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Nájdených záznamov: 17  
Vaša požiadavka: Autor-kód záznamu = "^umb_un_auth 0002970^"
  1. NázovReply to the comment on "variable structural styles and tectonic evolution of an ancient backstop boundary: the Pieniny Klippen Belt of the Western Carpathians" by Pelech et al. (this issue)
    Aut.údajeDušan Plašienka, Jana Bučová, Viera Šimonová
    Autor Plašienka Dušan (33,333%)
    Spoluautori Bučová Jana (33,334%)
    Šimonová Viera 1977- (33,333%) UMBFP01 - Katedra geografie a geológie
    Zdroj.dok. International Journal of Earth Sciences : Geologische Rundschau : journal of Geologische Vereinigung. Vol. 112, no. 4 (2023), pp. 1323-1329. - Berlín : Springer Nature, 2023
    Kľúč.slová geologické štruktúry   výskumy   bradlové pásma  
    Heslá geogr. Západné Karpaty (pohorie)
    Pieniny Klippen Belt
    Form.deskr.úvodníky - editorials
    Jazyk dok.angličtina
    KrajinaNemecko
    URLLink na plný text
    Kategória publikačnej činnosti GII
    Číslo archívnej kópie53517
    Katal.org.BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici
    Báza dátxpca - PUBLIKAČNÁ ČINNOSŤ
    OdkazyPERIODIKÁ-Súborný záznam periodika
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  2. NázovBackstop-edge tectonics: The Pieniny klippen belt of NE Slovakia
    Aut.údajeDušan Plašienka, Jana Bučová, Viera Šimonová
    Autor Plašienka Dušan (40%)
    Spoluautori Bučová Jana (30%)
    Šimonová Viera 1977- (30%) UMBFP01 - Katedra geografie a geológie
    Zdroj.dok. 18th meeting of the Central European tectonic studies groups & 25th meeting of the Czech tectonic studies group : book of abstracts : CETEG. S. 109-110. - Bratislava : Univerzita Komenského v Bratislave, 2021 / Gregáňová Margaréta ; Molčan Matejová Marína ; Šimonová Viera 1977- ; Meeting of the Central European tectonic studies groups medzinárodná konferencia ; Meeting of the Czech tectonic studies group medzinárodná konferencia
    Kľúč.slová tektonika - tectonic   bradlové pásma  
    Heslá geogr. Pieninské bradlové pásmo
    Form.deskr.abstrakty - abstracts
    Jazyk dok.angličtina
    KrajinaSlovenská republika
    Kategória publikačnej činnosti AFH
    Číslo archívnej kópie51327
    Katal.org.BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici
    Báza dátxpca - PUBLIKAČNÁ ČINNOSŤ
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  3. NázovVariable structural styles and tectonic evolution of an ancient backstop boundary: the Pieniny Klippen Belt of the Western Carpathians
    Aut.údajeDušan Plašienka ... [et al.]
    Autor Plašienka Dušan (60%)
    Spoluautori Bučová Jana (20%)
    Šimonová Viera 1977- (20%) UMBFP01 - Katedra geografie a geológie
    Zdroj.dok. International Journal of Earth Sciences : Geologische Rundschau : journal of Geologische Vereinigung. Vol. 109, no. 4 (2020), pp. 1355-1376. - Berlín : Springer Nature, 2020 ; Conference on Thermal and Mechanical Evolution of Collisional and Accretionary Orogens konferencia
    Kľúč.slová cretaceous volcanism   evolúcia - evolution  
    Heslá geogr. Západné Karpaty (pohorie)
    Pieniny Klippen Belt
    Form.deskr.články - journal articles
    Jazyk dok.angličtina
    KrajinaNemecko
    AnotáciaThe Pieniny Klippen Belt (PKB) and adjoining zones form a narrow, but lengthy belt that separates the Cretaceous nappe stack of the Central (Austroalpine) and the Cenozoic accretionary wedge of the External Western Carpathians (Flysch Belt). The PKB shares units and structures of both, in addition to the distinctive Oravic units, derived from a continental fragment in the Middle Penninic position. In map view, the northward-convex PKB consists of two branches—the western one striking roughly SW–NE and the eastern one oriented in the NW–SE direction. The western branch experienced a continuous NW–SE convergence and forward accretion of units derived from the foreland plate during the Late Cretaceous up to Oligocene. The developing accretionary wedge was supported by the backstop of the Central Carpathians. In contrast, the eastern branch originated by separation of PKB units and their dextral translation along the NE margin of the Central Carpathian block in the Late Eocene. During the Miocene reorganization of plate movements in the Carpathian area, the situation reversed. The eastern, formerly dextral transform margin was converted to the frontal backstop of the eastern part of the accretionary wedge. In contrast, the western, previously orthogonally convergent branch was affected by along-strike sinistral movements. Despite these considerable kinematic changes, the PKB remained fixed to both backstop edges and records deformation structures and associated sediments differentiated into several evolutionary stages.
