Tephrochronology of a distal tonstein layer within the Maritsa East lignite basin, Bulgaria: Potential sources of the Miocene large explosive eruption

This contribution presents the age of the detrital zircons from the coal bearing Miocene succession of the Maritsa East lignite basin. We report a new finding of thin kaolinized pyroclastic beds (tonstein) in the coal bearing succession. The analysis of the detrital age component shows sedimentary input from the basement of the proximal area. The most abundant age cluster 290-315 Ma shows that the predominant sources are the Early Permian-Late Carboni-ferous intrusions in the area. The newly-recognized tonstein beds represent the products of large, distal pyroclastic erup-tions and are an important element of the sedimentary succession. They are dated at 14.31 +/- 0.30 Ma, which corresponds to the absolute age of the organic matter deposition of the productive middle lignite seam. Their source could most likely be related to the Miocene acid paroxysm ignimbrite eruptions in the Pannonian basin.

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This contribution presents the age of detrital zircons in the coal-bearing Miocene succession of the Maritsa East lignite basin, along with a new finding of pyroclastic beds in the same succession. The detrital age component analysis reveals input from proximal area basement, with the most common age cluster indicating sources from Early Permian-Late Carboniferous intrusions. The newly-recognized pyroclastic beds are products of distal volcanic eruptions and play a significant role in the sedimentary succession.