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Bibliografia publikacji pracowników
Państwowej Szkoły Wyższej w Białej Podlaskiej

Baza tworzona przez Bibliotekę Akademii Bialskiej im. Jana Pawła II.


Zapytanie: ANDREJCZUK WIACZESŁAW
Liczba odnalezionych rekordów: 22



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1/22
Nr opisu: m karst in the Western Ukraine occurs in the southwestern outskirt of the Eastern European Craton and is a model example of evolution of intrastratal karst and of artesian transverse speleogenesis in this lithology. Speleogenesis commenced in the regionally extensive confined Miocene aquifer system, in which the Middle Miocene (Badenian) gypsum bed is sandwiched between two "normal" aquifers with diffused permeability. Speleogenesis developed due to ascending leakage across the gypsum induced by valleys incising into the upper confining sequence. Large gypsum caves in the region (including the five longest gypsum caves in the world) are generally stratiform multi-story mazes of passages developed along vertical and steeply inclined fissures. Cave patterns in plan and the cross section are variable depending on fracture stratigraphy, patterns and connectivity, areal distribution of recharge (at the lower contact) and discharge (at the upper contact) points, and local hydrodynamic conditions and history. Patterns and meso-morphology of the caves clearly demonstrate functional organization that evolved in response to ascending hydraulic communication between the aquifers in the Miocene aquifer system, reflecting the complex pattern of trans
Tytuł pracy w innym języku: The gypsum karst in the Western Ukraine occurs in the southwestern outskirt of the Eastern European Craton and is a model example of evolution of intrastratal karst and of artesian transverse speleogenesis in this lithology. Speleogenesis commenced in the regionally extensive confined Miocene aquifer system, in which the Middle Miocene (Badenian) gypsum bed is sandwiched between two "normal" aquifers with diffused permeability. Speleogenesis developed due to ascending leakage across the gypsum induced by valleys incising into the upper confining sequence. Large gypsum caves in the region (including the five longest gypsum caves in the world) are generally stratiform multi-story mazes of passages developed along vertical and steeply inclined fissures. Cave patterns in plan and the cross section are variable depending on fracture stratigraphy, patterns and connectivity, areal distribution of recharge (at the lower contact) and discharge (at the upper contact) points, and local hydrodynamic conditions and history. Patterns and meso-morphology of the caves clearly demonstrate functional organization that evolved in response to ascending hydraulic communication between the aquifers in the Miocene aquifer system, reflecting the complex pattern of transverse flow across the gypsum. This study demonstrates that artesian transverse speleogenesis is of fundamental im : OTHER
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  • recharge (at the lower contact) and discharge (at the upper contact) points, and local hydrodynamic conditions and history. Patterns and meso-morphology of the caves clearly demonstrate functional organization that evolved in response to ascending hydraulic communication between the aquifers in the Miocene aquifer system, reflecting the complex pattern of transverse flow across the gypsum. This study demonstrates that artesian transverse speleogenesis is of fundamental importance to groundwater circulation in the region-wide Miocene aquifer system. It has important implications for regional and site-specific hydrogeology, the origin of large bioepigenetic sulfur deposits, and assessment of collapse/subsidence hazard. The style and principal characteristics of the large maze caves in the gypsum karst in the Western Ukraine are not specific to dissolution of sulfate rocks but exemplify general regularities of artesian transverse speleogenesis that are applicable to other lithologies including carbonates.^aArtesian speleogenesis^amaze caves^agypsum karst^aWestern Ukraine


    2/22
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    3/22
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    Autorzy: , kras morskikras tropikalnykrajobraz krasowyarchipelagAzja południowo-wchodniaDissertations of Cultural Landscape Comission.
