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    Tytuł:
    Historia Oddziału Świętokrzyskiego Polskiego Towarzystwa Geologicznego
    History of the Holy Cross Branch of the Polish Geological Society
    Autorzy:
    Fijałkowska-Mader, Anna
    Powiązania:
    https://bibliotekanauki.pl/articles/2074312.pdf
    Data publikacji:
    2022
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Polskie Towarzystwo Geologiczne
    Oddział Świętokrzyski PTG
    historia
    Polish Geological Society
    Holy Cross Branch PGS
    history
    Opis:
    The Holy Cross Branch of the Polish Geological Society was established in 1963. Its first chairman was Czesław Żak. Among the presidents, who performed this function for several terms, the following should be mentioned: Henryk Jurkiewicz, Halina Żakowa, Jerzy Gągol and Anna Mader. The largest number, 120 members, was in 1981. Currently, it has 24 members. The activities of the Branch included organizing scientific meetings with papers on various topics, field conferences, both domestic and foreign, as well as scientific conferences and sessions and conventions of the Polish Geological Society in the Holy Cross Mountains.
    Źródło:
    Przegląd Geologiczny; 2022, 70, 4; 303--306
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Zastosowanie wskaźnika TAI (thermal alteration index) i analizy palinofacjalnej do określenia stopnia dojrzałości termicznej materii organicznej w utworach górnego permu i triasu w północnej części niecki nidziańskiej (Polska centralna)
    Application of the TAI (Thermal Alteration Index) and palynofacial analysis for determining the degree of organic matter termal maturity in the Upper Permian and Triassic deposits in the northern part of the Nida Basin (central Poland)
    Autorzy:
    Fijałkowska-Mader, Anna
    Powiązania:
    https://bibliotekanauki.pl/articles/1834094.pdf
    Data publikacji:
    2020
    Wydawca:
    Instytut Nafty i Gazu - Państwowy Instytut Badawczy
    Tematy:
    wskaźnik TAI
    palinofacja
    kerogen
    górny perm
    trias
    niecka nidziańska
    TAI
    palynofacies
    Upper Permian
    Triassic
    Nida basin
    Opis:
    Determining the thermal maturity of palynomorph based on their color is a method commonly used in hydrocarbon prospecting. The color of the outer membrane of miospores (exine) changes as a result of heating from pale yellow to black depending on the paleotemperature. Currently, there are many palynomorph color scales correlated with the value of vitrinite reflectance, temperature of burial and hydrocarbon generation stages. Due to the varied material, both in taxonomic and morphological terms, the author used the TAI AMOCO scale. Furthermore, the share of individual kerogen groups in palynofacies was analyzed in terms of their hydrocarbon potential. The Upper Permian and Triassic deposits from eleven boreholes located in the north part of the Nida Basin were investigated. They showed that the Triassic and in the Upper Permian samples from the Milianów IG 1 borehole, are dominated by the pale yellow to orange color of spores and pollen grains, corresponding to a TAI index from 1 to 4, i.e. the pre-generation, dry gas and the early oil generation windows. In turn, only the samples of the Upper Permian from the Pągów IG 1 borehole are dominated by the brown color of miospores, which corresponds to a TAI index from 4+ to 5, i.e. the peak oil prone. Dominant vitrinite reflectance Ro varies from 0,4% to 0,6%, so the degree of organic matter maturity in the Upper Permian and Triassic deposits is not very high, which indicates relatively low temperatures of sediment diagenesis (< 80°C). Analysis of palynofacies showed that the Upper Permian and Triassic deposits contain mixed and structural kerogen. Mixed kerogen, occurring in carbonate rocks, contains amorphous fine-scattered kerogen and “fluffy” of algae origin, as well as structural kerogen of terrigeneous origin, mainly exinite and vitrinite. Mixed kerogen is characterized by oil potential, whereas structural kerogen – by gas-oil potential.
