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  • 1
    Series available for loan
    Series available for loan
    Late Quaternary marine geology of Makkovik Bay, Labrador (1982)
    Ottawa : Geological Survey of Canada
    Associated volumes
    Details Availability
    Call number: SR 90.0008(81-17)
    In: Paper
    Type of Medium: Series available for loan
    Pages: 37 S.
    ISBN: 0660111047
    Series Statement: Paper / Geological Survey of Canada 81-17
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 2
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    Fine-grained Sediments : Deep-water Processes and Facies (1984)
    Oxford, London, Edinburgh, Boston, Palo Alto, Melbourne : Blackwell Scientific Publications
    Details
    Keywords: Feinkörniges Sediment ; Tiefseesediment
    Description / Table of Contents: Introduction --- D. A. V. Stow and D. J. W. Piper: Deep-water fine-grained sediments; history, methodology and terminology / Geological Society, London, Special Publications, 15:3-14, doi:10.1144/GSL.SP.1984.015.01.01 --- Processes --- D. S. Gorsline: A review of fine-grained sediment origins, characteristics, transport and deposition / Geological Society, London, Special Publications, 15:17-34, doi:10.1144/GSL.SP.1984.015.01.02 --- I. N. McCave: Erosion, transport and deposition of fine-grained marine sediments / Geological Society, London, Special Publications, 15:35-69, doi:10.1144/GSL.SP.1984.015.01.03 --- S. L. Eittreim: Methods and observations in the study of deep-sea suspended particulate matter / Geological Society, London, Special Publications, 15:71-82, doi:10.1144/GSL.SP.1984.015.01.04 --- Kate Kranck: Grain-size characteristics of turbidites / Geological Society, London, Special Publications, 15:83-92, doi:10.1144/GSL.SP.1984.015.01.05 --- Terrigenous Turbidites and Associated Facies --- T. C. E. van Weering and J. van Iperen: Fine-grained sediments of the Zaire deep-sea fan, southern Atlantic Ocean / Geological Society, London, Special Publications, 15:95-113, doi:10.1144/GSL.SP.1984.015.01.06 --- A. Monaco and Y. Mear: Sedimentary sequences on the north-west Mediterranean margin during the Late Quaternary: a dynamic interpretation / Geological Society, London, Special Publications, 15:115-125, doi:10.1144/GSL.SP.1984.015.01.07 --- D. A. V. Stow, M. Alam, and D. J. W. Piper: Sedimentology of the Halifax Formation, Nova Scotia: Lower Palaeozoic fine-grained turbidites / Geological Society, London, Special Publications, 15:127-144, doi:10.1144/GSL.SP.1984.015.01.08 --- R. B. Kidd and R. C. Searle: Sedimentation in the southern Cape Verde Basin: regional observations by long-range sidescan sonar / Geological Society, London, Special Publications, 15:145-152, doi:10.1144/GSL.SP.1984.015.01.09 --- G. A. Auffret, R. Le Suave, R. Kerbrat, B. Sichler, S. Roy, C. Laj, and C. Muller: Sedimentation in the southern Cape Verde Basin: seismic and sediment facies / Geological Society, London, Special Publications, 15:153-167, doi:10.1144/GSL.SP.1984.015.01.10 --- H. Got: Sedimentary processes on the west Hellenic Arc margin / Geological Society, London, Special Publications, 15:169-183, doi:10.1144/GSL.SP.1984.015.01.11 --- S. K. Chough: Fine-grained turbidites and associated mass-flow deposits in the Ulleung (Tsushima) Back-arc Basin, East Sea (Sea of Japan) / Geological Society, London, Special Publications, 15:185-196, doi:10.1144/GSL.SP.1984.015.01.12 --- Carbonate Turbidites and Associated Facies --- K. C. Heath and H. T. Mullins: Open-ocean, off-bank transport of fine-grained carbonate sediment in the Northern Bahamas / Geological Society, London, Special Publications, 15:199-208, doi:10.1144/GSL.SP.1984.015.01.13 --- J.-C. Faugères, M. Cremer, E. Gonthier, M. Noel, and J. Poutiers: Late Quaternary calcareous clayey-silty muds in the Obock Trough (Gulf of Aden): hemipelagites or fine-grained turbidites? / Geological Society, London, Special Publications, 15:209-222, doi:10.1144/GSL.SP.1984.015.01.14 --- D. A. V. Stow, S. C. R. Rainey, G. Angell, F. C. Wezel, and D. Savelli: Depositional model for calcilutites: Scaglia Rossa limestones, Umbro-Marchean Apennines / Geological Society, London, Special Publications, 15:223-241, doi:10.1144/GSL.SP.1984.015.01.15 --- Contourites --- D. A. V. Stow and J. A. Holbrook: North Atlantic contourites: an overview / Geological Society, London, Special Publications, 15:245-256, doi:10.1144/GSL.SP.1984.015.01.16 --- A. N. Shor, D. V. Kent, and R. D. Flood: Contourite or turbidite?: magnetic fabric of fine-grained Quaternary sediments, Nova Scotia continental rise / Geological Society, London, Special Publications, 15:257-273, doi:10.1144/GSL.SP.1984.015.01.17 --- E. G. Gonthier, J.