Özet:

The magnetic complex located in the southern part of Mersin (Mersin) is found as a block within the Mersin melange, consisting of granite, granodiorit, granophyrus, granite porphyrus, diomit and diabaz stones. Granite stones provide granular, microgranular porphyric micrographic tissue while they say they offer official, diabetic stones entergranular tissue. The primary element geochemistry shows that these rockets are subalcal character. Normalized by Condrite, the rare soil element diagram provides a slight consumption of slightly rare soil elements, negative EU anomaly, and a distribution close to the bed. While granite stones are normalized according to the ocean back granites, the mercury diagrams offer consumption in terms of large cation litofil elements and high-value cations, the mercury diagrams normalized according to the ocean middle back basals of the mercury and diabetic stones offer consumption with high-ion semi-dimensional elements, the durability of the high elements. In the tektonomagmatic environment separation diagrams based on constant trace elements against alteration, the stones of the magmatic complex indicate the tektonic environments associated with the foam.

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