Hydrothermally induced diagenesis: Evidence from shallow marine-deltaic sediments, Wilhelmøya, Svalbard
Sedimentary basins containing igneous intrusions within sedimentary reservoir units represent an important risk in petroleum exploration. The Upper Triassic to Lower Jurassic sediments at Wilhelmøya (Svalbard) contains reservoir heterogeneity as a result of sill emplacement and represent a unique ca...
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ftdoajarticles:oai:doaj.org/article:fab7c20e5f4b4d34ae61c505a434667b 2023-08-27T04:12:17+02:00 Hydrothermally induced diagenesis: Evidence from shallow marine-deltaic sediments, Wilhelmøya, Svalbard Beyene G. Haile Urszula Czarniecka Kelai Xi Aleksandra Smyrak-Sikora Jens Jahren Alvar Braathen Helge Hellevang 2019-03-01T00:00:00Z https://doi.org/10.1016/j.gsf.2018.02.015 https://doaj.org/article/fab7c20e5f4b4d34ae61c505a434667b EN eng Elsevier http://www.sciencedirect.com/science/article/pii/S167498711830080X https://doaj.org/toc/1674-9871 1674-9871 doi:10.1016/j.gsf.2018.02.015 https://doaj.org/article/fab7c20e5f4b4d34ae61c505a434667b Geoscience Frontiers, Vol 10, Iss 2, Pp 629-649 (2019) Geology QE1-996.5 article 2019 ftdoajarticles https://doi.org/10.1016/j.gsf.2018.02.015 2023-08-06T00:43:30Z Sedimentary basins containing igneous intrusions within sedimentary reservoir units represent an important risk in petroleum exploration. The Upper Triassic to Lower Jurassic sediments at Wilhelmøya (Svalbard) contains reservoir heterogeneity as a result of sill emplacement and represent a unique case study to better understand the effect of magmatic intrusions on the general burial diagenesis of siliciclastic sediments. Sills develop contact metamorphic aureoles by conduction as presented in many earlier studies. However, there is significant impact of localized hydrothermal circulation systems affecting reservoir sediments at considerable distance from the sill intrusions. Dolerite sill intrusions in the studied area are of limited vertical extent (∼12 m thick), but created localized hydrothermal convection cells affecting sediments at considerable distance (more than five times the thickness of the sill) from the intrusions. We present evidence that the sedimentary sequence can be divided into two units: (1) the bulk poorly lithified sediment with a maximum burial temperature much lower than 60–70 °C, and (2) thinner intervals outside the contact zone that have experienced hydrothermal temperatures (around 140 °C). The main diagenetic alteration associated with normal burial diagenesis is minor mechanical plastic deformation of ductile grains such as mica. Mineral grain contacts show no evidence of pressure dissolution and the vitrinite reflectance suggests a maximum temperature of ∼40 °C. Contrary to this, part of the sediment, preferentially along calcite cemented flow baffles, show evidence of hydrothermal alteration. These hydrothermally altered sediment sections are characterized by recrystallized carbonate cemented intervals. Further, the hydrothermal solutions have resulted in localized sericitization (illitization) of feldspars, albitization of both K-feldspar and plagioclase and the formation of fibrous illite nucleated on kaolinite. These observations suggest hydrothermal alteration at T > ... Article in Journal/Newspaper Svalbard Wilhelmøya Directory of Open Access Journals: DOAJ Articles Svalbard Wilhelmøya ENVELOPE(20.418,20.418,79.062,79.062) Geoscience Frontiers 10 2 629 649 |
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Geology QE1-996.5 |
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Geology QE1-996.5 Beyene G. Haile Urszula Czarniecka Kelai Xi Aleksandra Smyrak-Sikora Jens Jahren Alvar Braathen Helge Hellevang Hydrothermally induced diagenesis: Evidence from shallow marine-deltaic sediments, Wilhelmøya, Svalbard |
topic_facet |
Geology QE1-996.5 |
description |
