Wyniki wyszukiwania - Biblioteka Nauki

1

Civil society structures in Ukraine: formation and development in the latter half of 16th to 19th centuries

100%

Panfiłova T.

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2016

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nr 13

323-341

EN

Based on the sources and critical consideration of historiography of the problem, the author defines regularities and specific features of the formation of structures of Ukrainian civil society, as a factor which bolstered Ukrainian national idea.

2

Pereselennija Polakiw iz Zachidnoij Ukraijiny i Zachidnoij Bilorusi do Polszy w 1944-1946 r.: poribjal'nij analiz

100%

Samborskij J.

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nr 3: Historia

175-188

EN

The article presents a comparative analysis of the dynamics and progress of resettlement of the Polish population of the Western Ukraine and Western Belarus to Poland in 1944–1946. It also considers the repressive actions of the Soviet punitive organs regarding Poles in order to accelerate the resettlement action. The author establishes that despite the fact that the mentioned action was initiated in Moscow at the highest political level, in western regions of Ukraine and Belarus it proceeded in different ways and had its own distinctive features in each one.

3

The main stages of the history of research of the western area of the Trypillian culture

100%

Skakun N. , Terekhina V. , Tsvek E.

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tom 9

267–298

EN

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.

4

Remarks on the correlation of tectonic blocks in the foreland of the East European Craton in Poland with those in Ukraine

88%

Mizerski W. , Stupka O. , Olczak-Dusseldorp I.

Geological Quarterly

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2016

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tom Vol. 60, No. 1

124--132

EN

According to common interpretations, two narrow crustal blocks are supposed to occur on the south-western edge or in the foreland of the East European Craton. The first one, bounded on the NE by the Nowe Miasto-Radom-Rava Ruska fault system, and on the SW by the Holy Cross Fault, stretches NW-SE from the Łysogóry-Radom region in Poland to the Rava Ruska Zone in Ukraine. The second one, bounded on the NE by the Holy Cross Fault, and from the SW by the Chmielnik-Ryszkowa Wola–Krakovets fault zone, is thought to tie together the Kielce area of the Holy Cross region with the Kokhanivka Zone in Ukraine. Both these blocks may have formed in connection with the development of regional listric faults during Precambrian asymmetric stretching of the Baltica continent, and were part of the marginal zone of the East European Craton. The sedimentary development of the blocks can be comparable to the Blake Plateau off the Florida coast. Both the Paleozoic sections and tectonic deformation styles in the Polish and Ukrainian segments of these blocks are different. Paleozoic tectonic structures of the Holy Cross region have a southern vergence, while the Paleozoic rocks of the Rava Ruska and Kokhanivka regions in western Ukraine are thrust towards the NE. This demonstrates the different tectonic evolution of the Paleozoic succession between the Holy Cross region and western Ukraine, and makes questionable the genetic relationships between these two regions. In this situation, the tectonic blocks of the foreland should be considered heterogeneous. Structural-facies evidence suggests that the SW boundary of the East European Craton should be moved at least to the Chmielnik–Ryszkowa Wola-Krakovets fault.

5

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

88%

DOKASH O. Y.

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nr 12(19)

23-32

EN

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.

6

Palaeomagnetic studies of the loess-palaeosol sequence from the Kolodiiv section (East Carpathian Foreland, Ukraine)

88%

Nawrocki J. , Boguckyj A. , Łanczont M.

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2007

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tom Vol. 51, No 2

161-166

EN

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.

7

1-D modelling of the hydrocarbon generation history of the Jurassic source rocks in the Tarnogród–Stryi area (SE Poland – western Ukraine)

75%

Kosakowski P. , Wróbel M. , Koltun Y. V.

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tom Vol. 81, No 3

473-485

EN

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.

8

Facies of the Upper Jurassic–Lower Cretaceous sediments in the basement of the Carpathian Foredeep (western Ukraine)

75%

Krajewski M. , Król K. , Olszewska B. , Felisiak I. , Skwarczek M.

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tom Vol. 81, No 3

291-307

EN

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.

9

Precambrian and Palaeozoic basement of the Carpathian Foredeep and the adjacent Outer Carpathians (SE Poland and western Ukraine)

75%

Buła Z. , Habryn R.

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tom Vol. 81, No 3

221-239

EN

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.

10

Limpet-shaped gastropods of the genus Diodora (Vetigastropoda: Fissurellidae) from the Middle Miocene of Western Ukraine

63%

Dell'Angelo B. , Sosso M. , Anistratenko O. , Anistratenko V.

