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  • 1
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Oceanography. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (599 pages)
    Edition: 1st ed.
    ISBN: 9783319209791
    Series Statement: Advances in Natural and Technological Hazards Research Series ; v.41
    DDC: 551.468
    Language: English
    Note: Intro -- Preface -- Contents -- Chapter 1: Submarine Mass Movements and Their Consequences: Progress and Challenges -- 1.1 Introduction -- 1.2 The 2015 Volume -- 1.2.1 Part I: Submarine Mass Movement in Margin Construction and Economic Significance -- 1.2.2 Part II: Failure Dynamics from Landslide Geomorphology -- 1.2.3 Part III: Geotechnical Aspects of Mass Movement -- 1.2.4 Part IV: Multidisciplinary Case Studies -- 1.2.5 Part V: Tectonics and Mass Movement Processes -- 1.2.6 Part VI: Fluid Flow and Gas Hydrates -- 1.2.7 Part VII: Mass Transport Deposits in Modern and Outcrop Sedimentology -- 1.2.8 Part VIII: Numerical and Statistical Analysis -- 1.2.9 Part IX: Tsunami Generation from Slope Failure -- 1.3 Looking to the Future -- References -- Part I: Submarine Mass Movement in Margin Construction and Economic Significance -- Chapter 2: The Role of Submarine Landslides in the Law of the Sea -- 2.1 Introduction -- 2.2 Case Studies -- 2.2.1 Rift Margins -- 2.2.1.1 Ireland, Porcupine Bank -- 2.2.1.2 Norway, Bear Island (Bjørnøya) and Franz-Victoria Trough Mouth Fans (TMF) -- 2.2.2 Transform Margins -- 2.2.2.1 France: French Guiana -- 2.2.3 Active Margins -- 2.2.3.1 Indonesia: Northwest Sumatra -- 2.3 Conclusions -- References -- Chapter 3: Fabric Development and Pore-Throat Reduction in a Mass-Transport Deposit in the Jubilee Gas Field, Eastern Gulf of ... -- 3.1 Introduction -- 3.2 Geologic Setting -- 3.3 Available Data and Methodology -- 3.4 Subsurface Expression of the Top-Seal MTD -- 3.5 Clay Fabric of the Top-Seal MTD: XRD, MICP, and XRTG Results -- 3.6 Discussion and Conclusion -- References -- Chapter 4: Seismic Geomorphology of the Israel Slump Complex in the Levant Basin (SE Mediterranean) -- 4.1 Introduction -- 4.2 Geological Setting -- 4.3 Dataset and Methodology -- 4.4 Geomorphology of the MTDs -- 4.5 Discussion and Conclusions. , References -- Chapter 5: Multiple Megaslide Complexes and Their Significance for the Miocene Stratigraphic Evolution of the Offshore Amazon ... -- 5.1 Introduction -- 5.1.1 Database and Methods -- 5.2 Results -- 5.2.1 The Amap Megaslide Complex (AMC) -- 5.2.2 The Central Amazon Fan Megaslide Complex (CAFMC) -- 5.2.3 The Par-Maranhão Megaslide Complex (PMMC) -- 5.3 Discussion -- 5.4 Conclusions -- References -- Chapter 6: Kinematics of Submarine Slope Failures in the Deepwater Taranaki Basin, New Zealand -- 6.1 Introduction -- 6.2 Data and Methods -- 6.3 Geological Framework -- 6.4 Results and Interpretations -- 6.4.1 MTD 1 -- 6.4.2 MTD 2 -- 6.5 Discussion -- 6.6 Conclusions -- References -- Part II: Failure Dynamics from Landslide Geomorphology -- Chapter 7: Postglacial Mass Failures in the Inner Hardangerfjorden System, Western Norway -- 7.1 Introduction -- 7.2 Study Site and Geological Setting -- 7.3 Data and Methods -- 7.4 Main Observations and Interpretations -- 7.5 Discussion -- 7.6 Conclusions -- References -- Chapter 8: Onshore and Offshore Geomorphological Features of the El Golfo Debris Avalanche (El Hierro, Canary Islands) -- 8.1 Introduction -- 8.1.1 Geological and Geomorphological Setting -- 8.1.2 Methods -- 8.2 Results -- 8.2.1 Morphology and Backscatter Mapping -- 8.2.2 Seismic Mapping -- 8.3 Discussion and Conclusions -- References -- Chapter 9: New Insights on Failure and Post-failure Dynamics of Submarine Landslides on the Intra-slope Palmarola Ridge (Centr... -- 9.1 Introduction -- 9.2 Geological Setting -- 9.3 Data and Methods -- 9.4 Results -- 9.4.1 General Morphology of Palmarola Ridge -- 9.4.2 Landslide Scars and Deposits -- 9.5 Discussions and Conclusions -- References -- Chapter 10: Assessment of Canyon Wall Failure Process from Multibeam Bathymetry and Remotely Operated Vehicle (ROV) Observatio... -- 10.1 Introduction. , 10.2 Data -- 10.3 Results -- 10.3.1 Canyon Morphology and Exposed Lithologies -- 10.3.2 Benthic Communities -- 10.3.3 Failure Processes and Erosion -- 10.3.3.1 Cohesive Failure Processes -- 10.3.3.2 Erosion -- 10.4 ``Biomarkers´´ as Failure Timing and Magnitude Indicators -- 10.5 Future Work -- References -- Chapter 11: The Chuí Megaslide Complex: Regional-Scale Submarine Landslides on the Southern Brazilian Margin -- 11.1 Introduction and Backgrounds -- 11.2 Data and Methods -- 11.3 Results and Discussions -- 11.3.1 Geomorphological Characterization -- 11.3.2 Seismic Architecture and Depositional Features -- 11.3.3 Possible Preconditioning Parameters and Triggering Mechanisms -- 11.4 Conclusions -- References -- Chapter 12: Submarine Landslides and Incised Canyons of the Southeast Queensland Continental Margin -- 12.1 Introduction -- 12.2 Study Area Location and Bathymetric Features -- 12.3 Sediment Sample