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  • 1
    Keywords: Impact craters -- Barents Sea. ; Submarine geology. ; Cratering. ; Impact. ; Electronic books.
    Description / Table of Contents: This book describes the Mjølnir impact event in the context of the geological and geophysical history of the Barents Sea region, and goes on to present elaborative numerical models of its formation and associated tsunami generation.
    Type of Medium: Online Resource
    Pages: 1 online resource (324 pages)
    Edition: 1st ed.
    ISBN: 9783540882602
    Series Statement: Impact Studies
    Language: English
    Note: Intro -- Preface -- Acknowledgements -- Contents -- Contributors -- 1 Introduction -- 1.1 Background -- 1.2 Barents Sea Geology -- 1.3 Mjlnir Impact at Volgian/Ryazanian Boundary -- 1.4 The Investigation History of Mjlnir -- 1.5 The Search for Oil and Gas in the Barents Sea -- 1.6 Future Mjlnir Studies -- 1.7 Etymology -- 2 Geological Framework -- 2.1 Plate Tectonic Evolution of the Arctic -- 2.2 Mesozoic Stratigraphy and Depositional Environments of the Arctic -- 2.2.1 Geological and Palaeogeographical Setting -- 2.2.1.1 Cretaceous Palaeogeographic Setting -- 2.2.1.2 The Barents Sea in Time and Space -- 2.2.2 Svalbard -- 2.2.3 Barents Sea -- 2.2.4 Greenland -- 2.2.5 Siberia -- 2.2.6 Late Jurassic and Early Cretaceous Depositional Configuration -- 3 Impact Structure and Morphology -- 3.1 Seismic Reflection Database -- 3.2 Shallow Structure -- 3.2.1 Main Features -- 3.2.2 Detailed Seismic Correlation to Nearby Shallow Boreholes -- 3.2.2.1 Borehole 7430/10-U-01 -- 3.2.2.2 Borehole 7329/03-U-01 -- 3.2.2.3 Impact Timing as Revealed from Seismic Correlation -- 3.2.3 Impact-Induced Deformation -- 3.2.4 Near-Field Erosional Features -- 3.2.4.1 Resurge Gullies -- 3.2.4.2 Crater Rim -- 3.3 Deep Structure -- 3.3.1 Impact-Induced Disturbance -- 3.3.1.1 Seismic Reflectivity Patterns -- 3.3.1.2 Shape and Dimensions -- 4 Impact Geophysics and Modelling -- 4.1 Features Related to the Cratering Process -- 4.1.1 Excavated Crater and Breccia -- 4.1.2 Impact Melts -- 4.1.3 Gravitational Collapse -- 4.1.4 Structural Uplift -- 4.2 Impact into a Marine Sedimentary Basin -- 4.3 Impact Crater Modelling -- 4.3.1 Potential Field Data -- 4.3.2 Marine Gravity Anomalies and Modelling -- 4.3.3 Marine Magnetic Anomalies and Modelling -- 4.3.4 Traveltime/Velocity Anomalies and Modelling -- 4.4 Modelled Porosity Anomalies -- 4.4.1 Density-Derived Porosity Anomaly. , 4.4.2 Velocity-Derived Porosity Anomaly -- 4.4.3 Postimpact Deformation-Derived Porosity Anomaly -- 4.4.4 Porosity Anomaly and Pore Space Volume -- 4.4.5 Porosity Anomaly and Hydrocarbon Potential -- 4.5 Potential Non-impact Origin -- 4.5.1 Clay Diapir -- 4.5.2 Salt Diapir -- 4.5.3 Igneous Feature -- 4.6 Alternative Interpretation of Mjlnir Crater Dimensions Based on Regional Gravity and Aero-magnetic Profiles and Modelling -- 4.6.1 The Mjølnir Aero-magnetic Anomaly -- 4.6.2 The Mjølnir Regional Free-Air Gravity Anomaly -- 4.6.3 Alternative Interpretation of Mjølnir Crater Dimensions -- 4.7 Impact-Induced Changes in Physical Properties -- 4.8 Mjlnir as an Oblique Impact Event -- 4.8.1 Elongated Crater Diameter -- 4.8.2 Seismic Disturbance Asymmetry -- 4.8.3 Peak-Ring Character -- 4.8.4 Offsets in Brecciation and Structural Uplift -- 4.8.5 Impact Direction and Angle -- 4.8.6 Mjølnir Impact Obliquity Constrains Models for Near-Field Perturbations -- 4.8.6.1 Nature and Distribution of Proximal Ejecta -- 4.8.6.2 Tsunami-Wave Distribution -- 5 Impact Cratering and Post-impact Sedimentation -- 5.1 Introduction -- 5.2 The Mjlnir Crater Core (7329/03-U-01) -- 5.2.1 The Ragnarok Formation -- 5.2.2 Ragnarok Formation, Unit I -- 5.2.3 Ragnarok Formation, Unit II -- 5.2.4 Hekkingen Formation -- 5.2.5 Klippfisk Formation -- 5.2.6 Spectral Gamma Results -- 5.2.7 Paleontology of the Ragnarok Formation -- 5.2.8 Paleontology of the Hekkingen Formation -- 5.2.9 Magnetic Properties and Densities of the Mjølnir Crater Core (7329/03-U-01) -- 5.3 The Mjlnir Impact Event in a Sequence Stratigraphical Framework -- 5.4 The Evidence for Impact Crater Formation -- 5.4.1 The Crater: Its Structure and Shape -- 5.4.2 Fracturing and Conglomerates -- 5.4.3 Mineralogical Evidence of Impact Cratering -- 5.4.4 Geochemistry -- 5.4.5 Paleontological Evidence of Impact Cratering. , 6 Ejecta Geology -- 6.1 The Identification of Ejecta Beds -- 6.1.1 Introduction -- 6.1.2 The Ragnarok Formation and Sindre Bed -- 6.1.3 The Discoveries of Large Amounts of Soot in Mjølnir Related Sediments -- 6.2 The Stratigraphical Distribution of the Ejecta Beds -- 6.2.1 Borehole 7430/10-U-01 -- 6.2.2 Borehole 