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  • 2020-2024  (3)
  • 2015-2019  (1)
  • 1995-1999  (5)
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  • 1
    Online Resource
    Online Resource
    Tectonics of the Arctic (2021)
    Cham : Springer International Publishing | Cham : Imprint: Springer
    Details Availability
    Keywords: Geophysics. ; Structural geology. ; Sedimentology. ; Oceanography. ; Geotechnical engineering. ; Russland Nord ; Arktis ; Mittelozeanischer Rücken ; Nordpolarmeer ; Geologie ; Tektonik ; Wrangelinsel ; Tschuktschenhalbinsel ; Alpha Ridge ; Meeresgeologie ; Meeresboden ; Arktis ; Tiefenstruktur ; Paläogeografie
    Description / Table of Contents: New Tectonic map of the Arctic -- Deep structures of the Circumpolar Arctic -- Arctic sedimentary cover structure and Eastern Arctic structure maps -- Geological and paleogeographic map of the Eastern Arctic -- Study of the Arctic seabed rocks -- Geology of the Eastern Arctic islands and continental fridge of the Arctic seas -- Correlation of Chukotka, Wrangel Island and the Mendeleev Rise -- Tectonic model and evolution of the Arctic.
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource(XIII, 208 p. 126 illus., 119 illus. in color.)
    Edition: 1st ed. 2021.
    ISBN: 9783030468620
    Series Statement: Springer Geology
    URL: https://doi.org/10.1007/978-3-030-46862-0
    URL: https://swbplus.bsz-bw.de/bsz1756963002cov.jpg
    DOI: 10.1007/978-3-030-46862-0
    Language: English
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  • 2
    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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  • 3
    Image
    Image
    The Green Stone Age : exploration and exploitation of minerals for green technologies (2023)
    London : The Geological Society
    Details Availability
    Keywords: Mines and mineral resources Environmental aspects ; Sustainable development ; Aufsatzsammlung
    Type of Medium: Image
    Pages: vi, 346 Seiten , Illustrationen, Karten, Diagramme , 26 cm
    ISBN: 9781786205735 , 1786205734
    Series Statement: Geological Society special publication no. 526
    RVK:
    TH 6200
    Language: English
    Note: Includes bibliographical references and index
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  • 4
    Electronic Resource
    Electronic Resource
    The Klippfisk Formation—a new lithostratigraphic unit of Lower Cretaceous platform carbonates on the Western Barents Shelf (1998)
    Oxford, UK : Blackwell Publishing Ltd
    Polar research 17 (1998), S. 0 
    Details
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Notes: A new Lower Cretceous lithostratigraphic unit of the Western Barents Shelf, named the Klippfisk Formation, is formally introduced. The formation represents a condensed carbonate succession deposited on platform areas and structural highs, where it consists of limestones and marls, often glauconitic. The limestones may have a nodular appearance, and fossil debris, which are dominated by Inoceramus prisms, may be abundant. The Klippfisk Formation is composed of two members: the Kutling Member defined herein from cores drilled on the Bjarmeland Platform, and the coeval Tordenskjoldberget Member described on Kong Karls Land. The base of the formation is defined by the abrupt decrease in gamma-ray intensity, where the dark shales of the underlying Hekkingen or Agardhfjellet formations are replaced by marls. It is often unconformable. The Klippfisk Formation is of Berriasian to Early Barremian age and appears to be time-transgressive over parts of the Western Barents Shelf (including Kong Karls Land). It passes laterally into the basinal Knurr Formation. On Kongsøya (Kong Karls Land) a thin shale unit, bounded by unconformities, earlier included in the Tordenskjoldberget Member, represents the northernmost extension of the overlying Kolje Formation in the Barents Shelf.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1751-8369.1998.tb00271.x
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    Paper (German National Licenses)
    Fulltext
  • 5
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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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  • 6
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    (Table 1) Polarity chron boundaries at ODP Site 162-986 sediments (1999)
