Eocene-Quaternary magmatic activity in the Aegean: Implications for mantle metasomatism and magma genesis in an evolving orogeny
LITHOS, vol.180, pp.5-24, 2013 (SCI-Expanded, Scopus)
- Publication Type: Article / Article
- Volume: 180
- Publication Date: 2013
- Doi Number: 10.1016/j.lithos.2013.06.007
- Journal Name: LITHOS
- Journal Indexes: Science Citation Index Expanded (SCI-EXPANDED), Scopus
- Page Numbers: pp.5-24
- Keywords: Aegean, Potassic-ultrapotassic magmatism, Crustal accretion, Continental subduction, Mantle metasomatism
- Dokuz Eylül University Affiliated: Yes
Abstract
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.