Stages of Development in the Polish Carpathian Foredeep Basin
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Preliminary Catalog of the Sedimentary Basins of the United States
Preliminary Catalog of the Sedimentary Basins of the United States By James L. Coleman, Jr., and Steven M. Cahan Open-File Report 2012–1111 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. Suggested citation: Coleman, J.L., Jr., and Cahan, S.M., 2012, Preliminary catalog of the sedimentary basins of the United States: U.S. Geological Survey Open-File Report 2012–1111, 27 p. (plus 4 figures and 1 table available as separate files) Available online at http://pubs.usgs.gov/of/2012/1111/. iii Contents Abstract ...........................................................................................................................................................1 -
Tectonics and Sedimentation in Foreland Basins: Results from the Integrated Basin Studies Project
Downloaded from http://sp.lyellcollection.org/ by guest on September 30, 2021 Tectonics and sedimentation in foreland basins: results from the Integrated Basin Studies project ALAIN MASCLE 1 & CAI PUIGDEFABREGAS 2,3 IIFP School, 228-232 avenue Napoldon Bonaparte, 92852 Rueil-Malmaison Cedex, France (e-mail: [email protected]) 2Norsk Hydro Research Centre, Bergen, Norway. 3Institut de Ciences de la Terra, (?SIC, Barcelona, Spain. Why foreland basins? to a better understanding of some basic interact- ing tectonic, sedimentary and hydrologic pro- Over the last ten years or so, since the Fribourg cesses (More & Vrolijk 1992; Touret & van meeting in 1985 (Homewood et al. 1986), the Hinte 1992). Additional data have also been attention given by sedimentologists and struc- obtained through the development of analogue tural geologists to the geology of foreland basins and numerical models (Larroque et al. 1992; has been growing continuously, parallel to the Zoetemeijer 1993). The physical parameters increase of co-operative links between scientists controlling the forward propagation of d6colle- from the two disciplines. A number of reasons ments and thrusts (fluid pressure, roughness, lie behind this development. Attempting to sediment thickness, etc.) have been determined understand the growth of an orogen without and tested. The relationships between rapidly paying due attention to the stratigraphic record subsiding piggyback basins and growing ramp of the derived sediments would be unrealistic. It anticlines have also been imaged, although the would, moreover, be equally unrealistic to con- lack of deep-sea well control still prevents accu- struct restored sections across the chain without rate sedimentological studies. More significant considering the constraints imposed by the has been the progress in our understanding of basin-fill architecture, or to describe the basin- the role of fluids and pore pressure in the fill evolution disregarding the development of development of thrust belts. -
House in Carpathians1
Ethnologia Polona, 2014, 35, s. 25-77 Ethnologia Polona, vol. 35: 2014, 25 – 77 PL ISSN 0137 - 4079 HOUSE IN CARPATHIANS1 JIŘÍ LANGER AND HELENA BOČKOVÁ ROŽNOV POD RADHOŠTĚM and BRNO, CZECH REPUBLIC INTRODUCTION The problem of the folk culture has always been a great topic for the ethnographers. Since the last century an attention of many explorers from many countries has focused on it. A common interest in finding the answers to the questions of the causes of the specifications of their cultural manifestation in the Carpathians connected them. They seemed to be different from firmly rooted ideas about the typical features of individual nations. Anachronisms provoke everybody who was looking for the originalities of their own national or Slavonic culture. They served to the creating of romantic fanta- sies about the culture in the mountains surviving into the period in which European nations formed. From the point of view of a historian this culture is considered to be very young, having been created before our eyes. Our generation could still study it by the very