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    Wyświetlanie 1-5 z 5
    Tytuł:
    Cum grano salis, or about the Anartophracti in the Słonne Mountains
    Autorzy:
    Bochnak, Tomasz
    Twardo, S.
    Powiązania:
    https://bibliotekanauki.pl/articles/2041001.pdf
    Data publikacji:
    2021
    Wydawca:
    Uniwersytet Jagielloński. Wydawnictwo Uniwersytetu Jagiellońskiego
    Tematy:
    Anartophracti
    Ptolemy’s Geography
    the Carpathians
    San-Dnester Route
    Opis:
    At the end of the 20th century, as the researchers became more convinced about the existence of the La Tène culture settlement zone in south-eastern Poland, there were more and more attempts at identifying the ethnicity of this population. Some of the researchers allowed for connecting the said settlement with the Anartophracti, known from Claudius Ptolemy’ writings (Geography, III, 5, 8). However, in order to identify the La Tène culture population from south-eastern Poland with Ptolemy’s Anartophracti, it is necessary to prove that Ptolemy’s account concerned the peoples inhabiting the area of the upper San basin in the 3rd and possibly 2nd century B.C. It is thus necessary to prove that the geographical and chronological data are consistent. One more argument in support of the claim would be a proof that the name Anartophracti refers to a Celtic tribe. It would have to be also assumed a priori that the ethnonym of Anartophracti is not a duplicate of the name Anarti. In author’s opinion, Ptolemy’s writings do not allow to prove that the Anartophracti he mentions lived at the areas on the upper San river: they could have rather lived to the east or north-east of the Carpathians. Ptolemy’s account is not clear enough to locate the Anartophractis’ settlements. The above list of the written sources seems to indicate that the chronology of all the information concerning the Anarti ranges between the end of the 1st half of the 1st c. B.C. and the late 240s A.D. There are no premises to link with the Anarti any settlement concentrations from the north-eastern La Tène culture from phase LT C or LT D1.
    Źródło:
    Acta Archaeologica Carpathica; 2021, 56; 309-334
    0001-5229
    2719-4841
    Pojawia się w:
    Acta Archaeologica Carpathica
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    The nannofossil biostratigraphy of the youngest deposits of the Magura Nappe (East of the Szczawa river, Polish Flysch Carpathians)
    Biostratygrafia i warunki paleośrodowiskowe najmłodszych osadów płaszczowiny magurskiej na wschód od Skawy w oparciu o nannoplankton wapienny (polskie Karpaty fliszowe)
    Autorzy:
    Oszczypko-Clowes, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/191415.pdf
    Data publikacji:
    2001
    Wydawca:
    Polskie Towarzystwo Geologiczne
    Tematy:
    youngest deposits of the Magura Nappe
    calcareous nannofossil
    palaeoecology
    Middle Eocene-Lower Miocene
    West Carpathians
    Opis:
    The Magura Nappe is the largest and southernmost tectonic unit of the Western Outer Carpathians and differ in lithofacies development from the Middle and Marginal groups of units. The age studies of the youngest deposits of the Magura Nappe play an important role in understanding the tectogenesis of the Outer Carpathians. The aim of this work was to find the litho- and biostratigraphic correlation with the more external units. For this purpose the youngest deposits from selected sections of the Magura Nappe located east of the Skawa River, were chosen. For the lower limit of the youngest sediments, Middle/Upper Eocene variegated shales with Reticulophragmium amplectens Grzybowski were taken. The analysis of nannoplankton assemblages enable to establish the age of these deposits which varies from Middle Eocene (NP15) up to Upper Oligocene (NP25) and Lower Miocene (NN2). The Eocene/Oligocene boundary lies within the NP21 nanno-zone and was found in the Krynica Zone within the Globigerina Marls (Leluchów section), in the Rača Zone within Poprad Sandstone Mbr of the Magura Fm. and in the Siary Zone within supra-Magura (Budzów) Beds (Budzów section), Wątkowa Sandstone (Ropica and Małastów sections) and within Zembrzyce (sub-Magura) Beds (Folusz section). In the Rača and Krynica zones the youngest - Upper Oligocene deposits from the studied sections belong to the Malcov Fm., whereas in the Siary Zone they belong to the supra-Magura (Budzów) Beds. The age of the Malcov Fm. was determined as NP24 in Leluchów and as NP25 in the Nowy Sącz I borehole, whereas the Budzów Beds belong to zone NP24. The youngest deposits so far described from the Magura Nappe belong to the Zawada Fm. whose age was determined as NN2. In the Polish part of the Bystrica Zone deposits younger than NP18, have so far not been found. The analysis of autochtonous nannoplankton assemblages from the Magura Basin enable to follow the palaeoecological changes in the Magura Basin, both in regional and global sense, from Late Eocene through Oligocene. The global changes are the drop of the water temperature accompanied by the progressing eutrophication of the Magura Basin. Further events were also recorded in zone NP23. The assemblage of this zone was characterised by the presence of species which are believed to be indicative of brackish water and restricted to the Paratethys region.
