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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Naturwissenschaften 65 (1978), S. 652-653 
    ISSN: 1432-1904
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Chemistry and Pharmacology , Natural Sciences in General
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1432-0711
    Keywords: Urogenital tract ; Immunization ; Secretory antibodies ; Influenza vaccine
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Summary In order to investigate the possible stimulation of antibodies in the genital tract by immunization female NMRI-mice were given orally a live influenca vaccine (A/PR/8/34, HlNl) on two occasions which were 10 days apart. Subsequently, virus specific IgA antibodies measured by an enzyme immunoassay in homogenates of urinary bladder, uterus and vagina and also in uterine washings. Specific IgA antibodies were not detectable in the sera of immunized mice. The high IgA titer in uterine washings, and in the homogenates suggests enhancement by vaccine of IgA antibody production in the genital tract.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    International journal of earth sciences 84 (1995), S. 831-842 
    ISSN: 1437-3262
    Keywords: Austroalpine Crystalline Complex ; Tertiary mineralization ; Hydrothermal veins ; Stable isotope analyses ; Microthermometry
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The specularite deposit at Waldenstein is an epigenetic replacement/vein-type hematite mineralization with distinct alteration zones. It is situated in highly metamorphosed schists and, gneisses of the Koralm Crystalline Complex. Sericitization and chloritization are strictly bound to this alteration and occur within a few meters of the hematite veins. Radiometric dating of the sericitization and the implicity of the mineralization yield a Middle Eocene age. Petrographic evidence proves an early, relatively reduced paragenesis (magnetite, ilmenite) being partly replaced by hematite and chlorite during the main phase of ore formation. Fluid inclusion and stable isotope investigations indicate that formation temperatures were approximately 300°C during the main stage and decreased to 200°C in the latest stage of the hydrothermal event. The H-isotope compositions of chlorites and of fluid inclusions in quartz indicate the influence of seawater. This also explains the high salinities determined by fluid inclusion studies (20–30% NaCl equiv.). According to the genetic model presented in this paper the hydrothermal activity started when the deformation accompanying the uplift of the Koralm Crystalline Complex passed from a ductile to brittle regime (Middle Eocene). The brittle faults acted as channelways for rising, deep fluids, probably of metamorphic origin. Temperature differences between the different uplifting crustal segments supported fluid circulation. Precipitation of the ore occurred at shallow crustal levels where the hydraulic regime was dominated by seawater, and oxidation of the original reducing fluids took place.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Applicable algebra in engineering, communication and computing 7 (1996), S. 235-249 
    ISSN: 1432-0622
    Keywords: Standard bases ; Syzygies ; Computer algebra system ; Highest corner ; EcartMethod
    Source: Springer Online Journal Archives 1860-2000
    Topics: Computer Science , Mathematics , Technology
    Notes: Abstract We describe an implementation of a general standard basis algorithm, valid for any monomial ordering compatible with the natural semigroup structure. We concentrate on new strategies which have proved useful, in particular in the non-wellordering case. Moreover, we describe the first implementation of Schreyer's method to compute syzygies and compare it with other, more classical methods. Comparisons of the computing time of several examples in the system SINGULAR give hints as to which strategies should be used in different classes of examples.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Applicable algebra in engineering, communication and computing 7 (1996), S. 235-249 
    ISSN: 1432-0622
    Keywords: Key words Standard bases ; Syzygies ; Computer algebra system ; Highest corner ; EcartMethod.
    Source: Springer Online Journal Archives 1860-2000
    Topics: Computer Science , Mathematics , Technology
    Notes: Abstract  We describe an implementation of a general standard basis algorithm, valid for any monomial ordering compatible with the natural semigroup structure. We concentrate on new strategies which have proved useful, in particular in the non-wellordering case. Moreover, we describe the first implementation of Schreyer’s method to compute syzygies and compare it with other, more classical methods. Comparisons of the computing time of several examples in the system SINGULAR give hints as to which strategies should be used in different classes of examples.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Mineralium deposita 21 (1986), S. 228-233 
    ISSN: 1432-1866
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Résumé Basée sur les notes publiées sur l'évolution diagénétique des diapirs évaporitiques, et sur les données géologiques et les résultats préliminaires concernant la géochimie et les inclusions fluides, un nouveau modèle génétique est présenté pour les minerais sidéritiques métasomatiques du Maghreb. Dans l'ensemble, des saumures chaudes, issues des évaporites enfouies, et/ou des eaux derivées du gypse et d'autres sediments, semblent avoir réagi avec leurs roches hôtes durant la diagenèse précoce, devenant ainsi acides et réductrices. Ceci entraine la mise en solution et le transport du fer et d'autres cations. Ces saumures sont canalisées vers les parties apicales des diapirs, où elles déposent leurs solutés par processus métasomatiques dans les fractures du toit carbonaté. D'autres modes de dépôt, aussi bien par chute de température et de pression que par mélange avec les eaux de subsurface, sont marqués par des filons occasionels minéralisés en fer et très rarement en barytine et fluorine. Le modèle est tout à fait comparable à ce publié récemment sur l'origine des minéralisations à Pb-Zn de la même région. Il est évident que les deux groupes de minéralisation partagent des caractéristiques métallogéniques non seulement spatiotemporelles mais aussi causales.