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    Tytuł wynalazku: kras morskikras tropikalnykrajobraz krasowyarchipelagAzja południowo-wchodniaDissertations of Cultural Landscape Comission
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  • 4/22
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    Index Copernicus: ^80000-0002-7311-7061^w ^31^41;1^6tak^70000000013funau1^0^aSokołowska Barbara^b017^cWNZS0101^dWNZS^e*^f017^g0000000178^kSokołowska Barbara^2Sokołowska^5Barbara^iSokołowska^jBarbara^1Barbara^9B^lZakład Pielęgniarstwa^mWydział Nauk o Zdrowiu i Nauk Społecznych^oSokołowska Barbara^p925078^t0000002956^80000-0002-9711-122X^w ^32^42;2^6tak^70000000178funau2^0^a2^bWNET:1;1:1;1:1;1*WNZS:1;1:1;1:1;1^cUNIT:2;0:2;0:2;0^d2^e2^f2^gtak^aBertrandt
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  • 002-7311-7061^w ^31^41;1^6tak^70000000013funau1^0^aSokołowska Barbara^b017^cWNZS0101^dWNZS^e*^f017^g0000000178^kSokołowska Barbara^2Sokołowska^5Barbara^iSokołowska^jBarbara^1Barbara^9B^lZakład Pielęgniarstwa^mWydział Nauk o Zdrowiu i Nauk Społecznych^oSokołowska Barbara^p925078^t0000002956^80000-0002-9711-122X^w ^32^42;2^6tak^70000000178funau2^0^a2^bWNET:1;1:1;1:1;1*WNZS:1;1:1;1:1;1^cUNIT:2;0:2;0:2;0^d2^e2^f2^gtak^aBertrandt



    5/22
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  • 6/22
    Nr opisu: ^aZoloushka Cave, the third longest gypsum cave in the world (92 km) and the world's largest gypsum cave by volume (>0.7 million cubic meter), is an outstanding example of a large maze cave formed in a multi-story artesian aquifer system due to the upward leakage between the aquifers across a soluble unit. Although local settings and evolution caused some peculiar features in speleogenesis, as compared to other large maze caves in Western Ukraine, these singularities provide further insights on variants and mechanisms of both regional and general models of hypogene artesian speleogenesis. The cave is located in the area where the host aquifer system is generally confined until present, but in one of the more uplifted tectonic blocks where the gypsum was partially incised by the nearby valley of the Prut River during the Holocene and rapidly drained due to the quarry operations since 1946. The cave experienced considerable modifications and transformations in the course of the recent transition to unconfined conditions and subsequent artificial dewatering. The geomorphological breaching of the confined aquifer system in the cave area occurred in the Holocene, i.e., later than in the area where most other large maze caves in the region are located.
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    Słowa kluczowe ang.: _PUBLICATION^ePUBLISHER_WEBSITE^aZoloushka Cave, the third longest gypsum cave in the world (92 km) and the world's largest gypsum cave by volume (>0.7 million cubic meter), is an outstanding example of a large maze cave formed in a multi-story artesian aquifer system due to the upward leakage between the aquifers across a soluble unit. Although local settings and evolution caused some peculiar features in speleogenesis, as compared to other large maze caves in Western Ukraine, these singularities provide further insights on variants and mechanisms of both regional and general models of hypogene artesian speleogenesis. The cave is located in the area where the host aquifer system is generally confined until present, but in one of the more uplifted tectonic blocks where the gypsum was partially incised by the nearby valley of the Prut River during the Holocene and rapidly drained due to the quarry operations since 1946. The cave experienced considerable modifications and transformations in the course of the recent transition to unconfined conditions and subsequent artificial dewatering. The geomorphological breaching of the confined aquifer system in the cave area occurred in the Holocene, i.e., later than in the area where most other large maze caves in the region are located. A relatively stable position of the water table in the upper part of the gypsum during most of the Holocene caused pronounced widening of passages, which determined the anomalously large size of passages and high indices of areal karstification in some regions of the cave. The most intense development of conduits occurred in areas where the input of freshwater fr
