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  • English  (1,977)
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  • 1
    Call number: MOP 44018 ; MOP B 15744 ; MOP B 15730
    Type of Medium: Monograph available for loan
    Pages: XII, 1337 S. : 486 Ill.
    Edition: 1. Aufl.
    ISBN: 387144149X
    Uniform Title: Poradnik in±zyniera, matematyka
    Language: German
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  • 2
    Call number: M 93.0242
    In: (DE-B103)41191, Special publications / the Geological Society, London
    Description / Table of Contents: Subsurface aspects of the ore-forming process can be described in terms of standard chemical transport parameters such as T-P gradients, mineral solubilities, solvent chemistry and volume, diffusion parameters and energy flow. These necessary factors are rather easily assessed by geochemical, isotopic and structural studies. If deposition is in the surface environment, a complex array of factors will determine the success of the natural concentration process and the chances of preservation of a deposit. Basically, most large-scale ore-forming processes involve large fluid volumes and energy sources. Many environments where these requirements are met, the modern ocean ridge and the subduction environment, are still not well understood. The need for remote-sensing techniques in the submarine environment is stressed.
    Type of Medium: Monograph available for loan
    Pages: VI, 188 Seiten , Illustrationen
    ISBN: 0900488336
    Series Statement: Special publications / the Geological Society, London 7
    Language: English
    Note: Articles Introductory remarks on the transport problem W. S. Fyfe https://doi.org/10.1144/GSL.SP.1977.007.01.01 Model of hydrothermal ore genesis J. W. Elder https://doi.org/10.1144/GSL.SP.1977.007.01.02 Identification of ore-deposition environment from trace-element geochemistry of associated igneous host rocks J. A. Pearce and G. H. Gale https://doi.org/10.1144/GSL.SP.1977.007.01.03 Identification of the origin of oreforming solutions by the use of stable isotopes S. M. F. Sheppard https://doi.org/10.1144/GSL.SP.1977.007.01.04 Hydrogen and oxygen isotope evidence for sea-water-hydrothermal alteration and ore deposition, Troodos complex, Cyprus T. H. E. Heaton and S. M. F. Sheppard https://doi.org/10.1144/GSL.SP.1977.007.01.05 Hydrodynamic model for the origin of the ophiolitic cupriferous pyrite ore deposits of Cyprus E. T. C. Spooner https://doi.org/10.1144/GSL.SP.1977.007.01.06 Origin and emplacement of ophiolites I. G. Gass https://doi.org/10.1144/GSL.SP.1977.007.01.07 Hydrothermal alteration of the basaltic lavas of the Troodos Ophiolite Complex associated with the formation of the massive sulphide deposits G. Constantinou https://doi.org/10.1144/GSL.SP.1977.007.01.08 Rare-earth element evidence for the genesis of the metalliferous sediments of Troodos, Cyprus A. H. F. Robertson and A. J. Fleet https://doi.org/10.1144/GSL.SP.1977.007.01.09 Modern submarine hydrothermal mineralization: examples from Santorini and the Red Sea D. S. Cronan, P. A. Smith, and R. D. Bignell https://doi.org/10.1144/GSL.SP.1977.007.01.10 Mineralization at destructive plate boundaries: a brief review M. S. Garson and A. H. G. Mitchell https://doi.org/10.1144/GSL.SP.1977.007.01.11 Porphyry copper deposits J. P. Hunt https://doi.org/10.1144/GSL.SP.1977.007.01.12 Metallic mineralization affiliated to subaerial volcanism: a review R. H. Sillitoe https://doi.org/10.1144/GSL.SP.1977.007.01.13 Igneous geology and the evolution of hydrothermal systems in some sub-volcanic tin deposits of Bolivia J. N. Grant, C. Halls, W. Avila, and G. Avila https://doi.org/10.1144/GSL.SP.1977.007.01.14 Occurrence, origin and significance of mechanically transported sulphide ores at Buchans, Newfoundland J. G. Thurlow https://doi.org/10.1144/GSL.SP.1977.007.01.15 Geological setting of the Skorovas orebody within the allochthonous volcanic stratigraphy of the Gjersvik Nappe, central Norway C. Halls, A. Reinsbakken, I. Ferriday, A. Haugen, and A. Rankin https://doi.org/10.1144/GSL.SP.1977.007.01.16 The Planes-San Antonio pyritic deposit of Rio Tinto, Spain: its nature, environment and genesis D. Williams, R. L. Stanton, and F. Rambaud https://doi.org/10.1144/GSL.SP.1977.007.01.17 Kuroko deposits: their geology, geochemistry and origin Takeo Sato https://doi.org/10.1144/GSL.SP.1977.007.01.18 Stable isotope studies on Bougainville and in Matupi Harbour, New Britain, Papua New Guinea J. H. Ford, D. C. Green, J. R. Hulston, I. H. Crick, and S. M. F. Sheppard https://doi.org/10.1144/GSL.SP.1977.007.01.19 Volcanogenic mineralization at Avoca, Co. Wicklow, Ireland, and its regional implications J. W. Platt https://doi.org/10.1144/GSL.SP.1977.007.01.20 Discussion https://doi.org/10.1144/GSL.SP.1977.007.01.21
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  • 3
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    Hannover [u.a.]: Bundesanstalt für Bodenforschung [u.a.]
