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Tytuł:
Palaeomagnetic studies of the loess-palaeosol sequence from the Kolodiiv section (East Carpathian Foreland, Ukraine)
Autorzy:
Nawrocki, J.
Boguckyj, A.
Łanczont, M.
Powiązania:
https://bibliotekanauki.pl/articles/2059494.pdf
Data publikacji:
2007
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Western Ukraine
Kolodiiv
loess
Upper Pleistocene
palaeomagnetism
Opis:
The Upper Pleistocene loess-palaeosol sequence from the Kolodiiv section (East Carpathian Fore land) has been palaeomagnetically studied. Almost all samples displayed moderate to high positive palaeomagnetic inclinations and declinations en closed between 320° and 40°. How ever, one sample from the fossil soil of the last inter glacial pedocomplex (at 16.6 m pro file depth) was reverse magnetized and there fore can be correlated with the Blake Palaeomagnetic Event. Consequently that palaeosol can be related to (Oxygen Isotope Stage) OIS 5e1. An other sample from the Dubno 1 interstadial palaeosol demonstrated southern declination and significant lowering of inclination (up to 40°). This might be a record of the Laschamp Palaeomagnetic Event or of any Late Pleistocene palaeomagnetic excursion. The magnetic susceptibility and anhysteretic remanent magnetization data reflect the presence of several soils forming during the warm conditions of OIS 5 and the complex nature of the Eemian warming. Two palaeosols that developed between ca.115 ka and 120 ka indicate at least two climatic optima during the Eemian. High values of magnetic susceptibility (up to 300 Ą 10-6 SI units) noted in the middle of the section that contains slump deposits (9.5 m to 11m of depth) suggest that this material was derived from older soils of inter glacial type.
Źródło:
Geological Quarterly; 2007, 51, 2; 161-166
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
1-D modelling of the hydrocarbon generation history of the Jurassic source rocks in the Tarnogród–Stryi area (SE Poland – western Ukraine)
Autorzy:
Kosakowski, P.
Wróbel, M.
Koltun, Y. V.
Powiązania:
https://bibliotekanauki.pl/articles/191544.pdf
Data publikacji:
2011
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
source rocks
1-D modelling
hydrocarbon generation
hydrocarbon expulsion
Jurassic
SW Poland
Western Ukraine
Opis:
Reconstruction of burial and thermal history was modelled for the Mesozoic strata in the basement of the Polish and Ukrainian parts of the Carpathian Foredeep and in the marginal part of the Outer Carpathians. The 1-D modelling was carried out in profiles of the wells located in the area between Tarnogród and Stryi towns. In the Polish part, the modelling were performed in the profiles of the Księżpol 15, Lubliniec 9, Markowice 2 and Opaka 1 wells, and in the Ukrainian part in the profiles of the Chornokuntsi 1, Korolyn 6, Mosty 2, Podiltsi 1 and Voloshcha 1 wells. The geochemical characteristics of the Mesozoic stratigraphical horizons revealed that the best features of source rocks were present in the Middle Jurassic strata in the Polish part of the study area and in the Middle and Upper Jurassic strata in the Ukrainian part. Within these strata, the horizons of source rocks were distinguished and their quantitative evaluations were characterized. For these horizons, reconstruction of processes for hydrocarbon generation and expulsion were performed. The source rocks in the Polish part reached maturity only in the initial phase of “oil window”. However, the maturity achieved towards the end of the Upper Jurassic was insufficient to exceed the 10% threshold of the transformation degree for hydrocarbon generation. Therefore, the amount of generated hydrocarbons was minimal. Slightly higher maturity of organic matter in the Ukrainian part resulted in exceeding the thresholds of kerogen transformation and the initiation of hydrocarbon generation and expulsion processes. The process began after the deposition of thicker Miocene formations and developed even up to the main phase of the "oil window". The amount of the generated hydrocarbons reached ca. 150 mg/g TOC with an insignificant volume of expulsion.
Źródło:
Annales Societatis Geologorum Poloniae; 2011, 81, No 3; 473-485
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Facies of the Upper Jurassic–Lower Cretaceous sediments in the basement of the Carpathian Foredeep (western Ukraine)
Autorzy:
Krajewski, M.
Król, K.
Olszewska, B.
Felisiak, I.
Skwarczek, M.