-C. Faugères, and D. A. V. Stow: Contourite facies of the Faro Drift, Gulf of Cadiz / Geological Society, London, Special Publications, 15:275-292, doi:10.1144/GSL.SP.1984.015.01.18 --- J. D. Halfman and T. C. Johnson: The sediment texture of contourites in Lake Superior / Geological Society, London, Special Publications, 15:293-307, doi:10.1144/GSL.SP.1984.015.01.19 --- Hemipelagites and Associated Facies of Slopes and Slope Basins --- P. R. Hill: Facies and sequence analysis of Nova Scotian Slope muds: turbidite vs ‘hemipelagic’ deposition / Geological Society, London, Special Publications, 15:311-318, doi:10.1144/GSL.SP.1984.015.01.20 --- B. A. McGregor, T. A. Nelsen, W. L. Stubblefield, and G. F. Merrill: The role of canyons in late Quaternary deposition on the United States mid-Atlantic continental rise / Geological Society, London, Special Publications, 15:319-330, doi:10.1144/GSL.SP.1984.015.01.21 --- P. F. Ballance, M. R. Gregory, G. W. Gibson, G. C. H. Chaproniere, A. P. Kadar, and T. Sameshima: A late Miocene and early Pliocene upper slope-to-shelf sequence of calcareous fine sediment from the Pacific margin of New Zealand / Geological Society, London, Special Publications, 15:331-342, doi:10.1144/GSL.SP.1984.015.01.22 --- K. T. Pickering: Facies, facies-associations and sediment transport/deposition processes in a late Precambrian upper basin-slope/pro-delta,, Finnmark, N. Norway / Geological Society, London, Special Publications, 15:343-362, doi:10.1144/GSL.SP.1984.015.01.23 --- L. A. Krissek: Continental source area contributions to fine-grained sediments on the Oregon and Washington continental slope / Geological Society, London, Special Publications, 15:363-375, doi:10.1144/GSL.SP.1984.015.01.24 --- S. E. Thornton: Basin model for hemipelagic sedimentation in a tectonically active continental margin: Santa Barbara Basin, California Continental Borderland / Geological Society, London, Special Publications, 15:377-394, doi:10.1144/GSL.SP.1984.015.01.25 --- D. S. Gorsline, R. L. Kolpack, H. A. Karl, D. E. Drake, S. E. Thornton, J. R. Schwalbach, C. E. Savrda, and P. Fleischer: Studies of fine-grained sediment transport processes and products in the California Continental Borderland / Geological Society, London, Special Publications, 15:395-415, doi:10.1144/GSL.SP.1984.015.01.26 --- R. Bourrouilh and D. S. Gorsline: Fine-grained sediments associated with fan lobes: Santa Paula Creek, California / Geological Society, London, Special Publications, 15:417-433, doi:10.1144/GSL.SP.1984.015.01.27 --- Pelagites and Organic-Rich Sediments --- A. H. F. Robertson: Origin of varve-type lamination, graded claystones and limestone-shale ‘couplets’ in the lower Cretaceous of the western North Atlantic / Geological Society, London, Special Publications, 15:437-452, doi:10.1144/GSL.SP.1984.015.01.28 --- A. B. Hayward: Hemipelagic chalks in a clastic submarine fan sequence: Miocene SW Turkey / Geological Society, London, Special Publications, 15:453-467, doi:10.1144/GSL.SP.1984.015.01.29 --- P. D. Crevello, J. W. Patton, T. W. Oesleby, W. Schlager, and A. Droxler: Source rock potential of Bahamian Trough carbonates / Geological Society, London, Special Publications, 15:469-480, doi:10.1144/GSL.SP.1984.015.01.30 --- C. M. Isaacs: Hemipelagic deposits in a Miocene basin, California: toward a model of lithologic variation and sequence / Geological Society, London, Special Publications, 15:481-496, doi:10.1144/GSL.SP.1984.015.01.31 --- George C. Anastasakis and Daniel Jean Stanley: Sapropels and organic-rich variants in the Mediterranean: sequence development and classification / Geological Society, London, Special Publications, 15:497-510, doi:10.1144/GSL.SP.1984.015.01.32 --- A. Thickpenny: The sedimentology of the Swedish Alum Shales / Geological Society, London, Special Publications, 15:511-525, doi:10.1144/GSL.SP.1984.015.01.33 --- M. A. Arthur, W. E. Dean, and D. A. V. Stow: Models for the deposition of Mesozoic-Cenozoic fine-grained organic-carbon-rich sediment in the deep sea / Geological Society, London, Special Publications, 15:527-560, doi:10.1144/GSL.SP.1984.015.01.34 --- Internal Characteristics --- R. W. Faas: Plasticity and compaction characteristics of the Quaternary sediments penetrated on the Guatemalan Transect—DSDP Leg 67 / Geological Society, London, Special Publications, 15:563-577, doi:10.1144/GSL.SP.1984.015.01.35 --- C. F. Moon and C. W. Hurst: Fabric of muds and shales: an overview / Geological Society, London, Special Publications, 15:579-593, doi:10.1144/GSL.SP.1984.015.01.36 --- A. Wetzel: Bioturbation in deep-sea fine-grained sediments: influence of sediment texture, turbidite frequency and rates of environmental change / Geological Society, London, Special Publications, 15:595-608, doi:10.1144/GSL.SP.1984.015.01.37 --- Facies Models: Synthesis --- D. A. V. Stow and D. J. W. Piper: Deep-water fine-grained sediments: facies models / Geological Society, London, Special Publications, 15:611-646, doi:10.1144/GSL.SP.1984.015.01.38
    Pages: Online-Ressource (VI, 659 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 0632010754
    URL: http://sp.lyellcollection.org/content/15/1
    Language: English
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  • 3
