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  • 1
    Online Resource
    Online Resource
    Oxford :Elsevier Science & Technology,
    Keywords: Marine sediments. ; Sedimentation and deposition. ; Electronic books.
    Description / Table of Contents: Contourites are sediments deposited or substantially reworked by bottom currents. The study of contourites is crucial for several fields of fundamental and applied research: paleoclimatology and paleo-oceanography, since these fairly continuous and relatively high-resolution sediments hold the key for priceless information on the variability in circulation patter, current velocity, oceanographic history and basin interconnectivity; hydrocarbon exploration, since accumulation of source rocks may be favored by weak bottom currents, whereas "clean" deep-sea sands may be formed by robust flows; and slope stability, since low-permeability fine-grained contourites facilitate the formation of overpressurized gliding planes when fresh contourites with a high pore-water content becomes rapidly loaded, or when their rigid biosiliceous microfabric collapses due to diagenetic conditions. Despite its significance, this group of sediments is poorly known by the majority of non-specialists. Notwithstanding the growing interest and the intensified research in contourites, a textbook that might also serve as a reference book on contourites was missing until now. This book addresses all aspects of the knowledge in the field of contourites and provides an authoritative and comprehensive coverage of the subject. It also can serve as a standard reference work for non-specialists, and in particular postgraduate students, university teachers and lecturers, researchers and professionals who are seeking an authoritative source of information about contourites. * reviews both theoretical topics and case histories * provides practical advice on multidisciplinary research techniques * provides also nonspecialist users with an intuitively-accessible, cross-referenced, and comprehensive coverage of the knowledge in the field. * provides a helpful tool for research in the
    Type of Medium: Online Resource
    Pages: 1 online resource (793 pages)
    Edition: 1st ed.
    ISBN: 9780080931869
    Series Statement: Issn Series ; v.Volume 60
    DDC: 551.3
    Language: English
    Note: Front Cover -- Developments in Sedimentology, 60: Contourites -- Copyright Page -- Table of Contents -- Preface -- List of Contributors -- Part 1 Contourite Research -- Chapter 1 Contourite Research: A Field in Full Development -- 1.1 Bottom Currents -- 1.2 Contourites -- 1.3 Drifts -- 1.4 Sedimentary Structures -- 1.5 Prospects -- Chapter 2 Personal Reminiscences on the History of Contourites -- 2.1 Introduction -- 2.2 Not All Deep-Sea Sands are Turbidites -- 2.3 Turbidophiles and Turbidophobes -- 2.4 Erosional Unconformity Misinterpreted -- Chapter 3 Methods for Contourite Research -- 3.1 Introduction -- 3.2 Oceanographic Measurements -- 3.3 Geophysical Methods -- 3.4 Sampling Strategies -- 3.5 Analytical Methods -- 3.6 Onshore Studies of Ancient Sequences -- 3.7 Summary of Multidisciplinary Techniques -- Acknowledgements -- Part 2 Bottom Currents -- Chapter 4 Abyssal and Contour Currents -- 4.1 Introduction -- 4.2 Abyssal Currents in the Global Thermohaline Circulation -- 4.3 Contour Currents -- 4.4 Conclusion and Summary -- Acknowledgments -- Chapter 5 Deep-water Bottom Currents and Their