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2017

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tom Vol. 67, no. 2

235--247

EN

The genus Diodora Gray, 1821 is widely represented in the Middle Miocene of the Central Paratethys with specimens usually attributed to D. graeca (Linnaeus, 1758) or D. italic (Defrance, 1820), well-known recent species of the Atlantic / Mediterranean Basin. In samples from the Upper Badenian of Western Ukraine we found two clusters of Diodora specimens, showing a similarity with these species, but a review of shell diagnostic characters using a statistical approach has revealed their clear conchological separateness. The first species from Varovtsi and Horodok is attributed herein to D. nodosa (Eichwald, 1830), whereas the second species from Maksymivka is described as a new species, D. stalennuyi sp. nov. We consider that these molluscs inhabited the Polish-Ukrainian marginal part of the Late Badenian Basin. Detailed descriptions of the protoconch and teleoconch morphology of the taxa involved, including SEM images, are presented.

11

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

63%

Andreychouk V. , Worobiec E. , Gedl P. , Worobiec G.

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2014

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tom Vol. 84, No. 4

297--322

EN

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).

12

Semantic aspects of architectural dominants transformation in Western Ukrainian cities in the 1940s–1950s

63%

Isupova M.

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2020

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tom nr 43

261--268

EN

This article focuses on the semantic aspects of architectural dominants transformation in Western Ukraine in the second half of the 1940s - 1950s. On the example of cities-regional centres, such as Rivne, Lutsk and Ternopil, the so-called "socialist reconstruction", which created new dominants in the urban silhouette, embodying the Soviet ideological principles in the architectural space is examined.

13

Tożsamość ukraińskiego Lwowa: jak rodził się matecznik kulturowego oporu

63%

Urban M.

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nr 3

135-148

UK

Мета статті – представити та пояснити процес формування ідентичності сучасного Львова. Проблему досліджено відповідно до тези про те, що культурні фактори можуть безпосередньо впливати на політику. У статті досліджено основні культурні образи, які творять ідентичність міста, особливо ті, які є зразком для наслідування, і ті, які сприймаються як протилежність бажаного стану справ.

EN

The aim of the essay is to present and explain the process of creation of the identity of contemporary Lviv. According to the author, in order to analyze this process, it is necessary to remember about cultural factors which can influence political affairs. The essay includes an examination of the main cultural images composing the identity of the city, especially these believed to be attractive for the presented community, as well and these which are treated as the points of repulsion.

14

Disclosure of the value of urban heritage in the Western Ukraine as a way to its preservation

63%

Lukomska Z. , Polishchuk L. , Lukomska H.

Czasopismo Techniczne. Architektura

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2015

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tom Y. 112, iss. 7-A

39--50

EN

This paper presents the problem concerning preservation of urban heritage by developing the concept of regeneration of historic environment and implementation of specific programmes concerning its protection and preservation. Proposed programmes, concerning protection and preservation of historic potential of the described towns will enhance the value of urban heritage, will create an opportunity to inform the public about historic aspects of the urban development, and reduce the possibility of their mistreating – and inapt attitudes towards historic sites.

PL

W artykule przedstawiono sposób ochrony historycznych układów miejskich poprzez opracowanie urbanistycznych koncepcji ich rewaloryzacji w oparciu o badania archiwalne i studia terenowe. Sporządzanie konkretnych programów konserwatorskich sprzyja zachowaniu i podkreśleniu architektoniczno-urbanistycznych wartości dziedzictwa historycznego. Pozwoli to na uświadomienie społeczeństwu historycznego znaczenia tego dziedzictwa, co doprowadzić może do jego społecznej akceptacji i zapobieżeniu dalszej destrukcji.

15

The role of the tenement housing development in the urban structure of Western and Central Ukraine during the Secession era

63%

Orlenko M. , Ivashko Y.

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tom nr 27

52--60

EN

The principles of the formation of the urban planning space of cities of Western and Central Ukraine during the period of Secession, the role of profitable residential development in the city structure are analyzed. The differences between the Secession development of Lviv, Chernivtsi, Stanislaviv and Kiev are identified, examples of the main ensembles and individual buildings are given. Using the example of the house of architect Władysław Horodecki (the so-called House with Chimaeras), we have highlighted the specific features of restoration of buildings of the era of Secession.

16

Microbial gas system and prospectives of hydrocarbon exploration in Miocene strata of the Polish and Ukrainian Carpathian Foredeep

51%

Kotarba M. J. , Peryt T. M. , Koltun Y. V.

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tom Vol. 81, No 3

523-548

EN

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.