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TZUNTIL:20281029T010000Z
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DTSTAMP:20261105T154545Z
DESCRIPTION:The Neogene plate-tectonic evolution of the Carpathian-Pannonia
 n region led tolarge-scale volcanism that is unparalleled in Europe. In re
 cent years\, detailedvolcanological\, K-Ar and Ar-Ar geochronological\, an
 d juvenile glass geochemicalstudies have significantly refined our knowled
 ge regarding specific eruptions. Scenarios forcolossal (VEI 7) Middle- and
  Late-Miocene eruptions were identified in the northern part of the Pannon
 ian Basin\; these events had profound impacts on the environment\, which w
 as characterized by a transition zone between land and sea (Central Parate
 thys). While these eruptions\, occurring between 20 and 10 Ma\, were drive
 n by crustal extension and mantle differentiation\, volcanism resulting fr
 om inward-directed subduction&mdash\;primarily along the Carpathian Arc&md
 ash\;was also present from ca. 16 Ma onwards\, from Miocene to Quaternary 
 times. The youngest phase of the subduction-related volcanism took place a
 t the Ciomadul (Csom&aacute\;d) volcano in Romania\; its eruptions (explos
 ive activity\, lahars\, etc.) occurred within the last 30\,000 years and i
 nfluenced the everyday life of early humansalready present in the area.
DTSTART;TZID=Europe/Berlin:20261125T123000
DTEND;TZID=Europe/Berlin:20261125T140000
LOCATION:K1 GEO
SUMMARY:Prof. Dr. David Karátson\, Eötvös Lorand University\, Budabest\, Hu
 ngary (Homepage): Miocene-Quaternary volcanism in the Carpathians and its 
 environmental impacts
TRANSP:TRANSPARENT
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