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  • Age, dated; Age, strontium isotope; Comment; Corrected; DEPTH, sediment/rock; ECO2; Lithologic unit/sequence; Measured; Molo_Formation; Reference/source; Site; Strontium-87/Strontium-86 ratio; Strontium-87/Strontium-86 ratio, error; Sub-seabed CO2 Storage: Impact on Marine Ecosystems  (1)
  • Geology, Structural-Arctic regions.  (1)
Document type
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  • 1
    Online Resource
    Online Resource
    Tectonics of the Arctic. (2021)
    Cham :Springer International Publishing AG,
    Details
    Keywords: Geology, Structural-Arctic regions. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (215 pages)
    Edition: 1st ed.
    ISBN: 9783030468620
    Series Statement: Springer Geology Series
    URL: https://ebookcentral.proquest.com/lib/geomar/detail.action?docID=6546234
    DDC: 551.809113
    Language: English
    Note: Intro -- Acknowledgements -- Introduction -- Contents -- New Tectonic Map of the Arctic -- 1 History of the Tectonic Map Compilation -- 2 Tectonic Provinces of the Arctic -- References -- Deep Structures of the Circumpolar Arctic -- 1 Gravity and Magnetic Anomaly Maps -- 2 Earth's Crust Velocity Models by Wide-Angle Seismics -- 3 Set of Deep Structure Maps -- 4 Geotransect Across the Circumpolar Arctic -- References -- Arctic Sedimentary Cover Structure and Eastern Arctic Structure Maps -- 1 Sedimentary Cover Structure -- 1.1 Map of Seismic Knowledge -- 1.2 Correlation Chart Showing Stratigraphic Tie of Reflectors -- 1.3 Set of Composite Seismic Profiles Across Major Geological Structures of the Northeastern Arctic -- 2 Structural Maps of the Eastern Arctic -- 2.1 Acoustic Basement Structure Map -- 2.2 Top Cretaceous Structure Map (Reflector pCU) -- 2.3 Eocene Structure Map (Reflector UB) -- References -- Geological and Paleogeographic Map of the Eastern Arctic -- 1 Eastern Arctic Geological Map at Scale 1:5 M -- 2 Eastern Arctic Structural Geological Map -- 3 Map of Tectonic Zoning of the Eastern Arctic Basement -- 4 Paleogeographic Maps of the Eastern Arctic -- 4.1 Late Jurassic Paleogeographic Map (−145 Ma) -- 4.2 Early Cretaceous (Aptian-Albian) Paleogeographic Map (−112 Ma) -- 4.3 Paleogene (Eocene) Paleogeographic Map (−35 Ma) -- 4.4 Neogene (Miocene) Paleogeographic Map (−10 Ma) -- References -- Study of the Arctic Seabed Rocks -- 1 Study of the Arctic Basin Bottom-Rock Material -- 2 Geochemical and Isotope-Geochronological Knowledge of the Eastern Arctic -- 3 Geological Section of the Acoustic Basement of the Alpha-Mendeleev Rise -- References -- Geology of the Eastern Arctic Islands and Continental Fridge of the Arctic Seas -- 1 Severnaya Zemlya Archipelago -- 2 Taimyr Peninsula -- 3 New Siberian Islands Archipelago -- 4 Wrangel Island. , 5 Continental Eastern Arctic -- References -- Correlation of Chukotka, Wrangel Island and the Mendeleev Rise -- 1 Geologic Framework -- 2 Petrographic Data -- 3 Geochemical Data -- 4 U-Pb Dating -- 5 Results of the Studies -- 6 Conclusions -- References -- Tectonic Model and Evolution of the Arctic -- 1 Tectonic Model of the Arctic -- 2 Tectonic Evolution of the Eastern Arctic -- References.
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  • 2
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    Table1. Strontium isotope data from investigated wells (2017)
    PANGAEA
    In:  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, http://www.geologi.no/images/NJG_articles/Eidvin_et_al.pdf
    Details
    Publication Date: 2023-02-24
    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.
    Keywords: Age, dated; Age, strontium isotope; Comment; Corrected; DEPTH, sediment/rock; ECO2; Lithologic unit/sequence; Measured; Molo_Formation; Reference/source; Site; Strontium-87/Strontium-86 ratio; Strontium-87/Strontium-86 ratio, error; Sub-seabed CO2 Storage: Impact on Marine Ecosystems
    Type: Dataset
    Format: text/tab-separated-values, 144 data points
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