    Kategória publikačnej činnosti ADC
    Číslo archívnej kópie48914
    Katal.org.BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici
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    OdkazyPERIODIKÁ-Súborný záznam periodika
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  4. NázovNucleation and amplification of doubly-plunging anticlines - the Butkov pericline case study (Manín Unit, Western Carpathians)
    Aut.údajeDušan Plašienka, Viera Šimonová, Jana Bučová
    Autor Plašienka Dušan (50%)
    Spoluautori Šimonová Viera 1977- (25%) UMBFP01 - Katedra geografie a geológie
    Bučová Jana (25%)
    Zdroj.dok. Geologica Carpathica. Vol. 69, no. 4 (2018), pp. 365-381. - Bratislava : Veda, 2018
    Kľúč.slová štruktúrna analýza - structural analysis  
    Heslá geogr. Západné Karpaty (pohorie)
    Manínska tiesňava (Súľovské vrchy, Slovensko)
    Butkov - (vrch)
    Jazyk dok.angličtina
    KrajinaSlovenská republika
    Systematika 55
    AnotáciaThe Manín Unit represents a transitional tectonic element between the Central Western Carpathians and the Pieniny Klippen Belt. The overall map-view structure of the Manín Unit is dominated by elliptical antiforms composed of comparatively competent Jurassic and Lower Cretaceous strata, surrounded by soft Upper Cretaceous shales, marls and sandstones. During layer-parallel shortening, the Manín sedimentary succession behaved as a multilayer reinforced by a variously thick rigid layer of massive Urgonian limestone. The multilayer deformed by flexural slip folding, but the fold wavelength was controlled by the rigid layer undergoing buckling. It is inferred that, besides the lateral thickness differences in the rigid layer, development of brachyfolds and particularly periclines such as the Butkov fold also resulted from the interference of two perpendicular macroscopic fold systems
    Kategória publikačnej činnosti ADD
    Číslo archívnej kópie44026
    Katal.org.BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici
    Báza dátxpca - PUBLIKAČNÁ ČINNOSŤ
    OdkazyPERIODIKÁ-Súborný záznam periodika
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  5. NázovGeometria, založenie a rast butkovskej brachyantiklinály (manínska jednotka)
    Aut.údajeDušan Plašienka ... [et al.]
    Autor Plašienka Dušan (60%)
    Spoluautori Bučová Jana (20%)
    Šimonová Viera 1977- (20%) UMBFP01 - Katedra geografie a geológie
    Zdroj.dok. Mente et Malleo (MEM) : spravodajca Slovenskej geologickej spoločnosti : 15. predvianočný geologický seminár Nové poznatky o stavbe a vývoji Západných Karpát, Bratislava, 08.12.2016. Vol. 2, no. 1 (2017), s. 44-45. - Bratislava : Ústav vied o Zemi, 2017 ; Nové poznatky o stavbe a vývoji Západných Karpát geologický seminár
    Kľúč.slová geometria - geometry   manínska jednotka   brachyantiklinála  
    Jazyk dok.slovenčina
    Systematika 514
    URL Link na plný text
    Kategória publikačnej činnosti AFH
    Číslo archívnej kópie41053
    Katal.org.BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici
    Báza dátxpca - PUBLIKAČNÁ ČINNOSŤ
    OdkazyPERIODIKÁ-Súborný záznam periodika
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  6. NázovStratigraphic and tectonic control of deep-water scarp accumulation in Paleogene synorogenic basin: a case study of the Súľov Conglomerates (Middle Váh Valley, Western Carpathians)
    Aut.údajeJán Soták ... [et al.]