Characteristics and Ages -- 12.3.1 Dredge Sample Ages -- 12.3.2 Core Sample Ages -- 12.4 Discussion and Conclusions -- References -- Chapter 13: Novel Method to Map the Morphology of Submarine Landslide Headwall Scarps Using Remotely Operated Vehicles -- 13.1 Introduction -- 13.2 Rockall Bank -- 13.3 Method -- 13.3.1 Data Collection -- 13.3.2 Data Processing -- 13.4 Results -- 13.5 Interpretation and Discussion -- 13.6 Conclusions and Further Work -- References -- Chapter 14: Flow Behaviour of a Giant Landslide and Debris Flow Entering Agadir Canyon, NW Africa -- 14.1 Introduction -- 14.2 Methods -- 14.3 Results -- 14.3.1 The Headwall Area and the Slide Fairway -- 14.3.2 Slide Fairway into Lower Agadir Canyon -- 14.4 Discussion and Conclusion -- References -- Chapter 15: Fine-Scale Morphology of Tubeworm Slump, Monterey Canyon -- 15.1 Introduction -- 15.2 Methods -- 15.3 Results -- 15.3.1 Surface of Smooth Ridge Surrounding Tubeworm Slump. , 15.3.2 Main Headwall Scarp -- 15.3.3 Sole of Slide Scar -- 15.4 Discussion and Conclusions -- References -- Chapter 16: Submarine Slide Topography and the Distribution of Vulnerable Marine Ecosystems: A Case Study in the Ionian Sea (E... -- 16.1 Introduction -- 16.2 Submarine Slide Topography on the Ionian Margin -- 16.3 Deep-Sea Habitats of the Ionian Margin and Relationships with Landslide Morphologies -- 16.4 Economic Significance of Submarine Landslide Areas -- References -- Part III: Geotechnical Aspects of Mass Movement -- Chapter 17: Shear Strength of Siliciclastic Sediments from Passive and Active Margins (0-100m Below Seafloor): Insights into S... -- 17.1 Background and Significance -- 17.2 Global Shear Strength Trends -- 17.3 Ideal Type Sites -- 17.4 Hydrostatic Pore Pressure Conditions at Type Sites -- 17.5 Continental Margin Sediment Shear Strength -- References -- Chapter 18: A Small Volume Calibration Chamber for Cone Penetration Testing (CPT) on Submarine Soils -- 18.1 Introduction -- 18.2 Methods -- 18.2.1 New MARCC Calibration Chamber Design -- 18.2.2 Sensors, Control and Measurement Devices -- 18.3 Results -- 18.3.1 Specimen Preparation and Cuxhaven Test Sand -- 18.3.2 Laboratory CPT Experiments -- 18.4 Discussion -- 18.5 Conclusion and Outlook -- References -- Chapter 19: Underwater Mass Movements in Lake Mjøsa, Norway -- 19.1 Introduction -- 19.2 Methods -- 19.2.1 Morphology -- 19.2.2 Slope Stability -- 19.2.3 Discussion -- References -- Chapter 20: In Situ Cyclic Softening of Marine Silts by Vibratory CPTU at Orkdalsfjord Test Site, Mid Norway -- 20.1 Introduction -- 20.2 Geological Setting -- 20.3 Material and Methods -- 20.3.1 CPTU -- 20.3.2 Triaxial Laboratory Testing -- 20.4 Results -- 20.4.1 Geotechnical Characterization of Silt Layers -- 20.4.2 Cyclic Triaxial Response of Silt Layers -- 20.5 Discussion and Conclusion. , References -- Chapter 21: First Results of the Geotechnical In Situ Investigation for Soil Characterisation Along the Upper Slope Off Vester... -- 21.1 Landslides Along the Slope Off Vesterålen -- 21.2 Methods -- 21.2.1 Sub-bottom Mapping -- 21.2.2 CPTU Investigation of Slope Sediments -- 21.2.3 Pseudo-static Factor of Safety (FoS) -- 21.3 Results -- 21.3.1 Sedimentological and Geotechnical Characterisation of Slope Sediments -- 21.3.2 Pseudo-static Slope Stability Analysis -- 21.4 Discussion and Outlook -- References -- Chapter 22: A Novel Micro-shear Tester for Failure Analysis of Fine and Cohesive Granular Matter -- 22.1 Introduction -- 22.2 Characterization of the Calcium Carbonate Sample -- 22.3 Micro Shear Tester and X-ray Computed Tomography -- 22.3.1 Micro Shear Tester -- 22.3.2 X-ray Computed Tomography (XCT) -- 22.3.3 Combination of muST and XCT -- 22.4 Conclusion -- References -- Chapter 23: Knickpoint Migration Induced by Landslide: Evidence from Laboratory to Field Observations in Wabush Lake -- 23.1 Introduction -- 23.2 Wabush Lake -- 23.3 Methodology -- 23.3.1 Geotechnical Properties -- 23.3.2 Excess Pore Pressure and Stability Analysis -- 23.4 Results -- 23.4.1 Geotechnical Tests -- 23.4.2 Excess Pore Water Pressure and Stability Analysis -- 23.5 Discussion -- 23.6 Conclusion -- References -- Chapter 24: Multiple Flow Slide Experiment in the Westerschelde Estuary, The Netherlands -- 24.1 Introduction -- 24.2 Field Test Set-Up -- 24.3 Applied Instrumentation -- 24.4 Results and Conclusions -- References -- Part IV: Multidisciplinary Case Studies -- Chapter 25: Submarine Mass Wasting on Hovgaard Ridge, Fram Strait, European Arctic -- 25.1 Introduction -- 25.2 Study Area -- 25.3 Material and Methods -- 25.4 Results -- 25.4.1 Western Slope -- 25.4.2 Eastern Slope -- 25.5 Discussion -- 25.6 Conclusions -- References. , Chapter 26: 3D Seismic Investigations of Pleistocene Mass Transport Deposits and Glacigenic Debris Flows on the North Sea Fan,.
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  • 2
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Submarine topography. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (554 pages)
    Edition: 1st ed.
