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  • 1
    Monograph available for loan
    Monograph available for loan
    Fluids in the earth's crust : their significance in metamorphic, tectonic and chemical transport processes (1978)
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Details Availability
    Call number: 12021 ; 10/M 93.0073/1
    In: Developments in geochemistry
    Type of Medium: Monograph available for loan
    Pages: XVIII, 383 S.
    ISBN: 0444416366
    Series Statement: Developments in geochemistry 1
    Language: English
    Location: Upper compact magazine
    Location: Reading room
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Geochemistry of solids : an introduction (1964)
    New York, NY [u.a.] : McGraw-Hill
    Details Availability
    Call number: 11833
    Type of Medium: Monograph available for loan
    Pages: VII, 199 S. : graph. Darst.
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 3
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    (Table 1, page 204), Minor element concentrations in nodules of lake Ontario at Glenola, Bay of Quinte (1980)
    PANGAEA
    In:  Supplement to: Fyfe, William S; Kronberg, B I; Peirce, M; Leppard, G G (1980): Ferromanganese Nodules from Lake Ontario (Bay of Quinte): Minor Element Geochemistry. Journal of Great Lakes Research, 6(3), 203-209, https://doi.org/10.1016/S0380-1330(80)72101-9
    Details
    Publication Date: 2023-08-28
    Description: Spark source mass spectroscopy was used to analyze 61 elements in ten ferromanganese nodules found near Glenora in the Bay of Quinte at the eastern end of Lake Ontario. Most minor elements, including As, Pb, and Hg, have concentrations between 1-100 µg/g. F, S, Co, Zn, and La have concentrations in 100 µg/g range. Ba and Sr are present at levels of 1% and 0.1% respectively. Compared to similar measurements on nodules found in the Great Lakes and in other parts of the globe, values reported here are generally lower. Compared to their marine equivalents, lake nodules appear to be inferior scavengers of minor elements. Examination of all available data corroborates the postulate that marine biological material is an important source of minor elements found in oceanic nodules.
    Keywords: Arsenic; Barium; Bay of Quinte - Lake Ontario; Beryllium; Boron; Bromine; Cerium; Chlorine; Chromium; Cobalt; Copper; DEPTH, sediment/rock; Description; Dredge; DRG; Dysprosium; Fluorine; Gallium; Germanium; GLENORA_F; Iodine; Lanthanum; Lithium; Neodymium; Nickel; Niobium; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Praseodymium; Rubidium; Samarium; Scandium; Selenium; Spark Source Mass Spectrometer (JMS-01BM-2 JEOL); Strontium; Sulfur, total; Vanadium; Ytterbium; Yttrium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 32 data points
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  • 4
    facet.materialart.
    Unknown
    (Table 1) Peak intensity of minerals in ODP Hole 126-793B (1992)
    PANGAEA
    In:  Supplement to: Tazaki, Kazue; Fyfe, William S (1992): Diagenetic and hydrothermal mineral alteration observed in Izu-Bonin deep-sea sediments, Leg 126. In: Taylor, B; Fujioka, K; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 126, 101-112, https://doi.org/10.2973/odp.proc.sr.126.121.1992
    Details
    Publication Date: 2024-01-09
    Description: Sediments and rocks recovered during Ocean Drilling Program Leg 126 at Sites 792 and 793 in the Izu-Bonin forearc basin are described with a primary focus on clay mineralogy. Evidence for diagenetic hydrothermal alteration processes is present in the upper Oligocene to lower Miocene sediments at these sites. The vitric and pumiceous sand/sandstone and pumiceous gravel contain high concentrations of smectites, zeolites, and gypsum. Microscopic observations show that the volcanic glass and feldspars have been altered to smectites and zeolites. The authigenic mineral assemblages indicate that these minerals resulted from precipitation from circulating fluids, as well as from the alteration of glass and feldspar under temperature conditions that may have reached 200°-300°C. Mineral assemblages in microfractures display thermal gradients that possibly reflect cooling effects.