Deposits -- 5.1 Introduction -- 5.2 Thermohaline-Induced Geostrophic Bottom Currents -- 5.3 Wind-Driven Bottom Currents: The Loop Current -- 5.4 Deep-Water Tidal Bottom Currents -- 5.5 Internal Waves and Tides (Baroclinic Currents) -- 5.6 Conclusions -- Acknowledgments -- Chapter 6 Dynamics of the Bottom Boundary Layer -- 6.1 Introduction -- 6.2 Spectral Windows -- 6.3 Characteristics of the Bottom Boundary Layer -- 6.4 Analytical Approach of the BBL -- 6.5 Conclusions -- Acknowledgements -- Part 3 Processes -- Chapter 7 Sediment Entrainment -- 7.1 Introduction -- 7.2 Benthic Storms (Transportation and Resuspension of Particles) -- 7.3 Gravity Flows -- 7.4 Bioclastics-Forming Processes in Contourites -- 7.5 Volcaniclastics -- 7.6 Glacial Activity. , 7.7 Resuspension of Particles by Burrowing Activity of Benthic Organisms -- 7.8 Concluding Remarks -- Acknowledgements -- Chapter 8 Size Sorting During Transport and Deposition of Fine Sediments: Sortable Silt and Flow Speed -- 8.1 Introduction -- 8.2 Size Analysis of Fine Sediments -- 8.3 Unsorted Delivery to Deep Current Systems: Pelagic Flux and Down-Slope Transport -- 8.4 Controlling Factors for Input and Transport -- 8.5 Sorting in Suspension Transport -- 8.6 Processes of Deposition from Turbulent Boundary Layers -- 8.7 Deposits from Currents -- 8.8 Some Examples of Palaeoflow Inferred from Sortable-Silt records -- Acknowledgements -- Chapter 9 The Nature of Contourite Deposition -- 9.1 Introduction -- 9.2 Bottom-Current Characteristics -- 9.3 Sedimentation rates and budget -- 9.4 Drift Deposition and Erosion -- 9.5 Bottom-Current Bedforms -- 9.6 Contourite Facies and Features -- 9.7 Contourite Cyclicity -- 9.8 Summary -- Acknowledgements -- Part 4 Sediments -- Chapter 10 Traction Structures in Contourites -- 10.1 Introduction -- 10.2 The Traction-Structures Controversy -- 10.3 Setting the Stage for Sedimentary Structures in Contourites -- 10.4 Sedimentary Structures -- 10.5 Sedimentary Structures in Facies Models -- 10.6 Conclusions -- Acknowledgments -- Chapter 11 Bioturbation and Biogenic Sedimentary Structures in Contourites -- 11.1 Introduction -- 11.2 Effects of Contour Currents on Benthic Habitats -- 11.3 Examples of Bioturbation in Contourites -- 11.4 Discussion and Conclusions -- 11.5 Perspective -- Acknowledgements -- Chapter 12 Some Aspects of Diagenesis in Contourites -- 12.1 Introduction -- 12.2 Some Examples of Sedimentary Rhythms Associated with Changes in Colour -- 12.3 Diagenesis of Fine-Grained Contourites -- 12.4 Diagenesis of Coarse-Grained Contourites -- Acknowledgements -- Chapter 13 Contourite Facies and the Facies Model. , 13.1 Introduction -- 13.2 Historical Context -- 13.3 The Range of Contourite Facies -- 13.4 Contourite Facies Model and the Contourite Sequence -- 13.5 Lamination Versus Bioturbation in Contourites -- 13.6 Contourite-Related Facies -- Acknowledgements -- Appendix 1 Details of Contourite Facies Recovered from Modern Drift Systems Using Conventional Coring Techniques as Published Over the Past 15 Years -- 13A1.1 NW UK Continental Margin -- 13A1.2 Norwegian Continental Margin -- 13A1.3 Greenland Continental Margin -- 13A1.4 Gulf of Cadiz, Iberian Margin -- 13A1.5 Mediterranean Sea -- 13A1.6 East North American Continental Margin -- 13A1.7 East South American Continental Margin -- 13A1.8 East New Zealand Continental Margin, SW Pacific -- 13A1.9 Antarctic Continental Margin and Weddell Sea -- Part 5 Morphology, Geometry