Powiązania:
https://bibliotekanauki.pl/articles/191397.pdf
Data publikacji:
2011
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
microfacies
Upper Jurassic
Lower Cretaceous
SW margin of the East-European Platform
Carpathian Foredeep basement
Western Ukraine
Opis:
The Upper Jurassic–Lower Cretaceous carbonate sediments developed in a narrow, Ukrainian part of the basement of the Carpathian Foredeep show high facies diversity. Based upon thin section studies, the authors identified eleven principal microfacies varieties. Three main stages of development of carbonate platform were distinguished: (i) Oxfordian–Early Kimmeridgian, (ii) Kimmeridgian–Tithonian, and (iii) Berriasian–Valanginian. The Oxfordian sediments are rather thin and represent both the outer and inner, distally steepened ramp facies. In the Late Kimmeridgian and, mainly, in the Tithonian, the intensive growth of rimmed platform took place with distinct zones of peritidal, margin barrier and platform slope, bearing calciturbidite facies. Development of the rimmed platform was controlled by synsedimentary tectonic movements along faults rejuvenated southwest of the Holy Cross Mts. Fault Zone. In the Berriasian–Valanginian, the dominant process was sedimentation onto not-rimmed platform controlled by small sea-level changes. Both the facies development and literature data indicate that the Late Jurassic sedimentation in the Ukrainian part of the Carpathian Foredeep basement shows considerable differences in comparison to that of the Polish part. In the studied successions, large Oxfordian microbial-siliceous sponge reef complexes, known from the Polish part of the Carpathian Foredeep basement and other areas in Europe, were rare. In the study area carbonate buildups were encountered mainly in the intervals representing the Upper Kimmeridgian–Tithonian where small, microbial-sponge and microbial-coral biostromes or patch-reefs were formed. Their growth was presumably restricted to a narrow zone of the upper slope, close to ooidal-bioclastic margin platform facies. In the Polish part of the Carpathian Foredeep basement, the Late Jurassic sedimentation took place on a vast, homoclinal ramp while in the Ukrainian part it proceeded on a narrow, distally steepened ramp and rimmed platform with distinct marginal platform barrier. Similar platform facies distribution in both regions appeared mainly in the Early Cretaceous, although with some stratigraphical differences. The facies distribution of the Upper Jurassic sediments was closely controlled by the block structure of the basement and by orientation of the main, transcontinental Holy Cross Mts. Fault Zone, which supports the opinion on its activity in the Mesozoic era. The Ukrainian part of the Carpathian Foredeep basement located over the Palaeozoic Kokhanivka Block, between the Krakovets and Holy Cross fault zones, includes predominantly the slope, marginal and inner platform facies. Facies observed over the Palaeozoic Rava Ruska Block (south-western part of the East-European Platform), between the Holy Cross and Rava Ruska fault zones, represents mainly the inner platform and the peri-shore deposits.
Źródło:
Annales Societatis Geologorum Poloniae; 2011, 81, No 3; 291-307
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Microbial gas system and prospectives of hydrocarbon exploration in Miocene strata of the Polish and Ukrainian Carpathian Foredeep
Autorzy:
Kotarba, M. J.
Peryt, T. M.
Koltun, Y. V.
Powiązania:
https://bibliotekanauki.pl/articles/191552.pdf
Data publikacji:
2011
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
microbial gas
thermogenic gas
source rocks
hydrocarbon potential
organic geochemistry
prospectives of hydrocarbon exploration
autochthonous Miocene strata
Bilche-Volytsia Unit
Carpathian Foredeep
SW Poland
Western Ukraine
Opis:
Molecular composition of natural gases accumulated in autochthonous Miocene strata of the Polish and Ukrainian Carpathian Foredeep is dominated by methane, which usually constitutes over 98 vol%. Methane was generated by the carbon dioxide reduction pathway of microbial processes. Ethane was generated both during microbial and thermogenic processes ("oil window") and propane at the initial stage of the low-temperature thermogenic processes, and also by the microbial processes. The rhythmic and cyclic deposition of Miocene clays and sands as well as the vigorous generation of microbial methane caused that the gas produced in claystone beds was accumulated in the overlaying sandstones, and capped, in turn, by the succeeding claystones. Such generation and accumulation system of microbial gases gave rise to the formation of multi-horizontal gas fields. Analysis of the distribution of immature humic dispersed organic matter in the Upper Badenian and Lower Sarmatian sequences indicates that it is practically homogeneous. A migration range of microbial gases was insignificant and locations of their accumulations would depend only on the existence of proper type of traps (compactional anticlines situated above basement uplifts, sealed by the Carpathian Overthrust and/or by faults; stratigraphic pinching out and stratigraphic traps related to unconformities). Another situation is encountered in the south, beneath the Carpathian Overthrust. The thickness of the autochthonous Miocene strata in this area is more than 1,500 metres. Geochemical studies reveal that from a depth of 2,500 metres starts the process of low-temperature thermogenic hydrocarbon generation (“oil window”). At greater depths, more than 7,500 metres, within the autochthonous Lower Miocene basin only the high-temperature methane ("gas window") could be produced and accumulated.