    Keywords: 126-793B; Analcime, Intensity; Calcite, intensity; Chabazite, Intensity; Clay minerals, Intensity; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Feldspar, Intensity; Heulandite, Intensity; Joides Resolution; Leg126; Lithologic unit/sequence; North Pacific Ocean; Ocean Drilling Program; ODP; Quartz, intensity; Sample code/label; Texture; X-ray diffraction (XRD)
    Type: Dataset
    Format: text/tab-separated-values, 77 data points
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  • 5
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    (Table 1) Chemical composition of green clays in sandstone from different depths at ODP Site 126-793B (1992)
    PANGAEA
    In:  Supplement to: Tazaki, Kazue; Fyfe, William S (1992): Microbial green marine clay from Izu-Bonin (west Pacific) deep-sea sediments. Chemical Geology, 102(1-4), 105-118, https://doi.org/10.1016/0009-2541(92)90149-Y
    Details
    Publication Date: 2024-01-09
    Description: Microbial green marine clays in deep-sea sediments were recovered from the Izu-Bonin fore-arc basin at Leg 126 of the Ocean Drilling Program (ODP) along the Bonin-Mariana trench. Green spherical materials and remnants of dead microbial cells of filamentous bacteria are abundant in the green marine clays. Organic carbon and graphite were found in the volcanic sandstone. Transmission electron microscope observations clearly show processes of graphite mineralization from low-crystallinity to well-crystallized graphite. However, X-ray photoelectron spectrochemical analyses (micro-ESCA) indicate that the green marine clays contain high C (1s) of microbial origin carbon, and COO, C---O, C---C and graphite structures. Fourier transform infrared spectra (FT-IR spectra) of the green spherules show peaks between glauconite and celadonite. X-ray powder diffraction data show the presence of smectite and 1.03-1.22-nm mica-clay minerals with abundant zeolites, which are hydrothermal alteration products. The results suggest that fossil remnants of graphite mineralized organisms, in particular filamentous bacteria, might play an important role in the formation of green marine clays.
    Keywords: 126-793B; Aluminium; Calcium; Carbon, total; Chlorine; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Iron; Joides Resolution; Leg126; North Pacific Ocean; Ocean Drilling Program; ODP; Oxygen, gas; Potassium; Sample code/label; Silicon; X-ray photoelectron spectrochemical analysis
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 6
    Electronic Resource
    Electronic Resource
    Mercury removal from water by iron sulfide minerals. An electron spectroscopy for chemical analysis (ESCA) study (1979)
    s.l. : American Chemical Society
    Environmental science & technology 13 (1979), S. 1142-1144 
    Details
    ISSN: 1520-5851
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Energy, Environment Protection, Nuclear Power Engineering
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1021/es60157a013
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  • 7
    Electronic Resource
    Electronic Resource
    Sorption of iodide on copper (1980)
    s.l. : American Chemical Society
    Environmental science & technology 14 (1980), S. 1106-1110 
    Details
    ISSN: 1520-5851
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Energy, Environment Protection, Nuclear Power Engineering
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1021/es60169a014
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  • 8
    Electronic Resource
    Electronic Resource
    Grain-boundary graphite in Kapuskasing gneisses and implications for lower-crustal conductivity (1992)
    [s.l.] : Nature Publishing Group
    Nature 357 (1992), S. 674-676 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The presence of brines at grain boundaries is the explanation favoured by most geophysicists to explain the electrical signature of many deep crusts of Phanerozoic age7'9. Once the fluids had leaked into the upper crust by disrupting an impermeable zone at the ductile-brittle transition level, ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/357674a0
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  • 9
    Electronic Resource
    Electronic Resource
    Carbon ratios in the Amazon (1991)
    [s.l.] : Nature Publishing Group
    Nature 354 (1991), S. 271-272 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] SIR - Despite the importance of the rainforests of the Amazon basin to greenhouse gas fluxes, terrestrial carbon storage and global biodiversity1'2, there remains no consensus as to the nature of vegetation present in the region during the Last Glacial Maximum (LGM) . Although there is broad ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/354271b0
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  • 10
    Electronic Resource
    Electronic Resource
    Thermodynamic stability and kinetics of perovskite dissolution (1981)
    [s.l.] : Nature Publishing Group
    Nature 289 (1981), S. 358-362 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Perovskite, a SYNROC host mineral for nuclear wastes, is thermodynamically unstable in natural waters and in association with common minerals. Leach experiments demonstrate that CaTiO3 (perovskite), SrTiO3 and BaTiO3 are as reactive as some silicate glasses below ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/289358a0
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