<b>Enhanced Carboniferous Magmatism Reveals the Paleo-Tethys Dual Subduction System and Climatic Changes: New Detrital Zircon Evidence from Western Türkiye</b>

We present new detrital zircon U-Pb geochronology and trace element data from Mesozoic-Cenozoic sandstones in western Türkiye to investigate the distribution and tectonic significance of Carboniferous magmatic arcs in the Pontides and the Anatolide-Tauride Block.