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Relevant bibliographies by topics / Flysch Belt

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Academic literature on the topic 'Flysch Belt'

Author: Grafiati

Published: 4 June 2025

Last updated: 1 August 2025

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Journal articles on the topic "Flysch Belt"

1

Teťák, František. "Revízia geologickej mapy západného úseku flyšového pásma Západných Karpát s diskusiou k vybraným geologickým problémom." Geologické práce Správy 140 (December 2024): 75–106. https://doi.org/10.56623/gps.140.3.

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The work presents maps of the selected regions of the western Slovak section of the Flysch Belt of the Western Carpathians, including the contact with the Klippen Belt, compiled by the author in the period from 2001 to 2023. Geological maps of the Biele Karpaty Mts., Javorníky Mts., Kysuce region, Biela Orava region and Oravská Magura Mts. mapped by the author are digitally processed with a scale accuracy of 1 : 10,000 and subsequently reconstructed on a detailed LiDAR basis. They were developed according to a uniform legend of the map server of the ŠGÚDŠ and with a uniform approach to the int

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GOLONKA, JAN, MICHAŁ KROBICKI, ANNA WAŚKOWSKA, MAREK CIESZKOWSKI, and ANDRZEJ ŚLĄCZKA. "Olistostromes of the Pieniny Klippen Belt, Northern Carpathians." Geological Magazine 152, no. 2 (2014): 269–86. http://dx.doi.org/10.1017/s0016756814000211.

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AbstractThe olistostromes form two belts within the Pieniny Klippen Belt (PKB) in the Northern Carpathians. They mark an early stage of the development of the accretionary prism. The first belt was formed during Late Cretaceous time as a result of subduction of the southern part of the Alpine Tethys. The fore-arc basin originated along this subduction zone, with synorogenic flysch deposits. Huge olistoliths deposited within the Cretaceous–Palaeogene flysch of the Złatne Basin, presently located in the vicinity of the Haligovce village (eastern Slovakia), provide a good example of the fore-arc

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Kucharič, Ľudovít, Vladimír Bezák, Dušan Majcin, and Ján Vozár. "Carbonate complexes underlying Flysch belt and subsurface Neogene volcanic in the NE part of Slovakia – a potential for geothermal energy and raw materials." Contributions to Geophysics and Geodesy 42, no. 4 (2012): 283–94. http://dx.doi.org/10.2478/v10126-012-0013-8.

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Abstract A positive gravity anomaly was observed in the Flysch belt realm. Based on this fact and available geological knowledge we suppose that the source of gravity anomaly might be carbonate rocks lying perhaps in the footwall of Flysch sediments. The carbonates belong perhaps to the Penninic crust cover (a part of Klippen belt), or to lower structural stage of the Flysch belt. Besides this it is interpreted more volume of Neogene subvolcanic bodies in the frame of the Flysch belt based on the results of the newest magnetic measurements in the NE part of Slovakia (Kucharič et. al., in press

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Šamajová, Lenka, Jozef Hók, Tamás Csibri, et al. "Geophysical and geological interpretation of the Vienna Basin pre-Neogene basement (Slovak part of the Vienna Basin)." Geologica Carpathica 70, no. 5 (2019): 418–31. http://dx.doi.org/10.2478/geoca-2019-0024.

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Abstract The Vienna Basin is situated at the contact of the Bohemian Massif, Western Carpathians, and Eastern Alps. Deep borehole data and an existing magnetotelluric profile were used in density modelling of the pre-Neogene basement in the Slovak part of the Vienna Basin. Density modelling was carried out along a profile oriented in a NW–SE direction, across the expected contacts of the main geological structures. From bottom to top, four structural floors have been defined. Bohemian Massif crystalline basement with the autochthonous Mesozoic sedimentary cover sequence. The accretionary sedim

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Su, Wen, Shutong Xu, Laili Jiang, and Yican Liu. "Coesite from quartz-jadeitite in the Dabie Mountains, Eastern China." Mineralogical Magazine 60, no. 401 (1996): 659–62. http://dx.doi.org/10.1180/minmag.1996.060.401.12.