    ISBN: 9783319578521
    Series Statement: Springer Geology Series
    DDC: 551.4683
    Language: English
    Note: Intro -- Foreword -- Acknowledgements -- Contents -- 1 Introduction -- 1 Our Blue Planet -- 2 Submarine Geomorphology -- 3 History of Submarine Geomorphology -- References -- Data and Methods in Submarine Geomorphology -- 2 Sidescan Sonar -- Abstract -- 1 History of Sonar -- 2 Principles of Sidescan Sonar -- 3 State of the Art -- 4 Strengths and Weaknesses -- 5 Future Developments -- Acknowledgements -- References -- 3 Multibeam Echosounders -- Abstract -- 1 Introduction -- 1.1 Review and History -- 1.2 Current Uses in Submarine Geomorphology -- 2 Physical/Technical Principles of the Method -- 2.1 Imaging Geometry -- 2.2 Range Performance -- 2.3 Range Resolution -- 2.4 Angular Resolution -- 2.5 Bottom Detection -- 2.6 Sounding Density -- 3 Integrated Sensors -- 3.1 Vessel Reference Frame -- 3.2 Orientation -- 3.3 Horizontal Positioning -- 3.4 Vertical Positioning -- 3.5 Sound Speed -- 4 State of the Art Tools -- 5 Strength and Weaknesses of the Method for Investigating Submarine Geomorphology -- 6 Conclusions -- References -- 4 Reflection and Refraction Seismic Methods -- Abstract -- 1 History of Seismic Methods -- 2 Physical Principles -- 2.1 Basic Principles of the Seismic Reflection Method -- 2.2 Basic Principles of the Seismic Refraction Method -- 3 Survey Design and Processing -- 3.1 Seismic Reflection Surveys -- 3.1.1 Types of Marine Seismic Reflection Surveys -- 3.1.2 The Seismic Source -- 3.1.3 Receiver Arrays -- 3.1.4 Recording Parameters -- 3.1.5 Basic Processing Steps -- 3.2 Seismic Refraction Surveys -- 3.2.1 Acquisition Geometries -- 3.2.2 Receiver Types -- 3.2.3 Basic Processing Scheme -- 3.2.4 Forward and Inverse Modeling -- 4 State of the Art Tools and Methods -- 4.1 Overview -- 4.2 Parametric Single-Beam Echo-Sounding -- 4.3 Deep-Towed Seismic Acquisition -- 4.4 High-Resolution 3D Seismic Imaging -- 4.5 Broadband Imaging. , 4.6 Mirror Imaging of OBS Data -- 4.7 Joint Inversion of Refraction and Reflection Data -- 4.8 3D Full-Waveform Inversion of Wide-Angle, Multi-azimuth Data -- 5 Strengths and Weaknesses -- Acknowledgements -- References -- 5 Quantitative Analyses of Morphological Data -- Abstract -- 1 Mapping Submarine Morphologies -- 2 Quantitative Structures, Shapes and Their Variations -- 3 Geostatistics to Geographical Information Systems -- 3.1 Basic Measurements -- 3.2 Variations with Spatial Scales -- 3.3 Finding Trends and Patterns -- 4 Conclusions -- References -- 6 Seafloor Sediment and Rock Sampling -- Abstract -- 1 Introduction -- 2 Surface Sediment Sampling -- 2.1 Dredging -- 2.2 Box Corer -- 2.3 Grab Sampler -- 2.4 ROV Push Cores -- 3 Shallow Sediment Coring -- 3.1 Gravity Corer -- 3.2 Piston Corer -- 3.3 Kasten Corer -- 3.4 Vibrocorer -- 3.5 Multi-corer and Mega Corer -- 3.6 Giant Piston Corer and the CALYPSO Corer -- 4 Seafloor Drilling -- 4.1 Oil and Gas Industry Operations -- 4.2 International Ocean Discovery Program -- 4.3 Seafloor Drill Rigs -- 5 Core Handling -- References -- 7 ROVs and AUVs -- Abstract -- 1 Method Descriptions -- 1.1 Remotely Operated Vehicles -- 1.2 Autonomous Underwater Vehicles -- 1.3 Using Robotic Vehicles to Study Seafloor Geomorphology -- 2 Different Applications of ROVs and AUVs for Geomorphological Studies -- 2.1 High-Resolution Multibeam Bathymetry -- 2.2 True 3-Dimensional Morphology -- 2.3 Sidescan and Synthetic Aperture Sonar -- 2.4 Photomosaicking and Photogrammetry -- 2.5 Laser Line Scan -- 3 Future Directions -- Acknowledgements -- References -- Submarine Landforms and Processes -- 8 Origin and Geomorphic Characteristics of Ocean Basins -- Abstract -- 1 Introduction -- 1.1 Definition of Terms-Ocean Basins and Bathymetric Basins -- 1.2 Tectonic Origin of Ocean Basins. , 1.3 Multiple Origins of Bathymetric Ocean Basins -- 1.4 Aims of This Study -- 2 Methods -- 3 Results -- 4 Discussion -- 4.1 Key Drivers of Basin Evolution -- 4.2 Seamount Frequency of Occurrence and Sediment Thickness -- 4.3 Geomorphology and Global Bottom Water Circulation -- 5 Conclusions -- Acknowledgements -- References -- 9 Drivers of Seafloor Geomorphic Change -- Abstract -- 1 Introduction -- 2 Plate Tectonics-Continental Break-up and Fate of the Oceanic Lithosphere at Convergent Plate Boundaries -- 2.1 Oceanic Spreading Centres -- 2.2 Transform Faults and Fracture Zones -- 2.3 Subduction Zones -- 2.4 Volcanic Islands -- 3 Sediment Types -- 3.1 Terrigenous Sediments (Also: Lithogenous) -- 3.2 Biogenic Sediments (Also: Biogenous) -- 3.3 Authigenic Sediments (Also: Hydrogenous) -- 3.4 Volcanogenic Sediments -- 3.5 Cosmogenous Sediments -- 3.6 Plastics -- 4 Gravity-Density