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  • 1
    Monograph available for loan
    Monograph available for loan
    London : The Geological Society
    Associated volumes
    Call number: 9/M 07.0332
    In: Geological Society special publication
    Description / Table of Contents: Contents: New techniques in sediment core analysis: an introduction, R G Rothwell and F R Rack .- The Eagle III BKA system, a novel sediment core X-ray fluorescence analyser with very high spatial resolution, M Haschke. - The AVAATECH XRF Core Scanner: technical description and applications to NE Atlantic sediments, T O Richter, S Van Der Gaast, R Koster, A Vaars, R Gieles, H C de Stigter, H de Haas and T C E van Weering . - ITRAX: description and evaluation of a new multi-function X-ray core scanner, I W Croudace, A Rindby and R G Rothwell. - A geochemical application of the ITRAX scanner to a sediment core containing eastern Mediterranean sapropel units, J Thomson, I W Croudace and R G Rothwell . - Turbidite emplacement on the southern Balearic Abyssal Plain (western Mediterranean Sea) during Marine Isotope Stages 1-3: an application of ITRAX XRF scanning of sediment cores to lithostratigraphic analysis, R G Rothwell, B Hoogakker, J Thomson, I W Croudace and M Frenz. - Colour logging as a tool in high-resolution palaeoceanography, M Rogerson, P P E Weaver, E J Rohling, L J Lourens, J W Murray and A Hayes . - Sediment colour analysis from digital images and correlation with sediment composition, A J Nederbragt, R B Dunbar, A T Osborn, A Palmer, J W Thurow and T Wagner . - Sediment mineralogy based on visible and near-infrared reflectance spectroscopy, R D Jarrard and M D Vanden Berg . - Applications of confocal macroscope microscope luminescence imaging to sediment cores, A C Ribes, F R Rack, G Tsintzouras, S Damaskinos and A E Dixon . - Pressure coring, logging and sub-sampling with the HYACINTH system, P J Schultheiss, T J G Francis, M Holland, J A Roberts, H Amann, Thjunjoto, R J Parkes, D Martin, M Rothfuss, F Tyunder, and P D Jackson . - On-site geological core analysis using a portable X-ray computed tomographic system, B M Freifeld, T J Kneafsey and F R Rack . - Nuclear magnetic resonance pore-scale investigation of permafrost and gas hydrate sediments, R L Kleinberg . - Quantitative magnetic resonance imaging methods for core analysis, Q Chen, F R Rack and B J Balcom . - Rapid non-contacting resistivity logging of core, P D Jackson, M A Lovell, J A Roberts, P J Schultheiss, D Gunn, R C Flint, A Wood, R Holmes and T Frederichs . - Logging-while-coring - new technology from the simultaneous recovery of downhole cores and geophysical measurements, D Goldberg, G Myers, G J Iturrino, K Grigar, T Pettigrew and S Mrozewski . - Integration of the stratigraphic aspects of the very large sea-floor databases using information processing, C Jenkins, J Flocks and M Kulp . - Core data stewardship: a long-term perspective, C J Moore and R E Habermann. - The Janus database: providing worldwide access to ODP and IODP data, R Mithal and D G Becker.
    Type of Medium: Monograph available for loan
    Pages: 266 S. , Ill., graph. Darst., Kt.