watching. We know it from autopsy. It differed from neighbouring lower situated areas with the early evolution forms, transferring of their phenomena for long distances, strong penetration and co operation with neighbouring social environments and ethnic heterogeneity. This all enabled people in the mountains to survive even in the worst climatic and social conditions. The principles of the folk culture being thought to be specific for the whole Carpathians touching vast areas of Europe connected fairly different forms of the way of the life from the Balkan to White Russia and from the river Morava (CZ) as far as the coast of the Black Sea. -
The Election Attitudes Among the Polish Minority Inhabiting the Region of Zaolzie in the Czech Republic (1990-2018)
https://doi.org/10.4316/CC.2020.01.008 THE ELECTION ATTITUDES AMONG THE POLISH MINORITY INHABITING THE REGION OF ZAOLZIE IN THE CZECH REPUBLIC (1990-2018) Radosław ZENDEROWSKI Cardinal Stefan Wyszyński University in Warsaw, Poland E-mail: [email protected] Abstract. The paper analyses the election activity of the Polish inhabitants of the Zaolzie region (the Czech Republic) in the 1990-2018 period referring to national elections (Lower Chamber of Parliament, Senate, President of the Czech Republic) as well as local and regional elections. The theoretical section offers analyses of national and ethnic minorities as (collective) political actors. The empirical part provides an in-depth analysis of the votes in particular elections, taking into consideration the communes with a significant rate of Polish inhabitants as well as those communes there the Polish ethnos was rather scarce. The ethnic affiliation has been considered as a vital independent variable of the choices made; however, other variables explaining election behaviour have also been indicated. Keywords: Zaolzie, Czech Republic, Polish national minority, elections, politics Rezumat. Atitudinile electorale în rândul minorității poloneze din Regiunea Zaolzie a Republicii Cehe (1990-2018). Articolul analizează problema activității electorale a locuitorilor polonezi din regiunea Zaolzie (Republica Cehă) în perioada 1990-2018, refe- rindu-se la alegerile naționale (Camera inferioară a Parlamentului, Senatul, președintele Re- publicii Cehe), precum și la alegerile regionale și locale. Secțiunea teoretică prezintă minorită- țile naționale și etnice ca actori politici (colectivi). Partea empirică oferă o analiză aprofundată a voturilor la anumite alegeri, luând în considerare comunele cu o pondere semnificativă de locuitori polonezi, precum și acele comune unde etnicii polonezi sunt puțini la număr. -
Guidelines for Wildlife and Traffic in the Carpathians
Wildlife and Traffic in the Carpathians Guidelines how to minimize the impact of transport infrastructure development on nature in the Carpathian countries Wildlife and Traffic in the Carpathians Guidelines how to minimize the impact of transport infrastructure development on nature in the Carpathian countries Part of Output 3.2 Planning Toolkit TRANSGREEN Project “Integrated Transport and Green Infrastructure Planning in the Danube-Carpathian Region for the Benefit of People and Nature” Danube Transnational Programme, DTP1-187-3.1 April 2019 Project co-funded by the European Regional Development Fund (ERDF) www.interreg-danube.eu/transgreen Authors Václav Hlaváč (Nature Conservation Agency of the Czech Republic, Member of the Carpathian Convention Work- ing Group for Sustainable Transport, co-author of “COST 341 Habitat Fragmentation due to Trans- portation Infrastructure, Wildlife and Traffic, A European Handbook for Identifying Conflicts and Designing Solutions” and “On the permeability of roads for wildlife: a handbook, 2002”) Petr Anděl (Consultant, EVERNIA s.r.o. Liberec, Czech Republic, co-author of “On the permeability of roads for wildlife: a handbook, 2002”) Jitka Matoušová (Nature Conservation Agency of the Czech Republic) Ivo Dostál (Transport Research Centre, Czech Republic) Martin Strnad (Nature Conservation Agency of the Czech Republic, specialist in ecological connectivity) Contributors Andriy-Taras Bashta (Biologist, Institute of Ecology of the Carpathians, National Academy of Science in Ukraine) Katarína Gáliková (National -
