Eocene-Quaternary magmatic activity in the Aegean: Implications for mantle metasomatism and magma genesis in an evolving orogeny

ERSOY E. Y., Palmer M. R.

LITHOS, cilt.180, ss.5-24, 2013 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 180
  • Basım Tarihi: 2013
  • Doi Numarası: 10.1016/j.lithos.2013.06.007
  • Dergi Adı: LITHOS
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.5-24
  • Anahtar Kelimeler: Aegean, Potassic-ultrapotassic magmatism, Crustal accretion, Continental subduction, Mantle metasomatism, HIGH-PRESSURE METAMORPHISM, WESTERN ANATOLIA, TRACE-ELEMENT, GEODYNAMIC EVOLUTION, ISOTOPE GEOCHEMISTRY, VOLCANIC-ROCKS, NW ANATOLIA, SOURCE CONTAMINATION, EASTERN SREDNOGORIE, CENOZOIC MAGMATISM
  • Dokuz Eylül Üniversitesi Adresli: Evet

Özet

We present a compilation and comparison of geochemical data of Aegean Eocene to Recent magmatic rocks: (1) North Anatolian Eocene magmatic rocks (NAEM), (2) Aegean to west Anatolian Oligocene-Miocene magmatic rocks (AOMM), (3) Pliocene-Quaternary South Aegean volcanic arc (SAVA), (4) Pliocene-Quaternary Denizli-Isparta volcanics (DIV), and (5) Na-alkaline basalts with intra-plate geochemical affinity (IPV). These rocks are also compared with Miocene Galatean volcanics (GVP) from central Anatolia.