| ŠEŠULKA, Vojtěch, Iva SEDLÁKOVÁ, Ondřej BÁBEK a Antonín PŘICHYSTAL. Identification of a buried Late Cenozoic maar-diatreme structure (North Moravia, Czech Republic). Geologica Carpathica. Veda, 2014, roč. 65, č. 6, s. 471-479. ISSN 1335-0552. |
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@article{1213753,
author = {Šešulka, Vojtěch and Sedláková, Iva and Bábek, Ondřej and Přichystal, Antonín},
article_number = {6},
keywords = {applied geophysics;ground magnetometry;gravimetry;electrical resistivity tomography;maar-diatreme;Plio-Pleistocene;Central European Volcanic Province;Bohemian Massif},
language = {eng},
issn = {1335-0552},
journal = {Geologica Carpathica},
title = {Identification of a buried Late Cenozoic maar-diatreme structure (North Moravia, Czech Republic)},
url = {http://www.geologicacarpathica.com/browse-journal/volumes/65-6/article-746/},
volume = {65},
year = {2014}
}
TY - JOUR
ID - 1213753
AU - Šešulka, Vojtěch - Sedláková, Iva - Bábek, Ondřej - Přichystal, Antonín
PY - 2014
TI - Identification of a buried Late Cenozoic maar-diatreme structure (North Moravia, Czech Republic)
JF - Geologica Carpathica
VL - 65
IS - 6
SP - 471-479
EP - 471-479
PB - Veda
SN - 13350552
KW - applied geophysics;ground magnetometry;gravimetry;electrical resistivity tomography;maar-diatreme;Plio-Pleistocene;Central European Volcanic Province;Bohemian Massif
UR - http://www.geologicacarpathica.com/browse-journal/volumes/65-6/article-746/
L2 - http://www.geologicacarpathica.com/browse-journal/volumes/65-6/article-746/
N2 - 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 of the 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-diatreme formation could be an indirect conse- quence of effusive activity of the nearby Velký Roudný volcano. The Lomnice structure is the first Plio-Pleistocene maar-diatreme ever described in North Moravia and Silesia.
ER -
ŠEŠULKA, Vojtěch, Iva SEDLÁKOVÁ, Ondřej BÁBEK a Antonín PŘICHYSTAL. Identification of a buried Late Cenozoic maar-diatreme structure (North Moravia, Czech Republic). \textit{Geologica Carpathica}. Veda, 2014, roč.~65, č.~6, s.~471-479. ISSN~1335-0552.
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