    Electronic Resource
    Electronic Resource
    Modelling of turbidity currents on Navy Submarine Fan, California Continental Borderland (1984)
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 31 (1984), S. 0 
    Details
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Several Holocene turbidites can be correlated across much of Navy Fan through more than 100 sediment core localities. The uppermost muddy turbidite unit is mapped throughout the northern half of the fan; its volume, grain-size distribution and the maximum height of deposition on the basin slopes are known. These parameters can be related to the precise channel morphology and mesotopography revealed by deep-tow surveys. Thus there is sufficient information to estimate detailed flow characteristics for this turbidity current as it moved from fan valley to distal basin plain.On the upper fan, the gradient and the increasing downstream width of the channel and only limited flow overspill suggest that the flow had a Froude number close to 1.0. The sediment associated with the channel indicates friction velocities of about 0.06 m s−1 and flow velocities of about 0.75 m s−1. Using this flow velocity and channel dimensions, sediment concentration (∼2×10−3) and discharge are estimated, and from a knowledge of the total volume of sediment deposited, the flow duration is estimated to be from 2 to 9 days. It is shown that the estimates of Froude number, drag coefficient, and sediment concentration are not likely to vary by more than a factor of 2.On the mid-fan, the flow was much thicker than the height of the surface relief of the fan and it spread rapidly. The cross-flow slope, determined from the horizontal extent of turbidite sediment, is used to estimate flow velocity, which is confirmed by consideration of both sediment grain size and rate of deposition. This again allows sediment concentration and discharge to be estimated. The requirements of flow continuity, entrainment of water during flow expansion, and observed sediment deposition provide checks on all these estimates, and provide an integrated picture of the evolution of the flow. The flow characteristics of this muddy turbidity current are well constrained compared to those for more sand-rich late Pleistocene and early Holocene turbidity currents on the fan.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-3091.1984.tb01957.x
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  • 4
    Electronic Resource
    Electronic Resource
    Turbidite depositional patterns and flow characteristics, Navy Submarine Fan, California Borderland (1983)
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 30 (1983), S. 0 
    Details
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The late Pleistocene and Holocene stratigraphy of Navy Fan is mapped in detail from more than 100 cores. Thirteen 14C dates of plant detritus and of organic-rich mud beds show that a marked change in sediment supply from sandy to muddy turbidites occurred between 9000 and 12,000 years ago. They also confirm the correlation of several individual depositional units. The sediment dispersal pattern is primarily controlled by basin configuration and fan morphology, particularly the geometry of distributary channels, which show abrupt 60° bends related to the Pleistocene history of lobe progradation. The Holocene turbidity currents are depositing on, and modifying only slightly, a relict Pleistocene morphology.The uppermost turbidite is a thin sand to mud bed on the upper-fan valley levées and on parts of the mid-fan. Most of its sediment volume is in a mud bed on the lower fan and basin plain downslope from a sharp bend in the mid-fan distributary system. Little sediment occurs farther downstream within this distributary system. It appears that most of the turbidity current overtopped the levée at the channel bend, a process referred to as flow stripping. The muddy upper part of the flow continued straight down to the basin plain. The residual more sandy base of the flow in the distributary channel was not thick enough to maintain itself as gradient decreased and the channel opened out on to the mid-fan lobe.Flow stripping may occur in any turbidity current that is thick relative to channel depth and that flows in a channel with sharp bends. Where thick sandy currents are stripped, levée and mid-fan erosion may occur, but the residual current in the channel will lose much of its power and deposit rapidly. In thick muddy currents, progressive overflow of mud will cause less declaration of the residual channelised current. Thus both size and sand-to-mud ratio of turbidity currents feeding a fan are important factors controlling morphologic features and depositional areas on fans. The size-frequency variation for different types of turbidity currents is estimated from the literature and related to the evolution of fan morphology.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-3091.1983.tb00702.x
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  • 5