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  • e 1946. The cave experienced considerable modifications and transformations in the course of the recent transition to unconfined conditions and subsequent artificial dewatering. The geomorphological breaching of the confined aquifer system in the cave area occurred in the Holocene, i.e., later than in the area where most other large maze caves in the region are located. A relatively stable position of the water table in the upper part of the gypsum during most of the Holocene caused pronounced widening of passages, which determined the anomalously large size of passages and high indices of areal karstification in some regions of the cave. The most intense development of conduits occurred in areas where the input of freshwater from the lower aquifer was more abundant. Quarry operation and accompanying groundwater withdrawal during the last 70 years caused drastic and rapid transformations in the cave environment.^aArtesian speleogenesis^agypsum karst^aWestern Ukraine^aZoloushka Cave


    7/22
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    Tytuł równoległy: 1Andrejczukoriginal-article998899009999.0001897-5100003HimalajeGimalaiActa Geographica Silesiana20161897-51002016/2017Andrejczuk, WiaczesławHimalajeHimalayaKopia dostępna w Sekcji Bibliometrii.FINAL_PUBLISHEDThe article is the first of two parts of physical-geographical generalization devoted to the complex characteristics of the natural environment of the Himalayas. In turn de : WNZS:1;0:1;0:1;0 : Wiaczesław : Oryginalny artykuł naukowyACPartykuł w czasopiœmie polskim : 9999495.0000005.000PUNKTACJA KBNPUNKTACJA MINISTERSTWA5.000PUNKTACJA MNISW4L : 009994.000 : B : 003 : szkic fizycznogeograficzny - przyroda nieożywiona : fiziko-geografičeskij očerk - neživaâ priroda : CC-BY-ND
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    8/22
    Nr opisu: ^bthe physio-geographical review - inanimate nature
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    Tytuł wynalazku: regionHimalaya, the physio-geographical review - inanimate nature
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    Słowa kluczowe ang.: raphy^aregion^aregion^aHimalaya^bthe physio-geographical review - inanimate nature
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    9/22
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    10/22
    Nr opisu: labirynt jaskiniowy przez dłuższy czas jest zawodniony.^ajaskinie labiryntowe^amaze caves^aColumned halls as a stage in morphological development of maze caves. The article describes the original speleomorphological phenomenon - columned halls, developed into one of the world's largest maze caves in gypsum - Zoloushka Cave (Ukraine-Moldova). The mechanism of their development lies in the fact that when relatively long-term development of the labyrinth and close proximity of the neighbouring galleries, walls sharing them become thinner - until the disappearance and merging of adjacent passages into a common void space. Columned halls are developing in the conditions when cave labyrinth is filled with water for long time. This phenomenon is largely unique.^amorfologia jaskiń^acave morphology^aColumned halls as a stage in morphological develop
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    Tytuł wynalazku: jaskinie labiryntowemaze cavesColumned halls as a stage in morphological development of maze caves. The article describes the original speleomorphological phenomenon - columned halls, developed into one of the world's largest maze caves in gypsum - Zoloushka Cave (Ukraine-Moldova). The mechanism of their development lies in the fact that when relatively long-term development of the labyrinth and close proximity of the neighbouring galleries, walls sharing them become thinner - until the disappearance and merging of adjacent passages into a common void space. Columned halls are developing in the conditi
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    Słowa kluczowe ang.: ozwijają się w warunkach, kiedy labirynt jaskiniowy przez dłuższy czas jest zawodniony.^ajaskinie labiryntowe^amaze caves^aColumned halls as a stage in morphological development of maze caves. The article describes the original speleomorphological phenomenon - columned halls, developed into one of the world's largest maze caves in gypsum - Zoloushka Cave (Ukraine-Moldova). The mechanism of their development lies in the fact that when relatively long-term development of the labyrinth and close proximity of the neighbouring galleries, walls sharing them become thinner - until the disappearance and merging of adjacent passages into a common void space. Columned halls are developing in the conditions when cave labyrinth is filled with water for long time. This phenomenon is largely unique.^amorfologia jaskiń^acave morphology^aColumned halls as a stage in morphological development of maze caves
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    11/22
    Autorzy: , krajobraz krasowykarst landscapeochrona jaskińprotection of cavespodejście systemowesystem approach.
