S1:Svalbard Composite Tectono-Sedimentary Element, Barents Sea
Mississippian to Middle Pennsylvanian succession; the Billefjorden Group and the lower part of Gipsdalen Group. TSE 1: Uppermost Devonian to Lower Mississippian TSE 1 deposited in an interior continental sag basin possibly related to initial rift stage in SW. TSE 2: Serpukhovian to Moscovian synrift...
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2023
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Online Access: | https://doi.org/10.6084/m9.figshare.21968706.v1 https://figshare.com/articles/journal_contribution/S1_Svalbard_Composite_Tectono-Sedimentary_Element_Barents_Sea/21968706 |
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ftgeosoclonfig:oai:figshare.com:article/21968706 2023-05-15T15:38:38+02:00 S1:Svalbard Composite Tectono-Sedimentary Element, Barents Sea Snorre Olaussen Sten-Andreas Grundvåg Kim Senger Ingrid Anell Peter Betlem Thomas Birchall Alvar Braathen Winfried Dallmann Malte Jochmann Erik P. Johannessen Gareth Lord Atle Mørk Per T. Osmundsen Aleksandra Smyrak-Sikora Lars Stemmerik 2023-01-27T17:56:18Z https://doi.org/10.6084/m9.figshare.21968706.v1 https://figshare.com/articles/journal_contribution/S1_Svalbard_Composite_Tectono-Sedimentary_Element_Barents_Sea/21968706 unknown doi:10.6084/m9.figshare.21968706.v1 https://figshare.com/articles/journal_contribution/S1_Svalbard_Composite_Tectono-Sedimentary_Element_Barents_Sea/21968706 CC BY 4.0 CC-BY Geology stratigraphic elements represent global icehouse conditions svalbard composite tectono latest tectonic phase initial rift stage continental interior basins barents sea mississippian middle pennsylvanian succession rift basins middle pennsylvanian two tectono tectonic event late mississippian uppermost devonian tse 1 tropical semi tropical humid sedimentary element moscovian synrift lower part gipsdalen group deposition occurred climate changed billefjorden group Text Journal contribution 2023 ftgeosoclonfig https://doi.org/10.6084/m9.figshare.21968706.v1 2023-02-02T00:06:05Z Mississippian to Middle Pennsylvanian succession; the Billefjorden Group and the lower part of Gipsdalen Group. TSE 1: Uppermost Devonian to Lower Mississippian TSE 1 deposited in an interior continental sag basin possibly related to initial rift stage in SW. TSE 2: Serpukhovian to Moscovian synrift. These two tectono-stratigraphic elements represent the transition from Mississippian continental interior basins of TSE 1 (Figs a and b) to development of rift basins of TSE 2 in the late Mississippian to middle Pennsylvanian (Figs c and d). The continental interior basins of TSE 1 formed shortly after the latest tectonic phase of the Svalbardian (Ellesmerian) tectonic event. The climate changed from tropical humid to tropical semi-arid in the transition from TSE 1 to 2 (Figs a and d) and deposition occurred during global icehouse conditions. Other Non-Article Part of Journal/Newspaper Barents Sea Billefjorden Svalbard Geological Society of London: Figshare Barents Sea Billefjorden ENVELOPE(16.417,16.417,78.563,78.563) Gipsdalen ENVELOPE(16.877,16.877,78.505,78.505) Svalbard |
institution |
Open Polar |
collection |
Geological Society of London: Figshare |
op_collection_id |
ftgeosoclonfig |
language |
unknown |
topic |
Geology stratigraphic elements represent global icehouse conditions svalbard composite tectono latest tectonic phase initial rift stage continental interior basins barents sea mississippian middle pennsylvanian succession rift basins middle pennsylvanian two tectono tectonic event late mississippian uppermost devonian tse 1 tropical semi tropical humid sedimentary element moscovian synrift lower part gipsdalen group deposition occurred climate changed billefjorden group |
spellingShingle |
