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  • 1
    Monograph available for loan
    Monograph available for loan
    An introduction to metamorphic petrology (1990)
    Essex : Longman
    Details Availability
    Call number: FHD 350
    Type of Medium: Monograph available for loan
    Pages: XII, 248 S.
    Edition: Repr.
    Series Statement: Longman Earth Science Series
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    An introduction to metamorphic petrology (1993)
    Essex : Longman Scientific & Technical
    Details Availability
    Call number: M 94.0664
    Type of Medium: Monograph available for loan
    Pages: xii, 248 S.
    ISBN: 0582300967
    Series Statement: Longman earth science series
    Classification:
    Petrology, Petrography
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 3
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    Frontiers in Geofluids : a celebration of 10 years of the journal Geofluids (2011)
    Chichester : Wiley-Blackwell
    Details
    Keywords: geofluids
    Description / Table of Contents: Frontiers in Geofluids is a collection of invited papers chosen to highlight recent developments in our understanding of geological fluids in different parts of the Earth, and published to mark the first ten years of publication of the journal Geofluids. The scope of the volume ranges from the fundamental properties of fluids and the phase relationships of fluids encountered in nature, to case studies of the role of fluids in natural processes. New developments in analytical and theoretical approaches to understanding fluid compositions, fluid properties, and geological fluid dynamics across a wide range of environments are included. A recurrent theme of research published in Geofluids is the way in which similar approaches can be applied to geological fluids in very different settings and this is reflected in the diverse range of applications of fluid studies that are included here. They include deep groundwater flow, hydrocarbons in faulted sedimentary basins, hydrothermal ores, and multiphase flow in mid-ocean ridge systems. Other topics covered are geothermal waters, crustal metamorphism, and fluids in magmatic systems. The book will be of great interest to researchers and students interested in crustal and mantle fluids of all sorts.
    Pages: Online-Ressource (XIII, 318 Seiten)
    ISBN: 9781444333305
    URL: http://onlinelibrary.wiley.com/doi/10.1111/gfl.2010.10.issue-1-2/issuetoc
    Language: English
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    E-BOOK
  • 4
    Electronic Resource
    Electronic Resource
    Citation analysis Democracy on the rocks (2000)
    [s.l.] : Macmillan Magazines Ltd.
    Nature 403 (2000), S. 373-373 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Arguably the simplest way to review the state of a subject is not to commission an article by an expert reviewer, but just to make a statistical summary of what is going on in that field. Democracy does not have the same standing as a scientific methodology as it does as a principle for ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/35000319
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    Paper (German National Licenses)
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  • 5
    Electronic Resource
    Electronic Resource
    How wet is the Earth's crust? (1994)
    [s.l.] : Nature Publishing Group
    Nature 371 (1994), S. 205-206 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] THE past twenty years have seen enormous progress in our understanding of the interior of our planet, but some very simple questions about the crust remain controversial. A key question, which has implications for our understanding of how plates deform, how ore deposits develop, and for deep waste ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/371205a0
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  • 6
    Electronic Resource
    Electronic Resource
    Rocks of rare refinement (1994)
    [s.l.] : Nature Publishing Group
    Nature 369 (1994), S. 17-17 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] THE array of natural processes that the geochemist works with includes some that are remarkably effective at taking scarce metals from the most unpromising starting materials — common silicate rocks or melts — and concentrating them up to form ore bodies. Nevertheless, a few of the ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/369017a0
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  • 7
    Electronic Resource
    Electronic Resource
    Quick shifts in plate motion (1991)
    [s.l.] : Nature Publishing Group
    Nature 354 (1991), S. 269-270 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] GEOLOGICAL processes have a reputation for grinding exceedingly slowly. Even rapid events such as earthquakes or volcanic eruptions are part of a continuum of catastrophes affecting a part of the Earth's crust over a long time. Sometimes, however, as illustrated by Goldfarb et al. on page 296 ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/354269a0
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  • 8
    Electronic Resource
    Electronic Resource
    The nature and significance of the mechanism of sillimanite growth in the Connemara schists, Ireland (1977)
    Springer
    Contributions to mineralogy and petrology 65 (1977), S. 53-58 
    Details
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract During prograde metamorphism of the Connemara pelites, sillimanite first develops in biotite immediately adjacent to, or replacing, garnet. In some rocks, breakdown of garnet+muscovite and staurolite +muscovite+quartz leads to the development of fibrolite pseudomorphs after garnet. The textures indicate a constant volume replacement of garnet with movement of Al from staurolite and muscovite in the matrix towards the few, widely scattered, garnet sites. The complex ionic reaction patterns are the result of the strong preference of sillimanite to grow on biotite that is replacing garnet, and this pattern of preferred nucleations is taken to indicate that the equilibrium conditions for the reaction were only overstepped by the minimum required for initial sillimanite nucleation. Chemical movements were controlled by the heterogeneous nucleation pattern, not by intrinsic properties of the moving species. In order for extensive reaction to occur under near-equilibrium conditions, the rate at which the total thermal reaction proceeded must have been controlled by the supply of heat to the rocks rather than by diffusion or local reaction steps.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00373570
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  • 9
    Electronic Resource
    Electronic Resource
    The early metamorphic history of the Haast Schists and related rocks of New Zealand (1982)
    Springer
    Contributions to mineralogy and petrology 81 (1982), S. 317-327 
    Details
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Rare but widespread relics of sodic amphibole occur in metabasites and metacherts of the Haast Schists and related Caples Terrane rocks. Present main-stage metamorphic assemblages are frequently chemically equivalent to earlier sodic amphibole bearing assemblages, indicating that these rocks underwent an earlier, higher P/Tmetamorphism prior to formation of the present pumpellyite-actinolite and greenschist facies assemblages. The earlier assemblages were stable during and after early isoclinal folding, but were replaced by the present moderate P/T assemblages prior to the last major fabric-forming deformation. The change in conditions was due to thermal relaxation, probably accompanied by uplift and erosion, and peak metamorphic temperatures were about 350–370° C in the pumpellyite-actinolite zone of the Caples Terrane and near 390° C in the greenschist facies chlorite zone near Queenstown. According to Henley (1975) these greenschist facies rocks attained a pressure of at least 6.4±0.4 kb during their history, but a pressure of 4.6±0.6 kb has been estimated for a chlorite zone rock from Middlemarch, and so the 6.4 kb estimate probably refers to the maximum pressure attained during the earlier, higher P/T metamorphism. Similar changes in ‘metamorphic facies series’ with time occur in some older and more complex metamorphic belts such as the Caledonides, and this study suggests that it may be possible to interpret particular elements in the metamorphic development of such belts in terms of specific circum-Pacific analogues.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00371686
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  • 10
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    Note: CO2-mineral dissolution experiments using a rocking autoclave and a novel titanium reaction cell (2014)
    American Institute of Physics
    Details
    Publication Date: 2014-08-01
    Print ISSN: 0034-6748
    Electronic ISSN: 1089-7623
    Topics: Electrical Engineering, Measurement and Control Technology , Physics
    Published by American Institute of Physics
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