Źródło:
Annales Societatis Geologorum Poloniae; 2011, 81, No 3; 523-548
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Precambrian and Palaeozoic basement of the Carpathian Foredeep and the adjacent Outer Carpathians (SE Poland and western Ukraine)
Autorzy:
Buła, Z.
Habryn, R.
Powiązania:
https://bibliotekanauki.pl/articles/191447.pdf
Data publikacji:
2011
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
basement
Carpathians
Carpathian Foredeep
East European Platform
Trans-European Suture Zone
south-eastern Poland
Western Ukraine
Opis:
In south-eastern Poland and western Ukraine, the Outer Carpathian orogen and the Carpathian Foredeep developed in the foreland of the East-European Platform (Baltica). The area consists of a number of tectonic units included in the Trans-European Suture Zone (TESZ): the Łysogóry–Radom and Małopolska blocks in the territory of Poland, and the Rava Rus’ka Zone, Kokhanivka Zone and Leżajsk Massif in the Ukraine. The development of the TESZ began in the (?Middle) Late Neoproterozoic and was associated with rifting processes taking place along the western edge of the East-European Craton (Baltica) during the break-up of the Rodinia/ Pannotia supercontinent. The passive margin of Baltica evolved into the TESZ during collisional and/or strike-slip movements. In the TESZ (Małopolska Block and Leżajsk Massif), Ediacaran flysch-type siliciclastics were affected by weak metamorphism and folding during the Cadomian orogeny. The development of Cambrian deposits in the East-European Craton, Łysogóry–Radom Block, northeastern part of the Małopolska Block (Kielce Fold Belt) and in the Rava Rus’ka and Kokhanivka zones was associated with the post-rift thermal subsidence. Tectonic movements (so-called Sandomierz phase), which occurred probably due to an oblique collision of the Małopolska Block (included into the passive margin of Baltica) and the East-European Craton during late Middle Cambrian to Late Cambrian (possibly also Early Ordovician) times, resulted in the following: (1) development of stratigraphical (?erosional) gaps in the Middle and Upper Cambrian sections of the Lublin–Podlasie slope of the East-European Craton and the Kielce Fold Belt in the Małopolska Block; (2) intense tectonic subsidence of the Łysogóry–Radom Block during the deposition of Middle and Upper Cambrian sediments; (3) development of compressional folds in the Lower Cambrian to lower Middle Cambrian deposits of the Kielce Fold Belt on the Małopolska Block. Ordovician–Silurian series were deposited in a typical flexural foredeep basin, in which subsidence and deposition rates accelerated during Late Silurian (Ludlow–Pridoli) and Early Devonian (Lochkovian) times. It is postulated that the present position of the Małopolska Block relative to the Łysogóry–Radom Block and East-European Craton resulted from post-Silurian dextral movements between the Małopolska Block and the East-European Craton. Devonian–Carboniferous deposits occur only in the Małopolska Block located in the Variscan foreland. The Middle-Late Devonian and Early Carboniferous shallow-marine carbonate platforms developed under an extensional regime. The siliciclastic Upper Visean–Lower Namurian A Culm series were deposited in the flexural Variscan foreland basin. During the Late Namurian A, the Małopolska Block was uplifted in response to the build-up of compressional foreland stresses. During post-Carboniferous times, the Precambrian and Palaeozoic deposits were subject to erosion and restructuring during the Alpine orogeny.
Źródło:
Annales Societatis Geologorum Poloniae; 2011, 81, No 3; 221-239
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Assessment of hydrocarbon potential of the Lower Palaeozoic strata in the Tarnogród–Stryi area (SE Poland and western Ukraine)
Autorzy:
Więcław, D.