Sedimentary basins containing igneous intrusions within sedimentary reservoir units represent an important risk in petroleum exploration. The Upper Triassic to Lower Jurassic sediments at Wilhelmøya (Svalbard) contains reservoir heterogeneity as a result of sill emplacement and represent a unique case study to better understand the effect of magmatic intrusions on the general burial diagenesis of siliciclastic sediments. Sills develop contact metamorphic aureoles by conduction as presented in many earlier studies. However, there is significant impact of localized hydrothermal circulation systems affecting reservoir sediments at considerable distance from the sill intrusions. Dolerite sill intrusions in the studied area are of limited vertical extent (∼12 m thick), but created localized hydrothermal convection cells affecting sediments at considerable distance (more than five times the thickness of the sill) from the intrusions. We present evidence that the sedimentary sequence can be divided into two units: (1) the bulk poorly lithified sediment with a maximum burial temperature much lower than 60–70 °C, and (2) thinner intervals outside the contact zone that have experienced hydrothermal temperatures (around 140 °C). The main diagenetic alteration associated with normal burial diagenesis is minor mechanical plastic deformation of ductile grains such as mica. Mineral grain contacts show no evidence of pressure dissolution and the vitrinite reflectance suggests a maximum temperature of ∼40 °C. Contrary to this, part of the sediment, preferentially along calcite cemented flow baffles, show evidence of hydrothermal alteration. These hydrothermally altered sediment sections are characterized by recrystallized carbonate cemented intervals. Further, the hydrothermal solutions have resulted in localized sericitization (illitization) of feldspars, albitization of both K-feldspar and plagioclase and the formation of fibrous illite nucleated on kaolinite. These observations suggest hydrothermal alteration at T > ... |
format |
Article in Journal/Newspaper |
author |
Beyene G. Haile Urszula Czarniecka Kelai Xi Aleksandra Smyrak-Sikora Jens Jahren Alvar Braathen Helge Hellevang |
author_facet |
Beyene G. Haile Urszula Czarniecka Kelai Xi Aleksandra Smyrak-Sikora Jens Jahren Alvar Braathen Helge Hellevang |
author_sort |
Beyene G. Haile |
title |
Hydrothermally induced diagenesis: Evidence from shallow marine-deltaic sediments, Wilhelmøya, Svalbard |
title_short |
Hydrothermally induced diagenesis: Evidence from shallow marine-deltaic sediments, Wilhelmøya, Svalbard |
title_full |
Hydrothermally induced diagenesis: Evidence from shallow marine-deltaic sediments, Wilhelmøya, Svalbard |
title_fullStr |
Hydrothermally induced diagenesis: Evidence from shallow marine-deltaic sediments, Wilhelmøya, Svalbard |
title_full_unstemmed |
Hydrothermally induced diagenesis: Evidence from shallow marine-deltaic sediments, Wilhelmøya, Svalbard |
title_sort |
hydrothermally induced diagenesis: evidence from shallow marine-deltaic sediments, wilhelmøya, svalbard |
publisher |
Elsevier |
publishDate |
2019 |
url |
https://doi.org/10.1016/j.gsf.2018.02.015 https://doaj.org/article/fab7c20e5f4b4d34ae61c505a434667b |
long_lat |
ENVELOPE(20.418,20.418,79.062,79.062) |
geographic |
Svalbard Wilhelmøya |
geographic_facet |
Svalbard Wilhelmøya |
genre |
Svalbard Wilhelmøya |
genre_facet |
Svalbard Wilhelmøya |
op_source |
Geoscience Frontiers, Vol 10, Iss 2, Pp 629-649 (2019) |
op_relation |
http://www.sciencedirect.com/science/article/pii/S167498711830080X https://doaj.org/toc/1674-9871 1674-9871 doi:10.1016/j.gsf.2018.02.015 https://doaj.org/article/fab7c20e5f4b4d34ae61c505a434667b |
op_doi |
https://doi.org/10.1016/j.gsf.2018.02.015 |
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Geoscience Frontiers |
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10 |
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2 |
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629 |
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649 |
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