Magnetic fabric of granitic composite pluton of the Velka Fatra Mountains (Western Carpathians, Slovakia): A Variscan remnant within the Alpine edifice?
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F09%3A10001049" target="_blank" >RIV/00216208:11310/09:10001049 - isvavai.cz</a>
Result on the web
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DOI - Digital Object Identifier
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Alternative languages
Result language
angličtina
Original language name
Magnetic fabric of granitic composite pluton of the Velka Fatra Mountains (Western Carpathians, Slovakia): A Variscan remnant within the Alpine edifice?
Original language description
The AMS study has been performed on various types of the basement - Variscan granitic and surrounding - Mesozoic sedimentary rocks in the Vel'ka Fatra Mountains, Tatric Superunit of the Central Western Carpathians. The Vel'ka Fatra Mts. provides good opportunity for AMS study because of composite S-type and I-type granite character of pluton and clear relations to Mesozoic sedimentary rocks in the cover and nappe positions. The granitic massif consists of the three types of weakly magnetic peraluminousgranites (350 - 340 Ma in age), ranging from two-mica granites to biotite granodiorites in composition and carrying accessory monazite and ilmenite; whereby they resemble common S-type and/or Ilmenite Series granite.
Czech name
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Czech description
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Classification
Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DB - Geology and mineralogy
OECD FORD branch
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Result continuities
Project
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Continuities
Z - Vyzkumny zamer (s odkazem do CEZ)
Others
Publication year
2009
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
GEODINAMICA ACTA
ISSN
0985-3111
e-ISSN
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Volume of the periodical
22
Issue of the periodical within the volume
1-3
Country of publishing house
FR - FRANCE
Number of pages
17
Pages from-to
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UT code for WoS article
000272690200004
EID of the result in the Scopus database
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