Geochemistry and origin of the Battonya unit granitoids, SE Hungary
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 geochemistr...
Elmentve itt :
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| Dokumentumtípus: | Cikk |
| Megjelent: |
Department of Mineralogy, Geochemistry and Petrology, University of Szeged
Szeged
2002
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| Sorozat: | Acta mineralogica-petrographica
43 |
| Kulcsszavak: | Földtan, Kőzettan, Ásványtan, Geokémia |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/25099 |
| Tartalmi kivonat: | 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. |
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| Terjedelem/Fizikai jellemzők: | 65-69 |
| ISSN: | 0365-8066 |