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    Index Copernicus: and vertical interactions between them occurring in the vertical cross section, and the horizontal, i.e.geo-complex structure - complex units (cells) which build the landscape on the lateral plane, together with interactions between them. It has been shown that the two-fold structure of the karst landscape is crucial for its functioning, development and self-regulation. Because of the fact that the subterranean part of the landscape is closely correlated with the terraneous part, the principles of the karst landscape and caves protection should be based on a systemic approach. Two major principles have been considered. The first one says that the preservation of the two-fold geosystem must be complex and all-embracing: we should not preserve a cave pattern without taking care of the surface above it, or conversely: preserve the terraneous karst geocomplex we may not neglecting the cavities beneath it. The second rule (principle) suggests that while determining the lateral (horizontal) boundaries and buffer zone of the geosystem selected for preservation, it is necessary to take into account the extent of the paragenetic and paradynamic connections between the elements-geocomplexes comprising KL.^akrajobraz krasowy^akarst landscape^aochrona jaskiń^aprotection of caves^apodejście systemowe^asystem approach
    Słowa kluczowe ang.: landscape and vertical interactions between them occurring in the vertical cross section, and the horizontal, i.e.geo-complex structure - complex units (cells) which build the landscape on the lateral plane, together with interactions between them. It has been shown that the two-fold structure of the karst landscape is crucial for its functioning, development and self-regulation. Because of the fact that the subterranean part of the landscape is closely correlated with the terraneous part, the principles of the karst landscape and caves protection should be based on a systemic approach. Two major principles have been considered. The first one says that the preservation of the two-fold geosystem must be complex and all-embracing: we should not preserve a cave pattern without taking care of the surface above it, or conversely: preserve the terraneo ;
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    12/22
    Nr opisu: al types widespread on the walls of gypsum cave Zoloushka. They reflect development of the cave in phreatic conditions. Original pyramidal-grooved microforms were found on the walls of cylindrical wells, which represent by themselves an open pressure cupolas. According to the author, microforms are the result of stream downward movement of water on the walls in closed circulation environment of blind cupola and can testify in favor of the development of the cave in hypogenic conditions.^ażłobki krasowe^akarren^ajaskinia Zołuszka^aZoloushka Cave^aAn unique type of corrosional formations in the Zoloushka Cave (Ukraine-Moldova)
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    Tytuł wynalazku: żłobki krasowekarrenjaskinia ZołuszkaZoloushka CaveAn unique type of corrosional formations in the Zoloushka Cave (Ukraine-Moldova)
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    Zasięg terytorialny: kras hipogenic
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    Słowa kluczowe ang.: oforms of different morphological types widespread on the walls of gypsum cave Zoloushka. They reflect development of the cave in phreatic conditions. Original pyramidal-grooved microforms were found on the walls of cylindrical wells, which represent by themselves an open pressure cupolas. According to the author, microforms are the result of stream downward movement of water on the walls in closed circulation environment of blind cupola and can testify in favor of the development of the cave in hypogenic conditions.^ażłobki krasowe^akarren^ajaskinia Zołuszka^aZoloushka Cave^aAn unique type of corrosional formations in the Zoloushka Cave (Ukraine-Moldova)
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    13/22
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    14/22