Currents, Slope Instability and Mass Transport Deposits -- 4.1 The Ocean as a Sediment Sink -- 4.2 Density Currents, Erosion, Transport and Deposition -- 4.3 Submarine Slope Instability and Mass-Transport Deposits -- 5 Ice-Ice Bull-Dozing Effect from Land to the Sea on Polar Continental Margins -- 5.1 Ice Streams -- 5.2 Ice Grounding at the Continental Shelf Edge -- 5.3 Ice Retreating During Deglaciations -- 6 Compaction Disequilibrium-Pore Fluids Overpressure in Marine Sedimentary Sequences -- 7 Oceanic Circulation, Waves and Tides, and Sea Level Change -- 7.1 Bottom Currents -- 7.2 Waves and Tides -- 7.3 Sea Level Change -- 8 Chemical Precipitation/Dissolution and Bioconstructions -- 8.1 Methane-Derived Carbonate Precipitation -- 8.2 Weathering at Hydrothermal Vents -- 8.3 Salt Deformation -- 8.4 Submarine Karst -- 8.5 Benthic Organisms -- 9 Human Activity -- Suggested Reading -- Section 2 -- Section 3 -- Section 4 -- Section 5 -- Section 6 -- Section 7 -- Section 8. , Section 9 -- 10 Shallow Coastal Landforms -- Abstract -- 1 Introduction -- 2 Depositional Shallow Coastal Landforms -- 2.1 Ripples, Dunes, Sand Waves and Antidunes -- 2.2 Sand Ribbons, Sand Patches, Sand Banks -- 3 Erosional Shallow Coastal Landforms -- 3.1 Scours Produced by Vortex Flow: Flute Marks, Gutter Marks, and Furrows -- 3.2 Other Erosional Bedforms Produced by Turbulent Flow: Channels and Rills -- 3.3 Erosional Bedforms Caused by Imprints of Objects: Bounce, Brush, Skip, Prod, Groove, Roll and Chevron Marks -- 3.4 Bedforms Produced by Objects Lying on the Seafloor: Obstacle Marks and Current Crescents -- 4 Addressing Key Issues in Shallow Coastal Landform Evolution -- 4.1 Shallow Coastal Landform Changes: Geomorphometric Measurements -- 4.2 Shallow Coastal Landforms and Sediments: A New Approach to Benthic Habitat Mapping -- 5 Conclusions -- References -- 11 Continental Shelf Landforms -- Abstract -- 1 Introduction -- 2 Brief History of Research on Continental Shelf Landforms -- 3 Processes -- 4 Continental Shelf Landforms -- 4.1 Consolidated Bottoms -- 4.2 Erosive Morphologies -- 4.3 Prograding Landforms -- 4.4 Bedforms -- 4.5 Gas-Related Features -- 4.6 Anthropogenic Features -- 5 Key Research Questions and Future Directions -- Acknowledgements -- References -- 12 Submarine Glacial Landforms -- Abstract -- 1 Introduction -- 2 Landforms Produced in Different Glacial-Process Environments -- 2.1 Subglacial Landforms -- 2.1.1 Mega-Scale Glacial Lineations and Other Streamlined Subglacial Landforms -- 2.1.2 Hill-Hole Pairs -- 2.1.3 Crevasse-Fill Ridges -- 2.1.4 Subglacial Glacifluvial Landforms -- 2.2 Ice-Marginal Landforms -- 2.2.1 Moraine Ridges -- 2.2.2 Grounding-Zone Wedges -- 2.2.3 Ice-Proximal Fans -- 2.2.4 Lateral Moraines -- 2.2.5 Trough-Mouth Fans -- 2.3 Glacimarine Landforms -- 2.3.1 Iceberg Ploughmarks. , 2.3.2 Smooth Basin Fill from Meltwater Plumes -- 2.4 Marine Landforms -- 3 Glacial Landforms on the Norwegian Margin: A Case Study -- 3.1 Landforms in Cross-Shelf Troughs -- 3.2 Landforms on Inter-Trough Banks -- 3.3 Landsystem Models for Fast- and Slow-Flowing Ice -- 4 Future Research Objectives -- Acknowledgements -- References -- 13 Submarine Landslides -- Abstract -- 1 Introduction -- 2 Geomorphic Expression of Submarine Landslides -- 3 Investigating Submarine Landslides -- 3.1 Geomorphometric Analyses -- 3.2 Landslide Population Statistics -- 3.3 Very High Resolution Imaging and Repeat Surveying -- 3.4 3D Seismic Geomorphology of Submarine Landslides -- 4 Major Challenges and Future Directions -- 5 Conclusions -- References -- 14 Submarine Canyons and Gullies -- Abstract -- 1 Introduction -- 1.1 Definitions and Nomenclature -- 1.2 The Origin of Submarine Canyons -- 2 Submarine Canyon Morphology and Evolution -- 2.1 The Physiography of Submarine Canyons -- 2.2 A Brief Comparison with Fluvial Systems -- 2.3 Global Distribution of Submarine Canyons -- 2.4 Geomorphic Processes in Submarine Canyons -- 2.4.1 Sea Level and Regional Tectonic Forcing -- 2.4.2 Sedimentary and Hydrodynamic Processes -- 2.4.3 The Human Imprint -- 2.4.4 Marine Geohazards -- 3 Towards an Integrated Approach to Submarine Canyon Research -- Acknowledgments -- References -- 15 Submarine Fans and Their Channels, Levees, and Lobes -- Abstract -- 1 Introduction -- 2 Five Decades of Submarine Fan Research-Challenges and Progress -- 3 Processes -- 4 Morphology of Submarine Channels and Their Levees -- 5 Morphology of Submarine Lobes -- 6 Key Research Questions and Future Directions -- Acknowledgements -- References -- 16 Contourite Drifts and Associated Bedforms -- Abstract -- 1 Introduction -- 1.1 Scope and Terminology -- 1.2 Brief History of Study -- 2 Contourite Drifts. , 2.1 Sheeted Drifts.