    ISBN: 1862392102 , 978-1-86239-210-6
    Series Statement: Geological Society special publication 267
    Classification:
    Sedimentology
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
    Call number: AWI G5-15-0050
    In: Developments in paleoenvironmental research
    Description / Table of Contents: Contents: 1 Micro-XRF Studies of Sediment Cores: A Perspective on Capability and Application in the Environmental Sciences / R. Guy Rothwell and Ian W. Croudace. - PART 1 MARINE STUDIES. - 2 Twenty Years of XRF Core Scanning Marine Sediments: What Do Geochemical Proxies Tell Us? / R. Guy Rothwell and Ian W. Croudace. - 3 Optimization of Itrax Core Scanner Measurement Conditions for Sediments from Submarine Mud Volcanoes / Isabel Rodríguez-Germade, Belén Rubio, Daniel Rey, Federico Vilas, Carmen F. López-Rodríguez, Maria Carmen Comasand Francisca Martínez-Ruiz. - 4 Use of Calibrated ITRAX XRF Data in DeterminingTurbidite Geochemistry and Provenance in Agadir Basin, Northwest African Passive Margin / James E. Hunt, Ian W. Croudace and Suzanne E. MacLachlan. - 5 Identification, Correlation and Origin of Multistage Landslide Events in Volcaniclastic Turbidites in the Moroccan Turbidite System / James E. Hunt, Russell B. Wynn and Ian W. Croudace. - 6 An Empirical Assessment of Variable Water Content and Grain-Size on X-Ray Fluorescence Core-Scanning Measurements of Deep Sea Sediments / Suzanne E. MacLachlan, James E. Hunt and Ian W. Croudace. - PART 2 LAKE AND RIVER STUDIES. - 7 Micro-XRF Core Scanning in Palaeolimnology: Recent Developments / Sarah J. Davies, Henry F. Lamb and Stephen J. Roberts. - 8 Micro-XRF Applications in Fluvial Sedimentary Environments of Britain and Ireland: Progress and Prospects / Jonathan N. Turner, Anna F. Jones, Paul A. Brewer, Mark G. Macklin and Sara M. Rassner. - 9 Estimation of Biogenic Silica Concentrations Using Scanning XRF: Insights from Studies of Lake Malawi Sediments / Erik T. Brown. - 10 Optimization of Itrax Core Scanner Protocols for the Micro X-Ray Fluorescence Analysis of Finely Laminated Sediment: A Case Study of Lacustrine Varved Sediment from the High Arctic / Stéphanie Cuven, Pierre Francus, Jean François Crémerand Francis Bérubé. - 11 Investigating the Use of Scanning X-Ray Fluorescence to Locate Cryptotephra in Minerogenic Lacustrine Sediment: Experimental Results / Nicholas L. Balascio, Pierre Francus, Raymond S. Bradley, Benjamin B. Schupack, Gifford H. Miller, Bjørn C. Kvisvik, Jostein Bakke and Thorvaldur Thordarson. - 12 Combined [My]-XRF and Microfacies Techniques for Lake Sediment Analyses / Peter Dulski, Achim Brauer and Clara Mangili. - 13 Experiences with XRF-Scanning of Long Sediment Records / Christian Ohlendorf, Volker Wennrich and Dirk Enters. - 14 Approaches to Water Content Correction and Calibration for [My]XRF Core Scanning: Comparing X-ray Scattering with Simple Regression of Elemental Concentrations / John F. Boyle, Richard C. Chiverrell and Dan Schillereff. - PART 3 ENVIRONMENTAL GEOCHEMISTRY AND FORENSIC APPLICATIONS. - 15 X-Ray Core Scanners as an Environmental Forensics Tool: A Case Study of Polluted Harbour Sediment (Augusta Bay, Sicily) / Ian W. Croudace, Elena Romano, Antonella Ausili, Luisa Bergamin and R. Guy Rothwell. - 16 Modern Pollution Signals in Sediments from Windermere, NW England, Determined by Micro-XRF and Lead Isotope Analysis / Helen Miller, Ian W. Croudace, Jonathan M. Bull, Carol J. Cotterill, Justin