Kosakowski, P.
Kotarba, M.J.
Koltun, Y. V.
Kowalski, A.
Powiązania:
https://bibliotekanauki.pl/articles/191878.pdf
Data publikacji:
2012
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
source rock
hydrocarbon potential
Cambrian
Ordovician
Silurian
Carpathian Foredeep basement
SE Poland
Western Ukraine
Opis:
Quantity, genetic type and maturity of organic matter dispersed in the Lower Palaeozoic sequence from the Lower Cambrian to Silurian strata of the Polish and Ukrainian parts of the Carpathian Foredeep basement in the Tarnogród–Stryi area were evaluated based on the results of geochemical analyses of 475 rock samples collected from 45 wells. The best source rocks were found in the Silurian strata where the present total organic carbon (TOC) content is up to 2.6 wt%. They occur in the vicinity of Wola Obszańska, where the median of the present and the initial total organic carbon (TOC) contents in the individual wells amount to 0.98 and 1.6 wt%, respectively. The Cambrian and Ordovician strata have a poorer hydrocarbon potential and their present TOC content never exceeds 1 wt%. In all of the investigated Lower Palaeozoic strata, organic matter is represented by the oil-prone Type-II kerogen deposited in anoxic or sub-oxic conditions. The maturity of source rocks ranges from early mature (the initial phase of the low-temperature thermogenic processes) in selected zones of the Silurian strata in the vicinity of Wola Obszańska, through the middle and the final phase of “oil window” in the Ordovician and Cambrian strata in the Polish part of the study area, to the overmature stage in the Ordovician strata in the south-eastern part of the study area (Ukraine).
Źródło:
Annales Societatis Geologorum Poloniae; 2012, 82, 1; 65--80
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Mykolaiv Sands in Opole Minor and beyond : sedimentary features and biotic content of Middle Miocene (Badenian) sand shoals of Western Ukraine
Autorzy:
Wysocka, A.
Radwański, A.
Górka, M.
Powiązania:
https://bibliotekanauki.pl/articles/2059398.pdf
Data publikacji:
2012
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Western Ukraine
Middle Miocene
Badenian
eco-taphonomy
burrows
depositional structures
sedimentology
Opis:
The Mykolaiv Sands are a huge lithosome of Middle Miocene (Badenian) age, accommodated within the Fore-Carpathian Basin in the Western Ukraine. Typically developed in the area of Opole Minor, it spreads across adjacent regions of Opole to cover an area of about 1300 km2. The varied sedimentary structures and ubiquitous burrows, indicate their development as a stack of sand shoals or related bodies, up to a few tens of metres thick, some of which temporarily reached sea level. Amidst the shoals, storm scours intermittently formed channel-like infills, some with residual lags at the base. The reversed density stratification and/or an increasing gravity gradient involved mass movements, some of which may have been triggered by seismic shocks focused at the shore or the adjacent hinterland of Podolia and Volhynia. Special attention is paid to the diverse fossils, all taphonomically filtered (aragonite shells and chitinous carapaces being lost), but which locally are mass-aggregated. They typify particular sand sets/bodies, to form allochthonous assemblages, some members of which (the cirripedes Scalpellum and Creusia, the shark Hemipristis, the ray Myliobatis) are newly recognized in the Ukrainian part of the Fore-Carpathian Basin. The others enrich considerably the faunal content of the Middle Miocene (Badenian) Paratethyan basins, either in terms of taxonomic diversity, or the eco-taphonomy of selected taxa (the starfish Astropecten, diverse echinoids). The whole faunal content of the Mykolaiv Sands may owe its profuse development to the global Middle Miocene Climatic Optimum of early Badenian age.
Źródło:
Geological Quarterly; 2012, 56, 3; 475--492
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Contamination of soils with heavy metals in the industrialized region of western Ukraine: western Podole Upland
Zanieczyszczenia metalami ciężkimi gleb uprzemysłowionego rejonu zachodniej Ukrainy
Autorzy:
Mandryk, O.
Radlovska, K.