    Źródło:
    Annales Societatis Geologorum Poloniae; 2001, 71, No 3; 139-188
    0208-9068
    Pojawia się w:
    Annales Societatis Geologorum Poloniae
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Stratigraphic position of alkaline volcanic rocks in the autochthonous cover of the High-Tatric Unit (Western Tatra Mts., Central Western Carpathians, Slovakia)
    Autorzy:
    Madzin, J.
    Sýkora, M.
    Soták, J.
    Powiązania:
    https://bibliotekanauki.pl/articles/2059966.pdf
    Data publikacji:
    2014
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Central Western Carpathians
    Western Tatra Mountains
    autochthonous cover of the High-Tatric Unit
    alkaline volcanism
    biostratigraphy
    Opis:
    Biostratigraphic investigations of carbonate strata that sandwich volcanic rocks and studies of the volcanic rocks were made along five composite lithological sections across the Upper Jurassic-Lower Cretaceous carbonate rocks of autochthonous cover of the High-Tatric Unit in the Osobitá peak area of the Western Tatra Mts. A carbonate microbreccia that consists almost exclusively of limestone clasts containing calpionellids occurs immediately below the volcanics. The youngest identified microfossil Calpionella elliptica Cadisch in the individual limestone clasts showed the age of breccia formation to be younger than late Early-early Middle Berriasian. The volcanic rocks are overlain by the Osobitá Limestone Formation, which in the lowermost horizons consists of a few metres thick crinoidal limestone containing the foraminifers Meandrospira favrei (Charollais, Brönnimann & Zaninetti), Sabaudia minuta Hofker and Montsalevia salevensis (Charollais, Brönnimann & Zaninetti) indicating a Late Valanginian-Early Hauterivian age. The biostratigraphical and sedimentological data obtained show that volcanism took place in several phases. Less intense phases of volcanism are recorded as thin tuffitic laminae within the upper parts of the Tithonian-early Mid Berriasian Sobótka Limestone Member and as fragments of volcanic rock in the carbonate breccia. The main phase(s) of volcanism took place during the Late Berriasian-?Early Valanginian.
    Źródło:
    Geological Quarterly; 2014, 58, 1; 163--180
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Oil and gas fields in the Carpathians and the Carpathian Foredeep
    Autorzy:
    Górka, A.
    Gliniak, P.
    Madej, K.
    Maksym, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/2066022.pdf
    Data publikacji:
    2007
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    gas fields
    oil fields
    Carpathian Foredeep
    Carpathians
    sub-miocene basement
    reserves
    activity in the South of Poland
    Opis:
    Southeastern Poland is one of the oldest petroleum provinces in the world. Although hydrocarbon production has been conducted in this region since the middle of 19th century, there is still a good potential for more discoveries. 9 billion cubic meters of high methane gas reserves reported in the years 2000-2006, when combined with the previously discovered gas fields, essentially satisfy gas demand for this area. Currently, Miocene deposit of the Carpathian Foredeep is the most prolific exploration target area with more than 100 discoveries of high methane gas. The total reserves of these fields are 138 billion cubic meters, and the cumulative production is more than 90 billion cubic meters of natural gas. Large gas fields in terms of area and reserves that have already been discovered are followed by present discoveries of fields with relatively smaller area, their reserves are up to 2 billion cubic meters. Current exploration efforts are focused on good understanding of the sub-miocene basement configuration as well as detecting of seismic anomalies directly related to natural gas accumulations. Another very important element of exploration strategy for Southern Poland is the Mesozoic and Paleozoic deposits of the Carpathian Foredeep. The most prospective for discovering of sizeable hydrocarbon fields are Cretaceous (Cenomanian) sandstones and Upper Jurassic carbonates, locally also Middle Jurassic sandstone as well as Lower Carboniferous and Devonian carbonates. So far 13 gas fields and 10 oil fields have been discovered in the Mesozoic and Paleozoic of the Carpathian Foredeep and the sub-Carpathian basement with booked reserves of 7.5 billion cubic meters of natural gas and 4.7 million tons of oil. The cumulative production amounts to 6.1 billion cubic meters of gas and 4.3 million tons of oil. Different exploration problems have been encountered in the Carpathians. Most of the fields which have been discovered in the Flysch Carpathians occur in shallow, steep, narrow, commonly thrusted and faulted folds. Oil and gas fields discovered so far in the Carpathians have small reserves. Additionally, discovered and booked reserves of existing oil and gas fields are depleted to a large extent. 17 gas fields and 67 oil fields have been discovered in the Carpathians. Booked reserves amount to 16.6 billion cubic meters of natural gas and 12.3 million tons of oil. Cumulative production has been 15.2 billion cubic meters of gas and 11.9 million tons of oil. To sum up, it should be emphasized that the bulk of gas reserves discovered, booked and developed recently in Southern Poland comes from the autochthonous Miocene deposits. This trend, which involves high methane gas, is expected to continue for the next few years. Potential oil discoveries can be attributed mainly to the flysch Carpathians and Paleozoic, but requires more research and further exploration on a larger scale.
