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 |
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| 040 | |a SZTE Egyetemi Kiadványok Repozitórium |b hun | ||
| 041 | |a eng | ||
| 100 | 2 | |a Pál Molnár Elemér | |
| 245 | 1 | 0 | |a Geochemistry and origin of the Battonya unit granitoids, SE Hungary |h [elektronikus dokumentum] / |c Pál Molnár Elemér |
| 260 | |a Department of Mineralogy, Geochemistry and Petrology, University of Szeged |b Szeged |c 2002 | ||
| 300 | |a 65-69 | ||
| 490 | 0 | |a Acta mineralogica-petrographica |v 43 | |
| 520 | 3 | |a 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. | |
| 650 | 4 | |a Természettudományok | |
| 650 | 4 | |a Föld- és kapcsolódó környezettudományok | |
| 695 | |a Földtan, Kőzettan, Ásványtan, Geokémia | ||
| 700 | 0 | 1 | |a Kovács Gábor |e aut |
| 856 | 4 | 0 | |u http://acta.bibl.u-szeged.hu/25099/1/mineralogica_043_065-069.pdf |z Dokumentum-elérés |