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Magnetic fabric of Late Miocene clay-rich sediments from the southern Pannonian basin (CROSBI ID 182730)

Prilog u časopisu | izvorni znanstveni rad | međunarodna recenzija

Márton, Emö ; Tomljenović, Bruno ; Pavelić, Davor ; Pethe, Mihálj ; Avanić, Radovan ; Jelen, Bogomir Magnetic fabric of Late Miocene clay-rich sediments from the southern Pannonian basin // International journal of earth sciences, 101 (2012), 3; 879-888. doi: 10.1007/s00531-011-0669-8

Podaci o odgovornosti

Márton, Emö ; Tomljenović, Bruno ; Pavelić, Davor ; Pethe, Mihálj ; Avanić, Radovan ; Jelen, Bogomir

engleski

Magnetic fabric of Late Miocene clay-rich sediments from the southern Pannonian basin

The magnetic fabric of Late Miocene sediments from the southern Pannonian basin was studied on oriented samples collected from 19 geographically distributed localities. All of them are characterized by nearhorizontal magnetic foliation plane after tilt correction, indicating weak deformation. Well-developed lineations were observed for 16 localities, which are interpreted as due to compressional/transpressional deformation, except from three localities, where the fabric must have been formed in an extensional setting. Comparison between the orientation of the map-scale folds and faults and magnetic lineation directions shows that magnetic lineation is either related to NNE-SSW directed compression, leading to the formation of folds or it can be connected to NW–SE or NNE-SSW trending dextral faults.

magnetic fabric; clay-rich sediments; tectonic deformation; southern Pannonian basin

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Podaci o izdanju

101 (3)

2012.

879-888

objavljeno

1437-3254

10.1007/s00531-011-0669-8

Povezanost rada

Geologija

Poveznice
Indeksiranost