Xenoliths from Cretaceous lamprophyres of Alcsútdoboz-2 borehole, Transdanubian Central Mountains, Hungary

Szabó Csaba: Xenoliths from Cretaceous lamprophyres of Alcsútdoboz-2 borehole, Transdanubian Central Mountains, Hungary. In: Acta mineralogica-petrographica, (27). pp. 39-50. (1985)

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Abstract

Lower Triassic sediments of Alcsútdoboz-2 borehole (30 km W of Budapest (are cross-cut by alkaline lamprophyre dykes. These dykes contain xenoliths (megacrysts, ultramafic rocks, alkaline magmatité, quartzite inclusions and carbonatic evaporites) originated from different depths. Ultramafics contain phlogopite which is characteristic for lherzolite nodules of mantle origin. The alkaline magmatité xenoliths indicate contact of the melt with an alkaline intrusion in depth, which may bear significant economic importance.

Item Type: Article
Journal or Publication Title: Acta mineralogica-petrographica
Date: 1985
Volume: 27
ISSN: 0365-8066
Page Range: pp. 39-50
Language: English
Publisher: University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Place of Publication: Szeged
Related URLs: http://acta.bibl.u-szeged.hu/39405/
Uncontrolled Keywords: Kőzettan, Ásványtan, Földtan
Additional Information: Bibliogr.: 50. 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. Jul. 26. 11:19
URI: http://acta.bibl.u-szeged.hu/id/eprint/24726

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