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  • 1
    Monograph available for loan
    Monograph available for loan
    Sedimentology of paralic reservoirs : recent advances (2017)
    London : Geological Society
    Associated volumes
    Details Availability
    Call number: 9/M 07.0421(444)
    In: Geological Society special publication
    Type of Medium: Monograph available for loan
    Pages: 426 Seiten , Illustrationen, Diagramme, Karten , 26 cm
    ISBN: 1786202743 , 9781786202741
    Series Statement: Geological Society special publication 444
    URL: http://sp.lyellcollection.org/content/444/1
    Classification:
    Sedimentology
    Language: English
    Branch Library: GFZ Library
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  • 2
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    Sedimentology of Paralic Reservoirs : Recent Advances (2017)
    London : The Geological Society
    Details
    Keywords: sedimentology ; reservoirs ; basins
    Description / Table of Contents: Introduction to the sedimentology of paralic reservoirs: recent advances / Gary J. Hampson, Antony D. Reynolds, Boris Kostic and Martin R. Wells / Geological Society, London, Special Publications, 444, 1-6, 9 May 2017, https://doi.org/10.1144/SP444.14 --- Subsurface characterization of paralic reservoirs --- Paralic reservoirs / Antony D. Reynolds / Geological Society, London, Special Publications, 444, 7-34, 20 July 2016, https://doi.org/10.1144/SP444.10 --- Stratigraphic architecture of the Knarr Field, Norwegian North Sea: sedimentology and biostratigraphy of an evolving tide- to wave-dominated shoreline system / James M. Churchill, Matthew T. Poole, Silje S. Skarpeid and Matthew I. Wakefield / Geological Society, London, Special Publications, 444, 35-58, 12 August 2016, https://doi.org/10.1144/SP444.4 --- Challenges in characterizing subsurface paralic reservoir geometries: a detailed case study of the Mungaroo Formation, North West Shelf, Australia / G. Heldreich, J. Redfern, B. Legler, K. Gerdes and B. P. J. Williams / Geological Society, London, Special Publications, 444, 59-108, 8 May 2017, https://doi.org/10.1144/SP444.13 --- Analysis of floodplain sedimentation, avulsion style and channelized fluvial sandbody distribution in an upper coastal plain reservoir: Middle Jurassic Ness Formation, Brent Field, UK North Sea / Yvette S. Flood and Gary J. Hampson / Geological Society, London, Special Publications, 444, 109-140, 29 June 2016, https://doi.org/10.1144/SP444.3 --- Tidal heterogeneity in paralic systems --- Deflection of the progradational axis and asymmetry in tidal seaway and strait deltas: insights from two outcrop case studies / Sergio G. Longhitano and Ron J. Steel / Geological Society, London, Special Publications, 444, 141-172, 13 July 2016, https://doi.org/10.1144/SP444.8 --- Tidally influenced shoal water delta and estuary in the Middle Jurassic of the Søgne Basin, Norwegian North Sea: sedimentary response to rift initiation and salt tectonics / Donatella Mellere, Aruna Mannie, Sergio Longhitano, Mike Mazur, Hyelni Kulausa, Samme Brough and James Cotton / Geological Society, London, Special Publications, 444, 173-213, 21 September 2016, https://doi.org/10.1144/SP444.11 --- Sedimentology and stratigraphic architecture of a Miocene retrogradational, tide-dominated delta system: Balingian Province, offshore Sarawak, Malaysia / Meor H. Amir Hassan, Howard D. Johnson, Peter A. Allison and Wan H. Abdullah / Geological Society, London, Special Publications, 444, 215-250, 30 August 2016, https://doi.org/10.1144/SP444.12 --- Stratigraphic evolution of an estuarine fill succession and the reservoir characterization of inclined heterolithic strata, Cretaceous of southern Utah, USA / Cari L. Johnson, L. Stright, R. Purcell and P. Durkin / Geological Society, London, Special Publications, 444, 251-286, 29 June 2016, https://doi.org/10.1144/SP444.1 --- Recognizing seasonal fluvial influence in ancient tidal deposits / Annalize Q. McLean and Brent Wilson / Geological Society, London, Special Publications, 444, 287-303, 13 July 2016, https://doi.org/10.1144/SP444.6 --- Analogue studies --- Evolution and architectural styles of a forced-regressive Holocene delta and megafan, Mitchell River, Gulf of Carpentaria, Australia / T. I. Lane, R. A. Nanson, B. K. Vakarelov, R. B. Ainsworth and S. E. Dashtgard / Geological Society, London, Special Publications, 444, 305-334, 7 July 2016, https://doi.org/10.1144/SP444.9 --- Transgressive successions of the Mahakam Delta Province, Indonesia / Joseph J. Lambiase, Ridha S. Riadi, Nadia Nirsal and Salahuddin Husein / Geological Society, London, Special Publications, 444, 335-348, 29 June 2016, https://doi.org/10.1144/SP444.2 --- Time–space variability of paralic strata deposited in a high accommodation, high sediment supply setting: example from the Cretaceous of Utah / Julia S. Mulhern and Cari L. Johnson / Geological Society, London, Special Publications, 444, 349-392, 29 June 2016, https://doi.org/10.1144/SP444.7 --- Anatomy of a mixed-influence shelf edge delta, Karoo Basin, South Africa / Luz E. Gomis-Cartesio, Miquel Poyatos-Moré, Stephen S. Flint, David M. Hodgson, Rufus L. Brunt and Henry DeV. Wickens / Geological Society, London, Special Publications, 444, 393-418, 14 July 2016, https://doi.org/10.1144/SP444.5
