Özet:

With this study, the rocks of the old Elazığ Magmatites, which are floating around the castle district (Malatya), are studied in terms of geochemical properties. In the study area, except for the Elazığ Magmatites, the late Cretaceous Old Spender Offiolites and the Middle Eosen Old Mining Complex are floating again with the Middle Eosen and the younger old sedimentary stones. Surface rockers offer composition intervals ranging from basalt to riyolite; deep rockers offer composition intervals ranging from gabro to tonality and granite. During land studies, it is observed that plutonic rockets cut the surface rockets. Geochemical data indicate that the plutonic stones that show the basalt and gabro-tonality direction are low-K toleyts, the granite-granodiorite composite stones are kalk-alcalic and monzonic composite stones are shosonic. Magmatites, which are a part of the old Late Cretaceous Magmatites, which are widely floating in the area, are island emission products formed on the ocean-in-earth zone of the Neotetis Ocean, which is closed in the Late Cretaceous with a north-oriented deforestation.

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