    Nr opisu: amethodology^aewolucja^aevolution^aśrodowisko geograficzne^ageographical environment^aabiosfera^aabiosphere^abiosfera^abiosphere^anoosfera^anoosphere^aglobastema^aglobastema^aGeoevolutional paradigm of the modern geography
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    Tytuł wynalazku: metodologiamethodologyewolucjaevolutionśrodowisko geograficznegeographical environmentabiosferaabiospherebiosferabiospherenoosferanoosphereglobastemaglobastemaGeoevolutional paradigm of the modern geography
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    Słowa kluczowe ang.: cal significance.^ametodologia^amethodology^aewolucja^aevolution^aśrodowisko geograficzne^ageographical environment^aabiosfera^aabiosphere^abiosfera^abiosphere^anoosfera^anoosphere^aglobastema^aglobastema^aGeoevolutional paradigm of the modern geography ; ;
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    15/22
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    Tytuł wynalazku: S. 11-13ČernivciAndrejczuk, WiaczesławKRASKopia dostępna w Sekcji Bibliometrii.krajobraz krasowystrefa przyrodniczaRegional aspects of floristic and faunistic researchers, Druk ART, materials of the second international scientific and practical conference, 24-25 April 2015
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    16/22
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    Seria: cave networksrandom walkHurst exponent
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    17/22
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    Tytuł pracy w innym języku: 998899009999.000003Słownik polsko-ukraiński oraz ukraińsko-polski podstawowych terminów i pojęć z zakresu nauki o krajobraziePol'sko-ukraïns'kij ta ukraïns'ko-pol'skij slovnik bazovih terminiv ta ponât' z landšaftoznavstvaBiała Podlaska106 s.Bibliogr. s. 93.978-83-64881-01-5Richling, AndrzejkrajobrazAndrejczuk, Wiaczesławterminologiasłownik : 99979920.0000020.000PUNKTACJA KBNPUNKTACJA MINISTERSTWA : 009979.000 : 007 : Wydawnictwo PSW JPII : il. kol. : 7
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    Strony: 998899009999.000003Słownik polsko-ukraiński oraz ukraińsko-polski podstawowych terminów i pojęć z zakresu nauki o krajobraziePol'sko-ukraïns'kij ta ukraïns'ko-pol'skij slovnik bazovih terminiv ta ponât' z landšaftoznavstvaBiała Podlaska106 s.Bibliogr. s. 93.978-83-64881-01-5Richling, AndrzejkrajobrazAndrejczuk, Wiaczesławterminologiasłownik, 99979920.0000020.000PUNKTACJA KBNPUNKTACJA MINISTERSTWA, 009979.000, 007, Wydawnictwo PSW JPII, il. kol., 7, 009999.000, 2016-02-03, 10:48, 2015, 24 cm, y, x, 009999.000201520152015Słownik polsko-ukraiński oraz ukraińsko-polski podstawowych terminów i pojęć z zakresu nauki o kr00000314380000002881PUBLIKACJAPEŁNA PUBLIKACJAMJPautorstwo monografii - j. polski lub inny poza kongres.AFILIACJA PODANAPOLUKRPRACA RECENZOWANA150, 2016-03-16, 15:12
    ISBN:
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    Charakterystyka merytoryczna: Andrzej Zdzisław Andrejczuk Wiaczesław Rudenko Leonid Czechnij WiktorMPAmonografia polska (autor)^a998899^b99979920.0000020.000PUNKTACJA KBNPUNKTACJA MINISTERSTWA^a009999.000^b009979.000^c009999.000^d009999.000201520152015Słownik polsko-ukraiński oraz ukraińsko-polski podstawowych terminów i pojęć z zakresu nauki o kr00000314380000002881PUBLIKACJAPEŁNA PUBLIKACJAMJPautorstwo monografii - j. polski lub inny poza kongres.AFILIACJA PODANAPOLUKRPRACA RECENZOWANA150^a003^b007^c2016-02-03, 10:48^d2016-03-16, 15:12^e3829019191^f3827888727^aSłownik polsko-ukraiński oraz ukraińsko-polski podstawowych terminów i pojęć z zakresu nauki o krajobrazie^aPol'sko-ukraïns'kij ta ukraïns'ko-pol'skij slovnik bazovih terminiv ta ponât' z landšaftoznavstva^aBiała Podlaska^bWydawnictwo PSW JPII^c2015^a106 s.^bil. kol.^c24 cm^aBibliogr. s. 93.^a978-83-64881-01-5^b7^aRichling, Andrzej^cy^akrajobraz^aAndrejczuk, Wiaczesław^cx^aterminologia^asłownik
