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  • 1
    ISSN: 0168-9002
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Physics
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Journal of materials science 32 (1997), S. 3753-3758 
    ISSN: 1573-4803
    Source: Springer Online Journal Archives 1860-2000
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Notes: Abstract Solid solutions in the lead-based relaxor system Pb(Mg1/3Nb2/3)O3–PbTiO3 were modified by minor substitutions of Ba in the Pb-site of the perovskite lattice. The modified compositions were calcined at 830°C for 3 h to yield fine-grained, single-phase perovskite materials. A small amount of excess MgO(0.05 wt%), which mostly served as a sintering aid, was added to the calcined batches and the resulting mixtures were sintered at temperatures between 1150 and 1250°C for periods ranging from 3 to 5 h. The substitutions of BaO for PbO in the perovskite solid solution lattice caused a progressive lowering of the Curie point with increasing BaO content. On average, the Curie point decreased by about 10 °C for each mole of BaO substituted for PbO. Among the various Ba-substituted solid solutions studied, the one with a nominal composition Pb0.99Ba0.01[(Mg1/3Nb2/3)0.9Ti0.1]O3 which has a Curie point located near 28 °C, exhibited excellent dielectric properties. On sintering at 1250°C for 3 h, this composition yielded a density near 96% of the theoretical density. The peak dielectric constant of the composition at 1 KHz was slightly higher than 22000, and the corresponding tan δ value was 1.5% with a specific resistivity of 2.5×1012 Ω cm-1.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Mineralogy and petrology 37 (1987), S. 267-291 
    ISSN: 1438-1168
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Zusammenfassung Hydrothermale Alterationen in Zusammenhang mit einer Goldvererzung eines differenzierten eisenreichen gabbroischen Sills im Chibougamaugebiet wurden untersucht, um den Umwandlungsmechanismus zu ermitteln. Die Goldvererzung in der Ost-West verlaufenden Scherzone ist eng mit Zonen intensiver Alteration verbunden. 4 deutlich unterscheidbare Alterationsfazics, die mit zunehmender Entfernung von der Vererzung auftreten, sind: Ankerit - Serizit - Pyrit/Ankerit - Fuchsit - Chlorit/Ankerit -Serizit - Chlorit und Chlorit - Kalzit - Magnetit. Detailierte mineralogische, petrographische und geochemische Untersuchungen zeigen, daß sich von der Vererzung weg der Eisengehalt im Chlorit, erhöht, gleichzeitig aber in Karbonaten verringert. Die hydrothermale Alteration ist auf eine einzige fluide Phase mit ursprünglich hohem CO2/ H2O-Verhältnis zurückzuführen. Vorherrschend waren zunächst reduzierende Reaktionen. Mit zunehmender Wechselwirkung zwischen Fluid und Gestein erniedrigte sich das CO2/H2O-Verhältnis und oxidierende Reaktionen nahmen zu.
    Notes: Summary The pattern of hydrothermal alteration associated with a gold prospect located within a differentiated iron-rich gabbro sill in the Chibougamau region has been investigated in order to establish the alteration mechanism. The gold mineralization, occurring in east-west trending shear zone, shows a close spatial relationship to zones of intense alteration. Ankerite-sericite-pyrite/ankerite-fuchsite-chlorite/ankerite-sericite-chlorite, and chlorite-calcite-magnetite form four distinct alteration facies which extend outward from the mineralized zones. Detailed mineralogical, petrological and chemical studies show that the iron content of chlorite increases whereas the iron content of the carbonate decreases from the mineralized zone outwards. The hydrothermal alteration pattern is shown to be derived from a single fluid with a high initial CO2/H2O ratio. At first, reducing reactions prevailed and, with progressive fluid-rock interaction, the CO2/H2O ratio was lowered and oxidation reactions dominated.
    Type of Medium: Electronic Resource
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  • 4
    ISSN: 0168-9002
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Physics
    Type of Medium: Electronic Resource
    Library Location Call Number Volume/Issue/Year Availability
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Mineralium deposita 15 (1980), S. 361-381 
    ISSN: 1432-1866
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Abstract Many sulphide concentrations occur in formations containing the same elements in a disseminated state. It is generally admitted that these elements may be mobilised and reconcentrated into open spaces. The same mechanism has been envisaged in cases where vein deposits are spatially separated from the rocks which acted as a reservoir for sulphur and metals. Knowing the isotopic composition of the sulphide from the veins as well as the physico-chemical conditions of deposition, the theoretical value of the sulphur isotopic composition of the reservoir can be calculated and this can be compared with the values of the sulphides from the different reservoirs in order to indicate the most likely source. A series of isotopic analyses were untertaken on the sulphides from Henderson and Campbell Chibougamau Main Mines. These two deposits belong to the Cu-Au type of mineralisation associated with shear zones within the Lac Doré Complex. The mean isotopic composition of pyrite at Henderson is −2.9‰ which is close to the mean values measured at Campbell Chibougamau Main Mine (−2.8‰). The mean value of the chalcopyrite from the Henderson Mine is −3.2‰. Different possibilities concerning the provencance of sulphur are discussed. Based on existing thermodynamic model and on a set of new isotopic datas (pyrite and chalcopyrite) from volcanogenic mineralisation, it is possible to conclude that measured values correspond to mobilised volcanogenic sulfur.