Development of the Rocky Mountain Foreland Basin: Combined Structural
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 2007 DEVELOPMENT OF THE ROCKY MOUNTAIN FORELAND BASIN: COMBINED STRUCTURAL, MINERALOGICAL, AND GEOCHEMICAL ANALYSIS OF BASIN EVOLUTION, ROCKY MOUNTAIN THRUST FRONT, NORTHWEST MONTANA Emily Geraghty Ward The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Ward, Emily Geraghty, "DEVELOPMENT OF THE ROCKY MOUNTAIN FORELAND BASIN: COMBINED STRUCTURAL, MINERALOGICAL, AND GEOCHEMICAL ANALYSIS OF BASIN EVOLUTION, ROCKY MOUNTAIN THRUST FRONT, NORTHWEST MONTANA" (2007). Graduate Student Theses, Dissertations, & Professional Papers. 1234. https://scholarworks.umt.edu/etd/1234 This Dissertation is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. DEVELOPMENT OF THE ROCKY MOUNTAIN FORELAND BASIN: COMBINED STRUCTURAL, MINERALOGICAL, AND GEOCHEMICAL ANALYSIS OF BASIN EVOLUTION ROCKY MOUNTAIN THRUST FRONT, NORTHWEST MONTANA By Emily M. Geraghty Ward B.A., Whitman College, Walla Walla, WA, 1999 M.S., Washington State University, Pullman, WA, 2002 Dissertation presented in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Geology The University of Montana Missoula, MT Spring 2007 Approved by: Dr. David A. Strobel, Dean Graduate School James W. Sears, Chair Department of Geosciences Julia A. Baldwin Department of Geosciences Marc S. Hendrix Department of Geosciences Steven D. -
Neotectonics of the Polish Carpathians in the Light of Geomorphic Studies: a State of the Art
Acta Geodyn. Geomater., Vol. 6, No. 3 (155), 291-308, 2009 NEOTECTONICS OF THE POLISH CARPATHIANS IN THE LIGHT OF GEOMORPHIC STUDIES: A STATE OF THE ART Witold ZUCHIEWICZ Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, A. Mickiewicza 30, 30-059 Kraków, Poland *Corresponding author‘s e-mail: [email protected] (Received January 2009, accepted March 2009) ABSTRACT Neotectonics of the Carpathians used to be studied extensively, particular attention being paid to the effects of large-scale domal uplifts and open folding above marginal zones of thrusts and imbricated map-scale folds, and rarely to the characteristics of young faulting. Neotectonic faults tend to be associated with the margins of the Orava-Nowy Targ Basin, superposed on the boundary between the Inner and Outer Western Carpathians, as well as with some regions within the Outer Carpathians. The size of Quaternary tilting of the Tatra Mts. on the sub-Tatric fault were estimated at 100 to 300 m, and recent vertical crustal movements of this area detected by repeated precise levelling are in the range of 0.4-1.0 mm/yr in rate. Minor vertical block movements of oscillatory character (0.5-1 mm/yr) were detected along faults cutting the Pieniny Klippen Belt owing to repeated geodetic measurements performed on the Pieniny geodynamic test area. In the western part of the Western Outer Carpathians, middle and late Pleistocene reactivation of early Neogene thrust surfaces was suggested. Differentiated mobility of reactivated as normal Miocene faults (oriented (N-S to NNW-SSE and NNE-SSW) in the medial portion of the Dunajec River drainage basin appears to be indicated by the results of long-profile analyses of deformed straths, usually of early and middle Pleistocene age. -
The Species Composition on Agricultural Terraces in Nw Part of Slovakia