    PANGAEA
    Details
    Publication Date: 2024-01-09
    Keywords: 162-986C; 162-986D; Age model; Chronozone; Depth, composite; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Event label; Joides Resolution; Leg162; North Greenland Sea; Ocean Drilling Program; ODP
    Type: Dataset
    Format: text/tab-separated-values, 15 data points
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  • 7
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    (Table 2) Polarity chron boundaries at ODP Site 162-987 sediments (1999)
    PANGAEA
    Details
    Publication Date: 2024-01-09
    Keywords: 162-987A; 162-987B; 162-987D; 162-987E; Age model; Chronozone; Comment; Depth, composite; Depth, reference; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Event label; Iceland Sea; Joides Resolution; Leg162; Ocean Drilling Program; ODP
    Type: Dataset
    Format: text/tab-separated-values, 186 data points
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  • 8
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    (Table 3) Foraminiferal 87Sr/86Sr ratios and ages of ODP Hole 162-986D sediments (1999)
    PANGAEA
    Details
    Publication Date: 2024-01-09
    Keywords: 162-986D; Age, dated; Age, dated material; Age, derived using regression formula of Hodell et al. (1991); DEPTH, sediment/rock; DRILL; Drilling/drill rig; Joides Resolution; Leg162; North Greenland Sea; Ocean Drilling Program; ODP; Strontium-87/Strontium-86 ratio
    Type: Dataset
    Format: text/tab-separated-values, 30 data points
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  • 9
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    Polarity chron boundaries and foraminiferal 87Sr/86Sr ratios of ODP Sites 162-986 and 162-987 (1999)
    PANGAEA
    In:  Supplement to: Channell, James E T; Smelror, Morten; Jansen, Eystein; Higgins, Sean M; Lehman, Benoît; Eidvin, Tor; Solheim, Anders (1999): Age models for glacial fan deposits off East Greenland and Svalbard (Sites 986 and 987). In: Raymo, ME; Jansen, E; Blum, P; Herbert, TD (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 162, 1-18, https://doi.org/10.2973/odp.proc.sr.162.008.1999
    Details
    Publication Date: 2024-01-09
    Description: Cores recovered at Sites 986 and 987 comprise glacial fan sedimentation associated with the Svalbard-Barents Sea and Greenland Ice Sheets, respectively. At Site 986, the top 150 m and the basal 250 m yielded interpretable magnetic stratigraphies. The record from the intervening 550 m is compromised by drilling-related core deformation, poor recovery, and numerous debris flows. The uppermost 150 m appears to record the Brunhes/Matuyama boundary and the Jaramillo Subchron. The base of the drilled section (at ~950 meters below seafloor [mbsf]) is interpreted to lie within the Matuyama Chron (age 〈2.58 Ma) with an apparent normal polarity interval in the ~730-750 mbsf interval. Dinoflagellate cyst biostratigraphy and Sr isotopic ratios are consistent with a Matuyama age for the base of the drilled section and with the normal polarity interval as the Olduvai Subchron. On the other hand, the last occurrence of Neogloboquadrina atlantica (sinistral) and the last common occurrence of the warm-dwelling Globigerina bulloides at 647-650 mbsf in Hole 986D indicate an age for this level of ~2.3 Ma, inconsistent with the designation of the Olduvai Subchron in the ~730-750 mbsf interval. If the age at 647-650 mbsf in Hole 986D is taken as 2.3 Ma and the base of the hole lies within the Matuyama Chron, then the sedimentation rate in the basal 300 m of the cored section averages 1 m/k.y. At Site 987, the magnetic stratigraphy is fairly unambiguous throughout the section and yields an age of 7.5 Ma (Chron 4n) for the base of the drilled section. The paucity of calcareous and siliceous microfossils precludes biostratigraphic corroboration of the magnetostratigraphic interpretation, although dinoflagellate cysts provide general support, particularly at the base of the section. The age model indicates relatively low sedimentation rates (~5 cm/k.y.) at the base of the section with rates at least four to five times greater during intervals of debris flows at ~5-4.6 and ~2.6 Ma.
    Keywords: Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 3 datasets
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