    Pages: Online-Ressource (VI, 426 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 9781786202741
    URL: http://sp.lyellcollection.org/content/444/1
    Language: English
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  • 3
    Electronic Resource
    Electronic Resource
    Use of low frequencies for sub-basalt imaging (2003)
    Oxford, UK : Blackwell Science Ltd
    Geophysical prospecting 51 (2003), S. 0 
    Details
    ISSN: 1365-2478
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences , Physics
    Notes: Many prospective passive ocean margins are covered by large areas of basalts. These basalts are often extremely heterogeneous and scatter the seismic energy of the conventional seismic reflection system so that it becomes difficult to obtain information on deeper reflectors. Since high frequencies are scattered more than low frequencies, we argue that the acquisition system for sub-basalt targets should be modified to emphasize the low frequencies, using much larger airguns, and towing the source and receivers at about 20 m depth. In the summer of 2001 we obtained seismic reflection data over basalt in the northeast Atlantic using a system modified to enhance the low-frequency energy. These new data show deep reflections that are not visible on lines shot in the same places with a conventional system.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1046/j.1365-2478.2003.00363.x
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  • 4
    Electronic Resource
    Electronic Resource
    The effects of source and receiver motion on seismic data (1995)
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical prospecting 43 (1995), S. 0 
    Details
    ISSN: 1365-2478
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences , Physics
    Notes: The effects of source and receiver motion on seismic data are considered using extensions of the standard convolutional model. In particular, receiver motion introduces a time-variant spatial shift into data, while source motion converts the effect of the source signature from a single-channel convolution in time to a multichannel convolution in time and space. These results are consistent with classical Doppler theory and suggest that Doppler shifting can introduce distortions into seismic data even at relatively slow acquisition speeds. It is shown that, while both source and receiver motion are known to be important for marine vibroseis acquisition, receiver motion alone can produce significant artifacts in marine 3D data. Fortunately, the convolutional nature of the distortions renders them amenable to correction using simple deconvolution techniques. Specifically, the effects of receiver motion can be neutralized by applying an appropriate reverse time-variant spatial shift, while those due to source motion can be addressed by introducing time-variant spatial shifts both before and after standard, deterministic, signature deconvolution or correlation.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-2478.1995.tb00133.x
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  • 5
    Electronic Resource
    Electronic Resource
    Modelling ancient tides: the Upper Carboniferous epi-continental seaway of Northwest Europe (2005)
    Oxford, UK : Blackwell Science Ltd
    Sedimentology 52 (2005), S. 0 
    Details
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Due to a lack of modern analogues, debate surrounds the importance of tides in ancient epi-continental seas. However, numerical modelling can provide a quantitative means of investigating palaeo-tidality without recourse to analogues. Finite element modelling of the European Upper Carboniferous epi-continental seaway predicts an exceedingly low Lunar tidal range (ca 5 cm in the open water regions of the UK and Southern North Sea). The Imperial College Ocean Model (ICOM) uses finite element methods and an unstructured tetrahedral mesh that is computationally very efficient. The accuracy and sensitivity of ICOM tidal range predictions were tested using bathymetric data from the present-day Mediterranean Sea. The Mediterranean Sea is micro-tidal and varies in depth up to 5·4 km with an average depth of 1–2 km. ICOM accurately predicts the tidal range given both a realistic, but smoothed, bathymetry and a straight sided basin with a uniform depth of 1 km. Variation in uniform depth from 100 to 3000 m with and without islands consistently predicts micro-tidality, demonstrating that the model is robust and the effect of bathymetric uncertainty on model output is relatively small. The extremely low tidal range predicted for the European Upper Carboniferous is thus deemed robust. Putative Upper Carboniferous tidal deposits have been described in the UK and southern North Sea, but are represented by cyclic rhythmites and are limited to palaeo-estuaries. Calculations based on an embayed coast model show that the tidal range could have been amplified to ca 1 m in estuaries and that this is sufficient to form cyclic rhythmites. Without tidal mixing, the tropical equatorial heat and salinity enhancement would promote stratification in the open water body. The introduction of organic matter probably caused anoxia, biotic mortality and carbon accumulation, as evidenced by numerous black ‘marine-band’ shales.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-3091.2005.00718.x
