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Magnetic susceptibility correlation of km-thick Eifelian–Frasnian sections (Ardennes and Moravia)
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SYSNO ASEP 0345505 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title Magnetic susceptibility correlation of km-thick Eifelian–Frasnian sections (Ardennes and Moravia) Author(s) Boulvain, F. (BE)
da Silva, A.C. (BE)
Mabille, C. (BE)
Hladil, Jindřich (GLU-S) RID, SAI
Geršl, M. (CZ)
Koptíková, Leona (GLU-S) RID, SAI
Schnabl, Petr (GLU-S) RID, SAI, ORCIDSource Title GEOLOGICA BELGICA - ISSN 1374-8505
Roč. 13, č. 4 (2010), s. 309-318Number of pages 10 s. Publication form WWW - WWW Language eng - English Country BE - Belgium Keywords Devonian limestone ; magnetic susceptibility ; Moravian Karst ; Ardennes Subject RIV DB - Geology ; Mineralogy R&D Projects IAA300130702 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR) IAAX00130702 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR) CEZ AV0Z30130516 - GLU-S (2005-2011) UT WOS 000285908500003 EID SCOPUS 77954593020 Annotation This paper focuses on the comparison of the magnetic susceptibility (MS) curves over a large distance and across the facies. The Ardennes section shows an alternation of near shore platform, ramp and mound environments where detrital inputs are very important. Time-equivalent facies in the area of the Moravian Karst correspond to high purity limestones of open-sea platform type where Amphipora beds dominated shallow reef interior. In spite of these differences, the Eifelian-Frasnian MS pattern successions of Belgium have a great similarity to Moravia. The atmospheric circulation of dust and its widespread distribution on the Devonian globe is an appropriate mechanism through which this continuity can be explained. Workplace Institute of Geology Contact Jana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272 Year of Publishing 2011
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