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Enhanced carboniferous magmatism reveals the paleo-tethys dual subduction system: New detrital zircon evidence from western Türkiye
The tectonic evolution of the Paleo-Tethys Ocean in Türkiye is controversial, especially the polarity of subduction. This study reports new detrital zircon U-Pb ages and trace-element data from Mesozoic-Cenozoic sandstones of the Tavşanlı Zone and the Taurides Belt, both belonging to or tectonically
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