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  • 3
    Keywords: Earth sciences ; Earth Sciences ; Sedimentology ; Oceanography ; Natural disasters ; Geotechnical engineering ; Physical geography ; Earth sciences ; Sedimentology ; Oceanography ; Natural disasters ; Geotechnical engineering ; Physical geography ; Konferenzschrift 2015 ; Submarine Gleitung ; Meeresgeologie ; Submarine Gleitung ; Massenbewegung ; Meeresgeologie ; Meeresboden ; Suspensionsströmung ; Submarine Gleitung ; Turbidit
    Description / Table of Contents: 1. Submarine Mass Movements and Their Consequences: Progress and Challenges -- Part I Submarine Mass Movement in Margin Construction and Economic Significance2. The Role of Submarine Landslides in the Law of the Sea -- 3. Fabric Development and Pore-Throat Reduction in a Mass-Transport Deposit in the Jubilee Gas Field, Eastern Gulf of Mexico: Consequences for the Sealing Capacity of MTDs -- 4. Seismic geomorphology of the Israel Slump Complex in the central Levant Basin (SE Mediterranean) -- 5. Multiple Megaslide Complexes and their Significance for the Miocene stratigraphic evolution of the offshore Amazon Basin -- 6. Kinematics of submarine slope failures in the deepwater Taranaki Basin, New Zealand -- Part II Failure dynamics from landslide geomorphology -- 7. Postglacial Mass Failures in the Inner Hardangerfjorden System, Western Norway -- 8. Onshore and offshore geomorphological features of the El Golfo debris avalanche (El Hierro, Canary Islands) -- 9. New insights on failure and post-failure dynamics of submarine landslides on the intra-slope Palmarola ridge (Central Tyrrhenian Sea) -- 10. Assessment of Canyon Wall Failure Process from Multibeam Bathymetry and Remotely Operated Vehicle (ROV) Observations, U.S. Atlantic Continental Margin -- 11. The Chuí Megaslide Complex: regional-scale submarine landslides on the Southern Brazilian Margin -- 12. Submarine landslides and incised canyons of the southeast Queensland continental margin -- 13. Novel method to map the morphology of submarine landslide headwall scarps using Remotely Operated Vehicles -- 14. Flow behaviour of a giant landslide and debris flow entering Agadir Canyon, NW Africa -- 15. Fine-Scale Morphology of Tubeworm Slump, Monterey Canyon -- 16. Submarine slide topography and the Distribution of Vulnerable Marine Ecosystems: A Case Study in the Ionian Sea (Eastern Mediterranean) -- Part III Geotechnical aspects of mass movement -- 17. Shear Strength of Siliciclastic Sediments from Passive and Active Margins (0-100 meters below seafloor): Insights into Seismic Strengthening -- 18. A small volume calibration chamber for cone penetration testing (CPT) on submarine soils -- 19. Underwater Mass Movements in Lake Mjøsa, Norway -- 20. In situ cyclic softening of marine silts by vibratory CPTU at Orkdalsfjord test site, mid Norway -- 21. First results of the geotechnical in situ investigation for soil characterisation along the upper slope off Vesterålen - Northern Norway -- 22. A novel micro-shear tester for failure analysis of fine and cohesive granular matter -- 23. Knickpoint migration induced by landslide: Evidence from laboratory to field observations in Wabush Lake -- 24. Multiple flow slide experiment in the Westerschelde Estuary, The Netherlands -- Part IV Multidisciplinary case studies -- 25. Submarine mass wasting on Hovgaard Ridge, Fram Strait, European Arctic -- 26. 3D seismic investigations of Pleistocene Mass Transport Deposits and Glacigenic Debris Flows on the North Sea Fan, NE Atlantic Margin -- 27. Do embedded volcaniclastic layers serve as potential glide planes? – An integrated analysis from the Gela Basin offshore southern Sicily -- 28. Sediment failure affecting muddy contourites on the continental slope offshore northern Norway – lessons learned and some outstanding issues -- 29. Mass Wasting History within Lake Ohrid Basin (Albania/Macedonia) over the last 600ka -- 30. Implications of Sediment Dynamics in Mass Transport along the Pianosa Ridge (Northern Tyrrhenian Sea) -- 31. Late-Holocene Mass Movements in High Arctic East Lake, Melville Island (Western Canadian Arctic Archipelago) -- 32. Pleistocene Mass Transport Complexes off Barbados accretionary prism (Lesser Antilles) -- 33. Exploring the Influence of Deepwater Currents as Potential Triggers for Slope Instability -- Part V Tectonics and mass movements -- 34. French alpine foreland Holocene paleoseismicity revealed by coeval mass wasting deposits in glacial lakes -- 35. Spatial and temporal relation of submarine landslides and faults along the Israeli continental slope, eastern Mediterranean -- 36. Earthquake induced landslides in Lake Éternité, Québec, Canada -- 37. Large Mass Transport Deposits in Kumano Basin, Nankai Trough, Japan -- 38. Insights into Effectiveness of Simplified Seismic Displacement Procedures to Evaluate Earthquake Behavior of a Deepwater Slope -- Part VI Fluid flow and gas hydrates -- 39. Deriving the Rate of Salt Rise at the Cape Fear Slide Using New Seismic Data -- 40. Submarine slope instabilities coincident with shallow gas hydrate systems: insights from New Zealand examples -- 41. Eel Canyon Slump Scar and Associated Fluid Venting -- 42. Shallow gas and the development of a weak layer in submarine spreading, Hikurangi margin (New Zealand) -- 43. Stability of fine-grained sediments subject to gas hydrate dissociation in the Arctic continental margin -- Part VII Mass transport deposits in modern and outcrop sedimentology -- 44. Soft-sediment deformation associated with mass transport deposits of the aAnsa basin (Spanish Pyrenees) -- 45. Synsedimentary tectonics and mass wasting along the Alpine margin in Liassic time -- 46. Meso-scale kinematic indicators in exhumed mass transport deposits: definitions and implications -- 47. Morphodynamics of supercritical turbidity currents in the channel-lobe transition zone -- 48. Tiny fossils, big impact: the role of foraminifera-enriched condensed section in arresting the movement of a large retrogressive submarine landslide in the Gulf of Mexico -- 49. Inclusion of substrate blocks within a mass transport deposit: A case study from Cerro Bola, Argentina -- Part VIII Numerical and statistical analysis -- 50. GIS catalogue of submarine landslides in the Spanish Continental Shelf: potential and difficulties for susceptibility assessment -- 51. Tempo and triggering of large submarine landslides – Statistical analysis for hazard assessment -- 52. Morphological controls on submarine slab failures -- 53. Incorporating Correlated Variables into GIS-Based Probabilistic Submarine Slope Stability Assessments -- 54. Quantifying the key role of slope material peak strength – using Discrete Element simulations -- 55. Correction Factors for 1-D Runout Analyses of Selected Submarine Slides -- Part IX Tsunami generation from slope failure -- 56. Volcanic generation of tsunamis: Two New Zealand palaeo-events -- 57. Tsunami-genesis due to retrogressive landslides on an inclined seabed -- 58. Geothermal System as the Cause of the 1979 Landslide Tsunami in Lembata Island, Indonesia -- 59. Towards a spatial probabilistic submarine landslide hazard model for submarine canyons -- 60. Coupled modelling of the failure and tsunami of a submarine debris avalanche offshore central New Zealand -- 61. Observations of coastal landslide-generated tsunami under an ice cover: the case of Lac-des-Seize-Îles, Québec, Canada -- Index.
