Volcanic facies and hydrothermal processes in Triassic pillow basalts from the Darnó Unit, NE Hungary

Gabriella Kiss, F. Molnár, Ladislav A. Palinkaš

Research output: Contribution to journalArticle

16 Citations (Scopus)

Abstract

The Darnó Unit within the Zagorje-Mid-Transdanubian Megaunit is an allochtonous part of Dinarides in NE-Hungary and represents a relict of the Neotethyan accretionary complex. It contains blocks of submarine basalts of Triassic age in turbiditic sediments (olistrostrome) of Jurassic age. The lava clogged in the lime mud at the original site ofvolcanism and developed closely packed pillow, pillow fragment hyaloclastite breccia, and peperite facies. Interaction between the lava and the sea water produced mostly chloritic alteration of basalt and precipitation of hydrothermal calcite in amygdales, feeding channels of lava lobes and hyaloclastite breccia cements. Calcite is associated with chlorite, epidote, hematite and pyrite. Fluid inclusions in calcite infillings record conditions of fluid/rock interaction. Salinities of fluid inclusions (3.2-5.6 wt.%. NaCl equiv. wt.%.) are close to the salinity of recent sea water and their homogenization temperatures are in the range of 80-150°C. Fluid inclusion data support interpretation that volcanic fades represent rapidly cooled distal zones away from the submarine volcanic centre. This is also confirmed by the comparison to the volcanic and hydrothermal alteration facies of the submarine basalt lava-flow complex and associated pillow lava formation of Triassic age in the Hruškovec quarry in the Kalnik Mts., NW-Croatia. The obtained data contribute to understanding of the early history of Neotethyan evolution, i.e. dilemma about rifting or oceanization in Triassic time and offer new aspects of correlation between units of Dinaridic origin which had been displaced from their original setting by large scale Tertiary tectonic processes.

Original languageEnglish
Pages (from-to)385-394
Number of pages10
JournalGeologia Croatica
Volume61
Issue number2-3
Publication statusPublished - Dec 2008

Fingerprint

lava
hyaloclastite
fluid inclusion
Triassic
calcite
basalt
breccia
peperite
pillow lava
seawater
salinity
epidote
hydrothermal alteration
lava flow
quarry
hematite
lime
rifting
chlorite
pyrite

Keywords

  • Basalt pillow lavas
  • Darnó Unit
  • Dinarides
  • Fluid inclusions
  • NE-Hungary
  • NW-Croatia
  • Peperite
  • Triassic rifting
  • Zagorje - Mid-Transdanubian megaunit

ASJC Scopus subject areas

  • Geology

Cite this

Volcanic facies and hydrothermal processes in Triassic pillow basalts from the Darnó Unit, NE Hungary. / Kiss, Gabriella; Molnár, F.; Palinkaš, Ladislav A.

In: Geologia Croatica, Vol. 61, No. 2-3, 12.2008, p. 385-394.

Research output: Contribution to journalArticle

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