Detailed Information on Publication Record
2017
Quantitative allochem compositional analysis of Lochkovian-Pragian boundary sections in the Prague Basin (Czech Republic)
WEINEROVÁ, Hedvika, Karel HRON, Ondřej BÁBEK, Daniel ŠIMÍČEK, Jindřich HLADIL et. al.Basic information
Original name
Quantitative allochem compositional analysis of Lochkovian-Pragian boundary sections in the Prague Basin (Czech Republic)
Authors
WEINEROVÁ, Hedvika (203 Czech Republic, belonging to the institution), Karel HRON (203 Czech Republic), Ondřej BÁBEK (203 Czech Republic), Daniel ŠIMÍČEK (203 Czech Republic) and Jindřich HLADIL (203 Czech Republic)
Edition
Sedimentary Geology, Amsterdam, Elsevier Science, 2017, 0037-0738
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
10500 1.5. Earth and related environmental sciences
Country of publisher
Netherlands
Confidentiality degree
není předmětem státního či obchodního tajemství
References:
Impact factor
Impact factor: 2.575
RIV identification code
RIV/00216224:14310/17:00095376
Organization unit
Faculty of Science
UT WoS
000401597200004
Keywords in English
compositional analysis; carbonate petrography; multivariate statistics; log-ratio coordinates; Prague Basin; Lower Devonian
Tags
International impact, Reviewed
Změněno: 21/1/2020 09:38, Mgr. Marie Šípková, DiS.
Abstract
V originále
Quantitative allochem compositional trends across the Lochkovian-Pragian boundary Event were examined at three sections recording the proximal to more distal carbonate ramp environment of the Prague Basin. Multivariate statistical methods (principal component analysis, correspondence analysis, cluster analysis) of point-counted thin section data were used to reconstruct facies stacking patterns and sea-level history. Both the closed-nature allochem percentages and their centred log-ratio (clr) coordinates were used. Both these approaches allow for distinguishing of lowstand, transgressive and highstand system tracts within the Praha Formation, which show gradual transition from crinoid-dominated fades deposited above the storm wave base to dacryoconarid-dominated facies of deep-water environment below the storm wave base. Quantitative compositional data also indicate progradative-retrogradative trends in the macrolithologically monotonous shallow-water succession and enable its stratigraphic correlation with successions from deeper-water environments. Generally, the stratigraphic trends of the clr data are more sensitive to subtle changes in allochem composition in comparison to the results based on raw data. A heterozoan-dominated allochem association in shallow-water environments of the Praha Formation supports the carbonate ramp environment assumed by previous authors.
Links
GA14-18183S, research and development project |
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