Petroleum systems of the Barents shelf. A regional well-based study of the mesozoic

The entire Barents Sea area has experienced a complex geological evolution. From orogenic processes connected to Caledonian mountain building in Palaeozoic to basin formation related to the opening of the Atlantic Ocean in Paleogene. Uplift and erosion processes (Exhumation) that fined place in Cein...

Full description

Bibliographic Details
Main Author: Yankina, Anna
Format: Master Thesis
Language:English
Published: UiT Norges arktiske universitet 2017
Subjects:
Online Access:https://hdl.handle.net/10037/11486
_version_ 1829306457158320128
author Yankina, Anna
author_facet Yankina, Anna
author_sort Yankina, Anna
collection University of Tromsø: Munin Open Research Archive
description The entire Barents Sea area has experienced a complex geological evolution. From orogenic processes connected to Caledonian mountain building in Palaeozoic to basin formation related to the opening of the Atlantic Ocean in Paleogene. Uplift and erosion processes (Exhumation) that fined place in Ceinozoic contribute to erosion and redepositing of thick sedimentary sequences over Barents Sea area. Exhumation relates to one of the biggest problems due to petroleum exploration on Barents shelf. It has significant implication on source rock maturation, hydrocarbon potential and reservoir rock properties. Uplift and erosion processes affects basin geometry and burial sedimentary rock properties as well in that way that source rock uplifted to shallow level is not enough mature to produce hydrocarbons. Other consequences connected to exhumation are hydrocarbon redistribution and leakage from traps, decreasing in reservoir quality properties due to compaction processes and porosity reduction. Unfortunately, implication of exhumation processes on petroleum system in the Barents Sea is not fully understood and need more research. Uplift and erosion affects sedimentary rock properties. Log data from wells, especially velocity log, is very sensitive to lithological variation and compaction trends of the rocks. Velocity log data from wells are cruel in executing of analysis of sedimentary basins. It can provide information about burial evolution of the area and changing in temperature gradient. Velocity log data is also important due to recognition of lithological units, overpressure and fluid content in the formations.
format Master Thesis
genre Barents Sea
genre_facet Barents Sea
geographic Barents Sea
geographic_facet Barents Sea
id ftunivtroemsoe:oai:munin.uit.no:10037/11486
institution Open Polar
language English
op_collection_id ftunivtroemsoe
op_relation https://hdl.handle.net/10037/11486
op_rights Attribution-NonCommercial-ShareAlike 3.0 Unported (CC BY-NC-SA 3.0)
openAccess
Copyright 2017 The Author(s)
https://creativecommons.org/licenses/by-nc-sa/3.0
publishDate 2017
publisher UiT Norges arktiske universitet
record_format openpolar
spelling ftunivtroemsoe:oai:munin.uit.no:10037/11486 2025-04-13T14:16:24+00:00 Petroleum systems of the Barents shelf. A regional well-based study of the mesozoic Yankina, Anna 2017-06-30 https://hdl.handle.net/10037/11486 eng eng UiT Norges arktiske universitet UiT The Arctic University of Norway https://hdl.handle.net/10037/11486 Attribution-NonCommercial-ShareAlike 3.0 Unported (CC BY-NC-SA 3.0) openAccess Copyright 2017 The Author(s) https://creativecommons.org/licenses/by-nc-sa/3.0 VDP::Matematikk og Naturvitenskap: 400::Geofag: 450 VDP::Mathematics and natural science: 400::Geosciences: 450 GEO-3900 Master thesis Mastergradsoppgave 2017 ftunivtroemsoe 2025-03-14T05:17:56Z The entire Barents Sea area has experienced a complex geological evolution. From orogenic processes connected to Caledonian mountain building in Palaeozoic to basin formation related to the opening of the Atlantic Ocean in Paleogene. Uplift and erosion processes (Exhumation) that fined place in Ceinozoic contribute to erosion and redepositing of thick sedimentary sequences over Barents Sea area. Exhumation relates to one of the biggest problems due to petroleum exploration on Barents shelf. It has significant implication on source rock maturation, hydrocarbon potential and reservoir rock properties. Uplift and erosion processes affects basin geometry and burial sedimentary rock properties as well in that way that source rock uplifted to shallow level is not enough mature to produce hydrocarbons. Other consequences connected to exhumation are hydrocarbon redistribution and leakage from traps, decreasing in reservoir quality properties due to compaction processes and porosity reduction. Unfortunately, implication of exhumation processes on petroleum system in the Barents Sea is not fully understood and need more research. Uplift and erosion affects sedimentary rock properties. Log data from wells, especially velocity log, is very sensitive to lithological variation and compaction trends of the rocks. Velocity log data from wells are cruel in executing of analysis of sedimentary basins. It can provide information about burial evolution of the area and changing in temperature gradient. Velocity log data is also important due to recognition of lithological units, overpressure and fluid content in the formations. Master Thesis Barents Sea University of Tromsø: Munin Open Research Archive Barents Sea
spellingShingle VDP::Matematikk og Naturvitenskap: 400::Geofag: 450
VDP::Mathematics and natural science: 400::Geosciences: 450
GEO-3900
Yankina, Anna
Petroleum systems of the Barents shelf. A regional well-based study of the mesozoic
title Petroleum systems of the Barents shelf. A regional well-based study of the mesozoic
title_full Petroleum systems of the Barents shelf. A regional well-based study of the mesozoic
title_fullStr Petroleum systems of the Barents shelf. A regional well-based study of the mesozoic
title_full_unstemmed Petroleum systems of the Barents shelf. A regional well-based study of the mesozoic
title_short Petroleum systems of the Barents shelf. A regional well-based study of the mesozoic
title_sort petroleum systems of the barents shelf. a regional well-based study of the mesozoic
topic VDP::Matematikk og Naturvitenskap: 400::Geofag: 450
VDP::Mathematics and natural science: 400::Geosciences: 450
GEO-3900
topic_facet VDP::Matematikk og Naturvitenskap: 400::Geofag: 450
VDP::Mathematics and natural science: 400::Geosciences: 450
GEO-3900
url https://hdl.handle.net/10037/11486