Timing Aegean extension: Evidence from in situ U–Pb geochronology and cathodoluminescence imaging of granitoids from NW Turkey

Kinematic reconstructions and magmatic evolution illuminating crustal and mantle dynamics of the eastern Mediterranean region since the late Cretaceous

“…Oligocene-early Miocene [Black et al, 2013] and in the Menderes massif and the Cyclades in the Miocene (figure 5) [Faure and Bonneau, 1988;Altherr and Siebel, 2002;Piper, 2006, 2007;Iglseder et al, 2009;Denèle et al, 2011;Laurent et al, 2015;. Migmatites associated with S-type granites have also been described in the cores of these metamorphic domes [Jansen and Schuiling, 1976;Lister et al, 1984;Okay and Satır, 2000b;Vanderhaeghe, 2004;Bozkurt et al, 2010;Kruckenberg et al, 2011;Laurent et al, 2015;Beaudoin et al, 2015].…”

Peritectic assemblage entrainment and mafic–felsic magma interaction in the Late Oligocene–Early Miocene Karadağ Pluton in the Biga Peninsula, northwest Turkey: petrogenesis and geodynamic implications

“…In addition, Castro (2013) implied that mafic magmas were derived from metasomatized mantle, and that their high water content was effective on the texture of these rocks, such as euhedral hornblende. Black et al (2013) argued that granitic magmas were formed by the dehydration of subducting slabs, which induced fluid-flux melting of the lithospheric mantle and partial melting of the overlying Sakarya Zone.…”