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The Dabie Mountains is a collisional orogen between the North China and Yantze Continental plates. It is composed, from south to north, of the foreland fold and thrust belt alternated with molasse basin, the subducted cover and basement of the Yangtze continental plate, the meta-ophiolitic melange belt, the forearc meta-flysch nappe (bounded by southward and northward thrust belts) in which there may be a buried volcanic arc and a relict back-arc basin (Fig. 1A) (Xu et al., 1992a, 1994).

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Hnylko, O. M. "GEODYNAMICS." GEODYNAMICS 1(10)2011, no. 1(10) (2011): 47–57. http://dx.doi.org/10.23939/jgd2011.01.047.

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The tectonic units of the Carpathians are considered in terms of the terrain analysis. Carpathathian orogen is build up of three main elements: microcontinental terrains, sutures and flysch-molasse accretionary prism. There are two main terrains: a northern ALCAPA and a southern Tisza-Dacia. Sutures (Fore-Marmarosh suture, Pieniny Klippen Belt and others), marking the ancient oceanic basins, bound these terrains. The Flysch Carpathians are regarded as the Cretaceous-Neogene accretionary prism. Growing the prism was caused by the Alpine subduction of the Carpathian Flysch basin basement beneath

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PRENJASI, E., M. SINA, F. AVDULAJ, and Y. SULAJ. "Tectonic relationship between the Druja (Gavrovo) and the Ionian zones of the Albania thrust belt." Bulletin of the Geological Society of Greece 34, no. 1 (2001): 321. http://dx.doi.org/10.12681/bgsg.17029.

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The Kruja zone and the Ionian one are integral parts of the Albanian Thrust Belt, which lie directly in the northern continuation of the Western Hellenic Nappes up to their interruption against the thrust front. Flysch of the Oligocene and rarely carbonate deposits of Cretaceous-Eocene age consist the area along the boundary between the tow zones in question. Deposits of both tectonic zones are similar. But, despite the lithological similarities, presence of conglomerates in the Oligocene flysch and dolomites in the Cretaceous carbonates are the main characteristics of the Kruja zone. Whereas,

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Dolníček, Zdeněk, Michaela Krejčí Kotlánová, Jana Ulmanová, and Jiří Sejkora. "Remobilization of HFSE, Y, and REE during Diagenetic Alteration of Heavy Minerals in Sandstones from the Chvalčov Site, Flysch Belt of the Outer Western Carpathians, Czech Republic." Minerals 14, no. 1 (2023): 1. http://dx.doi.org/10.3390/min14010001.

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An in situ electron microprobe study of detrital minerals yielded important insights into the diagenetic history of the Cretaceous-to-Paleogene flysch sandstones from the Chvalčov site, Rača Unit, Flysch Belt of the Outer Western Carpathians. Detrital titanite and a Fe-Ti mineral (probably ilmenite) were almost completely altered to TiO2 minerals, which also newly crystallized in intergranular spaces of sandstone. Brookite, anatase, and, exceptionally, rutile were identified by Raman spectroscopy. Authigenic TiO2 phases show complex composition with occasionally elevated contents of Fe, Nb, Zr

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Cichostępski, Kamil, Jerzy Dec, Jan Golonka, and Anna Waśkowska. "Shallow Seismic Refraction Tomography Images from the Pieniny Klippen Belt (Southern Poland)." Minerals 14, no. 2 (2024): 155. http://dx.doi.org/10.3390/min14020155.