    Źródło:
    Przegląd Geologiczny; 2007, 55, 12/1; 993-998
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Górale huculscy w wojskowej propagandzie na rzecz przysposobienia społeczeństwa do wojny u schyłku Drugiej Rzeczypospolitej (Wybrane problemy badawcze)
    Autorzy:
    Kasprzyk, Artur
    Powiązania:
    https://bibliotekanauki.pl/articles/631737.pdf
    Data publikacji:
    2019
    Wydawca:
    Uniwersytet Marii Curie-Skłodowskiej. Wydawnictwo Uniwersytetu Marii Curie-Skłodowskiej
    Tematy:
    Second Republic of Poland
    army
    military propaganda
    defence of the state
    preparation of society for war
    Eastern Carpathians
    Mountain Festival
    Hutsuls
    Hutsul region
    Druga Rzeczypospolita
    wojsko
    propaganda wojskowa
    obrona państwa
    przysposobienie społeczeństwa do wojny
    Karpaty Wschodnie
    Święto Gór
    Huculi
    Huculszczyzna
    Opis:
    The article discusses research findings on issues related to the preparations for defending the country taken at the end of the 1930s by the leadership of the Polish armed forces. Although the current historiography contains a great number of studies and articles dealing with this subject, the impression is that the role played by military propaganda in these preparations received too little emphasis. Propaganda for the defence of the state was intended to include as many citizens of Polish society as possible, also from ethnically and geographically diverse backgrounds. Therefore, the article contains an analysis of extensive propaganda activities, which after 1935 were implemented by the Polish military authorities in the face of the growing threat of war, carried out mainly on the basis of archives from the resources of the Central Military Archives (Centralne Archiwum Wojskowe) in Warsaw. The essence of the discussion is the question why the military authorities of that time insisted that highlanders living in the Eastern Carpathians, primarily the Hutsuls, be involved in the defence preparations of the country. In the first place, propaganda measures were considered, with the help of which the army's leadership tried to influence the civilian population. Trying to explain why the use of the most effective propaganda tools, such as the press, radio and sound film turned out to be ineffective towards highlanders living in the furthest corners of the Carpathians, among other things, the lack of a well-developed communication network in that area was indicated. It was established that in the present situation the military authorities managed to involve the Hutsuls, Lemkos and Boykos in the life of the current state only thanks to the annual organisation of the ‘Mountain Festival’. The celebrations organised in order to unite all highlanders who lived in the territory of the Polish state were also conducive to carrying out effective military activities by the armed forces against the Polish population most distant from civilisation.            Research has shown that this type of activities was of great importance for the development of the situation in the Eastern Lesser Poland dominated by Ukrainian nationalists. Attention was drawn to the extremely valuable assets of the Hutsul region. It was an exceptionally attractive area in terms of tourism, sports and health. Thus, it had the chance to attract crowds of tourists from all over the country, which would strengthen the Polish element in the whole region. Hutsuls, however, were sceptical about the Ukrainian national movement, which made the army's leadership recognise them as an element easy to bind with the Polish state. Thereby, the inhabitants of the Hutsul region could be a counterbalance to the anti-state Ukrainian movement in Eastern Lesser Poland – an area of strategic importance! Unfortunately, advanced and properly conducted works were interrupted by the outbreak of the Second World War.
    Druga połowa lat trzydziestych upływała pod znakiem nasilającego się zagrożenia wojennego. Władze wojskowe Drugiej Rzeczypospolitej usiłowały objąć propagandą na rzecz obrony kraju, zróżnicowane pod wieloma względami społeczeństwo polskie. Z powodu napiętej sytuacji w Małopolsce Wschodniej, kierownictwu sił zbrojnych bardzo zależało, aby w przygotowania wojenne zaangażować górali zamieszkujących najdalsze zakątki Karpat, w szczególności Hucułów. Brak odpowiednio rozbudowanej sieci komunikacyjnej na terenie Karpat Wschodnich, nie pozwolił na zastosowanie najskuteczniejszych narzędzi propagandowych, jakimi wówczas były prasa, radio oraz film dźwiękowy. Zainteresowanie sprawami państwa wśród Hucułów, Łemków i Bojków – górali najbardziej oddalonych od cywilizacji, wzbudziło dopiero organizowane co roku (1935–1938) „Święto Gór”. Współpraca górali huculskich z armią, ułatwiała walkę z antypaństwowym ruchem ukraińskim w Małopolsce Wschodniej. Do wzmocnienia polskości w tym regionie przyczynić się miało również odpowiednie wykorzystanie nieocenionych walorów Huculszczyzny.
    Źródło:
    Res Historica; 2019, 48
    2082-6060
    Pojawia się w:
    Res Historica
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
      Wyświetlanie 1-5 z 5

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