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  • 6
    Electronic Resource
    Electronic Resource
    Reply (2001)
    Oxford UK : Blackwell Science Ltd
    Sedimentology 48 (2001), S. 0 
    Details
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1046/j.1365-3091.2001.0414b.x
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  • 7
    Electronic Resource
    Electronic Resource
    A sequence stratigraphic model for the Lower Coal Measures (Upper Carboniferous) of the Ruhr district, north-west Germany (1999)
    Oxford UK : Blackwell Science Ltd
    Sedimentology 46 (1999), S. 0 
    Details
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Upper Carboniferous Coal Measures strata have been interpreted traditionally in terms of cyclothems bounded by marine flooding surfaces (marine bands) and coal seams. Correlation of such cyclothems in an extensive grid of closely spaced coal exploration boreholes provides a robust stratigraphic framework in which to study the Lower Coal Measures (Namurian C–Westphalian A) of the Ruhr district, north-west Germany. Three distinct types of cyclothem are recognized, based on their bounding surfaces and internal facies architecture. (1) Type 1 cyclothems are bounded by marine bands. Each cyclothem comprises a thick (30–80 m), regionally extensive, coarsening-upward delta front succession of interbedded shales, siltstones and sandstones, which may be deeply incised by a major fluvial sandstone complex. The delta front succession is capped by a thin (〈1 m), regionally extensive coal seam and an overlying marine band defining the top of the cyclothem. (2) Type 2 cyclothems are bounded by thick (≈1 m), regionally extensive coal seams with few splits. The basal part of a typical cyclothem comprises a thick (15–50 m), widespread, coarsening-upward delta front or lake infill succession consisting of interbedded shales, siltstones and sandstones. Networks of major (〉5 km wide, 20–40 m thick), steep-sided, multistorey fluvial sandstone complexes erode deeply into and, in some cases, through these successions and are overlain by the coal seam defining the cyclothem top. (3) Type 3 cyclothems are bounded by regionally extensive coal seam groups, characterized by numerous seam splits on a local (0·1–10 km) scale. Intervening strata vary in thickness (15–60 m) and are characterized by strong local facies variability. Root-penetrated, aggradational floodplain heteroliths pass laterally into single-storey fluvial channel-fill sandstones and coarsening-upward, shallow lake infill successions of interbedded shales, siltstones and sandstones over distances of several hundred metres to a few kilometres. Narrow (〈2 km) but thick (20–50 m) multistorey fluvial sandstone complexes are rare, but occur in a few type 3 cyclothems. Several cyclothems are observed to change character from type 1 to type 2 and from type 2 to type 3 up the regional palaeoslope. Consequently, we envisage a model in which each cyclothem type represents a different palaeogeographic belt within the same, idealized delta system, subject to the same allogenic and autogenic controls on facies architecture. Type 1 cyclothems are dominated by deltaic shorelines deposited during a falling stage and lowstand of sea level. Type 2 cyclothems represent the coeval lower delta plain, which was deeply eroded by incised valleys that fed the falling stage and lowstand deltas. Type 3 cyclothems comprise mainly upper delta plain deposits in which the allogenic sea-level control was secondary to autogenic controls on facies architecture. The marine bands, widespread coals and coal seam groups that bound these three cyclothem types record abandonment of the delta system during periods of rapid sea-level rise. The model suggests that the extant cyclothem paradigm does not adequately describe the detailed facies architecture of Lower Coal Measures strata. Instead, these architectures may be better understood within a high-resolution stratigraphic framework incorporating sequence stratigraphic key surfaces, integrated with depositional models derived from analogous Pleistocene–Holocene fluvio-deltaic strata.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1046/j.1365-3091.1999.00273.x
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  • 8
    Electronic Resource
    Electronic Resource
    Geomorphological and sequence stratigraphic variability in wave-dominated, shoreface-shelf parasequences (2003)
    Oxford, UK : Blackwell Science Ltd
    Sedimentology 50 (2003), S. 0 
    Details
