NEHYBA, Slavomir. Role of extension within the evolution of the foreland basin - a case study from the Lower Badenian deposits of the Carpathian Foredeep [Czech Republic]. In Scenic sedimentology. Muscat: Sultan Qaboos University JVC, 2005, p. 116-116.
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Basic information
Original name Role of extension within the evolution of the foreland basin - a case study from the Lower Badenian deposits of the Carpathian Foredeep [Czech Republic]
Name in Czech Role extenze v ramci vyvoje predpolni panve - prikladova studie ze sedimentu spodniho badenu karpatske predhlubne
Authors NEHYBA, Slavomir (203 Czech Republic, guarantor).
Edition Muscat, Scenic sedimentology, p. 116-116, 1 pp. 2005.
Publisher Sultan Qaboos University JVC
Other information
Original language English
Type of outcome Proceedings paper
Field of Study 10500 1.5. Earth and related environmental sciences
Country of publisher Oman
Confidentiality degree is not subject to a state or trade secret
RIV identification code RIV/00216224:14310/05:00012350
Organization unit Faculty of Science
Keywords in English foreland basin; extension
Tags extension, foreland basin
Changed by Changed by: prof. RNDr. Slavomír Nehyba, Dr., učo 2710. Changed: 12/1/2005 07:23.
Abstract
All main stratigraphic units of the foreland basin are traditionally evaluated as the response of flexural subsidence of the foreland plate and thrust loading. Formation of the wedge shaped body of sediments issupposed with its thickening towards the orogenic front. Progressive thrusting should result to the characteristic distribution of deposits with various lithology and stratigraphy. The position of the Lower badenian deposits within the Carpathian Foredeep basin and their facies distribution is not in coincidence with this model.
Abstract (in Czech)
All main stratigraphic units of the foreland basin are traditionally evaluated as the response of flexural subsidence of the foreland plate and thrust loading. Formation of the wedge shaped body of sediments issupposed with its thickening towards the orogenic front. Progressive thrusting should result to the characteristic distribution of deposits with various lithology and stratigraphy. The position of the Lower badenian deposits within the Carpathian Foredeep basin and their facies distribution is not in coincidence with this model.
Links
GA205/03/1204, research and development projectName: Depoziční architektura sedimentů spodního badenu v jižní a střední části karpatské předhlubně na Moravě
Investor: Czech Science Foundation, Depositional archtecture of the Lower Badenian deposits in the southern and middle part of the carpathian Foredeep in Moravia
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