Počet záznamů: 1
Magnetic susceptibility correlation of km-thick Eifelian–Frasnian sections (Ardennes and Moravia)
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SYSNO ASEP 0345505 Druh ASEP J - Článek v odborném periodiku Zařazení RIV J - Článek v odborném periodiku Poddruh J Článek ve WOS Název Magnetic susceptibility correlation of km-thick Eifelian–Frasnian sections (Ardennes and Moravia) Tvůrce(i) 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, ORCIDZdroj.dok. GEOLOGICA BELGICA - ISSN 1374-8505
Roč. 13, č. 4 (2010), s. 309-318Poč.str. 10 s. Forma vydání WWW - WWW Jazyk dok. eng - angličtina Země vyd. BE - Belgie Klíč. slova Devonian limestone ; magnetic susceptibility ; Moravian Karst ; Ardennes Vědní obor RIV DB - Geologie a mineralogie CEP IAA300130702 GA AV ČR - Akademie věd IAAX00130702 GA AV ČR - Akademie věd CEZ AV0Z30130516 - GLU-S (2005-2011) UT WOS 000285908500003 EID SCOPUS 77954593020 Anotace 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. Pracoviště Geologický ústav Kontakt Jana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272 Rok sběru 2011
Počet záznamů: 1