    Autor Soták Ján (50%)
    Spoluautori Pulišová Zuzana (20%)
    Plašienka Dušan (15%)
    Šimonová Viera 1977- (15%) UMBFP01 - Katedra geografie a geológie
    Zdroj.dok. Geologica Carpathica. Vol. 68, no. 5 (2017), pp. 403-418. - Bratislava : Veda, 2017
    Kľúč.slová carbonate breccias   deep-water basins   subduction   tectonic erosion  
    Heslá geogr. Súľov
    Jazyk dok.angličtina
    KrajinaSlovenská republika
    Systematika 55
    AnotáciaThe Súľov Conglomerates represent mass-transport deposits of the Súľov–Domaniža Basin. Their lithosomes are intercalated by claystones of late Thanetian (Zones P3 – P4), early Ypresian (Zones P5 – E2) and late Ypresian to early Lutetian (Zones E5 – E9) age. Claystone interbeds contain rich planktonic and agglutinated microfauna, implying deep-water environments of gravity-flow deposition. The basin was supplied by continental margin deposystems, and filled with submarine landslides, fault-scarp breccias, base-of-slope aprons, debris-flow lobes and distal fans of debrite and turbidite deposits. Synsedimentary tectonics of the Súľov–Domaniža Basin started in the late Thanetian – early Ypresian by normal faulting and disintegration of the orogenic wedge margin. Fault-related fissures were filled by carbonate bedrock breccias and banded crystalline calcite veins (onyxites). The subsidence accelerated during the Ypresian and early Lutetian by gravitational collapse and subcrustal tectonic erosion of the CWC plate. The basin subsided to lower bathyal up to abyssal depth along with downslope accumulation of mass-flow deposits. Tectonic inversion of the basin resulted from the Oligocene – early Miocene transpression (σ1 rotated from NW–SE to NNW–SSE), which changed to a transpressional regime during the Middle Miocene (σ1 rotated from NNE–SSW to NE–SW). Late Miocene tectonics were dominated by an extensional regime with σ3 axis in NNW–SSE orientation
    Kategória publikačnej činnosti ADD
    Číslo archívnej kópie41037
    Kategória ohlasu PELECH, Ondrej - OLŠAVSKÝ, Mário. Post-early Eocene backthrusting in the northeastern Strážovské vrchy Mts. (Western Carpathians). In Mineralia Slovaca. ISSN 0369-2086, 2018, vol. 50, no. 2, pp. 149-158.
