Devonian sedimentary rocks tectonically incorporated into the Brno Massif, eastern margin of the Bohemian Massif
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F18%3A00106250" target="_blank" >RIV/00216224:14310/18:00106250 - isvavai.cz</a>
Result on the web
<a href="https://journals.muni.cz/gvms/article/view/9072" target="_blank" >https://journals.muni.cz/gvms/article/view/9072</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.5817/GVMS2018-1-2-92" target="_blank" >10.5817/GVMS2018-1-2-92</a>
Alternative languages
Result language
angličtina
Original language name
Devonian sedimentary rocks tectonically incorporated into the Brno Massif, eastern margin of the Bohemian Massif
Original language description
Th e Devonian clastic rocks in the northern vicinity of Brno are a segment of the north-south oriented Babí lom zone, cutting central part of the Brno Massif. Although the Devonian rocks form a seemingly isolated relict, the area of southern slope of Strážná hill (369 m a. s. l.) south of Lelekovice gives us key information for understanding the whole Babí lom zone structure: 1) Th e Devonian sediments are lithologically variable, with shale, siltstones, sandstones, and quartzitic conglomerates, which enables us to recognize bedding and younging. 2) Bedding changes its orientation: it is dipping towards the east in the west, vertical in the middle, and overturned with dip towards the west in the east. 3) Th e Devonian rocks are limited partially primarily with transgressive boundary (in the SW with relict of fossil weathering) and partially tectonically (in the E and NW). Th ese facts can be interpreted by the following explanation: 1) Th e Devonian beds form a recumbent fold, which is most likely an anticline with axial surface dipping towards the west. 2) Th e fold structure probably originated by dragging alongside a thrust fault and is a lower part of a tectonic sheet. 3) Th e Babí lom ridge may represent an upper part of the sheet. A segmentation of the structure is a result of subsequent brittle faulting.
Czech name
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Czech description
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Classification
Type
J<sub>SC</sub> - Article in a specialist periodical, which is included in the SCOPUS database
CEP classification
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OECD FORD branch
10505 - Geology
Result continuities
Project
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Continuities
S - Specificky vyzkum na vysokych skolach<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2018
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Geologické výzkumy na Moravě a ve Slezku
ISSN
1212-6209
e-ISSN
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Volume of the periodical
25
Issue of the periodical within the volume
1-2
Country of publishing house
CZ - CZECH REPUBLIC
Number of pages
5
Pages from-to
92-96
UT code for WoS article
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EID of the result in the Scopus database
2-s2.0-85060093784