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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
    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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  • 3
    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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  • 4
    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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  • 5
    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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  • 6
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    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
    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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