    Katal.org.BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici
    Báza dátxpca - PUBLIKAČNÁ ČINNOSŤ
    OdkazyPERIODIKÁ-Súborný záznam periodika
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  7. NázovStepwise clockwise rotation of the Cenozoic stress field in the Western Carpathians as revealed by kinematic analysis of minor faults in the Manin Unit (western Slovakia)
    Aut.údajeViera Šimonová, Dušan Plašienka
    Autor Šimonová Viera 1977- (60%) UMBFP01 - Katedra geografie a geológie
    Spoluautori Plašienka Dušan (40%)
    Zdroj.dok. Geological Quarterly. Vol. 61, no. 1 (2017), pp. 251-264. - Warszaw : Polish Geological Institute - National Research Institute, 2017
    Kľúč.slová tectonic regime   geodynamics  
    Heslá geogr. Západné Karpaty (pohorie)
    Jazyk dok.angličtina
    KrajinaPoľsko
    Systematika 55
    AnotáciaThis study aims at quantitative kinematic analysis of fault-slip data and palaeostress reconstruction of polyphase brittle structures developed in the Manin Unit cropping out in the Middle Vah River Valley of western Slovakia. The Manin Unit neighbours the Pieniny Klippen Belt that follows the boundary between the Paleogene accretionary wedge of the Outer Carpathians and the Cretaceous nappe system of the Central Western Carpathians. After the nappe emplacement during mid-Cretaceous times, the Manin Unit was incorporated into the Pieniny Klippen Belt and attained its complex tectonic style. Based on kinematic analysis of meso-scale faults with slickensides, six (D-1-D-6) brittle deformation stages have been discerned. The relative succession of individual palaeostress states was derived from field structural relationships; their strati graphic age was estimated primarily by comparison with other published data. Palaeostress analysis in the Manin Unit revealed the existence of six different palaeostress fields acting from the Middle Eocene to the Quaternary. The first three generations of meso-scale brittle structures were formed under a transpressional tectonic regime during the pre-Late Eocene-Early Miocene D-1-D-3 deformation. Generally, the maximum horizontal stress axis rotated clockwise from a W-E to an approximately N-S direction. Thereafter, a transtensional tectonic regime was characterized by a WNW-ESE to NNW-SSE oriented minimum horizontal stress axis during Middle and Late Miocene D-4-D-5 deformation. A general extensional tectonic regime influenced the structural evolution of the area in the Pliocene to Quaternary, when a gradual reorientation of the palaeostress field resulted in the development of variable, often reactivated, fault structures.
    Kategória publikačnej činnosti ADC
    Číslo archívnej kópie39708
    Katal.org.BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici
    Báza dátxpca - PUBLIKAČNÁ ČINNOSŤ
    OdkazyPERIODIKÁ-Súborný záznam periodika
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  8. NázovTectonics of the Carpathian klippen belt in the middle Váh River Valley (Western Slovakia)
    Aut.údajeDušan Plašienka ... [et al.]
    Autor Plašienka Dušan (70%)
    Spoluautori Bučová Jana (10%)
    Soták Ján (10%)
    Šimonová Viera 1977- (10%) UMBFP01 - Katedra geografie a geológie
    Zdroj.dok.CETEG 2015 : 13th meeting of the Central European Tectonic Groups & 20th meeting of the Czech Tectonic Studies Group (ČTS), Kadaň, 22-25 April 2015 : abstract volume. S. 70. - Prague : Charles University, Czech Geological Survey, 2015 ; CETEG 2015 medzinárodné stretnutie
    Kľúč.slová tektonika - tectonic  
    Heslá geogr. Pieniny Klippen Belt
    Váh (Slovensko : rieka)
    Jazyk dok.angličtina
    KrajinaČeská republika
    Systematika 553
    Kategória publikačnej činnosti AFG
    Číslo archívnej kópie38810
    Katal.org.BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici
    Báza dátxpca - PUBLIKAČNÁ ČINNOSŤ
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  9. NázovStructural pattern and emplacement mechanisms of the Krížna cover nappe (Central Western Carpathians)
    Aut.údajeRoberta Prokešová, Dušan Plašienka, Rastislav Milovský
    Autor Prokešová Roberta 1966- (50%) UMBFP11 - Inštitút výskumu krajiny a regiónov
    Spoluautori Plašienka Dušan (30%)
    Milovský Rastislav (20%)
    Zdroj.dok. Geologica Carpathica. Vol. 63, no. 1 (2012), pp. 13-32. - Bratislava : Veda, 2012
    Kľúč.slová krížňanský príkrov   fluidné inklúzie   Krížna Nappe   fluid inclusions  
    Heslá geogr. Západné Karpaty (pohorie)
    Jazyk dok.angličtina
    KrajinaSlovenská republika
    Systematika 551
    Kategória publikačnej činnosti ADD
    Číslo archívnej kópie22363
    Kategória ohlasu GRABOWSKI, J. - SCHNYDER, J. - SOBIEŃ, K. et al. Magnetic susceptibility and spectral gamma logs in the Tithonian-Berriasian pelagic carbonates in the Tatra Mts (Western Carpathians, Poland) : palaeoenvironmental changes at the Jurassic/Cretaceous boundary. In Cretaceous research. ISSN 0195-6671, 2013, vol. 43, pp. 1-17.