    Źródło:
    Nafta-Gaz; 2020, 76, 8; 495-500
    0867-8871
    Pojawia się w:
    Nafta-Gaz
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Kamień w architekturze Pałacu Biskupów Krakowskich w Kielcach – próba identyfikacji
    Stone in the architecture of the Palace of the Kraków Bishops in Kielce – an attempt of rock type identification
    Autorzy:
    Król, Paweł
    Fijałkowska-Mader, Anna
    Powiązania:
    https://bibliotekanauki.pl/articles/20208296.pdf
    Data publikacji:
    2023
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Pałac Biskupów Krakowskich w Kielcach
    marmurki kieleckie
    piaskowce dolnego triasu
    Palace of the Kraków Bishops in Kielce
    Kielce marbles
    Lower Triassic sandstones
    Opis:
    The authors were the first to attempt to identify the stones used in the architectural elements of the baroque Palace of the Kraków Bishops (built in 1637–1641) in Kielce. The founder of the residence was Bishop Jakub Zadzik of the Korab coat of arms. Despite the vicissitudes of fate, the residence defended itself against major transformations, retaining the original shape and as the decoration of the loggia, and is one of the most beautiful monuments from the Vasa era in Poland. However, the turbulent history of the palace, and especially numerous reconstructions, renovations, transfers of architectural elements as well as modifications and functional changes, caused difficulties in reconstructing the original interior design of the rooms, and especially in determining the periods from which the individual stone elements come. The stone decoration of the original palace was limited to the facade with loggias and figures of Swedish and Moscow envoys, a two-flight staircase and single portals inside the building, as well as the floor and fireplaces in the bishop’s rooms. The floor in the lower hallway and the lower diner room on the ground floor were probably also made of stone. Almost exclusively local stone was used: the so-called Kielce marbles (mainly Bolechowice limestone, “Zygmuntówka” conglomerate and Zelejowa rosa-like calcite) and various types of Lower Triassic sandstones from the Świętokrzyskie deposits. Few elements were made of black Dębnik limestone. Noteworthy is the Sanctuary of Marshal Józef Piłsudski, who was stationed in the palace, together with the legionary staff, in 1914. The interior of the main hall of the sanctuary is made of various types of Kielce marbles, mainly Bolechowice limestone, with elements of white Carrara marble. While the identification of carbonate rocks did not pose any major difficulties, assigning sandstone elements to a specific deposit turned out to be impossible in many cases, e.g. due to lack of comparative material.
    Źródło:
    Przegląd Geologiczny; 2023, 71, 1; 19-35
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Marine vs. terrestrial environments during Early Triassic deposition on the northeastern margin of the Central European Basin : a multidisciplinary study on the Middle Buntsandstein of the Bartoszyce IG 1 borehole, NE Poland
    Autorzy:
    Becker, Anna
    Fijałkowska-Mader, Anna
    Jasionowski, Marek
    Powiązania:
    https://bibliotekanauki.pl/articles/2060144.pdf
    Data publikacji:
    2020
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Lower Triassic
    northeastern Poland
    palynofacies
    clay mineralogy
    olite microfacies
    isotope geochemistry
    Opis:
    The Middle Buntsandstein Subgroup of the Lower Triassic of north-eastern Poland has been investigated in the context of possible marine ingressions into the Central European Basin. To better constrain these, palynofacies analysis and mineralogical analysis of mudstones were undertaken on samples taken from the Lidzbark and Malbork formations penetrated by the Bartoszyce IG 1 borehole, serving as stratotype section of both lithostratigraphic units. Microfacies and geochemical analyses, including C and O isotope analysis, were conducted additionally on oolitic limestones of the basal Lidzbark Formation (the lowermost Middle Buntsandstein), and the boron content was measured on all mudstone samples. Seven palynofacies types are distinguished: types 1 to 3 within the Malbork Formation and types 4 to 7 within the Lidzbark Formation. Types 1 and 2 originated on a floodplain, type 3 probably in a deltaic or barrier setting, and types 4 and 5 in a brackish lagoon or a more open basin, possibly of marine origin. Palynofacies type 6 reflects long transport and reworking, whereas palynofacies type 7 is interpreted as formed due to pedogenic processes. Clay minerals and quartz, accompanied by feldspars, calcite and dolomite are the main components of the mudstones investigated. The clay mineral association consists of illite or a mixture of illite and smectite, and chlorite. The Lidzbark Formation and the lowermost part of the Malbork Formation show less variability in mineralogical composition than the upper part of the Malbork Formation. Smectite admixtures were detected only in the upper part of the Malbork Formation (the uppermost Middle Buntsandstein). The boron content, achieved after aqua regia digestion, ranges from 70 to 121 mg/kg (96 mg/kg at average), oscillating generally around 90 mg/kg. A higher boron content, bound in silicate structure, is associated with the upper part of the Malbork Formation. All major mineralogical and geochemical changes coincide more or less with the transition from the supposed marine to the terrestrial environmental realm, interpreted from lithological and sedimentological observations within the lowermost part of the Malbork Formation. However, diagenetic alteration of the clay minerals, and of the boron content, could not be ruled out. The oolitic limestones, mainly grainstones, contain admixtures of quartz grains and rare bioclasts, the ooids nuclei being peloids or unrecognizable. The carbonates are almost exclusively composed of low-Mg calcite. A high content of Mg and the presence of small amounts of dolomite suggest that the ooids were primarily composed of high-Mg calcite and are comparable with similar Early Triassic deposits in Tethyan settings. The δ13C values range from -2 to +1%o VPDB, fitting well with the known ranges of Lower Triassic marine carbonates. An observed δ13C depletion towards the top of the oolite-bearing part of the section may reflect a local shallowing trend that led to overall salinity decrease. A possible connection with the one of the global oceanic geochemical episodes has to be tested further. The results obtained suggest a marine origin of the lower Middle Buntsandstein deposits studied and document a terrestrial origin for the upper Malbork Formation.