and Palaeoceanographic Reconstructions -- Chapter 14 Contourite Drifts: Nature, Evolution and Controls -- 14.1 Introduction -- 14.2 Drift Distribution and Characteristics -- 14.3 Growth History of the Blake Outer Ridge Drift System -- 14.4 Factors Controlling Drift Location, Morphology and Depositional Pattern -- 14.5 Contourite-Drift Types -- 14.6 Discussion -- Acknowledgements -- Chapter 15 Sediment Waves and Bedforms -- 15.1 Introduction -- 15.2 Location, Morphology and Genesis of Fine-Grained Sediment Waves -- 15.3 Location, Morphology and Genesis of Coarse-Grained Sediment Waves -- 15.4 Related Large-Scale Features Generated by Bottom Currents -- 15.5 Applications to Bottom-Current Reconstruction: A Case Study From the NW UK -- Acknowledgements -- Chapter 16 Seismic Expression of Contourite Depositional Systems -- 16.1 Introduction -- 16.2 Seismic Identification and Characteristics of Contourites -- 16.3 Seismic Methods and Interpretation Concepts in Contourite Studies -- 16.4 Summary -- Acknowledgements. , Chapter 17 Identification of Ancient Contourites: Problems and Palaeoceanographic Significance -- 17.1 Introduction -- 17.2 Examples of Fossil Contourites -- 17.3 Discussion -- Acknowledgements -- Part 6 Domains -- Chapter 18 Abyssal Plain Contourites -- 18.1 Introduction -- 18.2 Terminology -- 18.3 Case Studies of Abyssal Contourites -- 18.4 Oceanic Gateways -- 18.5 Principal Oceanographic and Sedimentary Processes -- 18.6 Main Characteristics of Abyssal Plain Contourites -- 18.7 Final Considerations -- Acknowledgements -- Chapter 19 Continental Slope Contourites -- 19.1 Introduction -- 19.2 Key Examples of Along-Slope Processes -- 19.3 Lower Slope to Continental Rise Transition and Other Kinds of Slopes -- 19.4 Principal Characteristics of Continental-Slope Contourites -- 19.5 Final Considerations -- Acknowledgements -- Chapter 20 Shallow-Water Contourites -- 20.1 Introduction -- 20.2 Bottom Currents Shaping Shallow-Water Contourite Deposits -- 20.3 Examples of Shallow-Water Contourites -- 20.4 Discussion -- 20.5 Summary -- Acknowledgements -- Chapter 21 Mixed Turbidite-Contourite Systems -- 21.1 Introduction -- 21.2 Contourite and Turbidite Alternation -- 21.3 Redistribution of Gravity Deposits by Contour Currents -- 21.4 Interaction of Synchronous Contour and Turbidity Currents -- 21.5 Conclusions -- Acknowledgements -- Chapter 22 High-Latitude Contourites -- 22.1 Introduction -- 22.2 Neogene and Quaternary Changes in Deep-Water Circulation of the Northern North Atlantic and in the Southern Ocean -- 22.3 Northeast Atlantic Margin Contourites -- 22.4 Antarctic Margin Contourites -- 22.5 Conclusions -- Acknowledgements -- Part 7 Importance -- Chapter 23 Economic Relevance of Contourites -- 23.1 Introduction -- 23.2 Major Implications of Contourite Studies -- 23.3 Contourites and Petroleum Exploration -- 23.4 Discussion -- Acknowledgements. , Chapter 24 Palaeoceanographic Significance of Contourite Drifts -- 24.1 Introduction -- 24.2 Oceanographic Settings of Contourites -- 24.3 Methods and Approaches -- 24.4 Palaeoceanographic Themes Addressed by Contourite Research -- 24.5 Summary -- Acknowledgements -- Chapter 25 The Significance of Contourites for Submarine Slope Stability -- 25.1 Introduction and Objective -- 25.2 Background -- 25.3 Case Studies of Contourites and Submarine Slope Stability -- 25.4 Discussion -- 25.5 Summary -- Acknowledgements -- References -- Index -- Color Plates.