K. Dix and Rex N. Taylor. - 17 ITRAX Core Scanner Capabilities Combined with Other Geochemical and Radiochemical Techniques to Evaluate Environmental Changes in a Local Catchment, South Sydney, NSW, Australia / P. Gadd, H. Heijnis, C. Chagué-Goff, A. Zawadzki, D. Fierro, P. Atahan, Ian W. Croudace and J. Goralewski. - PART 4 TECHNOLOGICAL ASPECTS. - 18 A Geochemical Approach to Improve Radiocarbon-Based Age-Depth Models in Non-laminated Sediment Series / Fabien Arnaud and Sidonie Révillon. - 19 Limited Influence of Sediment Grain Size on Elemental XRFCore Scanner Measurements / Sébastien Bertrand, Konrad Hughen and Liviu Giosan. - 20 Standardization and Calibration of X-Radiographs Acquired with the ITRAX Core Scanner / Pierre Francus, Kinuyo Kanamaru and David Fortin. - 21 Prediction of Geochemical Composition from XRF Core Scanner Data: A New Multivariate Approach Including Automatic Selection of Calibration Samples and Quantification of Uncertainties / G. J. Weltje, M. R. Bloemsma, R. Tjallingii, D. Heslop, U. Röhl and Ian W. Croudace. - 22 Parameter Optimisation for the ITRAX Core Scanner / Stuart Jarvis, Ian W. Croudace and R. Guy Rothwell. - 23 UV-Spectral Luminescence Scanning: Technical Updates and Calibration Developments / Craig A. Grove, Alberto Rodriguez-Ramirez, Gila Merschel, Rik Tjallingii, Jens Zinke, Adriano Macia and Geert-Jan A. Brummer. - 24 An Inter-comparison of [My]XRF Scanning Analytical Methods for Lake Sediments / Daniel N. Schillereff, Richard C. Chiverrell, Ian W. Croudace and John F. Boyle. - 25 Analysis of Coal Cores Using Micro-XRF Scanning Techniques / Sarah J. Kelloway, Colin R. Ward, Christopher E. Marjo, Irene E. Wainwright and David R. Cohen. - 26 ItraxPlot: An Intuitive Flexible Program for Rapidly Visualising Itrax Data / Ian W. Croudace and R. Guy Rothwell. - PART 5 THE FUTURE OF NON-DESTRUCTIVE CORE SCANNING. - 27 Future Developments and Innovations in High-ResolutionCore Scanning / Ian W. Croudace and R. Guy Rothwell. - Index.
    Description / Table of Contents: This volume presents papers on the use of micro-XRF core scanners in palaeoenvironmental research. It contains a broad ranging view of instrument capability and points to future developments that will help contribute to higher precision elemental data and faster core analysis. Readers will find a diverse range of research by leading experts that have used micro-XRF core scanners in a wide range of scientific applications. The book includes specific application papers reporting on the use of XRF core scanners in a variety of marine, lacustrine, and pollution studies. In addition, coverage also examines practical aspects of core scanner usage, data optimisation, and data calibration and interpretation. In a little over a decade, micro-XRF sediment core scanners have made a substantive contribution to palaeoenvironmental research. Their impact is based on their ability to rapidly, non-destructively, and automatically scan sediment cores. Not only do they rapidly provide important proxy data without damaging samples, but they can obtain environmental data at decadal, annual, and even sub-annual scales. This volume will help both experienced and new users of these non-destructive core scanners take full advantage of one of the most powerful geochemical screening tools in the environmental scientist's toolbox
    Type of Medium: Monograph available for loan
    Pages: XXIX, 656 S. : Ill., graph. Darst., Kt.