    Źródło:
    Geological Quarterly; 2020, 64, 4; 1023---1047
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Zarys historii górnictwa skalnego w rejonie Sitkówki (Góry Świętokrzyskie) w I połowie XX w.
    Outline of the history of rock quarrying in the vicinity of the Sitkówka region (Świętokrzyskie Mountains) in the first half of the 20th century
    Autorzy:
    Król, Paweł
    Pabian, Grzegorz
    Fijałkowska-Mader, Anna
    Powiązania:
    https://bibliotekanauki.pl/articles/2075926.pdf
    Data publikacji:
    2019
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    wydobywanie skał
    wapienie dewońskie
    Sitkówka
    rock quarrying
    Devonian limestones
    Opis:
    Rock quarrying in the vicinity of the Sitkówka (Sitkówka-Nowiny commune, Kielce county), which started at the beginning of the 20th century, has not yet been given a historical context. The authors based on archival sources, present the history of the development of six quarrying and processing plants involved in the extraction of rock raw materials in the first half of the XXth: Sitkówka, Jaźwica Mala, Sitkowieckie Nowiny, Belkowa, Kostrzewa and Stara Trzuskawica. The principal rochi extracted in these quarries were Middle Devonian-Givetian dolomites and stromatoporo- id-coral limestones of the Kowala Formation (Lower Sitkówka Beds). They were used mainly for the production of crushed stone, grits and lime, and less frequently of technical marbles. The modern, intensive activity of numerous industrial plants causes constant transformation of the Sitkówka area thus obscuring traces of the former quarrying activity and production infrastructure. That is why documentation of the remains of this exploitation is so important.
    Źródło:
    Przegląd Geologiczny; 2019, 67, 9; 758--766
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Walory geoedukacyjne i geoturystyczne kamieniołomu Zygmuntówka na Czerwonej Górze (Góry Świętokrzyskie)
    Geoeducational and geotourist value of the Zygmuntówka (Sigismund) quarry at Czerwona Góra (Holy Cross Mountains)
    Autorzy:
    Jewuła, Karol
    Fijałkowska-Mader, Anna
    Salwa, Sylwester
    Powiązania:
    https://bibliotekanauki.pl/articles/2074327.pdf
    Data publikacji:
    2022
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    kamieniołom Zygmuntówka
    zlepieńce
    górny perm-loping
    geoedukacja
    Zygmuntówka quarry
    conglomerates
    Upper Permian-Lopingian
    geoeducation
    Opis:
    The geosite Zygmuntówka (Sigismund ) quarry, located at Czerwona Góra near Chęciny in SW part of the Holy Cross Mountains, is the oldest and the most famous among the so-called Chęciny „marble” quarries which provided stones for constructing numerous important buildings in the region and beyond. Upper Permian conglomerates (Czerwona Góra Formation), with a thickness of several tens of metres, outcrop in this area. The conglomerates are clast- and locally mud-supported and consist of light grey and beige carbonate pebbles and cobbles chaotically distributed within the reddish-brown silty-carbonate-ferriferous matrix. The conglomerates represent continental alluvial fan deposits deposited under arid and semiarid climate conditions. The quarry, of a regional rank, is well suited for both geoeducation and geotourism purposes.
    Źródło:
    Przegląd Geologiczny; 2022, 70, 1; 25--33
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Działalność Oddziału Świętokrzyskiego PIG-PIB w zakresie geologii środowiskowej, ochrony przyrody nieożywionej oraz edukacji geologicznej
    Activity of the Holy Cross Mountains Branch of the Polish Geological Institute-NRI in the field of environmental geology, protection of inanimate nature and geological education
    Autorzy:
    Giełżecka-Mądry, Dorota
    Fijałkowska-Mader, Anna
    Szczepanik, Zbigniew
    Powiązania:
    https://bibliotekanauki.pl/articles/2076227.pdf
    Data publikacji:
    2021
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Góry Świętokrzyskie
    geologia środowiskowa
    ochrona cech geologicznych
    edukacja geologiczna
    Holy Cross Mts.