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    Język publikacji: Leonid Czechnij WiktorMPAmonografia polska (autor)^a998899^b99979920.0000020.000PUNKTACJA KBNPUNKTACJA MINISTERSTWA^a009999.000^b009979.000^c009999.000^d009999.000201520152015Słownik polsko-ukraiński oraz ukraińsko-polski podstawowych terminów i pojęć z zakresu nauki o kr00000314380000002881PUBLIKACJAPEŁNA PUBLIKACJAMJPautorstwo monografii - j. polski lub inny poza kongres.AFILIACJA PODANAPOLUKRPRACA RECENZOWANA150^a003^b007^c2016-02-03, 10:48^d2016-03-16, 15:12^e3829019191^f3827888727^aSłownik polsko-ukraiński oraz ukraińsko-polski podstawowych terminów i pojęć z zakresu nauki o krajobrazie^aPol'sko-ukraïns'kij ta ukraïns'ko-pol'skij slovnik bazovih terminiv ta ponât' z landšaftoznavstva^aBiała Podlaska^bWydawnictwo PSW JPII^c2015^a106 s.^bil. kol.^c24 cm^aBibliogr. s. 93.^a978-83-64881-01-5^b7^aRichling, Andrzej^cy^akrajobraz^aAndrejczuk, Wiaczesław^cx^aterminologia^asłownik,
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    KTACJA KBNPUNKTACJA MINISTERSTWA^a009999.000^b009979.000^c009999.000^d009999.000201520152015Słownik polsko-ukraiński oraz ukraińsko-polski podstawowych terminów i pojęć z zakresu nauki o kr00000314380000002881PUBLIKACJAPEŁNA PUBLIKACJAMJPautorstwo monografii - j. polski lub inny poza kongres.AFILIACJA PODANAPOLUKRPRACA RECENZOWANA150^a003^b007^c2016-02-03, 10:48^d2016-03-16, 15:12^e3829019191^f3827888727^aSłownik polsko-ukraiński oraz ukraińsko-polski podstawowych terminów i pojęć z zakresu nauki o krajobrazie^aPol'sko-ukraïns'kij ta ukraïns'ko-pol'skij slovnik bazovih terminiv ta ponât' z landšaftoznavstva^aBiała Podlaska^bWydawnictwo PSW JPII^c2015^a106 s.^bil. kol.^c24 cm^aBibliogr. s. 93.^a978-83-64881-01-5^b7^aRichling, Andrzej^cy^akrajobraz^aAndrejczuk, Wiaczesław^cx^aterminologia^asłownik

    18/22
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    Index Copernicus: jców National Park)^aMeždunarodna naučno-praktičeska konferenciâ "Zaŝiteni karstovi teritorii - obrazovanie i obučenie", 23-26 sentabri 2015 goda, Sofiâ^bzbornik dokladi^aS. 22-31^aSofiâ^bTerart^c2015^a978-954-9531-26-8^aAndrejczuk, Wiaczesław^cy^aeducation^aKopia dostępna w Sekcji Bibliometrii.^aprotected area^aatmosphere-land interaction^aglobal radiation^anet radiation^aCracow Upland^aInternational Scientific-Practical Conference "Protected karst territories - education and training" Bulgaria, Sofia, September 23-26, 2015^bproceedings
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  • 19/22
    Nr opisu:
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    Wskaźnik Impact Factor ISI: ro^jAgnieszka^1Agnieszka^9A^lObcy afilujšcy WNZS^mWydział Nauk o Zdrowiu i Nauk Społecznych^oMozyro Agnieszka^p930644^t0000015158^w ^32^40;2^6tak^70000000280funau2^0^a2^bWNZS:2;0:1;1:2;0^cUNIT:2;0:1;1:2;0^d2^e1^f2^gtak^aBłaszczak
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    20/22
    Autorzy: .
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    Opis nie został sporządzony z autopsji: Speleol
    Słowa kluczowe ang.: 009540^w ^31^41;1^6tak^70000000086funau1^0^a1^bWNET:1;0:1;0:1;0^cUNIT:1;0:1;0:1;0^d1^e1^f1^gtak^aKowalska
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    21/22
    Nr opisu: n 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).^apalinologia^apalynology^asporomorfy^asporomorphs^abruzdnice^adinoflagellate cysts^ajaskinia^acaves^aZachodnia Ukraina^aWestern Ukraine^aPlatforma Wschodnioeuropejska^aEastern European Platform^abaden^aBadenian
    Autorzy: , .
    Tytuł czasopisma:
    Tytuł wynalazku: 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 resu, OTHER
    Charakterystyka wg MNiSW:
    Słowa kluczowe ang.: e 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).^apalinologia^apalynology^asporomorfy^asporomorphs^abruzdnice^adinoflagellate cysts^ajaskinia^acaves^aZachodnia Ukraina^aWestern Ukraine^aPlatforma Wschodnioeuropejska^aEastern European Platform^abaden^aBadenian
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  • n 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).^apalinologia^apalynology^asporomorfy^asporomorphs^abruzdnice^adinoflagellate cysts^ajaskinia^acaves^aZachodnia Ukraina^aWestern Ukraine^aPlatforma Wschodnioeuropejska^aEastern European Platform^abaden^aBadenian


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    22/22
    Autorzy: .
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