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...
Published in: | Terra Nova |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
2023
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Subjects: | |
Online Access: | https://doi.org/10.1111/ter.12673 https://onlinelibrary.wiley.com/doi/pdf/10.1111/ter.12673 |
_version_ | 1827412235327111168 |
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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 |
record_format | openpolar |
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 |