    JUREWICZ, E. Procesy nasunieć płaszczowinowych w Tatrach. In Przeglad geologiczny. ISSN 0033-2151, 2012, vol. 60, no. 8, pp. 432-441.
    MIDRIAK, Rudolf. Výskum krajiny v Inštitúte výskumu krajiny a regiónov Fakulty prírodných vied UMB Banská Bystrica. In Geografická revue : geografické a geoekologické štúdie : vedecký časopis Katedry geografie a krajinnej ekológie a Inštitútu výskumu krajiny a regiónov Fakulty prírodných vied Univerzity Mateja Bela v Banskej Bystrici. ISSN 1336-7072, 2013, vol. 9, pp. 92-104.
    VOZAROVA, Anna - KONECNY, Patrik - VDACNY, Marek - VOZAR, Jozef - SARINOVA, Katarina. Provenance of Permian Maluzina Formation sandstones (Hronicum, Western Carpathians) : evidence from monazite geochronology. In Geologica Carpathica. ISSN 1335-0552, 2014, vol. 65, no. 5, pp. 329-U79.
    KRALIKOVA, Silvia - VOJTKO, Rastislav - SLIVA, Lubomir - MINAR, Jozef - FUEGENSCHUH, Bernhard - KOVAC, Michal - HOK, Jozef. Cretaceous-Quaternary tectonic evolution of the Tatra Mts (Western Carpathians) : constraints from structural, sedimentary, geomorphological, and fission track data. In Geologica Carpathica. ISSN 1335-0552, 2014, vol. 65, no. 4, pp. 307-326.
    ZABIELSKI, R. - IWANOW, A. New tectonic elements in the Križna nappe between Bystra Valley and Stra̧żyska Valley in the Tatra Mts. = Nowe elementy w tektonice płaszczowiny kriżniańskiej miȩdzy Dolina̧ Bystrej a Dolina̧ Stra̧żyska̧ w Tatrach. In Przeglad Geologiczny. ISSN 0033-2151, 2014, vol. 62, no. 2, pp. 86-96.
    NOVOTNA, N. - JERABEK, P. - PITRA, P. - LEXA, O. - RACEK, M. Repeated slip along a major decoupling horizon between crustal-scale nappes of the Central Western Carpathians documented in the Ochtina tectonic melange. In Tectonophysics. ISSN 0040-1951, 2015, vol. 646, pp. 50-64.
    SARKARINEJAD, Khalil - KESHAVARZ, Saeede - FAGHIH, Ali. Kinematics of the Sirjan mylonite nappe, Zagros Orogenic Belt : insights from strain and vorticity analyses. In Journal of geosciences. ISSN 1802-6222, 2015, vol. 60, no. 3, pp. 189-202.
    GRABOWSKI, Jacek - SOBIEN, Katarzyna. Variation in clastic input in the Berriasian of the lower sub-tatric (Krizna) succession in the Tatra mountains (Central Western Carpathians, Poland) : data from magnetic susceptibility and inorganic geochemistry. In Annales societatis geolorgum Poloniae. ISSN 0208-9068, 2015, vol. 85, no. 1, pp. 139-150.
    HÓK, Jozef - KOVÁČ, Michal - PELECH, Ondrej - PEŠKOVÁ, Ivana - VOJTKO, Rastislav - KRÁLIKOVÁ, Silvia. The Alpine tectonic evolution of the Danube Basin and its northern periphery (southwestern Slovakia). In Geologica Carpathica. ISSN 1335-0552, 2016, vol. 67, no. 5, pp. 495-505.
    CASTELLUCCIO, Ada - MAZZOLI, Stefano - ANDREUCCI, Benedetta - JANKOWSKI, Leszek - SZANIAWSKI, Rafal - ZATTIN, Massimiliano. Building and exhumation of the Western Carpathians: new constraints from sequentially restored, balanced cross sections integrated with low-temperature thermochronometry. In Tectonics. ISSN 0278-7407, 2016, vol. 35, no. 11, pp. 2698-2733.
