Geochemistry and Origin of the Battonya Unit Granitoids, SE Hungary | Szegedi Tudományegyetem, Ásványtani, Geokémiai és Kőzettani Tanszék

Reference:
Acta Mineralogica-Petrographica, Szeged 2002, Vol. 43, pp. 65-69

Szerző:
Dr. Pál-Molnár Elemér
Kovács Gábor

Abstract:
Boreholes deepened in the axis zone of the uplifted Pusztaföldvár-Battonya High (Battonya Unit, Békésia Terrane, Tisia Composite Terrane, Pannonian Basin) reached granitoid rocks in the Variscan crystalline basement at a depth of 1000-2000 m. On the basis of trace and rare earth elements geochemistry and zircon morphology investigations, the granitoids of the Pusztaföldvár-Battonya High have a peraluminous, subalkaline, calc-alkaline character. The studied rocks are S-type, and were formed in a syn-collisional (continent-continent collision zone) environment.

 
Letöltés

acta2002, Battonya Unit, crystalline basement, geochemistry, granite, Hungary, Tisia Composite Terrane