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  • 1
    Monograph available for loan
    Monograph available for loan
    London : The Geological Society
    Associated volumes
    Call number: 9/M 93.0904 ; 9/M 92.0411
    In: Geological Society special publication
    Description / Table of Contents: During the 1980s the increasing availability of seismic reflection data prompted an upsurge of interest in extensional tectonics, early work concentrating on ‘listric’ thrust-belt type models and the concepts of section balancing. However, earthquake seismology and detailed fault studies have shown recently that faults involved in crustal extension may be essentially planar. This volume concerns the geological setting and interpretation of both listric and planar normal faults. Normal faults are of particular importance in UK hydrocarbon exploration as they are directly or indirectly responsible for the majority of the pre-Tertiary oil and gas accumulations in the North Sea. As the economic size of fields reduces, the modern geologist will require an improved understanding of the origins, geometry and sealing capabilities of these faults. The volume is divided into four sections, dealing with: the geometry and kinematics of large-scale, crustal-stretching faults which typically delimit major hydrocarbon accumulations; case studies ranging from the small-scale fractures associated with the movement of salt to the large-scale intra-plate kinematics of whole fault arrays; studies of detailed displacement patterns shown by individual faults and small fault arrays; and modelling studies of normal fault geometry. The editors believe that this volume will clarify the circumstances in which the diverse models of normal fault geometry might be applicable and thus provide a useful source of reference for both industry- and academia-based research workers. Another volume on extensional tectonics? Yes, but not only is this one very nicely put together, it is also very timely … The editors have wisely placed the emphasis on observations and data … Roberts et al. deserve a great deal of credit for the very high standard of presentation. Most of the contributions contain sensible stuff that is clearly written. Illustrations are excellent … and there are hardly any typos … Ican thoroughly recommend this book to both libraries and individuals.
    Type of Medium: Monograph available for loan
    Pages: VIII, 264 S. , Ill., graph. Darst., Kt.
    ISBN: 0903317591
    Series Statement: Geological Society special publication 56
    Classification:
    Tectonics
    Language: English
    Note: R. F. P. Hardman and J. E. Booth: The significance of normal faults in the exploration and production of North Sea hydrocarbons / Geological Society, London, Special Publications, 56:1-13, doi:10.1144/GSL.SP.1991.056.01.01 --- Seismic and Subsurface Studies --- David Barr: Subsidence and sedimentation in semi-starved half-graben: a model based on North Sea data / Geological Society, London, Special Publications, 56:17-28, doi:10.1144/GSL.SP.1991.056.01.02 --- Joseph Cartwright: The kinematic evolution of the Coffee Soil Fault / Geological Society, London, Special Publications, 56:29-40, doi:10.1144/GSL.SP.1991.056.01.03 --- N. J. Kusznir, G. Marsden, and S. S. Egan: A flexural-cantilever simple-shear/pure-shear model of continental lithosphere extension: applications to the Jeanne d’Arc Basin, Grand Banks and Viking Graben, North Sea / Geological Society, London, Special Publications, 56:41-60, doi:10.1144/GSL.SP.1991.056.01.04 --- Alan M. Roberts and Graham Yielding: Deformation around basin-margin faults in the North Sea/mid-Norway rift / Geological Society, London, Special Publications, 56:61-78, doi:10.1144/GSL.SP.1991.056.01.05 --- G. Yielding, M. E. Badley, and B. Freeman: Seismic reflections from normal faults in the northern North Sea / Geological Society, London, Special Publications, 56:79-89, doi:10.1144/GSL.SP.1991.056.01.06 --- Field-Based Studies --- M. P. Coward, R. Gillcrist, and B. Trudgill: Extensional structures and their tectonic inversion in the Western Alps / Geological Society, London, Special Publications, 56:93-112, doi:10.1144/GSL.SP.1991.056.01.07 --- Andreas G. Koestler and Werner U. Ehrmann: Description of brittle extensional features in chalk on the crest of a salt ridge (NW Germany) / Geological Society, London, Special Publications, 56:113-123, doi:10.1144/GSL.SP.1991.056.01.08 --- Steven Roberts and James Jackson: Active normal faulting in central Greece: an overview / Geological Society, London, Special Publications, 56:125-142, doi:10.1144/GSL.SP.1991.056.01.09 --- Rob Westaway: Continental extension on sets of parallel faults: observational evidence and theoretical models / Geological Society, London, Special Publications, 56:143-169, doi:10.1144/GSL.SP.1991.056.01.10 --- Fault-Displacement Studies --- A. Beach and P. Trayner: The geometry of normal faults in a sector of the offshore Nile Delta, Egypt / Geological Society, London, Special Publications, 56:173-182, doi:10.1144/GSL.SP.1991.056.01.11 --- T. J. Chapman and A. W. Meneilly: The displacement patterns associated with a reverse-reactivated, normal growth fault / Geological Society, London, Special Publications, 56:183-191, doi:10.1144/GSL.SP.1991.056.01.12 --- John J. Walsh and Juan Watterson: Geometric and kinematic coherence and scale effects in normal fault systems / Geological Society, London, Special Publications, 56:193-203, doi:10.1144/GSL.SP.1991.056.01.13 --- Analogue-Modelling and Section-Balancing --- G. Dresen, U. Gwildis, and Th. Kluegel: Numerical and analogue modelling of normal fault geometry / Geological