Trace-Element Modeling and Source Constraints for Tholeiitic and Cale-alkaline Basalts from a Depleted Asthenospheric Mantle Source, Mt. Erciyes Stratovolcano, Turkey

@article{Kurkcuoglu2001TraceElementMA,
  title={Trace-Element Modeling and Source Constraints for Tholeiitic and Cale-alkaline Basalts from a Depleted Asthenospheric Mantle Source, Mt. Erciyes Stratovolcano, Turkey},
  author={B. Kurkcuoglu and E. Şen and A. Temel and E. Aydar and A. Gourgaud},
  journal={International Geology Review},
  year={2001},
  volume={43},
  pages={508 - 522}
}
The Mt. Erciyes stratovolcano was built up in an intraplate tectonic environment as a consequence of Eurasian and Afro-Arabian continental collision. However, the volcanic products generally exhibit a calc-alkaline character; minor amounts of tholeiitic basalts are also present. Tholeiitic basalts show high Fe2O3, MgO, CaO, low K2O, and depleted Ba, Nb, and especially Rb (2.3-5.97 ppm) contents, low 87Sr/86Sr (0.703344-0.703964), and high 143Nd/144Nd (0.512920-0.512780) isotopic ratios. These… Expand
13 Citations
Petrogenetic modelling of Quaternary post-collisional volcanism: a case study of central and eastern Anatolia
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