Geochemistry and origin of ultramafic enclaves and their basanitic host rock from Kula Volcano, Turkey

Gruetzner T., Prelevic D., AKAL C.

LITHOS, cilt.180, ss.58-73, 2013 (SCI-Expanded) identifier identifier

  • 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, WESTERN TURKEY, LOW-PRESSURE, MANTLE XENOLITHS, TRACE-ELEMENTS, ORTHO-PYROXENE, SILICATE MELT, ANATOLIA, ALKALINE, PROVINCE, EQUILIBRIA
  • 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.