Powiązania:
https://bibliotekanauki.pl/articles/385356.pdf
Data publikacji:
2013
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
soil contamination
heavy metals
air pollution
industrial emission
Western Ukraine
zanieczyszczenie gleby
metale ciężkie
zanieczyszczenia powietrza
zanieczyszczenie przemysłowe
zachodnia Ukraina
Opis:
Contamination of surface soil horizons with heavy metals is usually related to long-lasting air pollution and might potentially affect soil fauna, as well as plant growth, harvesting and health of plant consumer. In order to estimate potential health risk, we investigated surface and subsurface soil contamination with heavy metals in avable area in one of the most industrialized region of western Ukraine, western Podole Upland. In total 80 samples from the area of about 35 km2 were sampled and analyzed for content of zinc, nickel, copper, cobalt, lead, arsenic and quicksilver. The research revealed several anomalies, where the content of these elements exceed 3-5 Ukrainian quality guidance for avable soils. Soils are the most contaminated with arsenic and quicksilver, with maximum concentrations exceeding local geochemical background about 20 times. Maximum nickel and zinc concentrations are about 10 times higher than the background while the content of copper and cobalt is elevated up to several times.
Zanieczyszczenie powierzchni gleb metalami ciężkimi jest zazwyczaj wiązane z długotrwałym zanieczyszczeniem powietrza i może wpłynąć na faunę glebową, a także na wzrost roślin oraz zdrowie konsumentów. W celu oszacowania potencjalnego zagrożenia dla zdrowa autorzy badali zanieczyszczenie metalami ciężkimi powierzchni gruntów ornych w jednym z najbardziej uprzemysłowionych regionów zachodniej Ukrainy - zachodnim Podolu. Z powierzchni około 35 km2 pobrano w sumie 80 próbek, które przebadano i przeanalizowano pod względem zawartości cynku, niklu, miedzi, kobaltu, ołowiu, arsenu i rtęci. Badania wykazały liczne nieprawidłowości. Zawartość tych pierwiastków przekracza 3-5 ukraińskich norm jakości gleb uprawnych. Gleby te są najbardziej zanieczyszczone związkami arsenu i rtęci, których maksymalne stężenia lokalnie przekraczają normy geochemiczne aż 20-krotnie. Stężenie niklu i cynku wynosi maksymalnie około 10 razy więcej, niż przewiduje norma, podczas gdy zawartość miedzi i kobaltu jest podwyższona kilkukrotnie.
Źródło:
Geomatics and Environmental Engineering; 2013, 7, 1; 75-82
1898-1135
Pojawia się w:
Geomatics and Environmental Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Комуністична Партія України у період перебудови: особливості діяльності у західноукраїнських областях (1985-1991 рр.)
The Communist Party of Ukraine in the period of transition: the features of activities in western Ukraine in 1985–1991
Autorzy:
Murawśkyj, Ołeh
Powiązania:
https://bibliotekanauki.pl/articles/488093.pdf
Data publikacji:
2013
Wydawca:
Towarzystwo Nauki i Kultury Libra
Tematy:
Komunistyczna Partia Ukrainy
zachodnia Ukraina
Communist Party of Ukraine
western Ukraine
Opis:
Untrained reform of „perestroika” has profound ideological crisis of the Communist Party of Ukraine in 1985–1991. As a result, there has been complete loss of control over social and political processes. The authority of the Communist Party undermining the newly created „informal” organizations and political parties whose activities led to a breach of the monopoly of Communist Party, and the formation of a multiparty system. Crisis could not be avoided to unsatisfactory work of the apparatchiks of primary organizations (especially large industrial enterprises).
