Zircon trace element fingerprint of changing tectonic regimes in Permian rhyolites from the Central European Lowlands
Elżbieta Słodczyk,
Anna Pietranik,
Alexander Repstock
et al.
Abstract:The late Carboniferous/early Permian post-collisional rhyolites (305–285 Ma) that formed in Central Europe have generally similar whole rock compositions to that of older Late-Variscan rhyolites (330–310 Ma). However, data compilation combining zircon age with the chemical composition of rhyolites from 20 units shows a trend of increasing zircon saturation temperature with decreasing age. This trend is particularly well identified in rhyolites from the Central European Lowlands (CEL)—consisting of the NE Germa… Show more
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