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Abstract Physical stratigraphy within shoreface-shelf parasequences contains a detailed, but virtually unstudied, record of shallow-marine processes over a range of historical and geological timescales. Using high-quality outcrop data sets, it is possible to reconstruct ancient shoreface-shelf morphology from clinoform surfaces, and to track the evolving morphology of the ancient shoreface-shelf. Our results suggest that shoreface-shelf morphology varied considerably in response to processes that operate over a range of timescales. (1) Individual clinoform surfaces form as a result of enhanced wave scour and/or sediment starvation, which may be driven by minor fluctuations in relative sea level, sediment supply and/or wave climate over short timescales (101−103 years). These external controls cannot be distinguished in vertical facies successions, but may potentially be differentiated by the resulting clinoform geometries. (2) Clinoform geometry and distribution changes systematically within a single parasequence, reflecting the cycle in sea level and/or sediment supply that produced the parasequence (102−105 years). These changes record steepening of the shoreface-shelf profile during early progradation and maintenance of a relatively uniform profile during late progradation. Modern shorefaces are not representative of this stratigraphic variability. (3) Clinoform geometries vary greatly between different parasequences as a result of variations in parasequence stacking pattern and relict shelf morphology during shoreface progradation (105−108 years). These controls determine the external dimensions of the parasequence.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1046/j.1365-3091.2003.00570.x
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  • 9
    Electronic Resource
    Electronic Resource
    Shoreface tongue geometry constrains history of relative sea-level fall: examples from Late Cretaceous strata in the Book Cliffs area, Utah (2001)
    Oxford UK : Blackwell Science Ltd
    Terra nova 13 (2001), S. 0 
    Details
    ISSN: 1365-3121
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Progradational shoreface tongues preserve a near-complete depositional record of relative sea-level highstands, falls and lowstands. Two distinct styles of progradational shoreface tongue are examined in an extensive outcrop and subsurface dataset from Late Cretaceous strata of the Book Cliffs area, Utah, representing (i) highstand through attached lowstand progradation and (ii) highstand through detached lowstand progradation. Using this dataset, key geometrical attributes of the shoreface tongues and their internal facies architecture are identified and quantified that enable the reconstruction of relative sea-level fall history. For example, attached, wave-dominated lowstand shoreface deposits record a slow (0.2– 0.3 mm yr–1), low-magnitude (〉 14 m) relative sea-level fall punctuated by minor rises. Detached, weakly wave-influenced lowstand shoreface deposits record a more rapid (0.4–0.5 mm yr–1), high-magnitude (〉 45 m) relative sea-level fall synchronous with a marked change in sediment delivery and depositional process regime at the shoreline.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1046/j.1365-3121.2001.00337.x
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  • 10
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    Characterization of Controls on High-Resolution Stratigraphic Architecture in Wave-Dominated Shoreface-Shelf Parasequences Using Inverse Numerical Modeling (2011)
    Society for Sedimentary Geology (SEPM)
    Details
    Publication Date: 2011-08-01
    Description: A new inverse numerical modeling method is used to constrain the environmental parameters (e.g., relative-sea-level, sediment-supply, and wave climate histories) that control stratigraphic architecture in wave-dominated shallow-marine deposits. The method links a "process-response" forward stratigraphic model that simulates wave and storm processes (BARSIM) to a combination of inverse methods formulated in a Bayesian framework that allows full characterization of uncertainties. This method is applied for the first time to a real geologic dataset, collected at outcrop from two shoreface-shelf parasequences in the Aberdeen Member, Blackhawk Formation of the Book Cliffs, east-central Utah, USA. The environmental parameters that controlled the observed stratigraphic architecture are quantified, and key aspects of stratigraphic architecture are successfully predicted from limited data. Stratigraphic architecture at parasequence-stacking and intra-parasequence scales was driven principally by relative sea level (varying by up to about 55 m) and sediment supply (varying by up to 70 m2/yr), whose interplay determines the shoreline trajectory. Within zones of distinctive shoreline trajectory, variations in wave climate (of up to about 3 m in fairweather-wave height) controlled superimposed variations in sandstone and shale content (e.g., the development of upward-coarsening and upward-fining bedsets). The modeling results closely match the observed stratigraphic architecture, but their quality is limited by: (1) the formulation and assumptions of the forward-modeling algorithms, and (2) the observed data distribution and quality, which provide poor age constraint.
    Print ISSN: 1527-1404
    Topics: Geosciences
    Published by Society for Sedimentary Geology (SEPM)
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