Continental marine transition in the Devonian of Prince of Wales Island, Northwest Territories

In eastern Prince of Wales Island the Peel Sound Formation is subdivided into upper and lower members on the basis of lithology. The upper member comprises five laterally equivalent north–south facies belts which are in westward order:1) Conglomerate Facies: cobble and boulder conglomerates deposite...

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Published in:Canadian Journal of Earth Sciences
Main Author: Miall, A. D.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1970
Subjects:
Online Access:http://dx.doi.org/10.1139/e70-009
http://www.nrcresearchpress.com/doi/pdf/10.1139/e70-009
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spelling crcansciencepubl:10.1139/e70-009 2024-04-28T08:14:49+00:00 Continental marine transition in the Devonian of Prince of Wales Island, Northwest Territories Miall, A. D. 1970 http://dx.doi.org/10.1139/e70-009 http://www.nrcresearchpress.com/doi/pdf/10.1139/e70-009 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 7, issue 1, page 125-144 ISSN 0008-4077 1480-3313 General Earth and Planetary Sciences journal-article 1970 crcansciencepubl https://doi.org/10.1139/e70-009 2024-04-09T06:56:26Z In eastern Prince of Wales Island the Peel Sound Formation is subdivided into upper and lower members on the basis of lithology. The upper member comprises five laterally equivalent north–south facies belts which are in westward order:1) Conglomerate Facies: cobble and boulder conglomerates deposited on alluvial fans mainly by the action of debris floods.2) Conglomerate–Sandstone Facies: interbedded conglomerate, fine to coarse red sandstone and red siltstone in a repeated fining-upward succession, deposited by low sinuosity braided streams. Cyclic sedimentation is attributed to channel migration and infill.3) Sandstone Facies: the presence of laterally extensive planar cross sets suggests point bar deposition in high sinuosity streams. Tabular bedded sandstone was deposited by stream floods in upper regime flow.4) Sandstone–Carbonate Facies: streams flowing westward formed small deltas, accumulating red, pink, and buff sandstones as topset deposits, interbedded with dolomites containing marine fossils, and clean washed gray sandstones, shales and dolomites with ostracods, pelecypods, gastropods, and Lingula, indicating an estuarine environment.5) Carbonate Facies: dolomites with abundant marine fauna and limited clastic content. Sedimentary structures indicate quiet, shallow water conditions.Paleocurrent evidence indicates an easterly source, confirmed by conglomerate clasts derived from the Boothia Uplift, an area of Lower Paleozoic and Proterozoic rocks extending northwards from the Boothia Peninsula to Somerset Island. Article in Journal/Newspaper Boothia Peninsula Northwest Territories Prince of Wales Island Somerset Island Canadian Science Publishing Canadian Journal of Earth Sciences 7 1 125 144
institution Open Polar
collection Canadian Science Publishing
op_collection_id crcansciencepubl
language English
topic General Earth and Planetary Sciences
spellingShingle General Earth and Planetary Sciences
Miall, A. D.
Continental marine transition in the Devonian of Prince of Wales Island, Northwest Territories
topic_facet General Earth and Planetary Sciences
description In eastern Prince of Wales Island the Peel Sound Formation is subdivided into upper and lower members on the basis of lithology. The upper member comprises five laterally equivalent north–south facies belts which are in westward order:1) Conglomerate Facies: cobble and boulder conglomerates deposited on alluvial fans mainly by the action of debris floods.2) Conglomerate–Sandstone Facies: interbedded conglomerate, fine to coarse red sandstone and red siltstone in a repeated fining-upward succession, deposited by low sinuosity braided streams. Cyclic sedimentation is attributed to channel migration and infill.3) Sandstone Facies: the presence of laterally extensive planar cross sets suggests point bar deposition in high sinuosity streams. Tabular bedded sandstone was deposited by stream floods in upper regime flow.4) Sandstone–Carbonate Facies: streams flowing westward formed small deltas, accumulating red, pink, and buff sandstones as topset deposits, interbedded with dolomites containing marine fossils, and clean washed gray sandstones, shales and dolomites with ostracods, pelecypods, gastropods, and Lingula, indicating an estuarine environment.5) Carbonate Facies: dolomites with abundant marine fauna and limited clastic content. Sedimentary structures indicate quiet, shallow water conditions.Paleocurrent evidence indicates an easterly source, confirmed by conglomerate clasts derived from the Boothia Uplift, an area of Lower Paleozoic and Proterozoic rocks extending northwards from the Boothia Peninsula to Somerset Island.
format Article in Journal/Newspaper
author Miall, A. D.
author_facet Miall, A. D.
author_sort Miall, A. D.
title Continental marine transition in the Devonian of Prince of Wales Island, Northwest Territories
title_short Continental marine transition in the Devonian of Prince of Wales Island, Northwest Territories
title_full Continental marine transition in the Devonian of Prince of Wales Island, Northwest Territories
title_fullStr Continental marine transition in the Devonian of Prince of Wales Island, Northwest Territories
title_full_unstemmed Continental marine transition in the Devonian of Prince of Wales Island, Northwest Territories
title_sort continental marine transition in the devonian of prince of wales island, northwest territories
publisher Canadian Science Publishing
publishDate 1970
url http://dx.doi.org/10.1139/e70-009
http://www.nrcresearchpress.com/doi/pdf/10.1139/e70-009
genre Boothia Peninsula
Northwest Territories
Prince of Wales Island
Somerset Island
genre_facet Boothia Peninsula
Northwest Territories
Prince of Wales Island
Somerset Island
op_source Canadian Journal of Earth Sciences
volume 7, issue 1, page 125-144
ISSN 0008-4077 1480-3313
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/e70-009
container_title Canadian Journal of Earth Sciences
container_volume 7
container_issue 1
container_start_page 125
op_container_end_page 144
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