Źródło:
Komunizm: system – ludzie - dokumentacja; 2013, 2; 227-238
2299-890X
Pojawia się w:
Komunizm: system – ludzie - dokumentacja
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Czesław Miłosz on Conrad’s Polish stereotypes
Autorzy:
Dudek, Jolanta
Powiązania:
https://bibliotekanauki.pl/articles/638820.pdf
Data publikacji:
2014
Wydawca:
Uniwersytet Jagielloński. Wydawnictwo Uniwersytetu Jagiellońskiego
Tematy:
Czesław Miłosz, Joseph Conrad, Poland, Lithuania, Ruthenia, Ukraine, Russia, Apollo Korzeniowski, Adam Mickiewicz, Astolphe de Custine, Poland and Muscovy, Forefathers’ Eve, Under Western Eyes, The Secret Agent, Heart of Darkness, A Treatise on Poet
Opis:
In an essay entitled Conrad’s Stereotypes – published in 1957 – Miłosz sees Conrad as “the typical old Polish nobleman who remained faithful to the way in which he had lived and thought as a young man.” Miłosz speaks of his own affinity with Conrad (and Mickiewicz), explaining that it derives from a set of shared emotional and historical experiences that were deeply ingrained in the minds of the inhabitants of the ‘Eastern Borderlands’of the old Polish-Lithuanian-Ruthenian Commonwealth. This ‘Eastern Borderlands’ cultural identity may well have enabled Conrad to give an authentic portrayal of the Russian characters in Under Western Eyes. The counterpart to Mickiewicz’s and Conrad’s condemnation of autocracy and the fairness of their attitude towards Russians was Miłosz’s willingness to maintain friendly relations with contemporary Russian ‘dissidents’ who had stood up against the oppressive political system of the Soviet Union. Surprisingly, however, he does not draw any parallels between the Polish stereotype of Russia and the portrayal of Russia which is to be found in Russian political literature. Miłosz concludes by observing that in Under Western Eyes it was only through the purely artistic merits of his writing that Conrad could have hoped to win over his English-speaking readers, while at the same time remaining “faithful to a tradition that would have seemed exotic to anyone living in another country” – and for this achievement he deserves praise.
Źródło:
Yearbook of Conrad Studies; 2014, 9
2084-3941
Pojawia się w:
Yearbook of Conrad Studies
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Origin of the palaeokarst in Miocene evaporites on the SW periphery of the Eastern European Platform in the light of palynological studies : a case study of the Zoloushka Cave, Bukovina, Western Ukraine
Autorzy:
Andreychouk, V.
Worobiec, E.
Gedl, P.
Worobiec, G.
Powiązania:
https://bibliotekanauki.pl/articles/191838.pdf
Data publikacji:
2014
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
palaeokarst
palynology
sporomorphs
dinoflagellate cysts
caves
Western Ukraine
Eastern European Platform
Badenian
Opis:
The Zoloushka Cave belongs to a group of the largest gypsum caves in Western Ukraine (Bukovina region), developed in the middle Miocene (upper Badenian) evaporite series (Tyras Formation) on the SW periphery of the East European Platform. It is developed in the lower part of the evaporite series composed of gypsum, which is covered by a carbonate layer (Ratyn Limestone). The uneven upper surface of the gypsum at the contact with the limestone, the frequent occurrence of palaeokarst forms, and the presence of karstified fissures filled with allochthonous material indicate a sedimentation break between the gypsum and the overlying limestone. To support this thesis and to add new data on the age and palaeoenvironmental conditions of palaeokarst formation in the Bukovina region, palynological studies were carried out on material from the Zoloushka Cave. Palynofacies, sporomorphs and dinoflagellate cysts were studied. In total, over 70 sporomorph taxa and over 25 dinoflagellate cyst taxa have been identified in four samples collected from the filling of the palaeokarstic forms in the cave. The results of the analysis of sporomorphs and dinoflagellate cysts point to the formation of the palaeokarst during the sedimentation break that took place at the end of the late Badenian evaporitic cycle in the Western Ukraine region. The subsequent marine transgression led to the filling of the karst forms in gypsum with chemogenic carbonate material, precipitated from marine water (draperies) and with fine-grained, clastic material (pockets and fissures).
Źródło:
Annales Societatis Geologorum Poloniae; 2014, 84, 4; 297-322
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Sacred places in Lviv – their changing significance and functions
Autorzy:
Flaga, Małgorzata
Powiązania:
https://bibliotekanauki.pl/articles/634067.pdf
Data publikacji:
2014
Wydawca:
Uniwersytet Jagielloński. Wydawnictwo Uniwersytetu Jagiellońskiego
Tematy:
Lviv, Western Ukraine, religious diversity, functions of religious sites
Opis:
In the paper, issues of a multitude of functions of sacred places in Lviv are considered. The problem is presented on the example of selected religious sites that were established in distinct periods of the development of the city and refers to different religious denominations. At present, various functions are mixing in the sacred complexes of Lviv. The author tries to formulate some general conclusions concerning their contemporary role and leading types of activity. These findings are based, most of all, on analyses of the facts related to the history of Lviv, circumstances of its foundation, various transformations, and modern functions of the selected sites.