Society, London, Special Publications, 56:207-217, doi:10.1144/GSL.SP.1991.056.01.14 --- Robert W. Krantz: Normal fault geometry and fault reactivation in tectonic inversion experiments / Geological Society, London, Special Publications, 56:219-229, doi:10.1144/GSL.SP.1991.056.01.15 --- K. R. McClay, D. A. Waltham, A. D. Scott, and A. Abousetta: Physical and seismic modelling of listric normal fault geometries / Geological Society, London, Special Publications, 56:231-239, doi:10.1144/GSL.SP.1991.056.01.16 --- Bruno Vendeville: Mechanisms generating normal fault curvature: a review illustrated by physical models / Geological Society, London, Special Publications, 56:241-249, doi:10.1144/GSL.SP.1991.056.01.17 --- Nicky White and Graham Yielding: Calculating normal fault geometries at depth: theory and examples / Geological Society, London, Special Publications, 56:251-260, doi:10.1144/GSL.SP.1991.056.01.18
    Location: Reading room
    Location: Reading room
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 2
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science Ltd
    Plant pathology 52 (2003), S. 0 
    ISSN: 1365-3059
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: The sensitivity of a bioassay in detecting soil inoculum of Colletotrichum coccodes and Helminthosporium solani was examined using potato minitubers and microplants. Tests were conducted on soils which were collected from fields in which the interval after a previous potato crop differed, and which were also artificially infested with conidia or microsclerotia. For C. coccodes, determining plant infection based on the occurrence of infected roots after 9–12 weeks was a sensitive method for detecting and quantifying the amount of inoculum in soil. Infestations of less than 0·4 microsclerotia per g soil were detected in artificially infested soils. A semiselective medium, developed for isolating C. gloeosporioides from pepper, detected soil infestations by C. coccodes as low as nine conidia or one microsclerotium per g soil in artificially infested soil. For H. solani, infection on minitubers was a sensitive measure, with soil inoculum of fewer than 10 conidia per g soil being detected. Soil infestation could be quantified by assessing the percentage surface area of minitubers covered by sporulating lesions, which was strongly related to the amount of soil infestation. The results of these bioassay tests were compared with published results for real-time quantitative PCR assays on the same soils. The two methods were in good agreement in artificially infested soils, but the bioassay appeared to be more sensitive with naturally infested soils.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 228 (1970), S. 375-376 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Any mechanism which could cause live spermatozoa to migrate to the lower region in a velocity gradient could account for their behaviour in fluid streams. I have there-fore investigated the motion of bull sperm in horizontal glass tubes, 200-300 ptm in diameter, with a microscope arranged with its ...
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 223 (1969), S. 639-639 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The electrical current passing through a high and low resistance connected in series is practically independent of the value of the smaller resistance. Similarly, because the electrical conductivity of air (about 10-14 Q"1 m-1) is much smaller than that of the earth (10-6 to 102 Q-1 mr1) (ref. 2) ...
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 238 (1972), S. 223-225 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] At low sperm concentrations (〈 108?109 cm?3), when interactions between organisms are negligible, gravity produces two effects on each organism. First, there is the downward sedimentation velocity; my measurements on immobilized spermatozoa in normal semen show that this is about 0.3 µm ...
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 262 (1976), S. 493-494 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] When a brightly fluorescent chromosome inside a nucleus is examined under the ultraviolet microscope it appears as a bright spot against a less bright background which is produced by fluorescence from the other nuclear contents and from any unbound dye which may be present. The chromosome is ...
    Type of Medium: Electronic Resource
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  • 7
    Publication Date: 2016-07-06
    Description: GIANT API provides biomedical researchers programmatic access to tissue-specific and global networks in humans and model organisms, and associated tools, which includes functional re-prioritization of existing genome-wide association study (GWAS) data. Using tissue-specific interaction networks, researchers are able to predict relationships between genes specific to a tissue or cell lineage, identify the changing roles of genes across tissues and uncover disease-gene associations. Additionally, GIANT API enables computational tools like NetWAS, which leverages tissue-specific networks for re-prioritization of GWAS results. The web services covered by the API include 144 tissue-specific functional gene networks in human, global functional networks for human and six common model organisms and the NetWAS method. GIANT API conforms to the REST architecture, which makes it stateless, cacheable and highly scalable. It can be used by a diverse range of clients including web browsers, command terminals, programming languages and standalone apps for data analysis and visualization. The API is freely available for use at http://giant-api.princeton.edu .