    Type of Medium: Online Resource
    Pages: Online-Ressource (XIII, 621 p. 256 illus., 219 illus. in color, online resource)
    Edition: 1st ed. 2016
    ISBN: 9783319209791
    Series Statement: Advances in Natural and Technological Hazards Research 41
    RVK:
    Language: English
    Note: 1. Submarine Mass Movements and Their Consequences: Progress and ChallengesPart  I Submarine Mass Movement in Margin Construction and Economic Significance2. The Role of Submarine Landslides in the Law of the Sea -- 3. Fabric Development and Pore-Throat Reduction in a Mass-Transport Deposit in the Jubilee Gas Field, Eastern Gulf of Mexico: Consequences for the Sealing Capacity of MTDs -- 4. Seismic geomorphology of the Israel Slump Complex in the central Levant Basin (SE Mediterranean) -- 5. Multiple Megaslide Complexes and their Significance for the Miocene stratigraphic evolution of the offshore Amazon Basin -- 6. Kinematics of submarine slope failures in the deepwater Taranaki Basin, New Zealand -- Part II Failure dynamics from landslide geomorphology -- 7. Postglacial Mass Failures in the Inner Hardangerfjorden System, Western Norway -- 8. Onshore and offshore geomorphological features of the El Golfo debris avalanche (El Hierro, Canary Islands) -- 9. New insights on failure and post-failure dynamics of submarine landslides on the intra-slope Palmarola ridge (Central Tyrrhenian Sea) -- 10. Assessment of Canyon Wall Failure Process from Multibeam Bathymetry and Remotely Operated Vehicle (ROV) Observations, U.S. Atlantic Continental Margin -- 11. The Chuí Megaslide Complex: regional-scale submarine landslides on the Southern Brazilian Margin -- 12. Submarine landslides and incised canyons of the southeast Queensland continental margin -- 13. Novel method to map the morphology of submarine landslide headwall scarps using Remotely Operated Vehicles -- 14. Flow behaviour of a giant landslide and debris flow entering Agadir Canyon, NW Africa -- 15. Fine-Scale Morphology of Tubeworm Slump, Monterey Canyon -- 16. Submarine slide topography and the Distribution of Vulnerable Marine Ecosystems: A Case Study in the Ionian Sea (Eastern Mediterranean) -- Part III Geotechnical aspects of mass movement -- 17. Shear Strength of Siliciclastic Sediments from Passive and Active Margins (0-100 meters below seafloor): Insights into Seismic Strengthening -- 18. A small volume calibration chamber for cone penetration testing (CPT) on submarine soils -- 19. Underwater Mass Movements in Lake Mjøsa, Norway -- 20. In situ cyclic softening of marine silts by vibratory CPTU at Orkdalsfjord test site, mid Norway -- 21. First results of the geotechnical in situ investigation for soil characterisation along the upper slope off Vesterålen - Northern Norway -- 22. A novel micro-shear tester for failure analysis of fine and cohesive granular matter -- 23. Knickpoint migration induced by landslide: Evidence from laboratory to field observations in Wabush Lake -- 24. Multiple flow slide experiment in the Westerschelde Estuary, The Netherlands -- Part IV Multidisciplinary case studies -- 25. Submarine mass wasting on Hovgaard Ridge, Fram Strait, European Arctic -- 26. 3D seismic investigations of Pleistocene Mass Transport Deposits and Glacigenic Debris Flows on the North Sea Fan, NE Atlantic Margin -- 27. Do embedded volcaniclastic layers serve as potential glide planes? - An integrated analysis from the Gela Basin offshore southern Sicily -- 28. Sediment failure affecting muddy contourites on the continental slope offshore northern Norway - lessons learned and some outstanding issues -- 29. Mass Wasting History within Lake Ohrid Basin (Albania/Macedonia) over the last 600ka -- 30. Implications of Sediment Dynamics in Mass Transport along the Pianosa Ridge (Northern Tyrrhenian Sea) -- 31. Late-Holocene Mass Movements in High Arctic East Lake, Melville Island (Western Canadian Arctic Archipelago) -- 32. Pleistocene Mass Transport Complexes off Barbados accretionary prism (Lesser Antilles) -- 33. Exploring the Influence of Deepwater Currents as Potential Triggers for Slope Instability -- Part V Tectonics and mass movements -- 34. French alpine foreland Holocene paleoseismicity revealed by coeval mass wasting deposits in glacial lakes -- 35. Spatial and temporal relation of submarine landslides and faults along the Israeli continental slope, eastern Mediterranean -- 36. Earthquake induced landslides in Lake Éternité, Québec, Canada -- 37. Large Mass Transport Deposits in Kumano Basin, Nankai Trough, Japan -- 38. Insights into Effectiveness of Simplified Seismic Displacement Procedures to Evaluate Earthquake Behavior of a Deepwater Slope -- Part VI Fluid flow and gas hydrates -- 39. Deriving the Rate of Salt Rise at the Cape Fear Slide Using New Seismic Data -- 40. Submarine slope instabilities coincident with shallow gas hydrate systems: insights from New Zealand examples -- 41. Eel Canyon Slump Scar and Associated Fluid Venting -- 42. Shallow gas and the development of a weak layer in submarine spreading, Hikurangi margin (New Zealand) -- 43. Stability of fine-grained sediments subject to gas hydrate dissociation in the Arctic continental margin -- Part VII Mass transport deposits in modern and outcrop sedimentology -- 44. Soft-sediment deformation associated with mass transport deposits of the aAnsa basin (Spanish Pyrenees) -- 45. Synsedimentary tectonics and mass wasting along the Alpine margin in Liassic time -- 46. Meso-scale kinematic indicators in exhumed mass transport deposits: definitions and implications -- 47. Morphodynamics of supercritical turbidity currents in the channel-lobe transition zone -- 48. Tiny fossils, big impact: the role of foraminifera-enriched condensed section in arresting the movement of a large retrogressive submarine landslide in the Gulf of Mexico -- 49. Inclusion of substrate blocks within a mass transport deposit: A case study from Cerro Bola, Argentina -- Part VIII Numerical and statistical analysis -- 50. GIS catalogue of submarine landslides in the Spanish Continental Shelf: potential and difficulties for susceptibility assessment -- 51. Tempo and triggering of large submarine landslides - Statistical analysis for hazard assessment -- 52. Morphological controls on submarine slab failures -- 53. Incorporating Correlated Variables into GIS-Based Probabilistic Submarine Slope Stability Assessments -- 54. Quantifying the key role of slope material peak strength - using Discrete Element simulations -- 55. Correction Factors for 1-D Runout Analyses of Selected Submarine Slides -- Part IX Tsunami generation from slope failure -- 56. Volcanic generation of tsunamis: Two New Zealand palaeo-events -- 57. Tsunami-genesis due to retrogressive landslides on an inclined seabed -- 58. Geothermal System as the Cause of the 1979 Landslide Tsunami in Lembata Island, Indonesia -- 59. Towards a spatial probabilistic submarine landslide hazard model for submarine canyons -- 60. Coupled modelling of the failure and tsunami of a submarine debris avalanche offshore central New Zealand -- 61. Observations of coastal landslide-generated tsunami under an ice cover: the case of Lac-des-Seize-Îles, Québec, Canada -- Index.