    ISBN: 9789401798488
    Series Statement: Developments in paleoenvironmental research 17
    Branch Library: AWI Library
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  • 3
    ISSN: 1573-0581
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Long-range sidescan sonar (GLORIA) data over Porto and Vigo Seamounts collected in 1978 has been re-interpreted in the light of SEABEAM bathymetric surveys conducted in 1982. The application of quantitative bathymetric information enables the interpreter to allow for artefacts inherent in the GLORIA data and to separate topography-related primary backscattering variations on the sonographs from more subtle changes that result from textural, slope and outcrop effects. The distinctions are made easier when slant-range corrected GLORIA data are available. Use of the combined survey data to precisely locate seismic profiling tracks and to identify likely areas of outcrop has allowed refined geological maps of the seamounts to be drawn and regional fault trends detected. The overall outline of the seamounts appears strongly fault-controlled. Porto and Vigo Seamounts are made up of the same geological formations and have had a similar structural history since their uplift as continental fault blocks in the Late Cretaceous to Middle Eocene period. Ravines that dissect the presumably lithified scarps bounding the seamounts may be relict features but still appear to control sediment input to gulley and channel systems in the surrounding topography. Sedimentary ridges associated with the seamounts represent anomalously thick sequences of post-Eocene material and probably result from interaction of downslope sedimentary processes and contour-following boundary currents.
    Type of Medium: Electronic Resource
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  • 4
    Publication Date: 2007-10-08
    Description: The upper part (0-20 m) of a long piston core from the SE Balearic Abyssal Plain -- spanning the past 50 ka -- has been studied using the ITRAX micro-XRF core scanner to obtain downcore elemental profiles. The Ca/Fe ratio was found to be an effective parameter to distinguish between turbidites and pelagites, because turbidites generally have higher Fe contents and lower Ca contents compared with pelagic intervals. Beds that were obscure when visually logged could be identified as turbidites or pelagites on their geochemical characteristics, allowing more complete subdivision of the sequence into genetic units. The ITRAX XRF data also provide useful information on textural grading, bioturbative mixing, identification of geochemically distinctive marker beds, indications of differences in provenance, and confirm or query the presence of early arrivals during turbidite emplacement. A chronostratigraphic framework for the core based on accelerator mass spectrometry (AMS) radiocarbon dating and correlation with oxygen isotope stages of pelagic intervals in other cores (using calcium carbonate stratigraphy) was also established. This shows that turbidite emplacement on this part of the Balearic Abyssal Plain has been modulated strongly by climate and sea-level change, with turbidite emplacement most frequent during the early Holocene when the rate of post-glacial sea-level rise was greatest. Deposition of the coarsest (i.e. sand and silt-based) turbidites at the core site was restricted to the full and Late Glacial (11-25 ka). Turbidite emplacement during Oxygen Isotope Stage 3 was rare. Most of the turbidites at the site are distal, but some coarse-grained-based turbidites are characterized by higher Sr/Ca ratios (possibly indicating a higher aragonite content), higher Ca and lower Fe contents compared to other turbidites, and are interpreted as having a more proximal shelf source. Such turbidites are generally rare, however, and restricted to full Glacial and Younger Dryas time. There is little evidence for large-scale seismogenic turbidites (expected to be seen as randomly timed emplacement, seemingly independent of eustatic control) at the core site, despite proximity to the seismically active Algerian margin 100 km to the south. This suggests that seismogenic turbidites must largely bypass this part of the plain. Although the ITRAX core scanner provides a rapid and non-destructive means of characterizing downcore geochemical distributions in great detail, interpretation of the data requires caution and assessment from an informed standpoint. Analytical artefacts such as those caused by water or organic content, degree of compaction, grain-size and mineral effects, unevenness of the cut core surface and poor discrimination of closely spaced element XRF peaks need identification and elimination.
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  • 5
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    In:  Geological Society Special Publication 267: 51-63.
    Publication Date: 2007-10-08
    Description: A new automated multi-function core scanning instrument, named ITRAX, has been developed that records optical, radiographic and elemental variations from sediment half cores up to 1.8 m long at a resolution as fine as 200 {micro}m. An intense micro-X-ray beam focused through a flat capillary waveguide is used to irradiate samples to enable both X-radiography and X-ray fluorescence (XRF) analysis. Data are acquired incrementally by advancing a split core, via a programmable stepped motor drive, through the flat, rectangular-section X-ray beam. Traditional XRF determination of element composition in sediments provides high-quality data, but it takes a considerable time and normally consumes gram quantities of material that is often only available in limited quantities. The ITRAX core scanner non-destructively collects optical and X-radiographic images, and provides high-resolution elemental profiles that are invaluable for guiding sample selection for further (destructive) detailed sampling. This paper presents a description of the construction, characteristics and capabilities of the ITRAX system. High-resolution ITRAX data obtained from sediment cores are also presented and compared with results from traditional wavelength-dispersive XRF analysis at lower resolution. Finally, some recent technical developments linked to the second-generation ITRAX are presented.
