Search Results - "Triebold, Silke"

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  1. 1

    Rutile occurrence and trace element behavior in medium-grade metasedimentary rocks: example from the Erzgebirge, Germany by Luvizotto, George Luiz, Zack, Thomas, Triebold, Silke, von Eynatten, Hilmar

    Published in Mineralogy and petrology (01-12-2009)
    “…Metamorphic textures in medium-grade (~500–550°C) metasedimentary rocks from the Erzgebirge give evidence of prograde rutile crystallization from ilmenite…”
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    Journal Article
  2. 2

    Anorthite-calibrated backscattered electron profiles, trace elements, and growth textures in feldspars from the Teide–Pico Viejo volcanic complex (Tenerife) by Triebold, Silke, Kronz, Andreas, Wörner, Gerhard

    “…Magma chamber dynamics at the phonolitic to basanitic Teide–Pico Viejo volcanic complex on Tenerife, Canary Islands, have been investigated using feldspar…”
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    Journal Article
  3. 3

    A recipe for the use of rutile in sedimentary provenance analysis by Triebold, Silke, von Eynatten, Hilmar, Zack, Thomas

    Published in Sedimentary geology (30-12-2012)
    “…Rutile has received considerable attention in the last decade as a valuable petrogenetic indicator mineral. Based on both new and previously published data, we…”
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    Journal Article
  4. 4

    Deducing source rock lithology from detrital rutile geochemistry: An example from the Erzgebirge, Germany by Triebold, Silke, von Eynatten, Hilmar, Luvizotto, George Luiz, Zack, Thomas

    Published in Chemical geology (15-10-2007)
    “…This study evaluates the applicability of rutile trace element geochemistry to provenance studies. The study area is the Erzgebirge in eastern Germany, where…”
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    Journal Article
  5. 5

    Discrimination of TiO2 polymorphs in sedimentary and metamorphic rocks by Triebold, Silke, Luvizotto, George Luiz, Tolosana-Delgado, Raimon, Zack, Thomas, von Eynatten, Hilmar

    Published in Contributions to mineralogy and petrology (01-04-2011)
    “…Investigation by Raman spectroscopy of samples from different geological settings shows that the occurrence of TiO 2 polymorphs other than rutile can hardly be…”
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  6. 6