Autor: Wysocka, S. - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: Metaloproteinazy macierzy - ich struktura oraz znaczenie
Matrix metalloproteinases - their structure and function
Autorzy:: Wysocka, A.
Gizinski, S.
Lechowski, R.
Powiązania:: https://bibliotekanauki.pl/articles/860510.pdf
Data publikacji:: 2014
Wydawca:: Krajowa Izba Lekarsko-Weterynaryjna
Tematy:: enzymy proteolityczne
metaloproteinazy macierzy
budowa
aktywacja
funkcje biologiczne
matrylizyny
kolagenaza
zelatynaza
stromelizyny
metaloproteinazy blonowe
Źródło:: Życie Weterynaryjne; 2014, 89, 03
0137-6810
Pojawia się w:: Życie Weterynaryjne
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 2.

Tytuł:: The usefulness of ground-penetrating radar images for the research of a large sand-bed braided river: case study from the Vistula River (central Poland)
Autorzy:: Lejzerowicz, A.
Kowalczyk, S.
Wysocka, A.
Powiązania:: https://bibliotekanauki.pl/articles/94393.pdf
Data publikacji:: 2014
Wydawca:: Uniwersytet im. Adama Mickiewicza w Poznaniu
Tematy:: sedimentary architecture
sand-bed braided river
lithofacies
ground-penetrating radar
radar facies
Vistula River
architektura sedymentacyjna
piaskodenna rzeka roztokowa
litofacje
georadar
Wisła
Opis:: Ground-penetrating radar (GPR) surveys and sedimentological outcrop analyses were combined in order to determine the reflection patterns and internal architecture of terrace deposits of the Vistula River at Kępa Zawadowska in the southern part of Warsaw (central Poland). The sedimentary analyses concerned the granulometric composition and lithofacies analysis. The 34 GPR profiles, which were obtained in two outcrops, using a Malå RAMAC/GPR system with 500-MHz and 250-MHz shielded antennas, were up to 100 m long. The most characteristic ground-penetrating radar profiles are presented; they show a high-resolution data set of radar facies. The GPR data suggest the presence of three geophysically different units, namely with high-angle inclined reflections (radar facies 1), with discontinuous undulating or trough-shaped reflections (radar facies 2), and with low-angle reflections (radar facies 3). The internal structure of the fluvial deposits was obtained by integration of the GPR and sedimentological data, which combination provides a more accurate visualisation of sedimentary units than do reconstructions that are based only on standard lithologic point data.
Źródło:: Geologos; 2014, 20, 1; 35-47
1426-8981
2080-6574
Pojawia się w:: Geologos
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 3.

Tytuł:: The origin and depositional architecture of Paleogene quartz-glauconite sands in the Lubartów area, eastern Poland
Autorzy:: Czuryłowicz, K.
Lejzerowicz, A.
Kowalczyk, S.
Wysocka, A.
Powiązania:: https://bibliotekanauki.pl/articles/2059959.pdf
Data publikacji:: 2014
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: littoral facies
syndepositional tectonics
extensional graben
sequence stratigraphy
ground penetrating radar
3D modelling
Opis:: The study uses quantitative methods to analyse the latest Bartonian to Early Rupelian sedimentary succession at the SE outskirts of the Polish Lowland Paleogene Basin, in the back-bulge zone of the Carpathian orogenorebulge. The vertical lithotype proportion diagrams from a large number of well logs are compiled to reveal the area’s sequence stratigraphy. Six sequences are recognized and correlated with 3rd-order eustatic sea level cycles. The basal sequence of type 1 is overlain by three sequences of type 2 and followed by a fifth sequence of type 1, whose depositional forced-regressive and lowstand systems tracts brought the main volume of quartz-glauconite sand to the study area. The study focuses further on the deposits of this fifth sequence, exposed and surveyed with GPR in the Nowodwór-Piaski sand pit. Their sedimentary facies analysis reveals the local spatial pattern of a wave-dominated and tidally-influenced sedimentation, supporting the earlier notions of a southern palaeoshoreline and a tectonically-controlled sedimentation.The analysis, aided by multidimensional GPR survey, indicates syndepositional development of a tectonic graben filled laterally by fault scarp-attached large sand bars and an axial action of tidal ebb currents. The bars were formed of shore-derived sand swept by littoral waves from the graben footwall areas. As the graben’s tectonic activity ceased, it became buried by the lowstand regressive sands overlain by gravelly foreshore deposits, most of which were later removed by the Pleistocene glacial erosion. A 3D model of the deposits in the Nowodwór-Piaski area is constructed on the basis of outcrop and GPR data with the use of multiple-point statistical methodology to depict the internal architecture, heterogeneity and spatial relationships of main sedimentary facies. The model can serve as a guide for the future exploration and exploitation of the quartz-glauconite sands in the area and as instructive example of how a petroleum reservoir model of a complex sedimentary succession can be constructed with the use of modern statistical methods.
Źródło:: Geological Quarterly; 2014, 58, 1; 125--144
1641-7291
Pojawia się w:: Geological Quarterly
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 4.

