Identification of a buried Late Cenozoic maar-diatreme structure (North Moravia, Czech Republic)
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15310%2F14%3A33153005" target="_blank" >RIV/61989592:15310/14:33153005 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/00216224:14310/14:00077857
Výsledek na webu
<a href="http://www.geologicacarpathica.com/GeolCarp_Vol65_No6_471_479.html" target="_blank" >http://www.geologicacarpathica.com/GeolCarp_Vol65_No6_471_479.html</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1515/geoca-2015-0006" target="_blank" >10.1515/geoca-2015-0006</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Identification of a buried Late Cenozoic maar-diatreme structure (North Moravia, Czech Republic)
Popis výsledku v původním jazyce
The maar-diatreme volcanic structure in the vicinity of the village of Lomnice near the town of Bruntál (North Moravia, Czech Republic) has been investigated using a set of geophysical methods including ground magne- tometry, gravimetry and electrical resistivity tomography. The structure was detected by an aerial magnetic survey in the second half of the 20th century. Since its discovery only limited information about this buried structure has been available. The coherence of the magnetic anomaly of 190 nT and Bouguer anomaly of -4.7 mGal indicates a volcanic origin of the structure. The funnel-shaped maar-diatreme structure is filled with lacustrine clay and colluvium of Car- boniferous greywacke, which forms the country rock. The surface diameter ofthe structure is about 600 m, the depth is more than 400 m. The spatial association with other volcanic centers in the surroundings of the town of Bruntál infers the relative dating of the Lomnice maar. The phreatic eruption and maar-dia
Název v anglickém jazyce
Identification of a buried Late Cenozoic maar-diatreme structure (North Moravia, Czech Republic)
Popis výsledku anglicky
The maar-diatreme volcanic structure in the vicinity of the village of Lomnice near the town of Bruntál (North Moravia, Czech Republic) has been investigated using a set of geophysical methods including ground magne- tometry, gravimetry and electrical resistivity tomography. The structure was detected by an aerial magnetic survey in the second half of the 20th century. Since its discovery only limited information about this buried structure has been available. The coherence of the magnetic anomaly of 190 nT and Bouguer anomaly of -4.7 mGal indicates a volcanic origin of the structure. The funnel-shaped maar-diatreme structure is filled with lacustrine clay and colluvium of Car- boniferous greywacke, which forms the country rock. The surface diameter ofthe structure is about 600 m, the depth is more than 400 m. The spatial association with other volcanic centers in the surroundings of the town of Bruntál infers the relative dating of the Lomnice maar. The phreatic eruption and maar-dia
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DB - Geologie a mineralogie
OECD FORD obor
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Návaznosti výsledku
Projekt
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Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2014
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Geologica Carpathica
ISSN
1335-0552
e-ISSN
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Svazek periodika
65
Číslo periodika v rámci svazku
6
Stát vydavatele periodika
SK - Slovenská republika
Počet stran výsledku
9
Strana od-do
471-479
Kód UT WoS článku
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EID výsledku v databázi Scopus
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