Źródło:
Prace Geograficzne; 2014, 137
1644-3586
Pojawia się w:
Prace Geograficzne
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Structural and Functional Bases of Formational, Institutional and Procedural Mechanism Using Power Resources of Stalin’s Totalitarian Regime in Western Ukraine at the Final Stage of the Second World War
Autorzy:
DOKASH, Oksana Yuriivna
Powiązania:
https://bibliotekanauki.pl/articles/519883.pdf
Data publikacji:
2014
Wydawca:
Uniwersytet Mikołaja Kopernika w Toruniu. Wydawnictwo UMK
Tematy:
Western Ukraine
World War II
Stalin’s regime
repressive and punitive organs
political violence
Opis:
The presented scientific, theoretical and practical aspects of the topic are considered an important prerequisite for understanding the causes and results of the mass use of the deportation repressive tool in the intensive consolidation of Stalin’s totalitarian regime in “class hostile environment” and the consequences of such a policy for the western region development, particularly at modern stage, including the Ukrainian political nation-building and the independent Ukrainian state, which is now experiencing challenges and threats that are rooted in the totalitarian past. Stalinism, as a particular political regime, was established in the western regions of Ukraine at the final stages of World War II and can be defined as a kind of left extremist totalitarianism. The main components of the efficiency of the Stalinist totalitarian regime based on the mass use of political violence and terror through the branched structure of repressive secret police. Functions of the NKVS, NKVD, prosecutors, and courts followed the strategic objectives of Stalin’s totalitarian regime in a hostile social and national environment in Western Ukraine in the complex military and political conditions of the final phase of World War II. Effective and timely implementation of policy priorities of Stalinism in the region allowed to create an appropriate institutional and procedural system, which was based on the large-scale use of political violence and employed such characteristic tools as terror, repression, deportation.
Źródło:
Historia i Polityka; 2014, 12(19); 23-32
1899-5160
2391-7652
Pojawia się w:
Historia i Polityka
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The main stages of the history of research of the western area of the Trypillian culture
Główne etapy historii badań zachodniego obszaru kultury trypolskiej
Autorzy:
Skakun, Natalya
Terekhina, Vera
Tsvek, Elena
Powiązania:
https://bibliotekanauki.pl/articles/498138.pdf
Data publikacji:
2014
Wydawca:
Uniwersytet Rzeszowski. Instytut Archeologii Uniwersytetu Rzeszowskiego. Muzeum Okręgowe w Rzeszowie
Tematy:
Trypillian culture
Western Ukraine
the history of research
Opis:
The history of archaeological research on the Trypillian sites in the western regions of Ukraine can be subdivided into four stages, each of which is marked by certain achievements. The first explorations resulted in the discovery of new archaeological objects, which gave rise to the discussion about the interpretation of constructions and functions of the settlements. The questions related to chronology, periodization, and excavation methodology were discussed as well. However, this activity was irregular and spontaneous, and the materials of many sites were scattered over different museums of Europe. The later stages of research gave very important data about the material and sacral components of the Trypillian culture, as well as its development, ways of adaptation to natural conditions, relative chronology of the sites, and their distribution. In the last years, the systematic excavations conducted at the reference site of Bodaki shed an important light on the economic basics of Trypillia. They also gave new materials for reconstructing the connections between the north-western and central areas of the culture, and its connections with the coeval farming-herding cultures of Europe.
Źródło:
Analecta Archaeologica Ressoviensia; 2014, 9; 267-298
2084-4409
Pojawia się w:
Analecta Archaeologica Ressoviensia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The Ukrainian Diaspora and the Helsinki Process (Late 1980s – Early 1990s)
Autorzy:
NEDUZHKO, Yury Victorovich
Powiązania:
https://bibliotekanauki.pl/articles/519614.pdf
Data publikacji:
2014
Wydawca:
Uniwersytet Mikołaja Kopernika w Toruniu. Wydawnictwo UMK
Tematy:
freedom
democracy
human rights
Ukrainian diaspora
Western countries
Ukraine
Opis:
This article shows the struggle of the Ukrainian diaspora for the human rights in Ukraine. It analyses international and informational activity of the Ukrainian society in Western countries, which has the aim to guarantee freedom and democracy in Ukraine.
Źródło:
Historia i Polityka; 2014, 12(19); 83-95
1899-5160
2391-7652
Pojawia się w:
Historia i Polityka
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-15 z 56

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