Geophysical and structural pattern of the Knížecí Stolec pluton nad its host rocks in the south-western part of the Moldanubian Zone, Bohemian Massif
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F11%3A10111088" target="_blank" >RIV/00216208:11310/11:10111088 - isvavai.cz</a>
Result on the web
<a href="http://www.jgeosci.org/doi.php?ID=jgeosci.096" target="_blank" >http://www.jgeosci.org/doi.php?ID=jgeosci.096</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.3190/jgeosci.096" target="_blank" >10.3190/jgeosci.096</a>
Alternative languages
Result language
angličtina
Original language name
Geophysical and structural pattern of the Knížecí Stolec pluton nad its host rocks in the south-western part of the Moldanubian Zone, Bohemian Massif
Original language description
airborne magnetic and gamma-ray spectometric survey and ground gravity survey recently realized in the Šumava/Böhmerwald Region of the Moldanubin Unit supplied remarkable geophysical signatures of individual geological structures. The Knížecí Stolec durbachitic pluton appears as a body of high contents of natural radioactive elements (Th, U and K), of no magnetic anomalous response and of pronounced positive gravity anomaly.
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
2011
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Journal of Geosciences
ISSN
1802-6222
e-ISSN
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Volume of the periodical
56
Issue of the periodical within the volume
2
Country of publishing house
CZ - CZECH REPUBLIC
Number of pages
20
Pages from-to
143-162
UT code for WoS article
000298137600002
EID of the result in the Scopus database
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