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The Pieniny Klippen Belt (PKB) is located between the Central and the Outer (Flysch) Carpathians and forms a narrow zone with a complex structure, often described as a mélange. It is composed of numerous tectonic elements of different size including strike-slip-bounded tectonic blocks, thrust units, toe thrusts and olistostromes combined together and representing different lithologies. To aid the geological interpretation of the mélanges of the PKB in the Spiskie Pieniny Mountain Region (South Poland), seismic refraction tomography was conducted. Isolated limestone outcrops consist of Jurassic

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Golonka, Jan, Anna Waśkowska, Kamil Cichostępski, et al. "Mélange, Flysch and Cliffs in the Pieniny Klippen Belt (Poland): An Overview." Minerals 12, no. 9 (2022): 1149. http://dx.doi.org/10.3390/min12091149.

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The Pieniny Klippen Belt (PKB) is located in the suture zone between the Central and Outer (Flysch) Carpathians. Its structure is an effect of prolonged processes of the Cretaceous–Miocene folding, thrusting and uplifting. In this zone, tectonic components of different ages and features, including strike-slip-bounded tectonic blocks, thrust units, as well as toe-thrusts and olistostromes, result in the present-day mélange characteristics of the PKB, where individual tectonic units are difficult to distinguish. In the PKB, both tectonic and sedimentary events triggered the mélange creation. The

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Book chapters on the topic "Flysch Belt"

1

Plašienka, Dušan, and Ján Novotný. "Limestone Klippen Belt—Atypical Landforms in Flysch Uplands." In World Geomorphological Landscapes. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-89293-7_10.

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Galia, Tomáš, Jan Hradecký, and Václav Škarpich. "Sediment Transport in Headwater Streams of the Carpathian Flysch Belt: Its Nature and Recent Effects of Human Interventions." In Sediment Matters. Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-14696-6_2.

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Krejčí, O., I. Baroň, M. Bíl, et al. "Some examples of deep-seated landslides in the Flysch Belt of the Western Carpathians." In Landslides. Routledge, 2018. http://dx.doi.org/10.1201/9780203749197-51.

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Konečný, V., J. Lexa, and V. Hojstričová. "The Central Slovakia Neogene volcanic field." In Epithermal Mineralization of the Western Carpathians. Society of Economic Geologists, 1999. http://dx.doi.org/10.5382/gb.31.06.

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Abstract The Central Slovakia Volcanic Field (CSVF), of Badenian through Pannonian age (16.5–8.5 Ma), is related to both subduction of the flysch belt oceanic/suboceanic basement underneath the advancing Carpathian arc and to back-arc extension processes. Hercynian basement including Late Paleozoic and Mesozoic sedimentary rocks shows a distinct Basin and Range (horst and graben) structure. Volcanic rocks resemble medium- to high-K orogenic volcanic suites of evolved arcs and continental margins. Intrusive rocks show a granodiorite trend, locally with a slight shift towards monzonite. Petrogra

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Seltmann, Reimar, Richard J. Goldfarb, Bo Zu, Robert A. Creaser, Alla Dolgopolova, and Vitaly V. Shatov. "Chapter 24: Muruntau, Uzbekistan: The World’s Largest Epigenetic Gold Deposit." In Geology of the World’s Major Gold Deposits and Provinces. Society of Economic Geologists, 2020. http://dx.doi.org/10.5382/sp.23.24.

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Abstract Muruntau in the Central Kyzylkum desert of the South Tien Shan, western Uzbekistan, with past production of ~3,000 metric tons (t) Au since 1967, present annual production of ~60 t Au, and large remaining resources, is the world’s largest epigenetic Au deposit. The host rocks are the mainly Cambrian-Ordovician siliciclastic flysch of the Besapan sequence. The rocks were deformed into a broadly east-west fold-and-thrust belt prior to ca. 300 Ma during ocean closure along the South Tien Shan suture. A subsequent tectonic transition was characterized by left-lateral motion on regional sp

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Mitchell, Andrew. "Myanmar Orogens and Flysch, Potential for Mineral Discoveries, and Shan Scarps and Jade Mines Cross Sections." In Geological Belts, Plate Boundaries, and Mineral Deposits in Myanmar. Elsevier, 2018. http://dx.doi.org/10.1016/b978-0-12-803382-1.00018-3.

