Magnetic susceptibility correlation of km-thick Eifelian–Frasnian sections (Ardennes and Moravia)

0345505 - GLÚ 2011 RIV BE eng J - Článek v odborném periodiku
Boulvain, F. - da Silva, A.C. - Mabille, C. - Hladil, Jindřich - Geršl, M. - Koptíková, Leona - Schnabl, Petr
Magnetic susceptibility correlation of km-thick Eifelian–Frasnian sections (Ardennes and Moravia).
GEOLOGICA BELGICA. Roč. 13, č. 4 (2010), s. 309-318. ISSN 1374-8505. E-ISSN 2034-1954
Grant CEP: GA AV ČR IAA300130702; GA AV ČR IAAX00130702
Výzkumný záměr: CEZ:AV0Z30130516
Klíčová slova: Devonian limestone * magnetic susceptibility * Moravian Karst * Ardennes
Kód oboru RIV: DB - Geologie a mineralogie
Impakt faktor: 0.645, rok: 2010
http://popups.ulg.ac.be/Geol/docannexe.php?id=3181

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.
Trvalý link: http://hdl.handle.net/11104/0186762