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  1. No Access

    Article

    Geochemistry of phlogopite, diopside, calcite, anhydrite and apatite pegmatites and syenites of southern Madagascar: evidence for crustal silicocarbonatitic (CSC) melt formation in a Panafrican collisional tectonic setting

    The phlogopite, diopside, calcite, anhydrite and apatite pegmatites of Ampandrandava and Beraketa are examples for the many other pegmatites of similar silicocarbonatitic composition found in the Bekily and Be...

    G. Morteani, Y. A. Kostitsyn, H. A. Gilg in International Journal of Earth Sciences (2013)

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    Article

    The pink topaz-bearing calcite, quartz, white mica veins from Ghundao Hill (North West Frontier Province, Pakistan): K/Ar age, stable isotope and REE data

    In the area of the Ghundao Hill (Northern Frontier Province, Pakistan) an orange-yellow to cherry-red topaz is found in calcite, quartz, white mica veins crosscutting the schistosity of probably Silurian to De...

    G. Morteani, A. Voropaev in Mineralogy and Petrology (2007)

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    Article

    Geochemical and isotopic (Sr, C, O) data from the alkaline complex of Grønnedal-ĺka (South Greenland): evidence for unmixing and crustal contamination

    The alkaline intrusion of Grønnedal-ĺka (South Greenland) is the oldest of the ten major rift-related plutonic complexes of southern Greenland that intruded during the Gardar period between 1330 and 1150 Ma in...

    H. Taubald, G. Morteani, M. Satir in International Journal of Earth Sciences (2004)

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    Article

    Mineralogy and geochemistry of Al-phosphate and Al-borosilicate-bearing metaquartzites of the northern Serra do Espinhaço (State of Bahia, Brazil)

    The investigated Al-phosphate- and Al-borosilicate-bearing metaquartzite horizon belongs to the Middle Proterozoic Serra de Vereda member of the São Marcos Formation of the northern Espinhaço fold belt. Outcro...

    G. Morteani, D. Ackermand in Mineralogy and Petrology (2004)

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    Article

    Classification and mineralization potential of the pegmatites of the Eastern Brazilian Pegmatite Province

    The potential for Nb, Ta, Li, Sn-mineralization as well as for precious stones for the Eastern Brazilian Pegmatite Province (EBPP) has been evaluated on the basis of 530 K-feldspar and 550 muscovite major and...

    G. Morteani, C. Preinfalk, A. H. Horn in Mineralium Deposita (2000)

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    Article

    Fluid inclusion microthermometry and the P-T evolution of gold-bearing hydrothermal fluids in the Niuxinshan gold deposit, eastern Hebei province, NE China

    Niuxinshan is a typical example of the numerous mesothermal gold deposits formed during Mesozoic tectono-magmatic reactivation of the Archean North China Craton in eastern Hebei province. Gold occurs in quart...

    Y. Yao, G. Morteani, R. B. Trumbull in Mineralium Deposita (1999)

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    Article

    Experimental, geochemical, mineralogical and O-isotope constraints on the late-magmatic history of the Fichtelgebirge granites (Germany)

     Mineralogical, experimental, geochemical and stable-isotope data give evidence for an aqueous late-stage fluid which develops increasingly from the less to the more highly evolved granites of the Fichtelgebir...

    W. Irber, H.-J. Förster, L. Hecht, P. Möller, G. Morteani in Geologische Rundschau (1997)

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    Article

    Constraints on the origin of zonation of the granite complexes in the Fichtelgebirge (Germany and Czech Republic): evidence from a gravity and geochemical study

     Compositional zoning of granitic plutons is a common feature, but the spatial variation of zoning is rarely studied in detail. It is suggested that important additional information can emerge if the compositi...

    L. Hecht, J. L. Vigneresse, G. Morteani in Geologische Rundschau (1997)

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    Article

    Enclaves in the S-type granites of the Kösseine massif (Fichtelgebirge, Germany): implications for the origin of granites

     The Hercynian peraluminous granites of the Kösseine massif differ in composition and content of enclaves from the other granites of the Fichtelgebirge. They are garnet-, cordierite- and andalusite-bearing S-t...