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  • 6
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    In:  Geological Society Special Publication 267: 1-29.
    Publication Date: 2007-10-08
    Description: Marine sediment cores are the fundamental data source for information on seabed character, depositional history and environmental change. They provide raw data for a wide range of research including studies of global climate change, palaeoceanography, slope stability, oil exploration, pollution assessment and control, and sea-floor surveys for laying cables, pipelines and siting of sea-floor structures. During the last three decades, a varied suite of new technologies have been developed to analyse cores, often non-destructively, to produce high-quality, closely spaced, co-located downcore measurements, characterizing sediment physical properties, geochemistry and composition in unprecedented detail. Distributions of a variety of palaeoenvironmentally significant proxies can now be logged at decadal and, in some cases, even annual or subannual scales, allowing detailed insights into the history of climate and associated environmental change. These advances have had a profound effect on many aspects of the Earth Sciences, particularly palaeoceanography. In this paper, we review recent advances in analytical and logging technology, and their application to the analysis of sediment cores. Developments in providing access to core data and associated datasets, and data-mining technology, in order to integrate and interpret new and legacy datasets within the wider context of sea-floor studies, are also discussed. Despite the great advances in this field, however, challenges remain, particularly in the development of standard measurement and calibration methodologies and in the development of data analysis methods. New data visualization tools and techniques need to be developed to optimize the interpretation process and maximize scientific value. Amplified collaboration environments and tools are needed in order to capitalize on our analysis and interpretation capability of large, multi-parameter datasets. Sophisticated, yet simple to use, searchable Internet databases, with universal access and secure long-term funding, and data products resulting in user-defined data-mining query and display, so far pioneered in the USA and Australia, provide robust models for efficient and effective core data stewardship.
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  • 7
    Publication Date: 2002-01-01
    Description: The Late Pleistocene-Holocene (0-30 ka BP) allochthonous sedimentation in the Herodotus Basin of the eastern Mediterranean has been controlled, in part, by a combination of regional climatic change and eustatic sea-level fluctuation. A new series of radiocarbon dates, made on planktonic foraminifers and pteropod shells taken from the pelagic and hemipelagic intervals between individual turbidite units, has given bracketing dates for each major turbidity current event that deposited sand and mud on the Herodotus Basin plain. Two partly independent cycles are evident. Climate-induced cycles have lead to an alternation of periods of turbidites sourced from the Nile delta-fan system with those from the North African shelf and Anatolian rise. These correlate with pluvial and inter-pluvial climatic periods recognized in the Nile hinterland. Sea-level cycles have tended to focus turbidite emplacement, from whatever source, at periods of sea-level fall within the latest Wisconsin and sea-level rise from the Wisconsin-Holocene period. In addition to the Herodotus Basin Megaturbidite (HBM) described previously, six other beds with volumes in excess of 25 km3 and wide lateral extent across the basin can be termed megaturbidites. There is no simple sea-level or climate control on the timing of these events, so we must conclude that triggering and emplacement of megaturbidites is independent and variable.
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  • 8
  • 9
    Publication Date: 2002-01-01
    Print ISSN: 0305-8719
    Electronic ISSN: 2041-4927
    Topics: Geosciences
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  • 10
    Publication Date: 2006-01-01
    Print ISSN: 0305-8719
    Electronic ISSN: 2041-4927
    Topics: Geosciences
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