Uplift, deflation and marine onlap of a Jurassic rift dome, illustrated by a backstepping Middle–Upper Jurassic shelf‐to‐slope succession, Geographical Society Ø, East Greenland

Abstract “Doming–rifting–spreading” constitute the main phases of classical plate tectonics. The Middle–Upper Jurassic succession of East Greenland is interpreted as reflecting formation, deflation and onlap of a rift dome, similar to contemporaneous rift domes in the North Sea, Denmark and southern...

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Published in:Terra Nova
Main Authors: Surlyk, Finn, Alsen, Peter, Hovikoski, Jussi, Piasecki, Stefan
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:https://doi.org/10.1111/ter.12673
https://onlinelibrary.wiley.com/doi/pdf/10.1111/ter.12673
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author Surlyk, Finn
Alsen, Peter
Hovikoski, Jussi
Piasecki, Stefan
author_facet Surlyk, Finn
Alsen, Peter
Hovikoski, Jussi
Piasecki, Stefan
author_sort Surlyk, Finn
collection Wiley Online Library
container_issue 6
container_start_page 506
container_title Terra Nova
container_volume 35
description Abstract “Doming–rifting–spreading” constitute the main phases of classical plate tectonics. The Middle–Upper Jurassic succession of East Greenland is interpreted as reflecting formation, deflation and onlap of a rift dome, similar to contemporaneous rift domes in the North Sea, Denmark and southern Sweden. The succession forms a northwards backstepping and onlapping early rift succession in the N–S oriented basin. Deposition ranged from coastal over shallow marine and slope sands, through offshore siltstones to deep basinal mudstones. An outlier on the island Geographical Society Ø fills an important gap in the documentation of the doming, deflation and progressive onlap. Bajocian deposition took place in a shallow marine shelf. This was followed in the late Oxfordian by slope and base‐of‐slope deposition. The backstepping succession onlaps progressively older rocks towards the north, illustrating the gradual deflation, erosion and onlap of the dome, constituting the early part of the doming–rifting–spreading phases of classical plate tectonics.
format Article in Journal/Newspaper
genre East Greenland
Greenland
genre_facet East Greenland
Greenland
geographic Geographical Society Ø
Greenland
geographic_facet Geographical Society Ø
Greenland
id crwiley:10.1111/ter.12673
institution Open Polar
language English
long_lat ENVELOPE(-23.250,-23.250,72.950,72.950)
op_collection_id crwiley
op_container_end_page 513
op_doi https://doi.org/10.1111/ter.12673
op_rights http://creativecommons.org/licenses/by/4.0/
op_source Terra Nova
volume 35, issue 6, page 506-513
ISSN 0954-4879 1365-3121
publishDate 2023
publisher Wiley
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spelling crwiley:10.1111/ter.12673 2025-03-23T15:35:25+00:00 Uplift, deflation and marine onlap of a Jurassic rift dome, illustrated by a backstepping Middle–Upper Jurassic shelf‐to‐slope succession, Geographical Society Ø, East Greenland Surlyk, Finn Alsen, Peter Hovikoski, Jussi Piasecki, Stefan 2023 https://doi.org/10.1111/ter.12673 https://onlinelibrary.wiley.com/doi/pdf/10.1111/ter.12673 en eng Wiley http://creativecommons.org/licenses/by/4.0/ Terra Nova volume 35, issue 6, page 506-513 ISSN 0954-4879 1365-3121 journal-article 2023 crwiley https://doi.org/10.1111/ter.12673 2025-02-25T02:53:45Z Abstract “Doming–rifting–spreading” constitute the main phases of classical plate tectonics. The Middle–Upper Jurassic succession of East Greenland is interpreted as reflecting formation, deflation and onlap of a rift dome, similar to contemporaneous rift domes in the North Sea, Denmark and southern Sweden. The succession forms a northwards backstepping and onlapping early rift succession in the N–S oriented basin. Deposition ranged from coastal over shallow marine and slope sands, through offshore siltstones to deep basinal mudstones. An outlier on the island Geographical Society Ø fills an important gap in the documentation of the doming, deflation and progressive onlap. Bajocian deposition took place in a shallow marine shelf. This was followed in the late Oxfordian by slope and base‐of‐slope deposition. The backstepping succession onlaps progressively older rocks towards the north, illustrating the gradual deflation, erosion and onlap of the dome, constituting the early part of the doming–rifting–spreading phases of classical plate tectonics. Article in Journal/Newspaper East Greenland Greenland Wiley Online Library Geographical Society Ø ENVELOPE(-23.250,-23.250,72.950,72.950) Greenland Terra Nova 35 6 506 513
spellingShingle Surlyk, Finn
Alsen, Peter
Hovikoski, Jussi
Piasecki, Stefan
Uplift, deflation and marine onlap of a Jurassic rift dome, illustrated by a backstepping Middle–Upper Jurassic shelf‐to‐slope succession, Geographical Society Ø, East Greenland
title Uplift, deflation and marine onlap of a Jurassic rift dome, illustrated by a backstepping Middle–Upper Jurassic shelf‐to‐slope succession, Geographical Society Ø, East Greenland
title_full Uplift, deflation and marine onlap of a Jurassic rift dome, illustrated by a backstepping Middle–Upper Jurassic shelf‐to‐slope succession, Geographical Society Ø, East Greenland
title_fullStr Uplift, deflation and marine onlap of a Jurassic rift dome, illustrated by a backstepping Middle–Upper Jurassic shelf‐to‐slope succession, Geographical Society Ø, East Greenland
title_full_unstemmed Uplift, deflation and marine onlap of a Jurassic rift dome, illustrated by a backstepping Middle–Upper Jurassic shelf‐to‐slope succession, Geographical Society Ø, East Greenland
title_short Uplift, deflation and marine onlap of a Jurassic rift dome, illustrated by a backstepping Middle–Upper Jurassic shelf‐to‐slope succession, Geographical Society Ø, East Greenland
title_sort uplift, deflation and marine onlap of a jurassic rift dome, illustrated by a backstepping middle–upper jurassic shelf‐to‐slope succession, geographical society ø, east greenland
url https://doi.org/10.1111/ter.12673
https://onlinelibrary.wiley.com/doi/pdf/10.1111/ter.12673