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  • 4
    In: Marine geology, Amsterdam [u.a.] : Elsevier Science, 1964, 247(2008), 1/2, Seite 46-60, 1872-6151
    In: volume:247
    In: year:2008
    In: number:1/2
    In: pages:46-60
    Description / Table of Contents: This study documents the fractal characteristics of submarine mass movement statistics and morphology within the Storegga Slide. Geomorphometric mapping is used to identify one hundred and fifteen mass movements from within the Storegga Slide scar and to extract morphological information about their headwalls. Analyses of this morphological information reveal the occurrence of spatial scale invariance within the Storegga Slide. Non-cumulative frequency-area distribution of mass movements within the Storegga Slide satisfies an inverse power law with an exponent of 1.52. The headwalls exhibit geometric similarity at a wide range of scales and the lengths of headwalls scale with mass movement areas. Composite headwalls are self-similar. One of the explanations of the observed spatial scale invariance is that the Storegga Slide is a geomorphological system that may exhibit self-organized criticality. In such a system, the input of sediment is in the form of hemipelagic sedimentation and glacial sediment deposition, and the output is represented by mass movements that are spatially scale invariant. In comparison to subaerial mass movements, the aggregate behavior of the Storegga Slide mass movements is more comparable to that of the theoretical ‘sandpile’ model. The origin of spatial scale invariance may also be linked to the retrogressive nature of the Storegga Slide. The geometric similarity in headwall morphology implies that the slope failure processes are active on a range of scales, and that modeling of slope failures and geohazard assessment can extrapolate the properties of small landslides to those of larger landslides, within the limits of power law behavior. The results also have implications for the morphological classification of submarine mass movements, because headwall shape can be used as a proxy for the type of mass movement, which can otherwise only be detected with very high resolution acoustic data that are not commonly available.
    Type of Medium: Online Resource
    ISSN: 1872-6151
    Language: English
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  • 5
    Online Resource
    Online Resource
    Cham : Springer
    Keywords: Earth sciences ; Earth Sciences ; Geology ; Oceanography ; Geomorphology ; Meereskunde ; Meeresboden ; Meeresgeologie ; Meeressediment ; Geomorphologie ; Meeresboden ; Sonar ; Topografie ; Hydroakustik ; Relief ; Geomorphographie
    Description / Table of Contents: This book on the current state of knowledge of submarine geomorphology aims to achieve the goals of the Submarine Geomorphology working group, set up in 2013, by establishing submarine geomorphology as a field of research, disseminating its concepts and techniques among earth scientists and professionals, and encouraging students to develop their skills and knowledge in this field. Editors have invited 30 experts from around the world to contribute chapters to this book, which is divided into 4 sections - (i) Introduction & history, (ii) Data & methods, (ii) Submarine landforms & processes and (iv) Conclusions & future directions. Each chapter provides a review of a topic, establishes the state-of-the-art, identifies the key research questions that need to be addressed, and delineates a strategy on how to achieve this. Submarine geomorphology is a priority for many research institutions, government authorities and industries globally. The book is useful for undergraduate and graduate students, and professionals with limited training in this field
    Type of Medium: Online Resource
    Pages: Online-Ressource (XIII, 556 p. 195 illus., 55 illus. in color, online resource)
    ISBN: 9783319578521
    Series Statement: Springer Geology
    Language: English
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  • 6
    Book
    Book
    Cham, Switzerland : Springer
    Keywords: Earth sciences ; Geology ; Oceanography ; Geomorphology ; Earth Sciences ; Earth Sciences ; Earth sciences ; Geology ; Geomorphology ; Oceanography ; Earth sciences ; Geology ; Geomorphology ; Oceanography ; Aufsatzsammlung ; Geomorphologie ; Meereskunde ; Meeresboden ; Meeresgeologie
    Type of Medium: Book
    Pages: xiii, 556 Seiten , Illustrationen, Diagramme, Karten , 25 cm
    ISBN: 3319578529 , 9783319578514
    Series Statement: Springer geology
    DDC: 550
    RVK:
    RVK:
    Language: English
    Note: Includes bibliographical references
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  • 7
    Publication Date: 2024-05-02
    Description: Underway temperature and salinity data was collected along the cruise track with two autonomous thermosalinograph (TSG) systems, each consisting of a SBE21 TSG together with a SBE38 Thermometer. Both systems worked independent from each other throughout the cruise. While temperature is taken at the water inlet in about 5 m depth, salinity is estimated within the interior TSG from conductivity and interior temperature. No correction against independent data was performed for temperature and salinity. Finally, TSG1 was chosen for publication. For details to all processing steps see Data Processing Report.