Geology stratigraphic elements represent global icehouse conditions svalbard composite tectono latest tectonic phase initial rift stage continental interior basins barents sea mississippian middle pennsylvanian succession rift basins middle pennsylvanian two tectono tectonic event late mississippian uppermost devonian tse 1 tropical semi tropical humid sedimentary element moscovian synrift lower part gipsdalen group deposition occurred climate changed billefjorden group Snorre Olaussen Sten-Andreas Grundvåg Kim Senger Ingrid Anell Peter Betlem Thomas Birchall Alvar Braathen Winfried Dallmann Malte Jochmann Erik P. Johannessen Gareth Lord Atle Mørk Per T. Osmundsen Aleksandra Smyrak-Sikora Lars Stemmerik S1:Svalbard Composite Tectono-Sedimentary Element, Barents Sea |
topic_facet |
Geology stratigraphic elements represent global icehouse conditions svalbard composite tectono latest tectonic phase initial rift stage continental interior basins barents sea mississippian middle pennsylvanian succession rift basins middle pennsylvanian two tectono tectonic event late mississippian uppermost devonian tse 1 tropical semi tropical humid sedimentary element moscovian synrift lower part gipsdalen group deposition occurred climate changed billefjorden group |
description |
Mississippian to Middle Pennsylvanian succession; the Billefjorden Group and the lower part of Gipsdalen Group. TSE 1: Uppermost Devonian to Lower Mississippian TSE 1 deposited in an interior continental sag basin possibly related to initial rift stage in SW. TSE 2: Serpukhovian to Moscovian synrift. These two tectono-stratigraphic elements represent the transition from Mississippian continental interior basins of TSE 1 (Figs a and b) to development of rift basins of TSE 2 in the late Mississippian to middle Pennsylvanian (Figs c and d). The continental interior basins of TSE 1 formed shortly after the latest tectonic phase of the Svalbardian (Ellesmerian) tectonic event. The climate changed from tropical humid to tropical semi-arid in the transition from TSE 1 to 2 (Figs a and d) and deposition occurred during global icehouse conditions. |
format |
Other Non-Article Part of Journal/Newspaper |
author |
Snorre Olaussen Sten-Andreas Grundvåg Kim Senger Ingrid Anell Peter Betlem Thomas Birchall Alvar Braathen Winfried Dallmann Malte Jochmann Erik P. Johannessen Gareth Lord Atle Mørk Per T. Osmundsen Aleksandra Smyrak-Sikora Lars Stemmerik |
author_facet |
Snorre Olaussen Sten-Andreas Grundvåg Kim Senger Ingrid Anell Peter Betlem Thomas Birchall Alvar Braathen Winfried Dallmann Malte Jochmann Erik P. Johannessen Gareth Lord Atle Mørk Per T. Osmundsen Aleksandra Smyrak-Sikora Lars Stemmerik |
author_sort |
Snorre Olaussen |
title |
S1:Svalbard Composite Tectono-Sedimentary Element, Barents Sea |
title_short |
S1:Svalbard Composite Tectono-Sedimentary Element, Barents Sea |
title_full |
S1:Svalbard Composite Tectono-Sedimentary Element, Barents Sea |
title_fullStr |
S1:Svalbard Composite Tectono-Sedimentary Element, Barents Sea |
title_full_unstemmed |
S1:Svalbard Composite Tectono-Sedimentary Element, Barents Sea |
title_sort |
s1:svalbard composite tectono-sedimentary element, barents sea |
publishDate |
2023 |
url |
https://doi.org/10.6084/m9.figshare.21968706.v1 https://figshare.com/articles/journal_contribution/S1_Svalbard_Composite_Tectono-Sedimentary_Element_Barents_Sea/21968706 |
long_lat |
ENVELOPE(16.417,16.417,78.563,78.563) ENVELOPE(16.877,16.877,78.505,78.505) |
geographic |
Barents Sea Billefjorden Gipsdalen Svalbard |
geographic_facet |
Barents Sea Billefjorden Gipsdalen Svalbard |
genre |
Barents Sea Billefjorden Svalbard |
genre_facet |
Barents Sea Billefjorden Svalbard |
op_relation |
doi:10.6084/m9.figshare.21968706.v1 https://figshare.com/articles/journal_contribution/S1_Svalbard_Composite_Tectono-Sedimentary_Element_Barents_Sea/21968706 |
op_rights |
CC BY 4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.6084/m9.figshare.21968706.v1 |
_version_ |
1766369820229500928 |