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
  • Ocean Drilling Program; ODP  (2)
  • 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  (1)
  • Cratering.  (1)
Document type
Keywords
Language
Years
  • 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
    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 ...
  • 3
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Knies, Jochen; Matthiessen, Jens; Vogt, Christoph; Laberg, Jan Sverre; Hjelstuen, Berit O; Smelror, Morten; Larsen, Eiliv; Andreassen, Karin; Eidvin, Tor; Vorren, Tore O (2009): The Plio-Pleistocene glaciation of the Barents Sea–Svalbard region: a new model based on revised chronostratigraphy. Quaternary Science Reviews, 28(9-10), 812-829, https://doi.org/10.1016/j.quascirev.2008.12.002
    Publication Date: 2024-01-09
    Description: Based on a revised chronostratigraphy, and compilation of borehole data from the Barents Sea continental margin, a coherent glaciation model is proposed for the Barents Sea ice sheet over the past 3.5 million years (Ma). Three phases of ice growth are suggested: (1) The initial build-up phase, covering mountainous regions and reaching the coastline/shelf edge in the northern Barents Sea during short-term glacial intensification, is concomitant with the onset of the Northern Hemisphere Glaciation (3.6-2.4 Ma). (2) A transitional growth phase (2.4-1.0 Ma), during which the ice sheet expanded towards the southern Barents Sea and reached the northwestern Kara Sea. This is inferred from step-wise decrease of Siberian river-supplied smectite-rich sediments, likely caused by ice sheet blockade and possibly reduced sea ice formation in the Kara Sea as well as glacigenic wedge growth along the northwestern Barents Sea margin hampering entrainment and transport of sea ice sediments to the Arctic-Atlantic gateway. (3) Finally, large-scale glaciation in the Barents Sea occurred after 1 Ma with repeated advances to the shelf edge. The timing is inferred from ice grounding on the Yermak Plateau at about 0.95 Ma, and higher frequencies of gravity-driven mass movements along the western Barents Sea margin associated with expansive glacial growth.
    Keywords: Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 5 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    facet.materialart.
    Unknown
    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
    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...