Trace elements in metamorphic and granitoid rocks of the basement in the Central Danube-Tisza Interfluve (Hungary)

Tomschey Ottó: Trace elements in metamorphic and granitoid rocks of the basement in the Central Danube-Tisza Interfluve (Hungary). In: Acta mineralogica-petrographica, (28). pp. 47-55. (1986)

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Abstract

Trace elements of the metamorphic and granitoid rocks of the Kiskunhalas—Tazlar—Szank— Jaszszentlaszl6 region lying in the central part of the Danube—Tisza Interfluve were studied. By means of the trace element diagrams the trace element distribution of different rock types can be compared and the premetamorphic rocks can be identified with satisfactory approximation, as well. In the region in question the gneisses are of pelitic, the amphibolites of basis igneous origin, with high probability. Migmatitization and milonitization did not cause considerable changes in the trace element compositions of the rocks. The trace element distribution pattern of granitoids remarkably differs from that of the metamorphic rocks. Keywords: metamorphic rocks, granitoid rocks, trace element geochemistry, pedogenesis.

Item Type: Article
Journal or Publication Title: Acta mineralogica-petrographica
Date: 1986
Volume: 28
ISSN: 0365-8066
Page Range: pp. 47-55
Language: English
Publisher: University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Place of Publication: Szeged
Related URLs: http://acta.bibl.u-szeged.hu/39406/
Uncontrolled Keywords: Kőzettan, Ásványtan, Földtan
Additional Information: Bibliogr.: p. 54-55. ; 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. Jul. 26. 13:21
URI: http://acta.bibl.u-szeged.hu/id/eprint/24747

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