7018/05-U-01 -- 6.2.3 Janusfjellet, Central Spitsbergen -- 6.2.4 Nordvik Peninsula, North-Western Siberia -- 6.2.5 The Mjølnir Ejecta as a Regional Stratigraphic Marker -- 7 The Impact Dynamics -- 7.1 Introduction -- 7.2 Numerical Model -- 7.3 Cratering Process -- 7.4 Ejecta Formation and Distribution -- 7.5 Resurge Flow and Tsunami Generation -- 7.6 Conclusions -- 8 Structural Analysis of Deformed Central Peak Sediments -- 8.1 Structural Position of the Mjlnir Impact Crater -- 8.2 Structural Geological Analysis -- 8.2.1 Type A Structures: Early Extensional Micro-faults and Fissures -- 8.2.2 Type B-Structures: Fragmentation of Semi-consolidated or Consolidated Beds -- 8.2.3 Type C-Structures: Liquefaction and Shearing -- 8.2.4 Type D-Structures: Folds, Rotated Strata and Shear Bands -- 8.2.5 Type E-Structures: Intensely Sheared Sequences -- 8.2.6 Type F-Structures: Late Brittle Fractures and Microfaults -- 8.3 Deformation History of the Ragnarok Formation -- 9 Postimpact Deformation Due to Sediment Loading: The Mjlnir Paradigm -- 9.1 Postimpact Burial -- 9.2 Mjlnir Crater -- 9.2.1 Postimpact Infilling -- 9.2.2 Faulting and Differential Vertical Movements -- 9.3 Other Craters: Chesapeake Bay, Chicxulub, Bosumtwi, and Montagnais -- 9.4 Original Crater Relief Reconstruction -- 9.4.1 Mjølnir -- 9.4.2 Chicxulub -- 9.4.3 Bosumtwi -- 9.4.4 Chesapeake Bay -- 9.5 Correction of Crater Morphological and Structural Parameters -- 9.5.1 Parameters Prone to Postimpact Burial Modification -- 9.5.2 Postimpact Modification Correction Factor. , 10 The Mjlnir Tsunami -- 10.1 Introduction -- 10.2 Tsunami Models -- 10.3 Tsunami Generation -- 10.3.1 Near Field Evolution -- 10.3.2 Far Field Propagation -- 10.3.2.1 Estimates of Far-Field Behaviour -- 10.3.2.2 Computations of Far-Field Behaviour -- 10.4 Discussion -- References -- Index -- Index.
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  • 2
    Online Resource
    Online Resource
    Cham : Springer International Publishing | Cham : Imprint: Springer
    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
    Language: English
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  • 3
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    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
    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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  • 4
    Keywords: Mines and mineral resources Environmental aspects ; Sustainable development ; Aufsatzsammlung
    Type of Medium: Book
    Pages: vi, 346 Seiten , Illustrationen, Karten, Diagramme , 26 cm
    ISBN: 9781786205735 , 1786205734
    Series Statement: Geological Society special publication no. 526
    RVK:
    Language: English
    Note: Includes bibliographical references and index
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  • 5
    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
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  • 6
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Polar research 5 (1987), S. 0 
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Notes: Well preserved dinoflagellate cyst and acritarch assemblages are recorded from Upper Bathonian and Callovian deposits on Northbrook Island, Franz Josef Land. More than 45 species have been identified. Two new species are proposed: Parvocysta bjaerkei sp. nov., and Meiourogonyaulax spongiosa sp. nov. The recorded marine microfloras are compared with assemblages reported from contemporaneous strata in Svalbard.
    Type of Medium: Electronic Resource
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  • 7
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    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
    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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  • 8
    Publication Date: 2023-05-12
    Keywords: Area/locality; Conductivity, average; Depth, bottom/max; Heat flow; LATITUDE; LONGITUDE; Number of temperature data; Sample, optional label/labor no; Temperature gradient
    Type: Dataset
    Format: text/tab-separated-values, 7 data points
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  • 9
    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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  • 10
    Publication Date: 2024-01-09
    Keywords: 151-911A; Age, comment; Age model; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Joides Resolution; Leg151; North Greenland Sea; Ocean Drilling Program; ODP; Reference/source; Sedimentation rate
    Type: Dataset
    Format: text/tab-separated-values, 35 data points
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