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Wyszukujesz frazę "Polish zone" wg kryterium: Temat


Wyświetlanie 1-3 z 3
Tytuł:
The role of the day by day beach monitoring in shore transformation
Autorzy:
Wodzinowski, T.
Powiązania:
https://bibliotekanauki.pl/articles/1187368.pdf
Data publikacji:
2004
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
orthogonal photograms
shore zone
Polish Baltic Sea coast
Opis:
The new method of a detailed morphodynamic registration of sandy beaches has been presented. The digital oriented photograms have been taken from a stabilised point at least once a day. Occasionally also more often, for example every hour during a storm cycle. The analyses of the photograms are performed in digital mode using special computer software. This digital beach monitoring of the Polish Baltic coast was initiated in summer 2002. The test fields in Polanka Redłowska within Gdynia and Chłapowo near Władysławowo were selected. The beach areas of the length of about 200 m along the shore were registered there. Selected examples of short-term changes of the beach relief were presented. A range of spatiotemporal transformations related to different periods (hours, days, months etc.) was demonstrated.
Źródło:
Polish Geological Institute Special Papers; 2004, 11; 77-82
1507-9791
Pojawia się w:
Polish Geological Institute Special Papers
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Thermal lithosphere across the Trans-European Suture Zone in Poland
Autorzy:
Majorowicz, J. A.
Powiązania:
https://bibliotekanauki.pl/articles/2058766.pdf
Data publikacji:
2004
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Polish Basin
Trans-European Suture Zone
thermal lithosphere
heat flow
Opis:
Significant lateral variations of surface heat flow occur in the Polish Lowland area, ranging up to 30+/–10 mW/m2 across the transition from the East European Craton (EEC) and the northeastern part of the Teisseyre-Tornquist Zone (TTZ) to the accreted terranes in the south-west (Palaeozoic Platform) and up to 25 mW/m2 of change within the Trans-European Suture Zone (TESZ). Modelling of the crustal temperatures for the deep seismic profiles parallel to TESZ (P1, P5 and TTZ) and perpendicular to it (LT-7, P2, LT-2, P4, LT-4 and LT-5) shows evidence of extensive crustal-mantle warming (elevated mantle heat flow in the area between the Sudetes and the EEC). The EEC and the northern part of the TTZ have a much lower mantle heat contribution. Mantle heat flow variations are significant (approximately 20–40 mW/m2). Significant are also variations in thermal lithosphere thickness ranging from ca. 150–200 km in the craton and the northern part of the TTZ to 100–150 km (locally less than 100 km) in the accreted terranes to the south-west of the TTZ and in the central part of the TTZ. The TTZ is a thermally inhomogeneous zone.The thermal transition between the Palaeozoic Platform and the EEC is not a sharp one. Significant variations in the thickness of the thermal lithosphere do not follow major tectonic units of the crust.
Źródło:
Geological Quarterly; 2004, 48, 1; 1--14
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Architektura depozycyjna warstw magurskich w strefie Siar na południe od Gorlic (płaszczowina magurska, polskie Karpaty zewnętrzne)
Depositional architecture of the Magura Beds from the Siary zone, south of Gorlice (Magura Nappe, Polish Outer Carpathians)
Autorzy:
Warchoł, M.
Powiązania:
https://bibliotekanauki.pl/articles/2074525.pdf
Data publikacji:
2007
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
elementy architektoniczne
paleogen
system depozycyjny
płaszczowina magurska
strefa Siar
polskie Karpaty zewnętrzne
architectural element
depositional system
Magura Beds
Paleogene
Magura Basin
Siary zone
Polish Outer Carpathians
Opis:
Detailedanalysis of lithofacies and their distribution in the Magura Beds in 11 transects in the eastern part of the Siary zone, revealed 16 facies and 6 associations of genetically and spatially related facies. The facies spectrum evidences deposition from a variety of mass gravity processes and subordinately by hemipelagic rain. The facies associations reveal depositional patterns of submarine fans and include: channels, channel-levees, channel-lobe transitions, depositional lobes and slump bodies. Correlation results (9 sections) and facies distribution together with paleocurrent directions suggest that the deposition of this part of Magura Beds took place in a submarine ramp/apron hybrid setting fed from a multipoint source. The depositional pattern of the Magura Beds in the study area records a two-stage development, which began with the emplacement of a sand/mud-rich type system and was followed by a mud-dominated system.
Źródło:
Przegląd Geologiczny; 2007, 55, 7; 601-610
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-3 z 3

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