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  • 2
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Earth and Planetary Science Letters 109 (1992), S. 493-504 
    ISSN: 0012-821X
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1573-0581
    Keywords: Mediterranean Ridge ; mud diapirism ; mud volcano ; fluid circulation ; accretionary prism
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Mud volcanoes, mud cones, and mud ridges have been identified on the inner portion of the crestal area, and possibly on the inner escarpment, of the Mediterranean Ridge accretionary complex. Four areas containing one or more mud diapirs have been investigated through bathymetric profiling, single channel seismic reflection profiling, heat flow measurements, and coring. A sequence of events is identified in the evolution of the mud diapirs: initially the expulsion on the seafloor of gasrich mud produces a seafloor depression outlined in the seismic record by downward dip of the host sediment reflectors towards the mud conduit; subsequent eruptions of fluid mud may create a flat topped mud volcano with step-like profile; finally, the intrusion of viscous mud produces a mud cone. The origin of the diapirs is deep within the Mediterranean Ridge. Although a minimum depth of about 400 m below the seafloor has been computed from the hydrostatic balance between the diapiric sediments and the host sediments, a maximum depth, suggested by geometric considerations, ranges between 5.3 and 7 km. The presence of thermogenic gas in the diapiric sediments suggests a better constrained origin depth of at least 2.2 km. The heat flow measured within the Olimpi mud diapir field and along a transect orthogonal to the diapiric field is low, ranging between 16 ± 5 and 41 ± 6 mW m−2. Due to the presence of gas, the thermal conductivity of the diapiric sediments is lower than that of the host hemipelagic oozes (0.6–0.9 and 1.0–1.15 W m−1 K−1 respectively). We consider the distribution of mud diapirs to be controlled by the presence of tectonic features such as reverse faults or thrusts (inner escarpment) that develop where the thickness of the Late Miocene evaporites appears to be minimum. An upward migration through time of the position of the décollement within the stratigraphic column from the Upper Oligocene (diapiric sediments) to the Upper Miocene (present position) is identified.
    Type of Medium: Electronic Resource
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  • 4
    Publication Date: 2017-07-21
    Description: High-resolution seismic experiments, employing arrays of closely spaced, four-component ocean-bottom seismic recorders, were conducted at a site off western Svalbard and a site on the northern margin of the Storegga slide, off Norway to investigate how well seismic data can be used to determine the concentration of methane hydrate beneath the seabed. Data from P-waves and from S-waves generated by P–S conversion on reflection were inverted for P- and S-wave velocity (Vp and Vs), using 3D travel-time tomography, 2D ray-tracing inversion and 1D waveform inversion. At the NW Svalbard site, positive Vp anomalies above a sea-bottom-simulating reflector (BSR) indicate the presence of gas hydrate. A zone containing free gas up to 150-m thick, lying immediately beneath the BSR, is indicated by a large reduction in Vp without significant reduction in Vs. At the Storegga site, the lateral and vertical variation in Vp and Vs and the variation in amplitude and polarity of reflectors indicate a heterogeneous distribution of hydrate that is related to a stratigraphically mediated distribution of free gas beneath the BSR. Derivation of hydrate content from Vp and Vs was evaluated, using different models for how hydrate affects the seismic properties of the sediment host and different approaches for estimating the background-velocity of the sediment host. The error in the average Vp of an interval of 20-m thickness is about 2.5%, at 95% confidence, and yields a resolution of hydrate concentration of about 3%, if hydrate forms a connected framework, or about 7%, if it is both pore-filling and framework-forming. At NW Svalbard, in a zone about 90-m thick above the BSR, a Biot-theory-based method predicts hydrate concentrations of up to 11% of pore space, and an effective-medium-based method predicts concentrations of up to 6%, if hydrate forms a connected framework, or 12%, if hydrate is both pore-filling and framework-forming. At Storegga, hydrate concentrations of up to 10% or 20% were predicted, depending on the hydrate model, in a zone about 120-m thick above a BSR. With seismic techniques alone, we can only estimate with any confidence the average hydrate content of broad intervals containing more than one layer, not only because of the uncertainty in the layer-by-layer variation in lithology, but also because of the negative correlation in the errors of estimation of velocity between adjacent layers. In this investigation, an interval of about 20-m thickness (equivalent to between 2 and 5 layers in the model used for waveform inversion) was the smallest within which one could sensibly estimate the hydrate content. If lithological layering much thinner than 20-m thickness controls hydrate content, then hydrate concentrations within layers could significantly exceed or fall below the average values derived from seismic data.