    Keywords: Calculated from internal temperature and conductivity; Conductivity; DAM_Underway; DAM Underway Research Data; DATE/TIME; DEPTH, water; Digital oceanographic thermometer, Sea-Bird, SBE 38; LATITUDE; LONGITUDE; M191; M191_0_Underway-4; Measurement container; Meteor (1986); Quality flag, salinity; Quality flag, water temperature; Salinity; Seadatanet flag: Data quality control procedures according to SeaDataNet (2010); SUAVE; Temperature, water; Temperature, water, internal; Thermosalinograph; Thermosalinograph (TSG), Sea-Bird, SBE 21 SEACAT; TSG
    Type: Dataset
    Format: text/tab-separated-values, 190709 data points
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  • 8
    Publication Date: 2021-07-04
    Description: First reported in the 1960s, offshore freshened groundwater (OFG) has now been documented in most continental margins around the world. In this review we compile a database documenting OFG occurrences and analyze it to establish the general characteristics and controlling factors. We also assess methods used to map and characterize OFG, identify major knowledge gaps, and propose strategies to address them. OFG has a global volume of 1 × 106 km3; it predominantly occurs within 55 km of the coast and down to a water depth of 100 m. OFG is mainly hosted within siliciclastic aquifers on passive margins and recharged by meteoric water during Pleistocene sea level lowstands. Key factors influencing OFG distribution are topography‐driven flow, salinization via haline convection, permeability contrasts, and the continuity/connectivity of permeable and confining strata. Geochemical and stable isotope measurements of pore waters from boreholes have provided insights into OFG emplacement mechanisms, while recent advances in seismic reflection profiling, electromagnetic surveying, and numerical models have improved our understanding of OFG geometry and controls. Key knowledge gaps, such as the extent and function of OFG, and the timing of their emplacement, can be addressed by the application of isotopic age tracers, joint inversion of electromagnetic and seismic reflection data, and development of three‐dimensional hydrological models. We show that such advances, combined with site‐specific modeling, are necessary to assess the potential use of OFG as an unconventional source of water and its role in sub‐seafloor geomicrobiology.
    Description: Plain Language Summary: This review paper considers offshore freshened groundwater (OFG), which is water hosted in sediments and rocks below the seafloor, with a total dissolved solid concentration lower than seawater. We have compiled 〉300 records to demonstrate that freshened groundwater occurs offshore on most continents around the world and has a global volume of 1 × 106 km3. The majority of OFG was deposited when sea level was lower than today and is hosted in sandy sub‐seafloor layers that are located within 55 km of coasts in water depths less than 100 m. We present a range of geochemical, geophysical, and modeling approaches that have successfully been used to investigate OFG systems. We also propose approaches to address key scientific questions related to OFG, including whether it may be used as an unconventional source of potable water in coastal areas.
    Description: Key Points: Most known OFG is located at water depths of 〈100 m within 55 km of the coast, hosted in siliciclastic aquifers in passive margins. Key gaps in knowledge include the extent and function of OFG systems, as well as the mechanism and timing of emplacement. Isotopic tracers, jointly inverted geophysical data and 3‐D hydrological models can help address these knowledge gaps.
    Description: EC | H2020 | H2020 Priority Excellent Science | H2020 European Research Council (ERC) http://dx.doi.org/10.13039/100010663
    Description: National Science Foundation (NSF) http://dx.doi.org/10.13039/100000001
    Keywords: 551 ; offshore freshened groundwater ; continental margin ; marine hydrogeology ; geochemistry ; geophysics ; modeling
    Type: article
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  • 9
    Publication Date: 2022-04-22
    Description: The Maltese Islands, located in the central Mediterranean Sea, are intersected by two normal fault systems associated with continental rifting to the south. Due to a lack of evidence for offshore displacement and insignificant historical seismicity, the systems are thought to be inactive and the rift-related deformation is believed to have ceased. In this study we integrate aerial, marine and onshore geological, geophysical and geochemical data from the Maltese Islands to demonstrate that the majority of faults offshore the archipelago underwent extensional to transtensional deformation during the last 20 ka. We also document an active fluid flow system responsible for degassing of CH4 and CO2. The gases migrate through carbonate bedrock and overlying sedimentary layers via focused pathways, such as faults and pipe structures, and possibly via diffuse pathways, such as fractures. Where the gases seep offshore, they form pockmarks and rise through the water column into the atmosphere. Gas migration and seepage implies that the onshore and offshore faults systems are permeable and that they were active recently and simultaneously. The latter can be explained by a transtensional system involving two right-stepping, right-lateral NW-SE trending faults, either binding a pull-apart basin between the islands of Malta and Gozo or associated with minor connecting antitethic structures. Such a configuration may be responsible for the generation or reactivation of faults onshore and offshore the Maltese Islands, and fits into the modern divergent strain-stress regime inferred from geodetic data.
    Description: Published
    Description: 361-374
    Description: 6A. Geochimica per l'ambiente e geologia medica
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 10
    Publication Date: 2022-05-03
    Description: Shallow seabed depressions attributed to focused fluid seepage, known as pock- marks, have been documented in all continental margins. In this study, we dem- onstrate how pockmark formation can be the result of a combination of multiple factors— fluid type, overpressures, seafloor sediment type, stratigraphy and bot- tom currents. We integrate multibeam echosounder and seismic reflection data, sediment cores and pore water samples, with numerical models of groundwa- ter and gas hydrates, from the Canterbury Margin (off New Zealand). More than 6800 surface pockmarks, reaching densities of 100 per km2, and an undefined number of buried pockmarks, are identified in the middle to outer shelf and lower continental slope. Fluid conduits across the shelf and slope include shal- low to deep chimneys/pipes. Methane with a biogenic and/or thermogenic origin is the main fluid forming flow and escape features, although saline and fresh- ened groundwaters may also be seeping across the slope. The main drivers of fluid flow and seepage are overpressure across the slope generated by sediment loading and thin sediment overburden above the overpressured interval in the outer shelf. Other processes (e.g. methane generation and flow, a reduction in hydrostatic pressure due to sea- level lowering) may also account for fluid flow and seepage features, particularly across the shelf. Pockmark occurrence coin- cides with muddy sediments at the seafloor, whereas their planform is elongated by bottom currents.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , peerRev
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