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  • 1
    Call number: 9/M 07.0421(435)
    In: Geological Society Special Publication
    Description / Table of Contents: Abstract Reservoir quality is studied using a wide range of similar techniques in both sandstones and carbonates. Sandstone and carbonate reservoir quality both benefit from the study of modern analogues and experiments, but modelling approaches are currently quite different for these two types of reservoirs. There are many common controls on sandstone and carbonate reservoir quality, but also distinct differences due primarily to mineralogy. Numerous controversies remain including the question of oil inhibition, the key control on pressure solution and geochemical flux of material to or from reservoirs. This collection of papers contains case-study-based examples of sandstone and carbonate reservoir quality prediction as well as modern analogue, outcrop analogue, modelling and advanced analytical approaches.
    Type of Medium: Monograph available for loan
    Pages: 453 Seiten , farbige Abbildungen, Tabellen, Grafiken
    ISBN: 978-1-78620-139-3
    Series Statement: Geological Society Special Publication 435
    Language: English
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
    Keywords: reservoir quality ; petroleum reservoirs ; carbonate rocks ; carbonate reservoirs
    Description / Table of Contents: Petroleum reservoir quality prediction: overview and contrasting approaches from sandstone and carbonate communities / R. H. Worden, P. J. Armitage, A. R. Butcher, J. M. Churchill, A. E. Csoma, C. Hollis, R. H. Lander and J. E. Omma / Geological Society, London, Special Publications, 435, 1-31, 1 May 2018, https://doi.org/10.1144/SP435.21 --- Diagenetic pathways linked to labile Mg-clays in lacustrine carbonate reservoirs: a model for the origin of secondary porosity in the Cretaceous pre-salt Barra Velha Formation, offshore Brazil / Nicholas J. Tosca and V. Paul Wright / Geological Society, London, Special Publications, 435, 33-46, 20 November 2015, https://doi.org/10.1144/SP435.1 --- Origin and evolution of microporosity in packstones and grainstones in a Lower Cretaceous carbonate reservoir, United Arab Emirates / Daniel Morad, Matteo Paganoni, Amena Al Harthi, Sadoon Morad, Andrea Ceriani, Howri Mansurbeg, Aisha Al Suwaidi, Ihsan S. Al-Aasm and Stephen N. Ehrenberg / Geological Society, London, Special Publications, 435, 47-66, 21 December 2016, https://doi.org/10.1144/SP435.20 --- Distinguishing between eogenetic, unconformity-related and mesogenetic dissolution: a case study from the Panna and Mukta fields, offshore Mumbai, India / A. J. Barnett, V. P. Wright, V. S. Chandra and V. Jain / Geological Society, London, Special Publications, 435, 67-84, 18 December 2015, https://doi.org/10.1144/SP435.12 --- Role of facies diversity and cyclicity on the reservoir quality of the mid-Cretaceous Mishrif Formation in the southern Mesopotamian Basin, Iraq / Thamer A. Mahdi and Adnan A. M. Aqrawi / Geological Society, London, Special Publications, 435, 85-105, 22 February 2017, https://doi.org/10.1144/SP435.19 --- Burial estimates constrained by clumped isotope thermometry: example of the Lower Cretaceous Qishn Formation (Haushi-Huqf High, Oman) / Cédric M. John / Geological Society, London, Special Publications, 435, 107-121, 18 November 2015, https://doi.org/10.1144/SP435.5 --- Feldspar alteration and Fe minerals: origin, distribution and implications for sandstone reservoir quality in estuarine sediments / Ehsan Daneshvar and Richard H. Worden / Geological Society, London, Special Publications, 435, 123-139, 13 April 2017, https://doi.org/10.1144/SP435.17 --- Evolution of small-scale flow barriers in German Rotliegend siliciclastics / Benjamin Busch, Rebecca Winkler, Keyvan Osivandi, Georg Nover, Alexandra Amann-Hildenbrand and Christoph Hilgers / Geological Society, London, Special Publications, 435, 141-160, 18 November 2015, https://doi.org/10.1144/SP435.3 --- Deformation band development as a function of intrinsic host-rock properties in Triassic Sherwood Sandstone / Joshua Griffiths, Daniel R. Faulkner, Alexander P. Edwards and Richard H. Worden / Geological Society, London, Special Publications, 435, 161-176, 19 January 2016, https://doi.org/10.1144/SP435.11 --- Diagenetic controls on the location of reservoir sweet spots relative to palaeotopographical and structural highs / Jessica E. Poteet, Robert H. Goldstein and Evan K. Franseen / Geological Society, London, Special Publications, 435, 177-215, 21 December 2016, https://doi.org/10.1144/SP435.18 --- Evaluation of porosity change during chemo-mechanical compaction in flooding experiments