Pál Molnár Elemér and Kovács Gábor: Geochemistry and origin of the Battonya unit granitoids, SE Hungary. In: Acta mineralogica-petrographica, (43). pp. 65-69. (2002)
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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.
| Item Type: | Article |
|---|---|
| Heading title: | Notes |
| Journal or Publication Title: | Acta mineralogica-petrographica |
| Date: | 2002 |
| Volume: | 43 |
| ISSN: | 0365-8066 |
| Page Range: | pp. 65-69 |
| Language: | English |
| Publisher: | Department of Mineralogy, Geochemistry and Petrology, University of Szeged |
| Place of Publication: | Szeged |
| Related URLs: | http://acta.bibl.u-szeged.hu/39424/ |
| Uncontrolled Keywords: | Földtan, Kőzettan, Ásványtan, Geokémia |
| Additional Information: | Bibliogr.: 69. p. ; ill. ; összefoglalás angol nyelven |
| Subjects: | 01. Natural sciences 01. Natural sciences > 01.05. Earth and related environmental sciences |
| Date Deposited: | 2016. Oct. 17. 09:25 |
| Last Modified: | 2022. Aug. 11. 12:45 |
| URI: | http://acta.bibl.u-szeged.hu/id/eprint/25099 |
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