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  • 1
    Call number: G 8045
    Type of Medium: Monograph available for loan
    Pages: X, 196 S. : graph. Darst.
    ISBN: 3540093176
    Series Statement: Hochschultext
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Contributions to mineralogy and petrology 11 (1965), S. 614-620 
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Some of the upper cretaceous sedimentary rocks near Regensburg, Germany, are rich in glauconite pellets of 63–200µ diameter. The clay fractions 〈 2µ ϕ of the same rocks are rich in glauconite-mica too. X-ray analysis, chemical analysis and petrographical tests show that, the glauconite pellets must be excrements of marine animals which took up glauconite-mica from sea-bottom. The glauconite materials from these rocks are 1M-micapolymorphs. A comparison of this glauconite with 1M-glauconites cited in literature by other authors shows close aggreement in K2O/MgO- and K2O/Fe2O3 ratios. Within the range of analytical errors the structure formulae of all these 1M-glauconites differ from one another only by the oxidation ratio of iron and — corresponding to this ratio — by the aluminum contents of the octahedral lattice layer. The differences of the 1M-glauconites in octahedral layer populations may due to different redox potentials during glauconite formation or to oxidation during rock diagenesis or rock weathering later on. In a similar manner 1Md-polymorphs of glauconite-mica may have developed from 1M-glauconite by oxidation of iron and corresponding removement of K+ and (H3O)+ ions from interlayer lattice positions.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Contributions to mineralogy and petrology 8 (1961), S. 69-83 
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Summary Chemical analyses are used by many authors to describe processes of soil development or laterite formation. In this paper some methods of balance calculations are compared by using samples of a laterite profile on granite from India as testing material. It should be proved which of these calculations of transported matter between the different layers are fitting to the mineral analyses of the laterite profile. Only the results of the method proposed byMashall by using an index-mineral as a base for comparison is confirmed by the mineral analyses. The method ofStreng differs from the above described calculation by using a chemical element as an index. FollowingStreng it is supposed that this element remains unchanged during the weathering processes. But certain chemical elements can be constituents of several minerals of a parent rock. During laterite formation all or almost all minerals of the original rock will be altered and the elements will be transported by weathering solutions. Therefore chemical elements do not serve as an index for balance calculations within a laterite complex. UsingGrossers method one cannot decide wether the abundance of a certain element is caused by accumulation of this element or by lost of other constituents and vice-versa. The use of the method developed byMillot u.Bonifas is not advisable except the structure of the original rock is preserved unaltered during laterite formation. This is not indicated in our case.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Contributions to mineralogy and petrology 6 (1959), S. 199-200 
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Contributions to mineralogy and petrology 5 (1956), S. 23-64 
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Zusammenfassung Es wurden zwei indische Lateritprofile untersucht. Die Lateritproben wurden soweit unverfestigt, in Korngrößenklassen zerlegt. Mit röntgenographischen. differentialthermoanalytischen und optischen Methoden wurde der Mineralbestand quantitativ bestimmt. Die Änderungen des Mineralbestandes und die Änderungen der Mineralverteilung wurde in den Lateritprofilen verfolgt. Die Lateritprofile sind auf quarzhaltigen Gesteinen, einem grobkörnigen Granit und einem feinkörnigen Quarz-Glimmer-Sandstein, entstanden. Als Ursache der Lateritbildung ist bei beiden Profilen die Verwitterung und Kaolinisierung des Ausgangsgesteins