LA-ICP-MS U-Pb zircon geochronology data of the Early to Mid-Miocene syn-extensional massive silicic volcanism in the Pannonian Basin (East-Central Europe)
Réka Lukács,
Marcel Guillong,
Jakub Sliwinski,
István Dunkl,
Olivier Bachmann,
Szabolcs Harangi
Affiliations
Réka Lukács
MTA-ELTE Volcanology Research Group, 1117, Pázmány Péter sétány 1/C, Budapest, Hungary; Corresponding author at: MTA-ELTE Volcanology Research Group, 1117, Budapest Pázmány Péter sétány 1/C, Budapest, Hungary.
Marcel Guillong
Institute of Geochemistry and Petrology, Department of Earth Sciences, ETH Zürich, Clausiusstrasse 25, 8092 Zürich, Switzerland
Jakub Sliwinski
Institute of Geochemistry and Petrology, Department of Earth Sciences, ETH Zürich, Clausiusstrasse 25, 8092 Zürich, Switzerland
István Dunkl
Sedimentology & Environmental Geology, Geoscience Center, University of Göttingen, Goldschmidtstrasse 3, D-37077 Göttingen, Germany
Olivier Bachmann
Institute of Geochemistry and Petrology, Department of Earth Sciences, ETH Zürich, Clausiusstrasse 25, 8092 Zürich, Switzerland
Szabolcs Harangi
MTA-ELTE Volcanology Research Group, 1117, Pázmány Péter sétány 1/C, Budapest, Hungary; Department of Petrology and Geochemistry, Eötvös Loránd University, 1117, Budapest Pázmány Péter sétány 1/C, Budapest, Hungary
This article provides LA-ICP-MS in-situ U-Pb zircon dates performed on single crystals from dacitic to rhyolitic ignimbrites of the Bükkalja Volcanic Field (Hungary, East-Central Europe) temporally covering the main period of the Neogene silicic volcanic activity in the Pannonian Basin. The data include drift-corrected, alpha dose-corrected, Th-disequilibrium-corrected, and filtered data for geochronological use. The data presented in this article are interpreted and discussed in the research article entitled “Early to Mid-Miocene syn-extensional massive silicic volcanism in the Pannonian Basin (East-Central Europe): eruption chronology, correlation potential and geodynamic implications” by Lukács et al. (2018) [1].
