Nédli Zsuzsanna and M. Tóth Tivadar: Mantle xenolith in the mafic dyke at Beremend, Villány Mts., SW Hungary. In: Acta mineralogica-petrographica, (40). pp. 97-103. (1999)
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Abstract
Spinel lherzolite nodules of an U, Cretaceous mafic dyke in the Villány Mts. were studied. The xenolith consists of olivine, enstatite, Cr-diopside and Cr-Fe spinel as primary phases. No garnet or plagioclase is present. Alteration of the rock resulted in breakdown of olivine and formation of calcite, limonite and clay minerals. These processes can geochemically be followed by a significant loss of Mg and Ni as well as a gain of Ca relative to an average spinel lherzolite.
Item Type: | Article |
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Journal or Publication Title: | Acta mineralogica-petrographica |
Date: | 1999 |
Volume: | 40 |
ISSN: | 0365-8066 |
Page Range: | pp. 97-103 |
Language: | English |
Publisher: | University of Szeged, Department of Mineralogy, Geochemistry and Petrology |
Place of Publication: | Szeged |
Related URLs: | http://acta.bibl.u-szeged.hu/39419/ |
Uncontrolled Keywords: | Kőzettan, Ásványtan, Földtan |
Additional Information: | Bibliogr.: p. 102-103. ; 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. 27. 15:29 |
URI: | http://acta.bibl.u-szeged.hu/id/eprint/24881 |
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