During the Cenozoic widespread anorogenic magmatism, unrelated to recent supra-
subduction zone modification of its mantle source, developed within the Mediterranean and …

Experimental studies of synthetic and natural basalt systems suggest that conditions of
magma genesis and fractionation depend fundamentally on mantle temperatures and …

High-Mg ultrapotassic volcanic rock occurrences of lamproitic affinity are exposed in
southwestern Anatolia, mostly within the Menderes Massif. From north to south the lamproitic …

In the Mediterranean area, lamproitic provinces in Spain, Italy, Serbia and Macedonia have
uniform geological, geochemical and petrographic characteristics. Mediterranean lamproites …

Post-collisional magmatism in western Anatolia began in the Eocene, and has occurred in
discrete pulses throughout the Cenozoic as it propagated from north to south, producing …

Abstract The Middle Miocene Afyon alkaline volcanic complex (western Anatolia) erupted
lavas of highly variable geochemistry, ranging from silica-undersaturated to silica …

Paleogene mafic potassic and ultrapotassic volcanic rocks in western Yunnan, China, show
a compositional spectrum from potassic trachybasalt to latite (MgO= 6· 24–21· 8 wt%; SiO2 …

Melting experiments on ultramafic rocks rich in the hydrous minerals phlogopite or
phlogopite+ K-richterite, some including 5% of accessory phases, have been conducted at …

Abstract The modern Anatolian–African plate boundary is represented by a north-dip**
subduction zone that has been part of a broad domain of regional convergence between …

We present a compilation and comparison of geochemical data of Aegean Eocene to
Recent magmatic rocks:(1) North Anatolian Eocene magmatic rocks (NAEM),(2) Aegean to …