    Associated volumes
    Call number: 93.0271/7
    In: Untersuchungen über Angebot und Nachfrage mineralischer Rohstoffe [Bericht]
    Language: German
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  • 4
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    Berlin [u.a.]: Springer
    Call number: 93.0162
    Pages: XII, 450 S.
    Language: English
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  • 5
    Call number: M 93.0224
    In: U.S. Geological Survey bulletin
    Type of Medium: Monograph available for loan
    Pages: 456 S.
    Edition: repr. with corr.
    Series Statement: Bulletin / U.S. Geological Survey 1452
    Language: English
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  • 6
    Call number: O 5071
    Type of Medium: Monograph available for loan
    Pages: 522 S. : 373 graph. Darst.
    Uniform Title: Analóg integrált áramkörök
    Language: German
    Location: Upper compact magazine
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  • 7
    Monograph available for loan
    Monograph available for loan
    Amsterdam _[u.a.]_ : Elsevier
    Associated volumes
    Call number: 11/M 93.0094/6
    In: Handbook of strata-bound and stratiform ore deposits ; part II
    Type of Medium: Monograph available for loan
    Pages: XVI, 585 S.
    ISBN: 0444414061
    Language: English
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  • 8
    Monograph available for loan
    Monograph available for loan
    Gotha : VEB Hermann Haack
    Call number: MOP 42610 / Mitte ; AWI G4-18-14336
    Type of Medium: Monograph available for loan
    Pages: 224 Seiten , Illustrationen
    Edition: 2. Auflage
    Language: German
    Note: Inhaltsverzeichnis: Vorwort. - 1. Wasserkreislauf, Wassermengen und Eigenschaften des Wassers. - 1.1. Herkunft des Wassers auf dem Festlande. - 1.2. Wassermengen auf der Erde. - 1.3. Wichtige Eigenschaften des Wassers. - 2. Flüsse. - 2.1. Fluß und Flußsystem. - 2.1.1. Bildung von Flüssen. - 2.1.2. Wichtige Begriffe aus der Flußkunde. - 2.1.3. Wichtige flußmorphametrische Begriffe. - 2.2. Gewässersystemarten. - 2.2.1. Normaltyp. - 2.2.2. Jungmoränentyp. - 2.2.3. Fossiler Inlandeisrandtyp im nördlichen Mitteleuropa. - 2.2.4. Trockengebietstyp. - 2.2.5. Karsttyp. - 2.3. Fluß und Relief. - 2.3.1. Fluß- und Talanlage. - 2.3.2. Durchbruchstäler. - 2.3.2.1. Epigenetische Durchbruchstalstrecken. - 2.3.2.2. Antezedente Durchbruchstalstrecken. - 2.3.3. Flußanzapfungen und Überschüttung von Wasserscheiden. - 2.3.4. Gewässer und Relief im Jungmoränenland. - 2.3.4.1. Phasen der Flußentwicklung im Jungmoränengebiet. - 2.3.4.2. Phasen der Seenentwicklung im Jungmoränengebiet. - 2.3.4.3. Ineinandergreifen beider Entwicklungsreihen. - 2.4. Abfluß und Schwankungen des Abflusses. - 2.4.1. Erfassung des Wasserstandes und Abflusses. - 2.4.1.1. Wasserstandsmessung. - 2.4.1.2. Abflußmessung. - 2.4.1.3. Abflußkurve und Abflußtafel. - 2.4.1.4. Hydrologisches Jahr und hydrologische Hauptzahlen. - 2.4.2. Abfluß und Abflußschwankungen. - 2.4.2.1. Hochwasser. - 2.4.2.2. Niedrigwasser. - 2.4.3. Eisbildung in Flüssen. - 2.4.4. Materialtransport. - 2.5. Riesenströme und Abfluß von den Kontinenten. - 2.5.1. Ordnung der Stromriesen nach der Lauflänge. - 2.5.2. Rangordnung der Riesenströme nach ihrer Einzugsgebiets- bzw. ihrer Niederschlagsgebietsgröße. - 2.5.3. Mittlerer jährlicher Abfluß der größten Ströme. - 2.5.4. Abflußmäßig größte Flüsse Europas. - 2.5.5. Mittlerer jährlicher Abfluß (MQ) und weitere Abflußdaten (MHQ, MNQ, HHQ und NNQ) von Flüssen der DDR. - 2.5.6. Abfluß von den Kontinenten. - 2.6. Abflußregime. - 