Lower Badenian deposits of the Carpathian Foredeep on the locality Ptení
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F18%3A00105923" target="_blank" >RIV/00216224:14310/18:00105923 - isvavai.cz</a>
Result on the web
<a href="http://dx.doi.org/10.5817/GVMS2018-1-2-28" target="_blank" >http://dx.doi.org/10.5817/GVMS2018-1-2-28</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.5817/GVMS2018-1-2-28" target="_blank" >10.5817/GVMS2018-1-2-28</a>
Alternative languages
Result language
čeština
Original language name
SPODNOBADENSKÉ SEDIMENTY KARPATSKÉ PŘEDHLUBNĚ NA LOKALITĚ PTENÍ
Original language description
Neogene deposits of the Carpathian Foredeep were studied newly in the sedimentary succession from the drill hole Ptení 1. Three identified facies associations represent deposits of fluvio-deltaic, nearshore and open marine environments. The facies associations are organized into two upward deepening and upward fining cycles which are interpreted as transgressive-regressive cycles. Source area was located in the adjacent geological units with strong dominance of Culmian rocks. The source area was relative stable, material was buried relative rapidly with low role of its reworking. The studied deposits are connected with filling of a distal palaeovalley formed on the foreland plate and oriented oblique to the main basin axis.
Czech name
SPODNOBADENSKÉ SEDIMENTY KARPATSKÉ PŘEDHLUBNĚ NA LOKALITĚ PTENÍ
Czech description
Neogene deposits of the Carpathian Foredeep were studied newly in the sedimentary succession from the drill hole Ptení 1. Three identified facies associations represent deposits of fluvio-deltaic, nearshore and open marine environments. The facies associations are organized into two upward deepening and upward fining cycles which are interpreted as transgressive-regressive cycles. Source area was located in the adjacent geological units with strong dominance of Culmian rocks. The source area was relative stable, material was buried relative rapidly with low role of its reworking. The studied deposits are connected with filling of a distal palaeovalley formed on the foreland plate and oriented oblique to the main basin axis.
Classification
Type
J<sub>SC</sub> - Article in a specialist periodical, which is included in the SCOPUS database
CEP classification
—
OECD FORD branch
10505 - Geology
Result continuities
Project
—
Continuities
S - Specificky vyzkum na vysokych skolach
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 Slezsku
ISSN
1212-6209
e-ISSN
—
Volume of the periodical
25
Issue of the periodical within the volume
1-2
Country of publishing house
CZ - CZECH REPUBLIC
Number of pages
6
Pages from-to
28-33
UT code for WoS article
—
EID of the result in the Scopus database
2-s2.0-85060114302