on Liège outcrop chalk / Wenxia Wang, Merete V. Madland, Udo Zimmermann, Anders Nermoen, Reidar I. Korsnes, Silvana R. A. Bertolino and Tania Hildebrand-Habel / Geological Society, London, Special Publications, 435, 217-234, 26 October 2016, https://doi.org/10.1144/SP435.10 --- Hydrothermal dolomitization: simulation by reaction transport modelling / Alberto Consonni, Alfredo Frixa and Chiara Maragliulo / Geological Society, London, Special Publications, 435, 235-244, 14 June 2016, https://doi.org/10.1144/SP435.13 --- Reservoir quality prediction of deep-water Oligocene sandstones from the west Niger Delta by integrated petrological, petrophysical and basin modelling / O. K. Chudi, Helen Lewis, D. A. V. Stow and J. O. Buckman / Geological Society, London, Special Publications, 435, 245-264, 14 December 2016, https://doi.org/10.1144/SP435.8 --- Diagenesis, plagioclase dissolution and preservation of porosity in Eocene and Oligocene sandstones at the Greeley oil field, southern San Joaquin basin, California, USA / D. T. Nguyen, R. A. Horton and A. B. Kaess / Geological Society, London, Special Publications, 435, 265-282, 28 June 2016, https://doi.org/10.1144/SP435.14 --- History of hydrothermal fluid flow in the midcontinent, USA: the relationship between inverted thermal structure, unconformities and porosity distribution / Bradley D. King and Robert H. Goldstein / Geological Society, London, Special Publications, 435, 283-320, 17 August 2016, https://doi.org/10.1144/SP435.16 --- Enhanced porosity preservation by pore fluid overpressure and chlorite grain coatings in the Triassic Skagerrak, Central Graben, North Sea, UK / Stephan Stricker and Stuart J. Jones / Geological Society, London, Special Publications, 435, 321-341, 5 January 2016, https://doi.org/10.1144/SP435.4 --- Deciphering multiple controls on reservoir quality and inhibition of quartz cement in a complex reservoir: Ordovician glacial sandstones, Illizi Basin, Algeria / Martin Wells, Philip Hirst, Jon Bouch, Emma Whear and Nigel Clark / Geological Society, London, Special Publications, 435, 343-372, 11 December 2015, https://doi.org/10.1144/SP435.6 --- Trace element composition of authigenic quartz in sandstones and its correlation with fluid–rock interaction during diagenesis / Thomas Götte / Geological Society, London, Special Publications, 435, 373-387, 19 January 2016, https://doi.org/10.1144/SP435.2 --- Comparing clay mineral diagenesis in interbedded sandstones and mudstones, Vienna Basin, Austria / Susanne Gier, Richard H. Worden and Peter Krois / Geological Society, London, Special Publications, 435, 389-403, 20 November 2015, https://doi.org/10.1144/SP435.9 --- The relevance of dawsonite precipitation in CO2 sequestration in the Mihályi-Répcelak area, NW Hungary / Csilla Király, Eszter Sendula, Ágnes Szamosfalvi, Réka Káldos, Péter Kónya, István J. Kovács, Judit Füri, Zsolt Bendő and György Falus / Geological Society, London, Special Publications, 435, 405-418, 20 June 2016, https://doi.org/10.1144/SP435.15 --- Reactive transport modelling of compacting siliciclastic sediment diagenesis / C. Geloni, A. Ortenzi and A. Consonni / Geological Society, London, Special Publications, 435, 419-439, 10 December 2015, https://doi.org/10.1144/SP435.7
    Pages: Online-Ressource (VI, 453 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 9781786201393
    Language: English
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  • 3
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    In:  Geological Society Special Publication 231: 1-9.
    Publication Date: 2007-10-08
    Description: High-resolution scanning electron microscope (SEM)-based cathodoluminescence images were used to reconstruct incremental fracture opening in regional opening-mode fractures in sandstone. Opening is recorded by crack-seal texture in isolated mineral bridges that span opening-mode fractures formed in sandstone at moderate-great depth (c. 1000-6000 m). We restored opening histories of nine representative fractures with apertures of millimetres in five sandstones from five sedimentary basins. Gaps created by fracture widening in 11 bridges range from less than 1 {micro}m to more than 1 mm, but nearly all are less than 20 {micro}m and most are less than 5 {micro}m. These are the opening amounts that could be spanned by cement growth in these diagenetic environments. Our observations are the first evidence of opening amounts from mostly porous, opening-mode (joint-like) fractures formed in diagenetic environments. Patterns are consistent with a new structural diagenetic model of bridge growth that can use opening patterns to indicate rate of fracture opening as a function of time.
