Tectonostratigraphic development of the Upper Triassic to Middle Jurassic in the Hoop Area, Barents Sea: Implications for understanding ultra-condensed reservoir units

Bibliographic Details
Published in:Marine and Petroleum Geology
Main Authors: Müller, R., Klausen, T.G., Line, L.H., Hafeez, A., Planke, S., Eide, F., Stueland, E., Jahren, J., Rismyhr, B., Olaussen, S.
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier BV 2022
Subjects:
Online Access:http://dx.doi.org/10.1016/j.marpetgeo.2022.105787
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spelling crelsevierbv:10.1016/j.marpetgeo.2022.105787 2023-05-15T15:38:22+02:00 Tectonostratigraphic development of the Upper Triassic to Middle Jurassic in the Hoop Area, Barents Sea: Implications for understanding ultra-condensed reservoir units Müller, R. Klausen, T.G. Line, L.H. Hafeez, A. Planke, S. Eide, F. Stueland, E. Jahren, J. Rismyhr, B. Olaussen, S. 2022 http://dx.doi.org/10.1016/j.marpetgeo.2022.105787 https://api.elsevier.com/content/article/PII:S0264817222002653?httpAccept=text/xml https://api.elsevier.com/content/article/PII:S0264817222002653?httpAccept=text/plain en eng Elsevier BV https://www.elsevier.com/tdm/userlicense/1.0/ http://creativecommons.org/licenses/by/4.0/ CC-BY Marine and Petroleum Geology volume 145, page 105787 ISSN 0264-8172 Stratigraphy Economic Geology Geology Geophysics Oceanography journal-article 2022 crelsevierbv https://doi.org/10.1016/j.marpetgeo.2022.105787 2022-11-29T03:13:39Z Article in Journal/Newspaper Barents Sea ScienceDirect (Elsevier - via Crossref) Barents Sea Marine and Petroleum Geology 145 105787
institution Open Polar
collection ScienceDirect (Elsevier - via Crossref)
op_collection_id crelsevierbv
language English
topic Stratigraphy
Economic Geology
Geology
Geophysics
Oceanography
spellingShingle Stratigraphy
Economic Geology
Geology
Geophysics
Oceanography
Müller, R.
Klausen, T.G.
Line, L.H.
Hafeez, A.
Planke, S.
Eide, F.
Stueland, E.
Jahren, J.
Rismyhr, B.
Olaussen, S.
Tectonostratigraphic development of the Upper Triassic to Middle Jurassic in the Hoop Area, Barents Sea: Implications for understanding ultra-condensed reservoir units
topic_facet Stratigraphy
Economic Geology
Geology
Geophysics
Oceanography
format Article in Journal/Newspaper
author Müller, R.
Klausen, T.G.
Line, L.H.
Hafeez, A.
Planke, S.
Eide, F.
Stueland, E.
Jahren, J.
Rismyhr, B.
Olaussen, S.
author_facet Müller, R.
Klausen, T.G.
Line, L.H.
Hafeez, A.
Planke, S.
Eide, F.
Stueland, E.
Jahren, J.
Rismyhr, B.
Olaussen, S.
author_sort Müller, R.
title Tectonostratigraphic development of the Upper Triassic to Middle Jurassic in the Hoop Area, Barents Sea: Implications for understanding ultra-condensed reservoir units
title_short Tectonostratigraphic development of the Upper Triassic to Middle Jurassic in the Hoop Area, Barents Sea: Implications for understanding ultra-condensed reservoir units
title_full Tectonostratigraphic development of the Upper Triassic to Middle Jurassic in the Hoop Area, Barents Sea: Implications for understanding ultra-condensed reservoir units
title_fullStr Tectonostratigraphic development of the Upper Triassic to Middle Jurassic in the Hoop Area, Barents Sea: Implications for understanding ultra-condensed reservoir units
title_full_unstemmed Tectonostratigraphic development of the Upper Triassic to Middle Jurassic in the Hoop Area, Barents Sea: Implications for understanding ultra-condensed reservoir units
title_sort tectonostratigraphic development of the upper triassic to middle jurassic in the hoop area, barents sea: implications for understanding ultra-condensed reservoir units
publisher Elsevier BV
publishDate 2022
url http://dx.doi.org/10.1016/j.marpetgeo.2022.105787
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geographic Barents Sea
geographic_facet Barents Sea
genre Barents Sea
genre_facet Barents Sea
op_source Marine and Petroleum Geology
volume 145, page 105787
ISSN 0264-8172
op_rights https://www.elsevier.com/tdm/userlicense/1.0/
http://creativecommons.org/licenses/by/4.0/
op_rightsnorm CC-BY
op_doi https://doi.org/10.1016/j.marpetgeo.2022.105787
container_title Marine and Petroleum Geology
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