2.6.1. Abflußregime und Regimefaktoren. - 2.6.2. Abflußregime nach M. Parde. - 2.6.2.1. Grundlagen der Klassifizierung nach M. Parde. - 2.6.2.2. Übersicht über die Klassifikation der Abflußregime nach M. Parde. - 2.6.2.3. Einige Bemerkungen zur Klassifikation von M. Parde und weiterführende Versuche. - 3. Seen. - 3.1. Seenverbreitung. - 3.1.1. Seen in ehemaligen und heutigen Inlandeis und Gletschergebieten. - 3.1.2. Seen in Trockengebieten. - 3.1.3. Seen in Vulkangebieten und Bereichen junger Erdkrustenbewegungen. - 3.1.4. Seen in Karst- und Auslaugungsgebieten. - 3.1.5. Seen in breiten Flußebenen. - 3.1.6. Seen an Ausgleichsküsten. - 3.2. Seebeckenentstehung. - 3.2.1. Glazialbecken. - 3.2.1.1. Seebecken im Bereich heutiger Gebirgsvergletscherung oder Inlandeisbedeckung. - 3.2.1.2. Seebecken im Abtragungsbereich letzteiszeitlicher Vergletscherung und Inlandeisbedeckung. - 3.2.1.3. Seebecken im Aufschüttungsbereich letzteiszeitlicher Inlandeisbedeckung und Vergletscherung. - 3.2.2. Bergsturz- und Erdrutschbecken. - 3.2.3. Tektonisch und vulkanisch angelegte Becken. - 3.2.4. Windwirkungsbecken. - 3.2.5. Lösungs- und Auslaugungsbecken, Abdämmung durch Sinterbildung. - 3.2.6. Becken fluvialen Ursprungs. - 3.2.7. Becken an Küsten. - 3.2.8. Becken pflanzlichen und tierischen Ursprungs. - 3.2.9. Anthropogen (durch die menschliche Gesellschaft) geschaffene Becken. - 3.2.10. Meteoritenfallbecken. - 3.3. Gestaltung, Verlandung und Form der Seebecken. - 3.4. Wasserhaushalt von Seen. - 3.5. Dichtemaximum und temperaturabhängige Schichtung des Wassers. - 3.6. Zirkulation und Stagnation. - 3.7. Thermische Seetypen. - 3.8. Biologische Seetypen. - 4. Unterirdisches Wasser (von Josef Saratka). - 4.1. Arten des unterirdischen Wassers. - 4.2. Hydrogeologische Eigenschaften der Gesteine. - 4.3. Bildung des unterirdischen Wassers. - 4.4. Zehrung des unterirdischen Wassers. - 4.5. Einige wichtige geohydrologische Begriffe. - 4.6. Grundwasserbewegung. - 4.7. Grundwasserstandsschwankungen. - 4.8. Unterirdisches Wasser in Klüften und Spalten, auf Schichtflächen und in Karsthohlräumen. - 4.9. Quellen und Grundwasserblänken. - 4.10. Mineralwässer- Säuerlinge - Thermalwässer. - 5. Gletscher. - 5.1. Inlandeis- und Gletscherverbreitung sowie Mächtigkeiten. - 5.2. Gletscherbildung. - 5.2.1. Schneegrenzen und Firnlinie. - 5.2.2. Metamorphose (Umwandlung) des Schnees in Gletschereis. - 5.3. Gletschertypen. - 5.3.1. Geomorphologische Einteilung der Gletscher. - 5.3.2. Gletschertypen - im Sinne einer einheitlichen Terminologie (nach H.-J. Schneider). - 5.3.3. Geophysikalische Einteilung der Gletscher (nach H. W. Ahlmann und M. Lagally). - 5.3.4. Einteilung der Gletscher nach dem dynamischen Zustand (nach H. W. Ahlmann). - 5.4. Gletscherbewegung und -gefüge. - 5.4.1. Gletscherbewegung. - 5.4.2. Gletschergefüge. - 5.5. Gletscherhaushalt und Gletscherschwankungen. - 5.5.1. Gletscherhaushalt. - 5.5.2. Gletscherschwankungen. - 6. Wasserkreislauf und Wasserhaushaltsbilanz. - 6.1. Erforschung von Wasserkreislauf und Wasserhaushaltsbilanz. - 6.2. Wichtige Begriffe. - 6.3. Wasserhaushaltsgleichung für die Erde. - 6.4. Erfassung der Wasserhaushaltselemente. - 6.4.1. Niederschlag auf die Landflächen der Erde (N L). - 6.4.2. Abfluß von den Landflächen der Erde (AL). - 6.4.3. Verdunstung von den Landflächen (VL). - 6.4.4. Verdunstung von den Meeresflächen (VM). - 6.4.5. Niederschlag auf die Meeresflächen (NM). - 6.5. Wasserkreislauf und Wasserhaushaltsbilanz der Erde. - 6.5.1. Wasserhaushaltsbilanzen für die Erde. - 6.5.2. Wasserkreislauf und Wasserhaushaltsbilanz der Erde. - Literaturauswahl.