    Print ISSN: 0305-1048
    Electronic ISSN: 1362-4962
    Topics: Biology
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  • 8
    Publication Date: 2015-02-13
    Description: Author(s): T. Alharbi, P. H. Regan, N. Mărginean, Zs. Podolyák, O. J. Roberts, A. M. Bruce, N. Alkhomashi, R. Britton, D. Bucurescu, D. Deleanu, D. Filipescu, D. Ghită, T. Glodariu, C. Mihai, K. Mulholland, R. Lica, R. Mărginean, M. Nakhostin, A. Negret, C. R. Nita, L. Stroe, T. Sava, C. Townsley, and N. V. Zamfir The half-lives of the I π =5 − and I π =7 − yrast states with E x =1978 keV and E x =2307 keV in the N=78 isotone 136 Ce, have been measured to be 496(23) ps and 270(24) ps, respectively, using the coincident fast-timing spectroscopy technique following population by a 124 Sn( 16 O,4n) fusion-evaporation reaction... [Phys. Rev. C 91, 027302] Published Thu Feb 12, 2015
    Keywords: Nuclear Structure
    Print ISSN: 0556-2813
    Electronic ISSN: 1089-490X
    Topics: Physics
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  • 9
    Publication Date: 2013-02-02
    Description: An integrated workflow has been devised for the investigation of deep-water rifted continental margins. At a margin this allows us to predict the crustal structure, the distribution of continental-lithosphere thinning and the location of the ocean–continent transition with a new degree of confidence. The workflow combines the analytical techniques of 2D or 3D gravity inversion, 2D or 3D flexural backstripping with reverse thermal subsidence modelling, upper-crustal fault analysis and rifted margin forward modelling. No one technique on its own can provide all of the required answers, nor can it provide answers without some degree of uncertainty. The use of a combination of techniques, however, provides answers to several different problems and, crucially, more confidence in these answers. The workflow provides direct information on the present-day geometry of rifted margins and leads towards a better understanding of the geodynamic evolution of these margins. It also provides information which can inform the exploration process by making predictions about crustal structure at the ocean–continent transition, the location of the continent–ocean boundary, stretching-factor, heat-flow magnitude and history, palaeobathymetric history and subsurface palaeostructure. Application of the workflow is illustrated here with reference to the continental margins of West India, Brazil, West Australia, Norway and Newfoundland–Iberia.
    Print ISSN: 1354-0793
    Topics: Chemistry and Pharmacology , Geosciences
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  • 10
    Publication Date: 2018
    Description: 〈p〉The crustal structure of the Equatorial Atlantic conjugate margins (South America and West Africa) has been investigated using 3D gravity anomaly inversion, which allows for (1) the elevated geothermal gradient of the lithosphere following rifting and break-up and (2) magmatic addition to the crust during rifting and break-up. It is therefore particularly suitable for the analysis of rifted margins and their associated ocean basins. Maps of crustal thickness and conjugate-margin stretching, derived from gravity anomaly inversion, are used to illustrate how the Equatorial Atlantic opened as a set of stepped rift-transform segments, rather than as a simple orthogonal rifted margin. The influence of the transform faults and associated oceanic fracture zones is particularly clear when the results of the gravity anomaly inversion are combined with a shaded-relief display of the free-air gravity anomaly. A set of crustal cross-sections has been extracted from the results of the gravity inversion along both equatorial margins. These illustrate the crustal structure of both rifted-margin segments and transform-margin segments. The maps and cross-sections are used to delineate crustal type on the margins as (1) inboard, entirely continental, (2) outboard, entirely oceanic and (3) the ocean–continent transition in between where mixed continental and magmatic crust is likely to be present. For a given parameterization of melt generation the amount of magmatic addition within the ocean–continent transition is predicted by the gravity inversion. One of the strengths of the gravity-inversion technique is that these predictions can be made in the absence of any other directly acquired data. On both margins anomalously thick crust is resolved close to a number of oceanic fracture zones. On the South American margin we believe that this thick crust is probably the result of post-break-up magmatism within what was originally normal-thickness oceanic crust. On the West African margin, however, three possible origins are discussed: (1) continental crust extended oceanwards along the fracture zones; (2) oceanic crust magmatically thickened at the fracture zones; and (3) oceanic crust thickened by transpression along the fracture zones. Gravity inversion alone cannot discriminate between these possibilities. The cross-sections also show that, while ‘normal thickness’ oceanic crust (〈i〉c.〈/i〉 7 km) predominates regionally, local areas of thinner (〈i〉c.〈/i〉 5 km) and thicker (〈i〉c.〈/i〉 10 km) oceanic crust are also present along both margins. Finally, using maps of crustal thickness and thinning factor as input to plate reconstructions, the regional palaeogeography of the Equatorial Atlantic during and after break-up is displayed at 10 Ma increments.〈/p〉 〈p〉〈b〉Supplementary material:〈/b〉 Detailed illustrations of the crustal-thickness mapping, the crustal cross-sections and the plate reconstructions are available at: 〈a href="https://doi.org/10.6084/m9.figshare.c.4031266.v1"〉https://doi.org/10.6084/m9.figshare.c.4031266.v1〈/a〉〈/p〉
    Print ISSN: 0375-6440
    Electronic ISSN: 2041-4927
    Topics: Geosciences
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