Application of predictive modelling to the Lower Cretaceous sedimentary sequences of the central Scotian Basin

x, 169 leaves : colour illustrations, colour maps 29 cm + 1 USB flash drive Includes abstract and appendices. Includes bibliographical references (leaves 158-169). Forward stratigraphic modelling of the central Scotian Basin is used to evaluate proposed provenance pathways in the Early Cretaceous an...

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Main Author: Sangster, Christopher
Other Authors: Pe-Piper, Georgia
Format: Text
Language:English
Published: Halifax, N.S. : Saint Mary's University 2019
Subjects:
Online Access:http://library2.smu.ca/handle/01/29128
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spelling ftstmarysunivca:oai:library2:01/29128 2023-05-15T17:14:15+02:00 Application of predictive modelling to the Lower Cretaceous sedimentary sequences of the central Scotian Basin Sangster, Christopher Pe-Piper, Georgia 2019 application/pdf http://library2.smu.ca/handle/01/29128 en eng Halifax, N.S. : Saint Mary's University QE615.5 N55 S26 2019 http://library2.smu.ca/handle/01/29128 QE615.5.N55 Sedimentary basins -- North Atlantic Ocean Geology Stratigraphic -- Cretaceous Sedimentary structures -- North Atlantic Ocean -- Mathematical models Sequence stratigraphy Text 2019 ftstmarysunivca 2022-05-13T05:46:03Z x, 169 leaves : colour illustrations, colour maps 29 cm + 1 USB flash drive Includes abstract and appendices. Includes bibliographical references (leaves 158-169). Forward stratigraphic modelling of the central Scotian Basin is used to evaluate proposed provenance pathways in the Early Cretaceous and exploration risk. Modelling results confirm proposed pathways, supporting the diversion of the Sable and Banquereau rivers during the formation of the Naskapi Member, as well as likely episodic diversions during the Albian. Stratigraphic modelling techniques and petrographic studies predict the distribution of potential reservoir intervals and the influence of diagenesis on detrital minerals. Sand is dominantly trapped on the shelf in all units, with preferential accumulation in salt minibasins along the slope and shallow basin, and bypass to the deep basin. Simulation of feldspar grains and the presence of faulting and high permeability lithofacies suggest a zone of low risk to exploration on the shelf of the western and central Scotian Basin, and one of moderate risk in the eastern Scotian Basin. Text naskapi North Atlantic Saint Mary's University, Halifax: Institutional Repository
institution Open Polar
collection Saint Mary's University, Halifax: Institutional Repository
op_collection_id ftstmarysunivca
language English
topic QE615.5.N55
Sedimentary basins -- North Atlantic Ocean
Geology
Stratigraphic -- Cretaceous
Sedimentary structures -- North Atlantic Ocean -- Mathematical models
Sequence stratigraphy
spellingShingle QE615.5.N55
Sedimentary basins -- North Atlantic Ocean
Geology
Stratigraphic -- Cretaceous
Sedimentary structures -- North Atlantic Ocean -- Mathematical models
Sequence stratigraphy
Sangster, Christopher
Application of predictive modelling to the Lower Cretaceous sedimentary sequences of the central Scotian Basin
topic_facet QE615.5.N55
Sedimentary basins -- North Atlantic Ocean
Geology
Stratigraphic -- Cretaceous
Sedimentary structures -- North Atlantic Ocean -- Mathematical models
Sequence stratigraphy
description x, 169 leaves : colour illustrations, colour maps 29 cm + 1 USB flash drive Includes abstract and appendices. Includes bibliographical references (leaves 158-169). Forward stratigraphic modelling of the central Scotian Basin is used to evaluate proposed provenance pathways in the Early Cretaceous and exploration risk. Modelling results confirm proposed pathways, supporting the diversion of the Sable and Banquereau rivers during the formation of the Naskapi Member, as well as likely episodic diversions during the Albian. Stratigraphic modelling techniques and petrographic studies predict the distribution of potential reservoir intervals and the influence of diagenesis on detrital minerals. Sand is dominantly trapped on the shelf in all units, with preferential accumulation in salt minibasins along the slope and shallow basin, and bypass to the deep basin. Simulation of feldspar grains and the presence of faulting and high permeability lithofacies suggest a zone of low risk to exploration on the shelf of the western and central Scotian Basin, and one of moderate risk in the eastern Scotian Basin.
author2 Pe-Piper, Georgia
format Text
author Sangster, Christopher
author_facet Sangster, Christopher
author_sort Sangster, Christopher
title Application of predictive modelling to the Lower Cretaceous sedimentary sequences of the central Scotian Basin
title_short Application of predictive modelling to the Lower Cretaceous sedimentary sequences of the central Scotian Basin
title_full Application of predictive modelling to the Lower Cretaceous sedimentary sequences of the central Scotian Basin
title_fullStr Application of predictive modelling to the Lower Cretaceous sedimentary sequences of the central Scotian Basin
title_full_unstemmed Application of predictive modelling to the Lower Cretaceous sedimentary sequences of the central Scotian Basin
title_sort application of predictive modelling to the lower cretaceous sedimentary sequences of the central scotian basin
publisher Halifax, N.S. : Saint Mary's University
publishDate 2019
url http://library2.smu.ca/handle/01/29128
genre naskapi
North Atlantic
genre_facet naskapi
North Atlantic
op_relation QE615.5 N55 S26 2019
http://library2.smu.ca/handle/01/29128
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