Biography:
2020 – Profesor, Eurasia Institute of Earth Sciences, Istanbul Technical University (ITU)
2018 – Profesor, Coordinator of Eastern Mediterranean Oceanography and Limnology Research Center (EMCOL)
2014 – 2020 Assoc Prof., Istanbul Technical University Faculty of Mines, Geology Engineering Department
2010 – 2014 Assoc Prof., Fırat University Geology Engineering Department
2009 – 2010. Post-Doc researcher, Savoie University (Chambery), Fransa
2007 – 2009 Dr.Assistant, Istanbul Technical University Faculty of Mines, Geology Engineering Department
2002 – 2007 PhD, Istanbul Technical University Faculty of Mines, Geology Engineering Department
1999 – 2001 MSc, Istanbul Technical University Faculty of Mines, Geology Engineering Department
1991 – 1995 BSc, Fırat University Geology Engineering Department
Most important 5 publications:
Eriş, K. K., Arslan, T. N., & Sabuncu, A. 2017. Influences of Climate and Tectonic on the Middle to Late Holocene Deltaic Sedimentation in Lake Hazar, Eastern Turkey. Arabian Journal for Science and Engineering, 43 (7), 3685–3697.
Eriş, K. K., Ön, S. A., Çağatay, M. N., Ülgen, U. B., Ön, Z. B., Gürocak, Z., Arslan, T.N., Bal Akkoca, D., Damcı, E., İnceöz, M., Okan, Ö.Ö.2018. Late Pleistocene to Holocene Paleoenvironmental Evolution of Lake Hazar, Eastern Anatolia, Turkey. Quaternary International, 486, 4-16.
Çağatay,M.N., Eriş, K.K., Makaroğlu, Ö., Yakuboğlu, N., Henry, P., Leroy,S., Uçarkuş, G., Sakınç, M., Yalamaz, B., Bozyiğit, C., Kende, J. The Sea of Marmara during Marine Isotope Stages 5 and 6. Quaternary Science Reviews, Quaternary Science Reviews, 220, 124-141.
Eriş, K.K., Sabuncu, A., Gasperini, L., Polonia, A., Kındap, T. 2019. Influence of climate on the late Pleistocene depositional history of the Gulf of Gemlik (Sea of Marmara). Geo-Marine Letters, 39, Issue3, 205-221.
Yakupoğlu, N., Uçarkuş, G., Eriş, K.K., Henry, P., Çağatay, M.N. Sedimentological and geochemical evidence for seismoturbidite generation in the Kumburgaz Basin, Sea of Marmara: Implications for earthquake recurrence along the Central High Segment of the North Anatolian Fault. Sedimentary Geology, 380, 31-44.
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