On the interpretation of normal and inverse magnetic fabric in dikes: Examples from the Eger Graben, NW Bohemian Massif

Author:

Chadima Martin,Cajz Vladimír,Týcová Patricie

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference42 articles.

1. Intrusive geometries and Cenozoic stress history of the Northern part of the Bohemian Massif;Adamovič;Geolines,1999

2. Magnetic versus crystallographic fabric in a basaltic lava flow;Bascou;J. Volcanol. Geotherm. Res.,2005

3. Theoretical single-domain grain size range in magnetite and titanomagnetite;Butler;J. Geoph. Res.,1975

4. Magma flow directions of shallow dykes from the East Greenland volcanic margin inferred from magnetic fabric studies;Callot;Tectonophysics,2001

5. Dyke swarm pattern and tectonics in the České středohoří Mts. Volcanic Centre, Ohře (Eger) Rift, Central Europe (Starting Points for Further Research);Cajz;Geolines,2003

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