Table1. Strontium isotope data from investigated wells ...
The Molo Formation represents a characteristic depositional unit on the inner Mid-Norwegian continental shelf and extends along the coast for about 500 km from Møre to Lofoten. It was deposited by coastal progradation in a wave-dominated environment with extensive long-shore drift. The age and strat...
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ftdatacite:10.1594/pangaea.871881 2024-09-15T18:17:55+00:00 Table1. Strontium isotope data from investigated wells ... Eidvin, Tor Bugge, Tom Smelror, Morten 2017 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.871881 https://doi.pangaea.de/10.1594/PANGAEA.871881 en eng PANGAEA http://www.geologi.no/images/NJG_articles/Eidvin_et_al.pdf Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Site Reference/source Lithologic unit/sequence DEPTH, sediment/rock Strontium-87/Strontium-86 ratio Strontium-87/Strontium-86 ratio, error Age, dated Comment Measured Corrected Age, strontium isotope Sub-seabed CO2 Storage Impact on Marine Ecosystems ECO2 dataset Supplementary Dataset Dataset 2017 ftdatacite https://doi.org/10.1594/pangaea.871881 2024-08-01T10:57:37Z The Molo Formation represents a characteristic depositional unit on the inner Mid-Norwegian continental shelf and extends along the coast for about 500 km from Møre to Lofoten. It was deposited by coastal progradation in a wave-dominated environment with extensive long-shore drift. The age and stratigraphic relationships have been heavily debated since it was discovered and first described nearly forty years ago. Based on new age information from exploration wells in the Draugen Field on the Trøndelag Platform, the Molo Formation is now determined to be of Late Miocene to Early Pliocene age. It is interpreted to be the proximal equivalent to the deeper marine Kai Formation in the Norwegian Sea and a lateral equivalent to the Utsira Formation in the North Sea. These formations were all deposited as a result of the compression and uplift of mainland Norway in mid Miocene time. In this paper we describe and document the datings and formally define the Molo Formation as a new stratigraphic unit. ... : Supplement to: Eidvin, Tor; Bugge, Tom; Smelror, Morten (2007): The Molo Formation, deposited by coastal progradation on the inner Mid-Norwegian continental shelf, coeval with the Kai Formation to the west and the Utsira Formation in the North Sea. Norwegian Journal of Geology, 87, 75-142 ... Dataset Lofoten Norwegian Sea DataCite |
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Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Site Reference/source Lithologic unit/sequence DEPTH, sediment/rock Strontium-87/Strontium-86 ratio Strontium-87/Strontium-86 ratio, error Age, dated Comment Measured Corrected Age, strontium isotope Sub-seabed CO2 Storage Impact on Marine Ecosystems ECO2 |
spellingShingle |
Site Reference/source Lithologic unit/sequence DEPTH, sediment/rock Strontium-87/Strontium-86 ratio Strontium-87/Strontium-86 ratio, error Age, dated Comment Measured Corrected Age, strontium isotope Sub-seabed CO2 Storage Impact on Marine Ecosystems ECO2 Eidvin, Tor Bugge, Tom Smelror, Morten Table1. Strontium isotope data from investigated wells ... |
topic_facet |
Site Reference/source Lithologic unit/sequence DEPTH, sediment/rock Strontium-87/Strontium-86 ratio Strontium-87/Strontium-86 ratio, error Age, dated Comment Measured Corrected Age, strontium isotope Sub-seabed CO2 Storage Impact on Marine Ecosystems ECO2 |
description |
The Molo Formation represents a characteristic depositional unit on the inner Mid-Norwegian continental shelf and extends along the coast for about 500 km from Møre to Lofoten. It was deposited by coastal progradation in a wave-dominated environment with extensive long-shore drift. The age and stratigraphic relationships have been heavily debated since it was discovered and first described nearly forty years ago. Based on new age information from exploration wells in the Draugen Field on the Trøndelag Platform, the Molo Formation is now determined to be of Late Miocene to Early Pliocene age. It is interpreted to be the proximal equivalent to the deeper marine Kai Formation in the Norwegian Sea and a lateral equivalent to the Utsira Formation in the North Sea. These formations were all deposited as a result of the compression and uplift of mainland Norway in mid Miocene time. In this paper we describe and document the datings and formally define the Molo Formation as a new stratigraphic unit. ... : Supplement to: Eidvin, Tor; Bugge, Tom; Smelror, Morten (2007): The Molo Formation, deposited by coastal progradation on the inner Mid-Norwegian continental shelf, coeval with the Kai Formation to the west and the Utsira Formation in the North Sea. Norwegian Journal of Geology, 87, 75-142 ... |
format |
Dataset |
author |
Eidvin, Tor Bugge, Tom Smelror, Morten |
author_facet |
Eidvin, Tor Bugge, Tom Smelror, Morten |
author_sort |
Eidvin, Tor |
title |
Table1. Strontium isotope data from investigated wells ... |
title_short |
Table1. Strontium isotope data from investigated wells ... |
title_full |
Table1. Strontium isotope data from investigated wells ... |
title_fullStr |
Table1. Strontium isotope data from investigated wells ... |
title_full_unstemmed |
Table1. Strontium isotope data from investigated wells ... |
title_sort |
table1. strontium isotope data from investigated wells ... |
publisher |
PANGAEA |
publishDate |
2017 |
url |
https://dx.doi.org/10.1594/pangaea.871881 https://doi.pangaea.de/10.1594/PANGAEA.871881 |
genre |
Lofoten Norwegian Sea |
genre_facet |
Lofoten Norwegian Sea |
op_relation |
http://www.geologi.no/images/NJG_articles/Eidvin_et_al.pdf |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.871881 |
_version_ |
1810456041041690624 |