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

被引：4

作者：

Marton, Emo ^{[1
]}

Tomljenovic, Bruno ^{[2
]}

Pavelic, Davor ^{[2
]}

Pethe, Mihaly ^{[1
,3
]}

Avanic, Radovan ^{[4
]}

Jelen, Bogomir ^{[5
]}

机构：

[1] Eotvos Lorand Geophys Inst Hungary, Palaeomagnet Lab, H-1145 Budapest, Hungary

[2] Univ Zagreb, Fac Min Geol & Petr Engn, Zagreb 10000, Croatia

[3] Eotvos Lorand Univ, Dept Geophys, H-1117 Budapest, Hungary

[4] Croatian Geol Survey, Zagreb 10000, Croatia

[5] Geoloski Zavod Slovenije, Ljubljana 1109, Slovenia

来源：

INTERNATIONAL JOURNAL OF EARTH SCIENCES | 2012年 / 101卷 / 03期

基金：

匈牙利科学研究基金会;

关键词：

Magnetic fabric; Clay-rich sediments; Tectonic deformation; Southern Pannonian basin; COUNTERCLOCKWISE ROTATION; WESTERN CARPATHIANS; TECTONIC EVOLUTION; CENTRAL PARATETHYS; LAKE PANNON; NW CROATIA; SYSTEM; DEFORMATION; ANISOTROPY; DINARIDES;

D O I：

10.1007/s00531-011-0669-8

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

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 near-horizontal 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.

引用

页码：879 / 888

页数：10

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