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 |
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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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