anzusehen. Bei dem Granit wurden die Feldspäte sowie die Hornblende und der Biotit, bei dem Sandstein wurde der Muskowit kaolinisiert. Der Quarz wurde mehr oder weniger stark korrodiert. Durch die Anreicherung von oxydischen und hydroxydischen Eisenmineralen in bestimmten Zonen der Verwitterungsprofile kam es zur Ausbildung typischer Lateritprofile mit konkretionsführenden bzw. pisolithischen Horizonten. Die Anreicherung von Eisenmineralen in diesen Horizonten ist durch Zufuhr von Eisen aus Verwittrungslösungen erfolgt. Das Eisen entstammt bei dem ersten Profil den verwitternden eisenhaltigen Mineralen des Granites, der Hornblende und dem Biotit. Bei dem zweiten Profil ist die Herkunft des Eisens aus verwitternden hämatitreichen Rindern des Sandsteines abzuleiten. An hydroxydischen Aluminiummineralen sind in beiden Lateritprofilen nur geringe Mengen Diaspur vorhanden. Auflösung von Kaolinit, Wanderung der Kaolinsubstanz und Neubildung von Fireclaymineral wurde in beiden Profilen nachgewiesen.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Contributions to mineralogy and petrology 10 (1964), S. 27-31 
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Zusammenfassung Der Bleigehalt des Hirschau-Schnaittenbacher Kaolins (ca. 0.1% Pb) wird aus dem Entstehungszyklus der kaohnhaltigen Buntsandstein-Arkosen hergeleitet. Die Bleierzlagerstätte von Freihung kann als örtliche Konzentration des Bleigehaltes der Trias-Arkosen gedeutet werden.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Contributions to mineralogy and petrology 12 (1966), S. 168-172 
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract An x-ray fluorescence spectrographic method is described for the determination of rubidium, strontium, barium and lead in kaolins and clays. The method is most usefull within a concentration range of 50–2000 p.p.m. Rb, Sr, Ba or Pb in the sample. Dried powder samples of kaolins resp. clays are compressed in a suitably shaped die and its x-ray radiations are compared with those of the same kaolins or clays to which small amounts of Rb, Sr, Ba or Pb had been added. A homogenous distribution of small amounts of these elements in kaolins and clays is obtained by precipitation of Pb, Ba and Sr as sulfate and Rb as Rb[B(C5H6)4] in a concentrated clay resp. kaolin suspension. The prepared suspensions are filtered (by membran-filters) and dried before compressing and x-ray measuring. The instrumental conditions were: Siemens x-ray spectrograph “Kristalloflex IV” fitted with a lithium fluoride analysing crystall, molybdenum-target x-ray tube (type AG Mo 61), 50 kV 30 m.amp. for measuring of the Sr Kα-, Rb Kα-, Pb L/gB-lines and 60 kV 36 m.amp. for measuring of the Ba Kα-line. The standard deviations were: ± 3 p.p.m. Rb for samples containing 25– 150 p.p.m. of Rb ± 6 p.p.m. Sr for samples containing 200– 400 p.p.m. of Sr ± 60 p.p.m. Ba for samples containing 1000–2000 p.p.m. of Ba ± 9 p.p.m. Pb for samples containing 250– 800 p.p.m. of Pb
    Type of Medium: Electronic Resource
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  • 8
    Publication Date: 1977-03-01
    Description: ZusammenfassungDie kristallchemischen Strukturformeln von 2:1-Schichtsilikaten werden unter Voraussetzung der idealen Struktur mit 22 negativen Ladungen von 10 Sauerstoffen und 2 Hydroxylgruppen berechnet. Für die Verteilung der 22 Kationenladungen auf Tetraeder-, Oktaeder- und Zwischenschichtpositionen werden unter Berücksichtigung der direkt gemessenen Zwischenschichtladungen (Lagaly & Weiss 1971) bzw. Kationenumtauschkapazitäten Voraussetzungen und Berechnungsregeln angegeben. Als Beispiele werden die Formeln eines Glaukonits und eines Nontronits berechnet.Die Verteilung der Kationenladungen in der Kristallstruktur von 2:1-Schichtsilikaten wird am besten in einem Dreiecksdiagramm mit den Ecken Pyrophyllit-Seladonit-Muskowit dargestellt. Jeder Punkt im Dreieck stellt die gesamte Kationenladung in der Formeleinheit gleich 22 dar. Es ist die Summe der Ladungen aus Tetraeder-, Oktaeder- und Zwischenschichtkationen.
    Print ISSN: 0009-8558
    Electronic ISSN: 1471-8030
    Topics: Geosciences
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