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Ülgen, S. et al. (2018). The Strandja Massif and the İstanbul Zone were once parts of the same palaeotectonic unit: new data from Triassic detrital zircons. Geodinamica acta. 30 (1), pp. 212-224. [Online].
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Ülgen, S. et al. (2018). The Strandja Massif and the İstanbul Zone were once parts of the same palaeotectonic unit: new data from Triassic detrital zircons. Geodinamica acta. 30 (1), pp. 212-224. [Online].