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  • 9
    Call number: SR 90.0018(129) ; ZSP-183-129
    In: Bulletin / Grønlands Geologiske Undersøgelse, No. 129
    Description / Table of Contents: The Holocene stratigraphy in Scoresby Sund is based on climatic change as reflected by fluctuations in fjord and valley glaciers, immigration and extinction of marine molluscs, and the vegetation history recorded in pollen diagrams from five lakes. The histories are dated by C-14, and indirectly by emergence curves showing the patterns of isostatic uplift. From c. 10100-10400 to 9400 yr BP the major fjord glaciers showed oscillatory retreat with abundant moraine formation, the period of the Milne Land Moraines. The vegetation in the ice free areas was a sparse type of fell field vegetation but with thermophilous elements indicating temperatures similar to the present. From 9400 yr BP the fjord glaciers retreated rapidly in the narrow fjords, the few moraines formed are referred to the R0defjord stages and indicate topographically conditioned stillstands. At 8000 yr BP the low arctic Betula nana imigrated into the area, and in the period until 5000 yr BP dense dwarf shrub heath grew in areas where it is now absent. In the fjords the subarctic Mytilus edulis and Pecten islandica lived, suggesting a climate warmer than the present. From c. 5000 yr BP the dense dwarf shrub heath began to disappear in the coastal areas, and a 'poor' heath dominated by the high arctic Salix Arctica and Cassiope tetragona expanded. These two species, which are now extremely common, apparently did not grow in the area until c. 6000 yr BP. In lakes in the coastal area minerogenic sedimentation at c. 2800 yr BP, reflecting the general climatic deterioration.
    Type of Medium: Series available for loan
    Pages: 66 S. : Ill., graph. Darst., Kt. + 7 Beil.
    Series Statement: Bulletin / Grønlands Geologiske Undersøgelse 129
    Language: English
    Note: CONTENTS: Introduction. - Topography and hydrography. - Climate, glaciation, permafrost. - Notes on the scientific exploration of the area. - Sea level changes. - C-14 dates on shell material, corrections and errors. - Marine limits. - Emergence curves. - Marine faunas. - Glaciation history. - Pleistocene glaciation. - The Milne Land Moraines. - Glacial retreat, the Rødefjord stages. - Glacial readvance. - Climatic implications. - Comparison with other areas. - Pollen analytical investigations. - Field methods. - Lake sediments. - C-14 dates of lake sediments and rates of sedimentation. - Pollen preparation and calculation procedures. - Pollen identification. - Description of sites and pollen diagrams. - Notes on the present vegetation. - Discussion and reconstruction of vegetation types. - Plant immigration and climatic change. - Summary of the vegetation history. - Comparison with other areas. - General notes on the climatic development. - Acknowledgements. - References.
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  • 10
    Monograph available for loan
    Monograph available for loan
    Praha : Hydrometeorologický Ústav
    Associated volumes
    Call number: MOP 40270/2 / Mitte
    In: Meteorologická pozorování v Praze-Klementinu, II.
    Type of Medium: Monograph available for loan
    Pages: Seite 259-459
    Language: Czech , Russian , English
    Note: Contents Table 1 Daily records Table 2 Extreme temperatures Table 3 Montly means Table 4 Mean temperature in the years 1775-1975 Table 5 Daily means of extreme temperatures Table 6 Relative frequency of daily maximum temperature in months Table 7 Relative frequency of daily minimum temperature Table 8 Relative frequency of relative humidity Table 9 Relative frequency of pressure Table 10 Relative frequency of wind Table 11 Relative frequency of cloud amount Table 12 Relative frequency of daily rainfall Table 13 Statistical characteristics of daily observations Table 14 Monthly means in 5 years periods Table 15 Monthly means in 10 years periods Table 16 Monthly means in 50 years periods Table 17 Monthly means of statistical characteristics in the years 1776-1975 Table 18 Monthly means of statistical characteristics in 5 years periods Table 19 Monthly means of statistical characteristics in 10 years periods Table 20 Monthly means of statistical characteristics in 50 years periods Table 21 Mean daily temperature corresponding to the percent of the exceeding probability , In tschechischer, russischer und englischer Sprache
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