Molnár Sándor: Petrochemical character of the Lower Cretaceous rocks of the Great Hungarian Plain. In: Acta mineralogica-petrographica, (27). pp. 33-38. (1985)
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Abstract
Originally the Lower Cretaceous volcanics of the Great Plain proved to be olivine-free, pyroxene-bearing and feldspar-rich basaltic rocks. The initial magma was of tholeiitic composition. The volcanics were erupted in seawater and subsequently spilitized and auto-metasomatized. At the Lower and Upper Cretaceous boundary the rocks were uplifted and endured epigenic alteration. Their genesis is related to an early Cretaceous rift formation.
| Item Type: | Article |
|---|---|
| Journal or Publication Title: | Acta mineralogica-petrographica |
| Date: | 1985 |
| Volume: | 27 |
| ISSN: | 0365-8066 |
| Page Range: | pp. 33-38 |
| 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.: 38. 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. 11:10 |
| URI: | http://acta.bibl.u-szeged.hu/id/eprint/24725 |
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