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Lexa, J., J. Štohl, and V. Konečný. "The Banská Štiavnica ore district." In Epithermal Mineralization of the Western Carpathians. Society of Economic Geologists, 1999. http://dx.doi.org/10.5382/gb.31.09.

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Abstract The Banská Štiavnica ore district is in the central zone of the largest stratovolcano in the Central Slovakia Neogene Volcanic Field, which is situated at the inner side of the Carpathian arc over the Hercynian basement with the Late Paleozoic and Mesozoic sedimentary cover. Volcanic rocks of the High-K orogenic suite are of the Badenian through Pannonian age (16.5– 8.5 Ma). Their petrogenesis is closely related to subduction of flysch belt oceanic basement underneath the advancing Carpathian arc and to back-arc extension processes. The stratovolcano includes a large caldera 20 km in

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Kusky, Timothy M., Rose Ganley, Jennifer Lytwyn, and Ali Polat. "The Resurrection Peninsula Ophiolite, Mélange and Accreted Flysch Belts of Southern Alaska as an Analog for Trench-Forearc Systems in Precambrian Orogens." In Precambrian Ophiolites and Related Rocks. Elsevier, 2004. http://dx.doi.org/10.1016/s0166-2635(04)13020-x.

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Sakhlecha, Manish, Samir Bajpai, and Rajesh Kumar Singh. "Evaluating the Environmental Impact Score of a Residential Building Using Life Cycle Assessment." In Research Anthology on Environmental and Societal Well-Being Considerations in Buildings and Architecture. IGI Global, 2021. http://dx.doi.org/10.4018/978-1-7998-9032-4.ch006.

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Buildings consume major amount of energy as well as natural resources leading to negative environmental impacts like resource depletion and pollution. The current task for the construction sector is to develop an evaluation tool for rating of buildings based on their environmental impacts. There are various assessment tools and models developed by different agencies in different countries to evaluate building's effect on environment. Although these tools have been successfully used and implemented in the respective regions of their origin, the problems of application occur, especially during r

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Conference papers on the topic "Flysch Belt"

1

Ziarek, Zbigniew Jan. "DESIGNING GEOEDUCATIONAL TOOLS FOR GEOTOURISM NEEDS � A CASE STUDY OF THE OUTER FLYSCH CARPATHIANS." In 24th SGEM International Multidisciplinary Scientific GeoConference 24. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024/1.1/s01.06.

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A geoeducational tools are innovative solutions used to popularize knowledge in the field of Earth Sciences and the promotion of geotourism. These methods enhance the appreciation of geodiversity, raising awareness about cognitive and aesthetic values. By adopting this approach, there is a commitment to geoheritage protection for future generations. The efficacy of geoeducational instruments relates on a knowledge of geological processes and their outcomes, coupled with adept geointerpretation. During the geointerpretative phase it is important to maintain correctness and reliable explanation

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Pereszlény, M., J. Milicka, and R. Vitálos. "Outline of Petroleum Geology of the Flysch Belt, West Carpathians, Slovakia." In 60th EAGE Conference and Exhibition. European Association of Geoscientists & Engineers, 1998. http://dx.doi.org/10.3997/2214-4609.201408538.

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Zelman, J., M. Pereszlenyi, R. Vitalos, and J. Milicka. "New Oil Exploration Results in the Flysch Belt, the West Carpathians, Slovakia." In 61st EAGE Conference and Exhibition. European Association of Geoscientists & Engineers, 1999. http://dx.doi.org/10.3997/2214-4609.201408060.

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Krejcl, O., J. Svancara, F. Hubatka, and H. Thonová. "Internal structure and main evolution phases of the Flysch Belt, Carpathians, Czech Republic." In 58th EAEG Meeting. EAGE Publications BV, 1996. http://dx.doi.org/10.3997/2214-4609.201409143.

