The magmatic complex is located in south of Çamlıyayla (Mersin), as block in the Mersin melange and composed of granite, granodiorite, granophyre, granite porphyry, diorite, and diabase. Granitic rocks present granular, microgranular porphyric, micrographic textures while diorites present ophitic and diabase dikes present intergranular textures. The whole rock major and trace element geochemistry of the magmatic complex rocks indicate that they have subalkaline compositions. Chondrite-normalized rare earth elements diagram display slightly depletion in light rare earth elements and negative Eu anomalies with nearly flat patterns. Ocean ridge granites normalized spider diagram of granitic rocks show large ion litophile element and high field strength element depletion whereas mid-ocean ridge basalt normalized spider diagram of the diorite and diabase rocks exhibit large ion litophile element enrichment and high field strength element depletion. The magmatic complex rocks are plotted on arc setting based on the immobile trace element diagrams.
Primary Language | Turkish |
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Journal Section | Articles |
Authors | |
Publication Date | June 30, 2018 |
Published in Issue | Year 2018 Volume: 33 Issue: 2 |