Seismic stratigraphic analysis of the Lower Triassic on Norsel High, central Barents Sea

Master's thesis in Petroleum engineering Norsel High is located in the southeastern part of the Bjarmeland Platform area, close to the southwestern margin of the Nordkapp Basin. There is one well located on Norsel High, exploration well 7226/11-1. The Lower Triassic, the Havert Formation, is ve...

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Bibliographic Details
Main Author: Liknes, Veronica
Format: Master Thesis
Language:English
Published: University of Stavanger, Norway 2014
Subjects:
Online Access:http://hdl.handle.net/11250/224378
id ftunivstavanger:oai:uis.brage.unit.no:11250/224378
record_format openpolar
spelling ftunivstavanger:oai:uis.brage.unit.no:11250/224378 2023-06-11T04:10:34+02:00 Seismic stratigraphic analysis of the Lower Triassic on Norsel High, central Barents Sea Liknes, Veronica 2014-06-05 application/pdf http://hdl.handle.net/11250/224378 eng eng University of Stavanger, Norway Masteroppgave/UIS-TN-IPT/2014; http://hdl.handle.net/11250/224378 CC0 1.0 Universal http://creativecommons.org/publicdomain/zero/1.0/ petroleumsteknologi petroleumsgeologi Barentshavet seismic stratigraphic analysis VDP::Technology: 500::Rock and petroleum disciplines: 510::Geological engineering: 513 Master thesis 2014 ftunivstavanger 2023-05-29T16:01:54Z Master's thesis in Petroleum engineering Norsel High is located in the southeastern part of the Bjarmeland Platform area, close to the southwestern margin of the Nordkapp Basin. There is one well located on Norsel High, exploration well 7226/11-1. The Lower Triassic, the Havert Formation, is very deeply buried and seems to be a prograding tide – dominated delta system, which very often have poor or challenging reservoir qualities, and therefore has been a bit challenging. The Havert Formation has been interpreted to be dominated by mixed – influenced delta systems with impacts from fluvial input, tidal action and drift currents. This interpretation is based on different sets of data. These different dataset are core description, detailed well interpretation, 2D – and 3D seismic interpretation. The first dataset is the core description of the Havert Formation from three core samples, combined with the second dataset, a detailed well interpretation, which has been interpreted in sequences and depositional environments. The third dataset is seismic interpretation, comprising of both 2D and 3D seismic interpretation. Integrating these datasets gives the Havert Formation a thorough interpretation. The main goal for this study is to provide a better understanding of the Lower Triassic on Norsel High, focusing on the stratigraphic and tectonostratigraphic evolution of the Lower Triassic basin-fill. Master Thesis Barents Sea Barentshav* Nordkapp Nordkapp Basin University of Stavanger: UiS Brage Barents Sea Norsel ENVELOPE(-64.099,-64.099,-64.759,-64.759)
institution Open Polar
collection University of Stavanger: UiS Brage
op_collection_id ftunivstavanger
language English
topic petroleumsteknologi
petroleumsgeologi
Barentshavet
seismic stratigraphic analysis
VDP::Technology: 500::Rock and petroleum disciplines: 510::Geological engineering: 513
spellingShingle petroleumsteknologi
petroleumsgeologi
Barentshavet
seismic stratigraphic analysis
VDP::Technology: 500::Rock and petroleum disciplines: 510::Geological engineering: 513
Liknes, Veronica
Seismic stratigraphic analysis of the Lower Triassic on Norsel High, central Barents Sea
topic_facet petroleumsteknologi
petroleumsgeologi
Barentshavet
seismic stratigraphic analysis
VDP::Technology: 500::Rock and petroleum disciplines: 510::Geological engineering: 513
description Master's thesis in Petroleum engineering Norsel High is located in the southeastern part of the Bjarmeland Platform area, close to the southwestern margin of the Nordkapp Basin. There is one well located on Norsel High, exploration well 7226/11-1. The Lower Triassic, the Havert Formation, is very deeply buried and seems to be a prograding tide – dominated delta system, which very often have poor or challenging reservoir qualities, and therefore has been a bit challenging. The Havert Formation has been interpreted to be dominated by mixed – influenced delta systems with impacts from fluvial input, tidal action and drift currents. This interpretation is based on different sets of data. These different dataset are core description, detailed well interpretation, 2D – and 3D seismic interpretation. The first dataset is the core description of the Havert Formation from three core samples, combined with the second dataset, a detailed well interpretation, which has been interpreted in sequences and depositional environments. The third dataset is seismic interpretation, comprising of both 2D and 3D seismic interpretation. Integrating these datasets gives the Havert Formation a thorough interpretation. The main goal for this study is to provide a better understanding of the Lower Triassic on Norsel High, focusing on the stratigraphic and tectonostratigraphic evolution of the Lower Triassic basin-fill.
format Master Thesis
author Liknes, Veronica
author_facet Liknes, Veronica
author_sort Liknes, Veronica
title Seismic stratigraphic analysis of the Lower Triassic on Norsel High, central Barents Sea
title_short Seismic stratigraphic analysis of the Lower Triassic on Norsel High, central Barents Sea
title_full Seismic stratigraphic analysis of the Lower Triassic on Norsel High, central Barents Sea
title_fullStr Seismic stratigraphic analysis of the Lower Triassic on Norsel High, central Barents Sea
title_full_unstemmed Seismic stratigraphic analysis of the Lower Triassic on Norsel High, central Barents Sea
title_sort seismic stratigraphic analysis of the lower triassic on norsel high, central barents sea
publisher University of Stavanger, Norway
publishDate 2014
url http://hdl.handle.net/11250/224378
long_lat ENVELOPE(-64.099,-64.099,-64.759,-64.759)
geographic Barents Sea
Norsel
geographic_facet Barents Sea
Norsel
genre Barents Sea
Barentshav*
Nordkapp
Nordkapp Basin
genre_facet Barents Sea
Barentshav*
Nordkapp
Nordkapp Basin
op_relation Masteroppgave/UIS-TN-IPT/2014;
http://hdl.handle.net/11250/224378
op_rights CC0 1.0 Universal
http://creativecommons.org/publicdomain/zero/1.0/
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