All

What are you looking for?

All
Projects
Results
Organizations

Quick search

  • Projects supported by TA ČR
  • Excellent projects
  • Projects with the highest public support
  • Current projects

Smart search

  • That is how I find a specific +word
  • That is how I leave the -word out of the results
  • “That is how I can find the whole phrase”

Trace element composition of quartz from the Variscan Altenberg?Teplice caldera (Krušné hory/Erzgebirge Mts, Czech Republic/Germany): Insights into the volcano-plutonic complex evolution

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F12%3A00382712" target="_blank" >RIV/67985831:_____/12:00382712 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216224:14310/12:00066249

  • Result on the web

    <a href="http://dx.doi.org/10.1016/j.chemgeo.2012.07.028" target="_blank" >http://dx.doi.org/10.1016/j.chemgeo.2012.07.028</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.chemgeo.2012.07.028" target="_blank" >10.1016/j.chemgeo.2012.07.028</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Trace element composition of quartz from the Variscan Altenberg?Teplice caldera (Krušné hory/Erzgebirge Mts, Czech Republic/Germany): Insights into the volcano-plutonic complex evolution

  • Original language description

    The internal structures and appropriate trace-element distribution of quartz grains were studied using laser ablation ICP-MS technique combined with a hot- and scanning cathodoluminiscence analysis. Studied Variscan magmatic suite is located in the Altenberg-Teplice Caldera (eastern Krušné Hory/Erzebirge - along the Czech Republic/Germany border) and is composed from co-magmatic volcanics (peraluminous basal rhyolite and associated dacite, overlying three units of subaluminous Teplice rhyolite and granite porphyry), and plutonic granites (two intrusions of A-type biotite and zinnwaldite granites). The trace-element distribution in granite prorphyry and rhyolite quartz shows distinct zonality in cathodoluminiscence images and chemical compositions: coreis poor in Ti, outer rim zones enriched with Ti, whereas Al records an opposite trend. In contrast, quartz from granites are very weakly zonated or homogenous. Based on the chemical composition of quartz and their zoning, we assume that

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    DD - Geochemistry

  • OECD FORD branch

Result continuities

  • Project

    <a href="/en/project/GAP210%2F10%2F1105" target="_blank" >GAP210/10/1105: Trace elements in igneous quartz ? frozen information about silicate melt evolution</a><br>

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2012

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Chemical Geology

  • ISSN

    0009-2541

  • e-ISSN

  • Volume of the periodical

    326/327

  • Issue of the periodical within the volume

    9 October

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    16

  • Pages from-to

    36-50

  • UT code for WoS article

    000309847400004

  • EID of the result in the Scopus database