Ekológia (Bratislava) Vol. 33, No. 4, p. 307–320, 2014 doi:10.2478/eko-2014-0029 THE SPECIES COMPOSITION ON AGRICULTURAL TERRACES IN NW PART OF SLOVAKIA IVA MACHOVÁ, KAREL KUBÁT Jan Evangelista Purkyně University in Ústí nad Labem, Faculty of Environment, Králova výšina 7, 400 96 Ústí nad Labem, Czech Republic; e-mail: [email protected] Jan Evangelista Purkyně University in Ústí nad Labem, Faculty of Science, Za Válcovnou 8, 400 96 Ústí nad Labem, Czech Republic; e-mail: [email protected] Abstract Machová I., Kubát K.: The species composition on agricultural terraces in NW part of Slovakia. Ekológia (Bratislava), Vol. 33, No. 4, p. 307–320, 2014. The article contributes to a deeper understanding of agricultural terraces in NW Slovakia. The agri- cultural terraces found in 12 mountain ranges were characterised in detail on 32 localities. The slope parts of the studied terraces are on average only 2.3 m wide and current and former agricultural areas between them are on average 11 m wide. Furthermore, seventy phytosociological relevés were made on the terraces. Overall, 360 species of vascular plants were found in the relevés, 66 of which appeared regularly. The localities were evaluated by DCA analysis. The main factor influencing the species com- position appears to be the geological composition of the bedrock and, probably, the altitude as well. High coverage of the herb layer (median value 95%), low coverage of the shrub layer (median value 5%) and the absence or a very low coverage of the tree layer is typical for these terraces. Key words: NW Slovakia, agricultural terraces, vascular plants species, properties of the terraces. -
Lithospheric Folding and Sedimentary Basin Evolution: a Review and Analysis of Formation Mechanisms Sierd Cloething, Evgenii Burov
Lithospheric folding and sedimentary basin evolution: a review and analysis of formation mechanisms Sierd Cloething, Evgenii Burov To cite this version: Sierd Cloething, Evgenii Burov. Lithospheric folding and sedimentary basin evolution: a review and analysis of formation mechanisms. Basin Research, Wiley, 2011, 23 (3), pp.257-290. 10.1111/j.1365- 2117.2010.00490.x. hal-00640964 HAL Id: hal-00640964 https://hal.archives-ouvertes.fr/hal-00640964 Submitted on 24 Nov 2011 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Basin Research For Review Only Page 1 of 91 Basin Research 1 2 3 4 1 Lithospheric folding and sedimentary basin evolution: 5 6 2 a review and analysis of formation mechanisms 7 8 9 3 10 11 4 12 13 5 14 a,* b 15 6 Sierd Cloetingh and Evgenii Burov 16 7 17 18 8 aNetherlands ResearchFor Centre forReview Integrated Solid EarthOnly Sciences, Faculty of Earth and Life 19 20 9 Sciences, VU University Amsterdam, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands. 21 10 22 23 11 bUniversité Pierre et Marie Curie, Laboratoire de Tectonique, 4 Place Jussieu, 24 25 12 75252 Paris Cedex 05, France. -
Boudinage Arrangement Tracking of Hydrothermal Veins in the Shear Zone: Example from the Argentiferous Strieborna Vein (Western Carpathians)
Journal of Geosciences, 64 (2019), 179–195 DOI: 10.3190/jgeosci.291 Original paper Boudinage arrangement tracking of hydrothermal veins in the shear zone: example from the argentiferous Strieborna vein (Western Carpathians) Stanislav JACKO1*, Roman FARKAŠOVSKÝ1, Julián KONDELA1, Tomáš MIKUŠ2, Barbora ŠČERBÁKOVÁ1, Diana DIRNEROVÁ1 1 Technical University of Košice, Institute of Geosciences, Letná 9, 040 01 Košice, Slovakia; [email protected] 2 Slovak Academy of Sciences, Earth Science Institute, Ďumbierska 1, 974 01 Banská Bystrica, Slovakia * Corresponding author Argentiferous Strieborna vein of the Rožňava ore field occurs at the southwestern margin of the Gemeric Unit (Slovakia). The hydrothermal mineralization of the vein closely related to the Early Cretaceous tectonometamorphic shortening of the Western Carpathians. For their emplacement, the vein used the steeply dipping, fan-like cleavage and dislocation set of the Alpine regional structure. Successively the vein was integrated into the sinistral transpressional regime of the Transgemeric shear zone. A polyphase vein filling comprises Variscan metasomatic siderite remnants and the Early Cretaceous syntectonic hydrothermal mineralization, the latter consisting of two mineralization phases, quartz–siderite and quartz–sulphidic. During Cretaceous shear zone transpressional events, the vein was segmented into five individual bodies and redistributed to kinematically and geometrically different tensional and compressional boudins. The vein asymmetry increase, different vertical mineralization content and spatial distribution of mineral phases representing individual mineralization periods directly relate to a rheological contrast between the vein and surrounding rocks stress and pressure shadows distribution. The actual form and distribution of the Strieborna vein segments is the product of four boudin evolution stages: (1) pre-deformation, (2) initial, (3) boudin-forming and (4) boudin-differentiation stage that controlled vertical mineralization distribution. -
