The Menderes Massif of western Turkey and the Cycladic Massif in the Aegean - do they really correlate?

Ring U., Gessner K., GÜNGÖR T., Passchier C.

JOURNAL OF THE GEOLOGICAL SOCIETY, cilt.156, ss.3-6, 1999 (SCI-Expanded, Scopus) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 156
  • Basım Tarihi: 1999
  • Doi Numarası: 10.1144/gsjgs.156.1.0003
  • Dergi Adı: JOURNAL OF THE GEOLOGICAL SOCIETY
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.3-6
  • Anahtar Kelimeler: Eastern Mediterranean, Menderes Massif, Cycladic Massif, tectonics, palaeogeography
  • Dokuz Eylül Üniversitesi Adresli: Evet

Özet

Based on lithostratigraphic comparisons the Menderes Massif has been correlated with the Cycladic Massif, thereby implying that the eastern Mediterranean consists of a narrow pre-Alpine basement belt which is laterally continuous over a long distance and which experienced a similar Alpine orogenic history. Our work indicates that the architecture, the age of basement and the pre-Alpine and Alpine tectonometamorphic history of both massifs differ fundamentally from each other. The Menderes Massif consists of remnants of the Cycladic Massif which overly an exotic unit, the Menderes nappes, Both massifs do not represent lateral continuations which has implications for palaeogeographic reconstructions.