    Notes: Abstract Based on published accounts of the diagenetic evolution of evaporite diapirs and geological, preliminary geochemical, and fluid inclusion data a new genetic model is presented for the North African metasomatic siderite deposits. Essentially, hot brines from the buried evaporites, gypsum-derived and/or other formation waters are thought to have reacted with their host rocks during early diagenesis becoming acid and reducing, thus allowing solution and transport of Fe and other cations. They were channeled toward the apical parts of diapirs where they deposited their solute by metasomatic processes in fractured roof carbonates. Other depositional modes by pressure and temperature drop as well as by mixing with near-surface waters are indicated by the occasional vein-type iron ores and very minor barite and fluorite. The model is quite comparable to recently published thoughts on the origin of the Pb-Zn deposits of the same area. Obviously, both groups of deposits share not only temporal and spatial but also causal metallogenic characteristics.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Molecular and cellular biochemistry 24 (1979), S. 128-128 
    ISSN: 1573-4919
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Chemistry and Pharmacology , Medicine
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Mineralium deposita 34 (1999), S. 614-629 
    ISSN: 1432-1866
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The two Alpine orogenic phases of the Eastern Alps, in the Cretaceous and in the Tertiary, were both accompanied by the formation of mineral deposits. However, subduction-related magmatic belts as well as the typical “Andean” ore deposits are missing. Therefore, the role of metamorphism in East Alpine metallogeny was tentatively explored for more than 60 y, although for a long time without tangible results. Microthermometric, geochemical and isotopic investigations of fluid inclusions from selected Alpine mineral deposits presented allow a preliminary confirmation of the involvement of metamorphic fluids in their origin. Deposits which were formed immediately after the first, Cretaceous orogeny, were produced at high pressures by fluids of very high salinity and high density, and with an isotopic composition of the water falling into the metamorphic field. These fluids are best understood as products of metamorphic de-volatilization of rocks of the subducted South Pennine domain. In contrast to this, the deposits formed after the second, Tertiary orogeny, originated at relatively low pressures from fluids with an appreciable content of CO2 and of low to moderate salinities. Isotopic compositions of this carbon indicate a deep crustal or even mantle source for CO2, while the water is isotopically more heterogeneous and may have mixed sources, both surficial and metamorphic. Tectonic control of these mineralizations is late-orogenic trans-tensional faulting, which exposed hot metamorphic rocks to fluid convection along brittle structures. These deposits conform best to the model of metamorphogenic metallogenesis by retrograde leaching, although ponded metamorphic fluids and mantle volatiles may also have been involved.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Geologische Rundschau 84 (1995), S. 831-842 
    ISSN: 0016-7835
    Keywords: Key words Austroalpine Crystalline Complex ; Tertiary mineralization ; Hydrothermal veins ; Stable isotope analyses ; Microthermometry
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  The specularite deposit at Waldenstein is an epigenetic replacement/vein-type hematite mineralization with distinct alteration zones. It is situated in highly metamorphosed schists and gneisses of the Koralm Crystalline Complex. Sericitization and chloritization are strictly bound to this alteration and occur within a few meters of the hematite veins. Radiometric dating of the sericitization and the implicity of the mineralization yield a Middle Eocene age. Petrographic evidence proves an early, relatively reduced paragenesis (magnetite, ilmenite) being partly replaced by hematite and chlorite during the main phase of ore formation. Fluid inclusion and stable isotope investigations indicate that formation temperatures were approximately 300  °C during the main stage and decreased to 200  °C in the latest stage of the hydrothermal event. The H-isotope compositions of chlorites and of fluid inclusions in quartz indicate the influence of seawater. This also explains the high salinities determined by fluid inclusion studies (20–30% NaCl equiv.). According to the genetic model presented in this paper the hydrothermal activity started when the deformation accompanying the uplift of the Koralm Crystalline Complex passed from a ductile to brittle regime (Middle Eocene). The brittle faults acted as channelways for rising, deep fluids, probably of metamorphic origin. Temperature differences between the different uplifting crustal segments supported fluid circulation. Precipitation of the ore occurred at shallow crustal levels where the hydraulic regime was dominated by seawater, and oxidation of the original reducing fluids took place.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Fresenius' Zeitschrift für analytische Chemie 48 (1909), S. 114-115 
    ISSN: 1618-2650
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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