Tytuł:: Pozyskanie zabytkowego 100-letniego mostu do celów dydaktycznych
An acquisition of the historic 100 years old bridge for educational purposes
Autorzy:: Błazik-Borowa, E.
Karaś, S.
Kowal, M.
Łagowski, S.
Szepietowski, Z.
Wysocka, A.
Powiązania:: https://bibliotekanauki.pl/articles/143542.pdf
Data publikacji:: 2015
Wydawca:: Stowarzyszenie Inżynierów i Techników Komunikacji Rzeczpospolitej Polskiej
Tematy:: mosty historyczne
most żelbetowy
ochrona zabytków
historic bridges
reinforced concrete bridge
preservation of monuments
Opis:: W artykule przedstawiono starania o ocalenie stuletniego mostu żelbetowego, przypadkowo odnalezionego w nasypie drogowym w miejscowości Łabunie koło Zamościa. Zaangażowanie środowisk inżynierów drogowo-mostowych doprowadziło do przeniesienia mostu na tereny Politechniki Lubelskiej, gdzie będzie obiektem dydaktycznym i ozdobą uczelni. Przedstawiona działalność jest przykładem prawidłowych zabiegów o ochronę technicznego dziedzictwa narodowego.
Efforts for saving the one hundred years old RC bridge discovered accidentally as embedded in road embankment at the vicinity of site Labunie near Zamość were presented in the paper. The engagement of the road and bridge engineers allow to transfer the bridge on the Lublin Polytechnic area where it will serve as educational object and valuable specimen for the school. Presented activity is an example of correct efforts for preservation of national technical heritage.
Źródło:: Drogownictwo; 2015, 9; 296-301
0012-6357
Pojawia się w:: Drogownictwo
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 5.

