Geochemistry and origin of ultramafic enclaves and their basanitic host rock from Kula Volcano, Turkey
LITHOS, cilt.180, ss.58-73, 2013 (SCI-Expanded, Scopus)
- Yayın Türü: Makale / Tam Makale
- Cilt numarası: 180
- Basım Tarihi: 2013
- Doi Numarası: 10.1016/j.lithos.2013.08.001
- Dergi Adı: LITHOS
- Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
- Sayfa Sayıları: ss.58-73
- Anahtar Kelimeler: Mediterranean, Continental volcanism, cumulates, Rhonite, Green-core clinopyroxene, Olivine
- Dokuz Eylül Üniversitesi Adresli: Evet
Özet
The Quaternary Kula Volcanic Province is located in western Anatolia, Turkey. This Na-alkaline anorogenic volcanism includes exposures of around 80 cinder cones, lava flows, and tuffs, representing one of the youngest volcanic activities in this region (1.9-0.026 Ma). The magmatism is related to an extensional regime and is interpreted as being derived predominantly from the asthenospheric mantle.