    environmental geology
    protection of geological features
    geological education
    Opis:
    The Holy Cross Mts. and their vicinities is a unique area on the geological map of Europe since rocks of all Phanerozoic systems, including the Cambrian to Quaternary, are exposed there. The variable rock types provide great cognitive and educational opportunities, but also stimulate the exploitation of various types of minerals. On the one hand, mining activities contributed to the recognition and better exposure of rocks, but on the other hand, they often threaten the natural environment and become burdensome for the inhabitants. The study of the balance between environmental protection and human mining activity is carried out by environmental geology, which is an important part of the activity in the Holy Cross Mts. Branch of the Polish Geological Institute (PGI), where various tasks in this field have been carried out for over half a century. The care for protection and promotion of the geological heritage of the Holy Cross Mts has been an important task of geologists working in the Kielce Branch of the PGI throughout its over 80-year history. It is manifested in the legal protection of the most interesting geological areas and geosites, and the promotion of geological knowledge in wide public opinion. The geological education in the Holy Cross Mts. plays a special role because the inanimate nature is a very valuable element of natural environment that distinguishes the Kielce region from other regions of Poland.
    Źródło:
    Przegląd Geologiczny; 2021, 69, 4; 250--258
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Integrated palynostratigraphy and magnetostratigraphy of the Middle and Upper Buntsandstein in NE Poland : an approach to correlating Lower Triassic regional isochronous horizons
    Autorzy:
    Becker, Anna
    Fijałkowska-Mader, Anna
    Nawrocki, Jerzy
    Sobień, Katarzyna
    Powiązania:
    https://bibliotekanauki.pl/articles/2059689.pdf
    Data publikacji:
    2020
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Buntsandstein
    Lower Triassic
    northeastern Poland
    palynostratigraphy
    magnetostratigraphy
    Opis:
    Despite years of research, Lower Triassic deposits of the epicontinental Central European Basin still lack a detailed stratigraphy that would allow regional correlation of isochronous horizons. The best chronostratigraphic results have up to now been achieved by microspore-based biostratigraphy and magnetostratigraphy. Integrated palynostratigraphic and magnetostratigraphic investigations, carried out on Buntsandstein cores from northeastern Poland representing the eastern margin of the basin, have made precise correlations with the better-explored basin centre. The Lidzbark and Malbork formations of the Bartoszyce IG 1 borehole were examined by means of palynology and palaeomagnetic studies. Further palaeomagnetic studies were applied to the Lidzbark, Malbork and Elbląg formations of the Nidzica IG 1 borehole and the Elbląg Fm. of the Pasłęk IG 1. Two spore-poll en assemblages were distinguished representing the Densoisporites nejburgii Subzone of the D. nejburgii Zone within the lower part of the Lidzbark Fm. and the lowermost part of the Malbork Fm. Mostly reversed polarity was detected within the lower part of the succession investigated, whereas normal polarity prevailed within its upper part. A normal polarity local zone was correlated with the undivided Tbn6-Tbn7 standard magnetozones of western Poland. The reversely polarized part of the succession corresponds most probably to the Tbr5 standard magnetozone. The base of the Tbn6-Tbn7 magnetozone can serve as a good correlation horizon for regional reconstructions.
    Źródło:
    Geological Quarterly; 2020, 64, 2; 460--479
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Lost Norian fluvial tracks : Sedimentology and stratigraphy of the Upper Triassic coarse-grained deposits in Kamienica Śląska (Upper Silesia, southern Poland)
    Autorzy:
    Fijałkowska-Mader, Anna
    Paszkowski, Mariusz
    Kędzior, Artur
    Jewuła, Karol
    Powiązania:
    https://bibliotekanauki.pl/articles/2171816.pdf
    Data publikacji:
    2022
    Wydawca:
    Polskie Towarzystwo Geologiczne
    Tematy:
    Upper Norian-lower Rhaetian
    braided river alluvium
    facies analysis
    sedimentology
    palynology
    regional correlation
    Opis:
    In the Triassic-Jurassic boundary profiles of the Upper Silesian region, there are locally developed coarse clastic deposits, commonly known as the Połomia Gravels, Połomia Beds or “Połomia Formation’’ (informal name). Due to the lack of reliable stratigraphic tools, the chronostratigraphic position of these deposits remains one of the most controversial aspects of the Triassic-Jurassic lithostratigraphy in the region. Sparse biostratigraphic data from the overlying and underlying deposits indicate a wide range of ages, from the Late Triassic to Early Jurassic. This paper presents the results of sedimentological, petrographical and palynological analyses of the coarse-grained deposits from the Kamienica Śląska gravel pit, which is currently one of the biggest facilities of this type in Upper Silesia. The outcrop section, with a total thickness of up to 20 m, is dominated by friable, light grey to beige and locally dark grey, large-scale planar to trough cross-stratified conglomerates and coarse-grained sandstones with subordinate thin interbeds of grey and reddish brown mudstones. Three facies associations have been distinguished, representing a main channel belt, secondary channels and floodplains subenvironments. Facies analysis points to a braided river tract with localised floodplain sediments. The grain composition of the Kamienica Śląska gravel/conglomerate is less diversified than that of the polymictic typical Połomia Beds of the Myszków area and resembles oligomictic conglomerates known from the Grabowa Formation of the Norian age and/or conglomerates of the Gorzów Beds of Rhaetian age, which also occur on the studied region. Palynological analysis of mudstone interbeds within the conglomeratic deposits shows the presence of miospores guiding and characteristic for subzone c of the Corollina meyeriana zone of the late Norian-early Rhaetian age. The appearance of the coarse-grained deposits in late Norian could be associated with the development of a long-reach braided fluvial tract, draining the S and SE part of the Sudetian-Malopolska-Lublin land (S-M-L land) in response to the tectonic rearrangement in the source area and gradual climatic change from semi-arid to humid in the Rhaetian.