    BAK, Krzysztof - FABIANSKA, Monika - BAK, Marta - MISZ-KENNAN, Magdalena - ZIELINSKA, Magdalena - DULEMBA, Pawel - BRYNDAL, Tomasz - NAGLIK, Beata. Organic matter in upper Albian marine sediments in the High-Tatric units, central western Carpathians related to Oceanic Anoxic Event 1d-Geochemistry, microfacies and palynology. In Palaeogeography palaeoclimatology palaeoecology. ISSN 0031-0182, 2016, vol. 454, pp. 212-227.
    WOLSKA, Anna - BAK, Krzysztof - BAK, Marta. Siliciclastic input into upper Cenomanian synorogenic sediments of the High-Tatric unit, Central Western Carpathians (Tatra Mountains); petrography, geochemistry and provenance. In Geological Quarterly. ISSN 1641-7291, 2016, vol. 60, no. 4, pp. 919-934.
    MARTON, Emo - GRABOWSKI, Jacek - TOKARSKI, Antek K. - TUNYI, Igor. Palaeomagnetic results from the fold and thrust belt of the Western Carpathians: an overview. In Palaeomagnetism in fold and thrust belts: new perspectives. ISSN 0305-8719, 2016, vol. 425, pp. 7-36.
    PELECH, Ondrej - HÓK, Jozef - HAVRILA, Milan - PEŠKOVÁ, Ivana. Structural position of the upper cretaceous sediments in the Považský Inovec Mts. (Western Carpathians). In Acta Geologica Slovaca. ISSN 1338-0044, 2016, vol. 8, no. 1, pp. 43-58.
    PELECH, Ondrej - HÓK, Jozef - JÓZSA, Štefan. Turonian-Santonian sediments in the Tatricum of the Povazsky Inovec Mts. (Internal Western Carpathians, Slovakia). In Austrian journal of earth sciences. ISSN 2072-7151, 2017, vol. 110, no. 1, pp. 19-33.
    NABAVI, Seyed Tohid - RAHIMI-CHAKDEL, Aziz - KHADEMI, Mohsen. Structural pattern and emplacement mechanism of the Neka Valley nappe complex, eastern Alborz, Iran. In International journal of earth sciences. ISSN 1437-3254, 2017, vol. 106, no. 7, pp. 2387-2405.
    BAK, Krzysztof - KOWALCZYK, Joanna - WOLSKA, Anna - BAK, Marta - NATKANIEC-NOWAK, Lucyna. Iron and silica enrichments in the middle Albian neptunian dykes from the High-Tatric Unit, Central Western Carpathians: an indication of hydrothermal activity for an extensional tectonic regime. In Geological magazine. ISSN 0016-7568, 2018, vol. 155, no. 1, pp. 1-19.
    Katal.org.BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici
    Báza dátxpca - PUBLIKAČNÁ ČINNOSŤ
    OdkazyPERIODIKÁ-Súborný záznam periodika
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  10. NázovDid the Metamorphic Fluid Flow Trigger Thin-skinned Thrusting?
    Aut.údajeRastislav Milovský, Roberta Prokešová, Dušan Plašienka
    Autor Milovský Rastislav
    Spoluautori Prokešová Roberta 1966- UMBFP11 - Inštitút výskumu krajiny a regiónov
    Plašienka Dušan
    Zdroj.dok. CorseAlp 2011 : 10th Alpine workshop : abstract volume. S. 62. - Pisa : Universita di Pisa, 2011 / Carmina Bernardo ; CorseAlp 2011 alpine workshop
    Kľúč.slová fluidné inklúzie   fluid inclusions   emplacement mechanisms  
    Heslá geogr. Slovensko
    Západné Karpaty (pohorie)
    Krížna Nappe
    Jazyk dok.angličtina
    KrajinaTaliansko
    Systematika 553
    Kategória publikačnej činnosti AFG
    Číslo archívnej kópie19257
    Katal.org.BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici
    Báza dátxpca - PUBLIKAČNÁ ČINNOSŤ
    nerozpoznaný

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