Abstract: The Tauride-Anatolide Platfom includes of widespread Paleozoic (Cambrian to Permian) units, whichrarely consist magmatic rocks that were identified in two areas: Eastern Taurides (SW of Tufanbeyli and Yahyalı) andCentral Taurides (Northern Konya). There are problematic views related to the magmatic evolution of these rocks.The available geochemical database is mostly concentrated on the magmatics from the Central Taurides (KonyaRegion).In this study, the mafic volcanic rocks were recently found in the Eastern Taurides (Develi-Kayseri). These maficvolcanics are intercalated with the Late Devonian limestones and covered by the Early Carboniferous sandstones.The geochemical charateristics of the volcanic rocks exhibit back arc basin (BAB) features with slightly negative Nbanomalies, normal-MORB (NMORB)-like high field strength element (HFSE) patterns and flat REE profile.The newly found basic volcanic rocks in the Eastern Taurides geochemically resemble the meta-diabase dykes in theKonya and Yahyalı regions, which were assigned to a subduction related event. The new data reported in this studywill benefit to better understand the mid-Paleozoic evolution of the Taurides.