GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • PANGAEA  (12)
  • Berlin, Heidelberg :Springer Berlin / Heidelberg,  (1)
Document type
Keywords
Language
  • 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.
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    facet.materialart.
    Unknown
    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
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    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
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    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
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 5
    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
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 6
    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
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 7
    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
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 8
    Publication Date: 2024-01-09
    Keywords: 151-908A; Age, comment; Age model; Comment; 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, 72 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 9
    Publication Date: 2024-01-09
    Keywords: 151-909C; 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, 25 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 10
    Publication Date: 2024-01-09
    Keywords: 162-986C; 162-986D; Age, comment; Age model; Comment; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Event label; Joides Resolution; Leg162; North Greenland Sea; Ocean Drilling Program; ODP; Reference/source; Sedimentation rate
    Type: Dataset
    Format: text/tab-separated-values, 61 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...