    Electronic Resource
    Electronic Resource
    Surface textures of turbidite sand grains, Laurentian Fan and Sohm Abyssal Plain (1982)
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 29 (1982), S. 0 
    Details
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Surface textures of quartz grains have been examined from five samples from the Laurentian Fan and Sohm Abyssal Plain, representing varied transport distances and power of the depositing turbidity current. The grains retain their primary irregular shape derived from glacial erosion, and glacial surface textures are preserved in dish-shaped depressions. These features have been superimposed by a slight rounding of edges and an abundance of collision-induced markings, particularly mechanical V-forms. The most intense current modification of this sort occurs in mid-Wisconsinan or earlier sands that have been transported over 1000 km to the distal Sohm Abyssal Plain by turbidity currents. Collision textures probably develop during grain flow on the steep continental slope: delicate resedimented shelf foraminifera are preserved in the same turbidites and most have been transported exclusively in suspension.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-3091.1982.tb00077.x
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  • 6
    Electronic Resource
    Electronic Resource
    Navy Fan, California Borderland: Growth pattern and depositional processes (1984)
    Springer
    Geo-marine letters 3 (1984), S. 101-108 
    Details
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Navy Fan is a Late Pleistocene sand-rich fan prograding into an irregularly shaped basin in the southern California Borderland. The middle fan, characterized by one active and two abandoned “distributary” channels and associated lobe deposits, at present onlaps part of the basin slope directly opposite from the upper-fan valley, thus dividing the lower-fan/basin-plain regions into two separate parts of different depths. Fine-scale mesotopographic relief on the fan surface and correlation of individual turbidite beds through nearly 40 cores on the middle and lower fan provide data for evaluating the Late Pleistocene and Holocene depositional processes.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02462454
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  • 7
    Electronic Resource
    Electronic Resource
    The Laurentian Fan: Sohm Abyssal Plain (1984)
    Springer
    Geo-marine letters 3 (1984), S. 141-146 
    Details
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The 0.5- to 2-km thick Quaternary Laurentian Fan is built over Tertiary and Mesozoic sediments that rest on oceanic crust. Two 400-km long fan valleys, with asymmetric levees up to 700-m high, lead to an equally long, sandy, lobate basin plain (northern Sohm Abyssal Plain). The muddy distal Sohm Abyssal Plain is a further 400-km long. The sediment supplied to the fan is glacial in origin, and in part results from seismically triggered slumping on the upper continental slope. Sandy turbidity currents, such as the 1929 Grand Banks earthquake event, probably erode the fan-valley floors; but thick muddy turbidity currents build up the high levees.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02462459
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  • 8
    Electronic Resource
    Electronic Resource
    Storm graded sand at 200 m water depth, Scotian Shelf, Eastern Canada (1982)
    Springer
    Geo-marine letters 2 (1982), S. 77-81 
    Details
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Graded sand-to-mud beds are a common shelf facies in the rock record. Similar beds were studied in nine cores from the sandmud transition at the edge of Emerald Basin to determine their frequency and mode of origin. Graded sand-to-mud beds 5 to 20 cm thick can be correlated between cores and thicken basinwards, with average sand content decreasing from 60% to 5% over 7 km. European weed pollen distribution indicates only the top bed is less than 200 years old. The graded beds were deposited from suspension during storms with a several hundred year recurrence interval.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02462804
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  • 9
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    Navy Fan, California Borderland: Growth pattern and depositional processes (1983)
    Springer
    Details
    Publication Date: 1983-06-01
    Print ISSN: 0276-0460
    Electronic ISSN: 1432-1157
    Topics: Geosciences
    Published by Springer
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  • 10
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    The Laurentian Fan: Sohm abyssal plain (1983)
    Springer
    Details
    Publication Date: 1983-06-01
    Print ISSN: 0276-0460
    Electronic ISSN: 1432-1157
    Topics: Geosciences
    Published by Springer
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