Tytuł:: Survivin expression in canine lymphomas in relation with proliferative markers
Autorzy:: Sokolowska, J.
Urbanska, K.
Gizinski, S.
Wysocka, A.
Cywinska, A.
Lechowski, R.
Powiązania:: https://bibliotekanauki.pl/articles/2087990.pdf
Data publikacji:: 2015
Wydawca:: Polska Akademia Nauk. Czytelnia Czasopism PAN
Opis:: Survivin is a member of apoptosis inhibiting proteins family. Apart from its antiapoptotic activity it plays a critical role in regulating the cell cycle and mitosis. It is overexpressed in most human malignancies. While the prognostic significance of survivin expression is widely investigated in human non-Hodgkin's lymphomas, little is known about its expression in canine lymphomas. The aim of the study was to evaluate the expression of survivin in canine lymphomas in relation to proliferation markers (mitotic index and percentage of Ki67-positive cells). Survivin was found in all examined lymphomas belonging to 6 different morphological subtypes with nuclear immunoreactivity. In most of lymphomas (18/25) survivin expression ranged 10%-25% of positive cells. Only single cases had lower (0-10% positive cells, 1/25) or higher (25-50% and >50% positive cells, 5/25 and 1/25, respectively) index of survivin. Neither mitotic index nor proliferative index correlated with survivin expression when the values quantified randomly in whole specimens were compared. However, when survivin expression were quantified in selected tumor areas of low and high proliferation activity the high correlations between survivin expression and proliferation index were found. The results indicated that survivin is commonly expressed in canine lymphomas. Nuclear labelling together with the relation of its expression and proliferative activity in highly proliferative areas of neoplastic tissue suggest a potential role of survivin in cell cycle activation in canine lymphoma cells. However, further studies of the relation between expression of survivin and other proteins involved in cell cycle regulation are needed. Moreover, the results suggest that survivin may pose the therapeutic target in canine lymphomas.
Źródło:: Polish Journal of Veterinary Sciences; 2015, 18, 1
1505-1773
Pojawia się w:: Polish Journal of Veterinary Sciences
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 6.

Tytuł:: Ewolucja utworów mioceńskich zapadliska przedkarpackiego w rejonie Rzeszowa (obszar zdjęcia sejsmicznego 3D Sokołów-Smolarzyny)
Evolution of the Miocene deposits of the Carpathian Foredeep in the vicinity of Rzeszów (the Sokołów-Smolarzyny 3D seismic survey area)
Autorzy:: Krzywiec, P.
Wysocka, A.
Oszczypko, N.
Mastalerz, K.
Papiernik, B.
Wróbel, G.
Oszczypko-Clowes, M.
Aleksandrowski, P.
Madej, K
Kijewska, S.
Powiązania:: https://bibliotekanauki.pl/articles/2074574.pdf
Data publikacji:: 2008
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: zapadlisko przedkarpackie
miocen
zdjęcie sejsmiczne 3D
Carpathian foredeep
Miocene
3D seismic data
Opis:: The Miocene Carpathian foredeep basin in Poland (CFB) developed in front of the Outer Carpathian fold-and-thrust belt, at the junction of the East European craton and the Palaeozoic platform. 3D seismic data, cores and well logs from Sokołów area (vicinity of Rzeszów) were used in order to construct new depositional model of the Miocene succession of the Carpathian foredeep. The gas-bearing Miocene infill of the CFB is characterized by a shallowing-upward trend of sedimentation and consists of hemipelagic, turbiditic and deltaic and nearshore-to-estuarine facies associations. Lowermost part of the Miocene infill seems to has been deposited from the North. Such direction of sediment supply was related to influence of existing relief of the pre-Miocene basement, where very deep (up to 1,5 km) erosional valleys cut into the pre-Miocene (Precambrian) basement due to inversion and uplift of the SE segment of theMid-Polish Trough are located. Upper part of theMiocene infill reflects sediment progradation from the South, from the Carpathian area into the foredeep basin. In the Rzeszów area existence of the so-called anhydrite-less island, i.e. relatively large area devoid of the Badenian evaporitic cover caused by the post-Badenian uplift and widespread erosion of evaporites,has been postulated for many years. Interpretation of 3D seismic data showed that such model should be abandoned. In the studied part of the CFB, Late Badenian evaporitic sedimentation was restricted to the axial parts of deep paleovalleys. Evaporites deposited in these valleys have been rarely encountered by exploration wells as such wells were almost exclusively located above basement highs separating erosional paleovalleys, hence giving incorrect assumption regarding regional lack of evaporitic cover. It is possible that in axial parts of these valleys important gas accumulations might exist, charged from the South and sealed by the Badenian evaporites.
Źródło:: Przegląd Geologiczny; 2008, 56, 3; 232-232
0033-2151
Pojawia się w:: Przegląd Geologiczny
Dostawca treści:: Biblioteka Nauki

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