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The role of paramagnetic minerals in clay sediments magnetic anisotropy: correlation between magnetic fabric and chlorite preferred orientation
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SYSNO ASEP 0050506 Document Type A - Abstract R&D Document Type The record was not marked in the RIV R&D Document Type Není vybrán druh dokumentu Title The role of paramagnetic minerals in clay sediments magnetic anisotropy: correlation between magnetic fabric and chlorite preferred orientation Title Význam paramagnetických minerálů v magnetické anizotropii jílových sedimentů: korelace mezi magnetickou stavbou a přednostní orientací chloritů Author(s) Cifelli, F. (IT)
Mattei, M. (IT)
Chadima, Martin (GLU-S) RID, SAI
Hirt, A. M. (CH)
Lenser, S. (DE)Source Title Travaux Géophysiques. - : Geofyzikální ústav AV ČR, v. v. i. - ISSN 0231-5548
Roč. 38, - (2006), s. 24-24Number of pages 1 s. Action Castle Meeting New Trends in Geomagnetism, Paleo, Rock and Environmental Magnetism /10./ Event date 03.09.2006-08.09.2006 VEvent location Valtice Country CZ - Czech Republic Event type WRD Language eng - English Country CZ - Czech Republic Keywords magnetic anisotropy ; neutron diffraction analysis ; clay sediments Subject RIV DB - Geology ; Mineralogy CEZ AV0Z30130516 - GLU-S (2005-2011) Annotation In this study we investigate the mechanism that is responsible for the magnetic lineation in apparently homogeneous clay sediments where deformation is not visible at the outcrop scale. The studied rocks are Neogene clay sediments sampled from different tectonic settings: the Calabrian Arc (Southern Italy) and the Rif Chain (Morocco). These results demonstrate the great potential of the AMS to determine the mineral orientation fabric. Workplace Institute of Geology Contact Jana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272 Year of Publishing 2007
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