    Notes: Résumé Beaucoup de minéralisations sulfurées filoniennes sont encaissées dans des formations qui contiennent les mêmes éléments mais à l'état disséminé. En ce cas, on admet généralement que ces éléments ont été mobilisés et reconcentrés dans des structures tectoniques distensives. Le même mécanisme peut encore être envisagé quand de telles minéralisations sont spatialement éloignées des formations réservoirs de soufre et de métaux. Connaissant la composition isotopique des sulfures filoniens ainsi que les conditions physico-chimiques de leur dépôt il est possible de calculer la valeur théorique de la composition isotopique des sulfures du réservoir. Celle-ci peut alors être comparée aux compositions isotopiques effectives des sulfures provenant des différents réservoirs potentiels dans le but de déterminer quel est le réservoir de soufre et de métaux le plus probable. Une série d' analyses isotopiques a été entreprise sur les sulfures des minéralisations de Henderson et de Campbell Chibougamau Main Mine. Ces minéralisations du type Cu-Au sont en relation spatiale avec des zones de cisaillement développées dans le complexe du Lac Doré. La composition isotopique moyenne de la pyrite de Henderson vaut −2.9‰. Cette valeur est très proche de la moyenne des compositions isotopiques de la pyrite de Chibougamau Main Mine (−2.8‰). La composition isotopique moyenne de la chalcopyrite de Henderson est de −3.2‰. En se fondant sur le modèle thermodynamique proposé d'une part, sur les compositions isotopiques de la pyrite et de la chalcopyrite d'une minéralisation stratiforme encaissée dans le réservoir présumé d'autre part, il est possible de conclure que les sulfures des minéralisations filoniennes ont été remobilisés des formations volcano-sédimentaires.
    Type of Medium: Electronic Resource
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  • 6
    ISSN: 1432-1866
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The Chibougamau mining camp, a major gold producer, has so far produced a total of 1,050 mt of gold at an average grade of 1.85 g/tonne. In contrast to a general tendency to group the deposits as vein type with varying compositions, this paper demonstrates the strong influence of regional lithologic and tectonic evolution of the area on the gold mineralization patterns. A syn-volcanic period of mineralization comprises both the volcanogenic massive sulphide and disseminated mineralization, and the subsequent epithermal mineralization. The latter is also associated with evolving volcanic landforms and syn-volcanic intrusions. The emplacement of the typical Archean lode-gold deposits and later Cu-Au deposits of uncertain origin coincides with the syn-deformational (Kenoran) period. The spatial relationship between the east-west-trending shear zones and a north-east-trending fault system is shown to be a possible mechanism for generating added dilatancy during the gold mineralizing phase. A late-to-post Kenoran shear system controlled the emplacement of the last major phase of gold mineralization within a stratiform intrusion.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Journal of thermal analysis and calorimetry 9 (1976), S. 37-41 
    ISSN: 1572-8943
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology
    Description / Table of Contents: Résumé On a étudié les transformations polymorphiques de BaGeO3 par ATD et diffraction des rayons X et comparé les résultats avec ceux obtenus antérieurement. A 1100° C BaGeO3 subit une transformation de phase réversible de la forme hexagonale stable à basse température à la forme stable à moyenne température, de structure cristalline inconnue, qui se transforme réversiblement à 1200° C en une phase orthorhombique qui reste stable jusqu'à 1287° C. Au refroidissement, la forme stable à haute température peut être maintenue à l'état métastable à la température ambiante, mais elle se transforme à 900° C en la forme stable à basse température.
    Abstract: Zusammenfassung Polymorphe Umwandlungen von BaGeO3 wurden unter Anwendung der DTA- und Röntgendiffraktionsmethoden untersucht und die erhaltenen Angaben mit den früher veröffentlichten verglichen. Bei 1100° vollzieht sich eine reversible Phasentransformation der BaGeO3 von der hexagonalen Struktur bei niedrigen Temperaturen in eine Verbindung unbekannter Kristallstruktur bei mittleren Temperaturen, welche wiederum bei 1200° eine weitere reversible Umwandlung in eine orthorhombische Struktur erfuhr und sich bis zur Schmelztemperatur von 1287° als stabil erwies. Beim Abkühlen der Schmelze kann die Form bei hohen Temperaturen bei Zimmertemperatur in metastabilem Zustand erhalten bleiben, wird jedoch bei 900° in die Form bei niedrigen Temperaturen umgewandelt.
    Notes: Abstract Polymorphic transformations of BaGeO3 were investigated by DTA and X-ray diffraction methods and the data obtained were compared with those previously published. BaGeO3 undergoes a reversible phase transformation at 1100° from a low-temperature hexagonal polymorph to a medium-temperature polymorph having an unknown crystal structure, which undergoes a further reversible transformation at 1200° to a high-temperature orthorhombic polymorph found to be stable up to the melting temperature of 1287°. On cooling from the melt, the high-temperature form can be retained metastably at room temperature, but transforms to the low-temperature form at 900°.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Journal of materials science 14 (1979), S. 1744-1748 
    ISSN: 1573-4803
    Source: Springer Online Journal Archives 1860-2000
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Notes: Abstract Phase equilibria in the system BaO-GeO2 were studied using several complementary methods and a number of modifications made to the previously published phase diagram. The system contains four compounds, Ba3GeO5, Ba2GeO4, BaGeO3 and BaGe4O9. Evidence is presented to show that the previously reported compounds Ba3Ge207 and BaGe19O39 do not exist. Four invariant points were established in the system and defined as simple eutectic. A revised phase diagram showing the solid-liquid equilibria existing between the various phases is presented.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Journal of materials science 15 (1980), S. 521-522 
    ISSN: 1573-4803
    Source: Springer Online Journal Archives 1860-2000
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Journal of materials science 15 (1980), S. 262-263 
    ISSN: 1573-4803
    Source: Springer Online Journal Archives 1860-2000
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Type of Medium: Electronic Resource
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