate Deposit: Sedimentology and Stratigraphy of the Gore Point Member, Roche Point Formation, Arctic Islands, Canada ... |
title_fullStr |
Upper Triassic Mid-Latitude Cool-Water Carbonate Deposit: Sedimentology and Stratigraphy of the Gore Point Member, Roche Point Formation, Arctic Islands, Canada ... |
title_full_unstemmed |
Upper Triassic Mid-Latitude Cool-Water Carbonate Deposit: Sedimentology and Stratigraphy of the Gore Point Member, Roche Point Formation, Arctic Islands, Canada ... |
title_sort |
upper triassic mid-latitude cool-water carbonate deposit: sedimentology and stratigraphy of the gore point member, roche point formation, arctic islands, canada ... |
publisher |
Science |
publishDate |
2021 |
url |
https://dx.doi.org/10.11575/prism/38630 https://prism.ucalgary.ca/handle/1880/113068 |
long_lat |
ENVELOPE(-58.100,-58.100,-62.000,-62.000) ENVELOPE(-111.989,-111.989,77.768,77.768) ENVELOPE(-109.464,-109.464,76.726,76.726) |
geographic |
Arctic Ellesmere Island Canada King Island Mackenzie King Island Roche Point |
geographic_facet |
Arctic Ellesmere Island Canada King Island Mackenzie King Island Roche Point |
genre |
Arctic Ellesmere Island sverdrup basin |
genre_facet |
Arctic Ellesmere Island 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/38630 |
_version_ |
1775348330519330816 |