Background and Introduction
Chapter One: Background and Introduction Chapter One Background and Introduction title chapter page 17 © Libor Vojtíšek, Ján Lacika, Jan W. Jongepier, Florentina Pop CHAPTER?INDD Chapter One: Background and Introduction he Carpathian Mountains encompass Their total length of 1,500 km is greater than that many unique landscapes, and natural and of the Alps at 1,000 km, the Dinaric Alps at 800 Tcultural sites, in an expression of both km and the Pyrenees at 500 km (Dragomirescu geographical diversity and a distinctive regional 1987). The Carpathians’ average altitude, how- evolution of human-environment relations over ever, of approximately 850 m. is lower compared time. In this KEO Report, the “Carpathian to 1,350 m. in the Alps. The northwestern and Region” is defined as the Carpathian Mountains southern parts, with heights over 2,000 m., are and their surrounding areas. The box below the highest and most massive, reaching their offers a full explanation of the different delimi- greatest elevation at Slovakia’s Gerlachovsky tations or boundaries of the Carpathian Mountain Peak (2,655 m.). region and how the chain itself and surrounding areas relate to each other. Stretching like an arc across Central Europe, they span seven countries starting from the The Carpathian Mountains are the largest, Czech Republic in the northwest, then running longest and most twisted and fragmented moun- east and southwards through Slovakia, Poland, tain chain in Europe. Their total surface area is Hungary, Ukraine and Romania, and finally 161,805 sq km1, far greater than that of the Alps Serbia in the Carpathians’ extreme southern at 140,000 sq km. -
Western Carpathians, Poland)
Geological Quarterly, 2006, 50 (1): 169–194 Late Jurassic-Miocene evolution of the Outer Carpathian fold-and-thrust belt and its foredeep basin (Western Carpathians, Poland) Nestor OSZCZYPKO Oszczypko N. (2006) — Late Jurassic-Miocene evolution of the Outer Carpathian fold-and-thrust belt and its foredeep basin (Western Carpathians, Poland). Geol. Quart., 50 (1): 169–194. Warszawa. The Outer Carpathian Basin domain developed in its initial stage as a Jurassic-Early Cretaceous rifted passive margin that faced the east- ern parts of the oceanic Alpine Tethys. Following closure of this oceanic basin during the Late Cretaceous and collision of the Inner Western Carpathian orogenic wedge with the Outer Carpathian passive margin at the Cretaceous-Paleocene transition, the Outer Carpathian Basin domain was transformed into a foreland basin that was progressively scooped out by nappes and thrust sheets. In the pre- and syn-orogenic evolution of the Outer Carpathian basins the following prominent periods can be distinguished: (1) Middle Juras- sic-Early Cretaceous syn-rift opening of basins followed by Early Cretaceous post-rift thermal subsidence, (2) latest Creta- ceous-Paleocene syn-collisional inversion, (3) Late Paleocene to Middle Eocene flexural subsidence and (4) Late Eocene-Early Miocene synorogenic closure of the basins. In the Outer Carpathian domain driving forces of tectonic subsidence were syn-rift and thermal post-rift processes, as well as tectonic loads related to the emplacement of nappes and slab-pull. Similar to other orogenic belts, folding of the Outer Carpathians commenced in their internal parts and progressed in time towards the continental foreland. This process was initi- ated at the end of the Paleocene at the Pieniny Klippen Belt/Magura Basin boundary and was completed during early Burdigalian in the northern part of the Krosno Flysch Basin.