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  • 4
    Publication Date: 2018-05-03
    Description: The porosity and permeability of sandstone and carbonate reservoirs (known as reservoir quality) are essential inputs for successful oil and gas resource exploration and exploitation. This chapter introduces basic concepts, analytical and modelling techniques and some of the key controversies to be discussed in 20 research papers that were initially presented at a Geological Society conference in 2014 titled ‘Reservoir Quality of Clastic and Carbonate Rocks: Analysis, Modelling and Prediction’. Reservoir quality in both sandstones and carbonates is studied using a wide range of techniques: log analysis and petrophysical core analysis, core description, routine petrographic tools and, ideally, less routine techniques such as stable isotope analysis, fluid inclusion analysis and other geochemical approaches. Sandstone and carbonate reservoirs both benefit from the study of modern analogues to constrain the primary character of sediment before they become a hydrocarbon reservoir. Prediction of sandstone and carbonate reservoir properties also benefits from running constrained experiments to simulate diagenetic processes during burial, compaction and heating. There are many common controls on sandstone and carbonate reservoir quality, including environment of deposition, rate of deposition and rate and magnitude of sea-level change, and many eogenetic processes. Compactional and mesogenetic processes tend to affect sandstone and carbonate somewhat differently but are both influenced by rate of burial, and the thermal and pressure history of a basin. Key differences in sandstone and carbonate reservoir quality include the specific influence of stratigraphic age on seawater composition (calcite v. aragonite oceans), the greater role of compaction in sandstones and the greater reactivity and geochemical openness of carbonate systems. Some of the key controversies in sandstone and carbonate reservoir quality focus on the role of petroleum emplacement on diagenesis and porosity loss, the role of effective stress in chemical compaction (pressure solution) and the degree of geochemical openness of reservoirs during diagenesis and cementation. This collection of papers contains case study-based examples of sandstone and carbonate reservoir quality prediction as well as modern analogue, outcrop analogue, modelling and advanced analytical approaches.
    Print ISSN: 0305-8719
    Electronic ISSN: 2041-4927
    Topics: Geosciences
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  • 5
    Publication Date: 2015-03-07
    Description: A new model accounts for crystal growth patterns and internal textures in quartz cement in sandstone fractures, including massive sealing deposits, thin rinds or veneers that line open fracture surfaces, and bridge structures that span otherwise open fractures. High-resolution cathodoluminescence imaging of bridge structures and massive sealing deposits indicates that they form in association with repeated micron-scale fracturing of growing quartz crystals, whereas thin rinds do not. Model results indicate that the three morphology types develop in response to (1) the ratio of the rates of quartz growth to fracture opening and (2) the substantially faster growth rate that occurs on noneuhedral surfaces in certain crystallographic orientations compared to euhedral crystal faces. Rind morphologies develop when the fracture opening rate exceeds two times the fastest rate of quartz growth (along the c axis on noneuhedral surfaces) because growing crystals develop slow-growing euhedral faces. Massive sealing, on the other hand, develops where the net rate of fracture opening is less than twice the rate of quartz growth on euhedral faces because all quartz growth surfaces along the fracture wall seal the fracture between fracturing events. Bridge structures form at fracture opening rates that are intermediate between the massive sealing and rind cases and are associated with crystallographic orientations that allow growth to span the fracture between fracturing events. Subsequent fractures break the spanned crystal, introducing new, fast-growing noneuhedral growth surfaces where quartz grows more rapidly compared to the euhedral faces of nonspanning crystals. As the ratio of fracture opening to quartz growth rate increases, the proportion of overgrowths that span the fracture decreases, and the range in c -axis orientations for these crystals comes progressively closer to perpendicular to the fracture wall until the maximum spanning limit is reached. Simulation results also reproduce "stretched crystal," "radiator structure," and "elongate blocky" textures in metamorphic quartz veins. The model replicates a well-characterized quartz bridge from the Cretaceous Travis Peak Formation as well as quartz cement abundances, internal textures, and morphologies in the sandstone host rock and fracture zone using the same kinetic parameters while honoring fluid-inclusion and thermal-history constraints. The same fundamental driving forces, in both in the host rock and fracture system, are responsible for quartz cementation, with the only significant difference within the fracture zone being the creation of new pore space as well as new noneuhedral surfaces for cases where overgrowths span fractures between fracturing events. Rates of fracture growth and sealing may be inferred from fracture cement textures using model results.
    Print ISSN: 0016-7606
    Electronic ISSN: 1943-2674
    Topics: Geosciences
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  • 6
    Publication Date: 2004-01-01
    Print ISSN: 0305-8719
    Electronic ISSN: 2041-4927
    Topics: Geosciences
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    Publication Date: 1993-03-01
    Print ISSN: 0016-7606
    Electronic ISSN: 1943-2674
    Topics: Geosciences
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  • 10
    Publication Date: 2014-10-06
    Print ISSN: 0016-7606
    Electronic ISSN: 1943-2674
    Topics: Geosciences
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