    Źródło:
    Annales Societatis Geologorum Poloniae; 2022, 92, 3; 277--293
    0208-9068
    Pojawia się w:
    Annales Societatis Geologorum Poloniae
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Piaskowce dolnego dewonu na górze Barczy (Góry Świętokrzyskie) i historia ich eksploatacji
    History of exploitation of the Lower Devonian sandstones at the Barcza Hill (Holy Cross Mountains)
    Autorzy:
    Król, Paweł
    Fijałkowska-Mader, Anna
    Kozak, Bartosz
    Giełżecka-Mądry, Dorota
    Powiązania:
    https://bibliotekanauki.pl/articles/2076211.pdf
    Data publikacji:
    2021
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    piaskowce
    dolny dewon
    eksploatacja
    Barcza
    sandstones
    Lower Devonian
    exploitation
    Opis:
    The beginning of exploitation of the Lower Devonian sandstones on Barcza Hill, located in the Klonów Range in the central part of the Holy Cross Mountains, dates back to the first decade of the last century. Sandstones of the lower Emsian Barcza Beds, known in older literature as “placoderm sandstones” were mined here. By the time of World War II, there were seven mines that produced mainly paving stones and crushed stone. Three of them resumed work after the war: “Kopalnia Nowa”, “Byk” and “Przy Pomniku”. Unfavourable deposit conditions and competition of the neighbouring mining plants "Bukowa Góra” and "Wiśniówka” led to the abandonment of mining on Barcza Hill in the late 1950s. In 1984, the “Barcza” nature reserve was created, which included the two largest quarries: "Kopalnia Nowa”and "Byk”.
    Źródło:
    Przegląd Geologiczny; 2021, 69, 2; 81--90
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Historia eksploatacji surowców skalnych w dolinie Świśliny (Góry Świętokrzyskie)
    The history of rock mining exploitation in the Świślina Valley (Holy Cross Mountains)
    Autorzy:
    Fijałkowska-Mader, Anna
    Stoiński, Andrzej
    Tyczyński, Zbigniew
    Gawron, Paweł
    Kozak, Bartosz
    Król, Paweł
    Trela, Wiesław
    Powiązania:
    https://bibliotekanauki.pl/articles/2074298.pdf
    Data publikacji:
    2022
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    piaskowce
    dolomity
    dewon
    trias
    eksploatacja
    dolina Świśliny
    sandstones
    dolomites
    Devonian
    Triassic
    exploitation
    Świślina Valley
    Opis:
    The beginning of exploitation of Lower Triassic (Röt, Olenekian) sandstones in Doły Biskupie dates back to the 17th century. The village is situated 12 km west of Ostrowiec Świętokrzyski, in the Świślina Valley, in the north-eastern part of the Holy Cross Mountains. In addition to sandstones, a wide spectrum of other rocks types were excavated in the adjacent areas: Lower Devonian (Emsian) sandstones in Godów, Middle Devonian (Efelian) dolomites in the Doły Opacie quarry and Lower Triassic (Middle Buntsandstein, Olenekian) sandstonesin Wióry. The last quarry at Doły Opacie was closed in 1984. The Doły Opacie and Doły Biskupie quarries currently provide a number of inanimate nature monuments.
    Źródło:
    Przegląd Geologiczny; 2022, 70, 2; 100--114
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
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