A Miskolc-7, Miskolc-8 és Nyékládháza-1 fúrások miocén vulkáni kőzetei és párhuzamosításuk a Bükkalja vulkáni képződményeivel

Translated title of the contribution: The Miocene pyroclastic rocks of the boreholes Miskolc-7, Miskolc-8 and Nyékládháza-1 and their correlation with the ignimbrites of Bükkalja

Lukács Réka, Harangi Szabolcs, Radócz Gyula, Kádár Marianna, Pécskay Zoltán, Theodoros Ntaflos

Research output: Contribution to journalArticle

3 Citations (Scopus)


The nearly continuous drilling cores of the boreholes Miskolc-7, Miskolc-8 and Nyékládháza-1 provide a unique opportunity to investigate the nature of the thick Miocene volcanic formations present in the boreholes. The large number of volcanic layers implies there was repeated, intense volcanic activity from 19 Ma to 12 Ma. This work focuses on the volcanological, petrologic, geochemical and geochronological characterization of the thickest volcanic units. Most of the pyroclastic products were formed during the course of deposition from pumiceous pyroclastic flows under subaerial conditions, and therefore they are ignimbrites. The 18-19 Ma-old non-welded to welded ignimbrite shows many features similar to the pumiceous pyroclastic deposits which occurred over a wide area in the northern Pannonian Basin beneath the Ottnangian-Karpathian coal-bearing sequence. The large thickness (>140 metres) in the studied boreholes indicates an eruption of significant magnitude, possibly accompanied with the formation of a caldera or repeated explosive eruptions in the proximity of the area of the boreholes. The borehole Nyékládháza-1 revealed a 250 metre-thick volcanic suite above the coal-bearing sedimentary series. The data indicate a large temporal difference (ca. 3 Myr) between the lower and upper portion of this sequence! The respective volcanological nature and composition of the phenocrysts of the lower, 15-16 Ma-old ignimbrite are different from those characterize the ignimbrites of the middle volcanic suite of the Bükkalja. Therefore, an eruption of compositionally different silicic magmas could have occurred almost contempor-aneously in the northern Pannonian Basin during the Middle Miocene. In contrast, the 12-13 Ma-old ignimbrite found in the upper part of this thick volcanic sequence can be unambiguously correlated with the Harsány ignimbrite unit from the eastern part of the Bükkalja. The results obtained strongly suggest that the well-defined regional volcanic key-horizons in the Pannonian Basin should be revised. In contrast earlier suppositions, the present study emphasizes repeated volcanic eruptions throughout the Miocene and additionally, compositionally different magmas could have erupted frequently and contemporaneously, even in spatially restricted areas.

Original languageHungarian
Pages (from-to)31-48
Number of pages18
JournalFoldtani Kozlony
Issue number1
Publication statusPublished - Jan 1 2010


ASJC Scopus subject areas

  • Geology
  • Geochemistry and Petrology
  • Stratigraphy
  • Palaeontology

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