Crystallization conditions and petrography of eocene volcanic rocks in the Gumusdamla-Erikdibi area (Bayburt, NE Turkey)

  • Abdullah Kaygusuz Gumushane University
  • Damla Selvi Gumushane University
Keywords: Mineralogy-petrography, clinopyroxene, geothermobarometer, eocene volcanics, Bayburt, Eastern Pontides

Abstract

The Eocene Gumusdamla-Erikdibi (Bayburt) volcanics in the south zone of the Eastern Pontides were studied as mineral chemistry and petrography. The main units in the study area are Late Cretaceous Ardic Volcanites, Eocene Sirataslar Formation, Eocene Yazyurdu Formation and Eocene Tasliburun Diorite that cuts these units. The youngest unit in the field is Quaternary alluviums. The studied volcanic rocks are basalt, basaltic andesite and andesite in composition and the main minerals are plagioclase, alkali-feldspar, pyroxene, hornblende, biotite and opaque minerals. Pyroxenes are clino-pyroxene in composition (Wo40-48En39-46Fs9-19) and differ from diopside to augite. Crystallization temperatures calculated from clinopyroxene minerals are 819 °C to 1157 °C, and pressure values are 0.14 to 7.79 kbar. Based on the obtained data, it is suggested that the magmas had undergone anhydrous and hydrous crystallizations in the shallow to mid-crustal magma chambers

Author Biographies

Abdullah Kaygusuz, Gumushane University

Department of Geology

Damla Selvi, Gumushane University

Department of Geology

References

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Published
2020-12-31
How to Cite
Kaygusuz, A., & Selvi, D. (2020). Crystallization conditions and petrography of eocene volcanic rocks in the Gumusdamla-Erikdibi area (Bayburt, NE Turkey). Journal of Engineering Research and Applied Science, 9(2), 1529-1537. Retrieved from http://www.journaleras.com/index.php/jeras/article/view/217
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