Structural evolution of mylonitized gneiss zone from the northern flank of the Szeghalom dome (Pannonian Basin, SE Hungary) | Szegedi Tudományegyetem, Ásványtani, Geokémiai és Kőzettani Tanszék

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Structural evolution of mylonitized gneiss zone from the northern flank of the Szeghalom dome (Pannonian Basin, SE Hungary)

Reference:
Acta Mineralogica-Petrographica, Szeged 2001, Vol. 42, pp. 59-64

Szerző:
Dr. Schubert Félix
Dr. M. Tóth Tivadar

Abstract:
Metamorphic basement of the Pannonian Basin consists of blocks of incompatible metamorphic and structural evolution in the area of the Szeghalom high. Here evolution of a large-scale shear zone from the northern flank of the uplifted dome is studied. Textural relics suggest that the original rock type was orthogneiss widespread in the surroundings. Deformation produced a wide (over 200 m) shear zone with well-developed mylonite in the centre. We show, that the deformation followed the last progressive metamorphic event of the basement.

Letöltés:
AMP_schubertVol42.pdf

 

acta2001, mylonite, orthogneiss, Pannonian Basin, shear zone




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