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Kuk, Edyta. "ANALYSIS OF CCS-EOR APPLICATION ON EXEMPLARY OIL FIELD FROM CARPATHIAN FLYSCH BELT." In 19th SGEM International Multidisciplinary Scientific GeoConference EXPO Proceedings. STEF92 Technology, 2019. http://dx.doi.org/10.5593/sgem2019v/1.4/s01.013.

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Francu, J., H. S. Poelchau, Z. Stránik, and J. Adámek. "Burial and thermal history of the Carpathian flysch belt in the Eastern Moravia Czech Republic." In 58th EAEG Meeting. EAGE Publications BV, 1996. http://dx.doi.org/10.3997/2214-4609.201409122.

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Dhima, S., E. Prenjasi, S. Nazaj, and V. Silo. "Evaluation of thrusting tectonics and reflection of flysch folds at top limestone level in Albania thrust belt (Western Balkan), based on geo-seismic study." In Geophysics of the 21st Century - The Leap into the Future. European Association of Geoscientists & Engineers, 2003. http://dx.doi.org/10.3997/2214-4609-pdb.38.f069.

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ГУСЕВ Н, И., Ю. РОМАНОВА Л, and Г. СКУБЛОВ С. "GEOCHEMISTRY AND AGE OF ZIRCON FROM KHAPCHAN ACCRETIONAL OLISTOSTROM OF ANABAR SHIELD." In ГЕОЛОГИЯ И МИНЕРАЛЬНО-СЫРЬЕВЫЕ РЕСУРСЫ СЕВЕРО-ВОСТОКА РОССИИ 2024. Crossref, 2024. http://dx.doi.org/10.53954/9785604990100_302.

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Chaotic breccias in carbonate rocks of the Paleoproterozoic Khapchan series of the Anabar Shield were characterized for the first time. Breccias belong to the flysch-carbonate subtype of accretionary olistostrome and confirm the existence of a subduction zone in the Paleoproterozoic in the east of the Anabar Shield. The olistostrome was formed in connection with underwater thrusts during the destruction of an accretionary uplift composed of weakly lithified and loose sedimentary material. The Sm-Nd isotope system of olistostrome rocks indicates a Paleoproterozoic age (TNd(DM2) = 2.34-2.42 Ga)

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Hinsch, Ralph. "Indications of Deep Marine Fans in the Early Miocene Foredeep of Lower Austria: A Potential New Play." In Abu Dhabi International Petroleum Exhibition & Conference. SPE, 2021. http://dx.doi.org/10.2118/208133-ms.

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Abstract The petroleum province in Lower Austria resulted from the Alpine collision and the subsequent formation of the Vienna Basin. OMV is active in this area since its foundation in 1956. Several plays have been successfully tested and produced in this complex geological region. The main exploration focus is currently on the deep plays. However, this paper proposes a so far unrecognized and therefore undrilled play in a shallower level to broaden OMV's portfolio in Austria. Seismic re-interpretations of reprocessed 3D seismic data and structural reconstructions were used to review some of t

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Chenevey, Paige, Alexandre Thibeault, Joshua Beard, and Eric Bergeron. "Modernizing Aerial Patrol - Real Life Remote Sensing for Liquid Leak and Threat Detection Along the Right of Way: First Detection Demonstrations of a Real Pipeline Seeper Leak, Encroachments, and Exposed Pipes Using a Traditional Aerial Patrol Plane." In 2024 15th International Pipeline Conference. American Society of Mechanical Engineers, 2024. https://doi.org/10.1115/ipc2024-123410.

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Abstract Since the end of 2022, Marathon Pipe Line LLC (MPL) has been using and testing Flyscan Systems’ (Flyscan) remote sensing technology over their liquid pipeline right of way (ROW) to benchmark and validate the use of machine learning (ML) algorithms, photogrammetry, and hyperspectral imaging to perform real-time threat detection, liquid leak detection of crude oil and refined products, as well as other advanced imaging features related to geo-hazards. This paper presents scientific approaches and real-life results from over 200 aerial patrols between November 2022 and December 2023, cov

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