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Petrogenesis of strongly peraluminous plutonic rocks of the Eastern Sakarya Zone (Trabzon, Turkey): implications for crustal melting and evolution

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Abstract

The Eastern Sakarya Zone in northeastern Turkey contributes for a natural laboratory to study subduction- to collision-related intrusive rocks. This paper presents data on a Carboniferous-aged Duzkoy pluton containing mainly peraluminous granitoids. In addition to plagioclase, K-feldspar and quartz, the rocks include biotite, zircon, apatite and opaque minerals. Sericitization, chloritization, epidotization, and carbonatization are  the main alteration types. The rocks display generally enrichment in large-ion lithophile elements (Rb, Th, U, K), and depletion in high field strength elements (Sr, Nb, Ta, P) in the primitive mantle-normalized trace element diagrams. The Duzkoy samples show mainly light rare earth elements-enriched patterns with marked negative Eu anomalies in the chondrite-normalized rare earth elements diagrams. The compositions of the Duzkoy plutonic rocks are consistent with their origin via partial melting of amphibolites or metagreywackes. Crystal fractionation is also likely an important process in the formation of these rocks. The origin of these rocks could be related to the delamination or slab breakoff processes during the Variscan orogeny.

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Acknowledgements

The present study is a part of the MSc thesis of author S.R. The XRF and ICP-MS analyses of the studied samples were undertaken at the Bureau Veritas (Canada) Inc. The authors would like to express their appreciation to two anonymous reviewers and handling Editor Leonid Dansuyhevsky for their constructive revisions that improved the manuscript. S.R. acknowledges financial support from the Akdeniz University Scientific Research Projects Coordination Unit (project FYL-2017-2559).

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Rasimgil, S., Ilbeyli, N., Gunes, A. et al. Petrogenesis of strongly peraluminous plutonic rocks of the Eastern Sakarya Zone (Trabzon, Turkey): implications for crustal melting and evolution. Miner Petrol 117, 79–97 (2023). https://doi.org/10.1007/s00710-022-00800-3

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