    S. Schödlbauer, L. Hecht, A. Höhndorf, G. Morteani in Geologische Rundschau (1997)

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    Article

    Experimental determination of the upper stability of scorzalite, FeAl2[OH/PO4]2, and the occurrence of minerals with a composition intermediate between scorzalite and lazulite(ss) up to the conditions of the amphibolite facies

    The stability field of scorzalite (FeAl2[OH/PO4]2) was investigated in the P-T range from 487 to 684 °C and 0.1 to 0.3 GPa. in hydrothermal experiments. The oxygen fugacity was fixed by the Ni/NiO buffer. Scorzal...

    P. Schmid-Beurmann, G. Morteani, L. Cemič in Mineralogy and Petrology (1997)

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    Article

    Geochemical and petrographic studies of Ta mineralization in the Nuweibi albite granite complex, Eastern Desert, Egypt

    The Nuweibi albite granite is one of 14 known Sn-Ta-Nb bearing granitoids in the Eastern Desert region of Egypt. The granite is a highly leucocratic, albite-rich rock with accessory columbite-tantalite, cassi...

    H. Helba, R. B. Trumbull, G. Morteani, S. O. Khalil, A. Arslan in Mineralium Deposita (1997)

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    Chapter

    Mineral Economics, Mineralogy, Geochemistry and Structure of Gold Deposits: An Overview

    The desire for gold has dramatically influenced the history of man. Its price is clearly related to its reputation as a safe store of wealth, the fear of inflation and war increasing it markedly. Because gold ...

    G. Morteani in Prehistoric Gold in Europe (1995)

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    Chapter

    Coin Moulds and other Ceramic Material: A Key to Celtic Precious Metal Working

    Coin moulds from the Celtic oppidum of Manching together with fragments of precious metal melting hearths used there and some reference materials were studied by various scientific methods to determine the met...

    R. Gebhard, G. Lehrberger, G. Morteani, Ch. Raub in Prehistoric Gold in Europe (1995)

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    Article

    Biogenic and lithogenic magnetic minerals in Atlantic and Pacific deep sea sediments and their paleomagnetic significance

    Die Träger der Magnetisierung von Tiefseesedimenten wurden mineralogisch, elektronenmikroskopisch und gesteinsmagnetisch untersucht. Magnetische Eindomänen (SD) und Pseudo-Eindomänen (PSD) Partikel, die für ei...

    H. Vali, T. von Dobeneck, G. Amarantidis, O. Förster, G. Morteani in Geologische Rundschau (1989)

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    Chapter and Conference Paper

    Prospection for Niobium-Rich Alkaline Rocks

    Nb belongs to the fifth group of the periodic table of the elements. Its atomic number is 41, its atomic weight is 92.9046 and its electronegativity is 1.6. In a six-fold coordination its ionic radius is 0.64,...

    G. Morteani in Lanthanides, Tantalum and Niobium (1989)

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    Chapter and Conference Paper

    The Industrial Applications of Rare Earth Elements

    Rare earth elements are used in several high technology industrial products. Their presence in alloys, ceramic and glass compounds and in oxide compounds provide special material properties. In metallurgy, all...

    C. Preinfalk, G. Morteani in Lanthanides, Tantalum and Niobium (1989)

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    Chapter and Conference Paper

    Geochemical Evaluation of the Tantalum Potential of Pegmatites

    Besides alkali granites, granitic pegmatites with local Ta2O5 concentrations of up to 0.1 wt.% are the most important economic sources for tantalum. Pegmatites very often occur in large swarms scattered over a wi...

    G. Morteani, R. Gaupp in Lanthanides, Tantalum and Niobium (1989)

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    Chapter and Conference Paper

    The Bastnaesite-Fluorite-Barite Deposit of the Kizilcaören District, Eskisehir, Turkey

    There are about 100 minerals known to contain lanthanides in more than trace amounts. But there are only two of commercial importance, monazite, a mixed Th-REE-phosphate and bastnaesite, an REE-fluorocarbonate (M

    G. Morteani, M. Satir in Lanthanides, Tantalum and Niobium (1989)

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    Article

    Time calibration of a PT-path from the Western Tauern Window, Eastern Alps: the problem of closure temperatures

    New Hornblende K-Ar and 39Ar-40Ar and mica Rb-Sr and K-Ar ages are used to place specific timemarks on a well-constrained pressure-temperature path for the late Alpine metamorphism in the Western Tauern Window. A...

    F. v. Blanckenburg, I. M. Villa, H. Baur in Contributions to Mineralogy and Petrology (1989)

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    Article

    Im Gedenken an Bruno Sander

    G. Morteani, H. Zankl in Geologische Rundschau (1983)

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