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Wyszukujesz frazę "Królikowski, C." wg kryterium: Autor


Wyświetlanie 1-3 z 3
Tytuł:
Crustal-scale complexity of the contact zone between the Palaeozoic Platform and the East European Craton in the NWPoland
Autorzy:
Królikowski, C.
Powiązania:
https://bibliotekanauki.pl/articles/2058936.pdf
Data publikacji:
2006
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
edge of the craton
seismic cross-sections
magnetic anomalies
geothermal field
Opis:
Hypotheses on the trace and nature of the SW margin of the East European Craton (EEC) are reviewed. As new geophysical data was acquired, the location of the EEC margin was repeatedly revised.Magnetic anomalies associated with the SWpart of the EEC and their relationship with the contact zone between the EEC and the Palaeozoic Platform are described. Based on an analysis of magnetic anomalies, seismic cross-sections, the LT-7, P1, P2 and P4 wide-angle reflection and refraction profiles, and the results of recent geothermal modeling, the geometry of the contact zone between the EEC and the Palaeozoic Platform in NW Poland has been redefined. Three important boundaries are distinguished, namely the Teisseyre-Tornquist Line marking the SW limit of the EEC at upper and middle crustal levels, the SW margin of the West Pomeranian Magnetic Anomaly that delimits the NE extension of the reversely magnetised lower crust of the Palaeozoic Platform, and the SWtermination of the high velocity lower crust of the EEC. These boundaries and their characteristics reflect the tectonic complexity of the SW margin of the EEC in its Polish sector.
Źródło:
Geological Quarterly; 2006, 50, 1; 33-42
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Gęstość objętościowa pokrywy osadowej na Lubelszczyźnie
Bulk density of sedimentary cover in the Lublin region
Autorzy:
Rosowiecka, O.
Królikowski, C.
Powiązania:
https://bibliotekanauki.pl/articles/2075166.pdf
Data publikacji:
2014
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
bulk density
laboratory data
estimated data
Lublin area
gęstość objętościowa
dane laboratoryjne
dane szacunkowe
Lubelszczyzna
Opis:
The paper presents the results of analyzes executed within the project carried out by the Polish Geological Institute – National Research Institute. The purpose was to develop a density model of sedimentary cover in, inter alia, the Lublin region, on the basis of archival laboratory measurements. The source material consisted primarily of a database of archival measurements made on samples taken from drill cores. Since the sampling was often fragmentary and missed long intervals of the section, it was necessary to develop a methodology for estimating the density of such blank intervals. Trend equations of density changes with depth were determined on the basis of existing measurements, which helped in the estimation. For each stratigraphic period, density weighted average was calculated, where the thickness of each depth interval was the weight. Juxtaposition of such average densities with the arithmetic means, with or without taking into account the estimated values, indicates the pros and cons of the methodology. The final step was to construct the following: density maps of each stratigraphic period, maps of density contrast at the top-bottom contact of two stratigraphic periods and density maps at selected depth levels.
Źródło:
Przegląd Geologiczny; 2014, 62, 9; 456--462
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Lithospheric structure across the Trans-European Suture Zone in NW Poland based on gravity data interpretation
Autorzy:
Królikowski, C.
Petecki, Z.
Powiązania:
https://bibliotekanauki.pl/articles/2059901.pdf
Data publikacji:
2002
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Trans-European Suture Zone
gravity anomalies
structural-density model
gravity stripping
lithospheric structure
Opis:
We provide an analysis of geophysical and geological data from the Baltic segment of the Trans-European Suture Zone (TESZ). The construction of structural and density maps of the Zechstein-Mesozoic-Cenozoic complex has allowed identification of anomalies of basement orgin. As a result of interpretation of these anomalies, major structural elements of the lithosphere have been characterised. According to gravity modelling the crustal structure is more complicated than shown on velocity model along refraction and wide-angle reflection profile LT-7. Long-wavelength anomalies have been modelled in terms of lateral heterogeneity within the lower crust and upper mantle. In order to achieve a match between the observed and calculated gravity effects, it was necessary to assume dense upper mantle beneath the TESZ. Gravity data also indicate the presence of high-density bodies in the upper crust, and a complex transitional zone between crust and upper mantle in the TESZ.
Źródło:
Geological Quarterly; 2002, 46, 3; 235-246
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-3 z 3

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