    Type: Article , PeerReviewed
    Format: text
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  • 5
    Publication Date: 2019-09-24
    Type: Article , NonPeerReviewed
    Format: text
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  • 6
    Publication Date: 2016-09-08
    Type: Article , NonPeerReviewed
    Format: text
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  • 7
    Publication Date: 2016-10-15
    Description: An analysis of multichannel seismic reflection data was conducted focusing on the comparison between the Messinian Salinity Crisis (MSC) and Plio-Quaternary (PQ) evolution of the eastern Sardo-Provencal and northern Algero-Balearic basins and related margins in the West Mediterranean Sea. Both basins were completely opened during the MSC and their well-defined seismic stratigraphy is very similar in the deep parts. The primary difference between these two basins is due to their different pre-MSC extensional history, including the opening age and the stretching factors. These factors influenced the occurrence of post-MSC salt tectonics on these margins.
    Print ISSN: 1354-0793
    Topics: Chemistry and Pharmacology , Geosciences
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  • 8
    Publication Date: 2021-01-25
    Description: The deep sea and its sub-seafloor contain a vast reservoir of physical, mineral and biological resources that are rapidly coming into the window of exploitation. Assessing the opportunities and the risks involved requires a serious commitment to excellent deep sea research. There are numerous areas in this field in which Europe has cutting-edge technological potential. These include drilling and monitoring technology in the field of renewable energies such as geothermal, offshore wind and seafloor resources. Scientific ocean drilling will continue to play a valuable role, for example in the exploration of resource opportunities, in obtaining estimates for ecosystem and Earth climate sensitivity, or in improving understanding about the controlling factors governing processes and recurrence intervals of submarine geohazards. In Europe, there is also the scientific expertise needed to define a framework for policymakers for environmental protection measures and to carry out ecological impact assessments before, during and after commercial exploitation. Taking up these societal challenges will strengthen European scientific and educational networks and promote the development of world-class technology and industrial leadership.
    Description: Published
    Description: 3.7. Dinamica del clima e dell'oceano
    Description: 4.6. Oceanografia operativa per la valutazione dei rischi in aree marine
    Description: open
    Keywords: Marine Geophysics ; Deep Sea ; Sea Technology ; Research Infrastructure ; 03. Hydrosphere::03.01. General::03.01.07. Physical and biogeochemical interactions
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: book
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  • 9
    Publication Date: 2017-04-04
    Description: Recent developments in paleomagnetism and environmental magnetism provide new tools for the detailed correlation of climatically induced magnetic mineralogy changes in sedimentary sequences. Studies of these changes contribute to the reconstruction of climate history for the glacial^interglacial cycles of the Late Pleistocene and to the delineation of the range of natural variability for global climate during the past hundred thousands years. Here we show that sharp coercivity minima observed in fine-grained sediments from the continental rise of the western Antarctic Peninsula correlate to the major rapid cooling events of the northern Atlantic (Heinrich layers). We interpret such an environmental magnetic signal in terms of variations in deep sea diagenetic processes of sulfide formation, which reflect changes in the input of detrital organic matter controlled by sea-ice extent. With the inherent uncertainties in age controls, the sedimentary paleoclimatic markers of the two hemispheres are almost contemporaneous, but interhemispheric time lags or leads of the order of 1-2 kyr (such as those recently reported from the Greenland and Antarctic ice cores) are also compatible with the data.
    Description: Published
    Description: 65-80
    Description: 2.2. Laboratorio di paleomagnetismo
    Description: JCR Journal
    Description: reserved
    Keywords: paleomagnetism ; paleointensity ; Antarctica ; Heinrich events ; climatic correlation ; 04. Solid Earth::04.05. Geomagnetism::04.05.06. Paleomagnetism
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 10
    Publication Date: 2019-07-16
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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