Mineral Chemistry and Petrochemistry of Post-Collisional Tertiary Mafic to Felsic Cogenetic Volcanics in the Ulubey (Ordu) Area, Eastern Pontides, NE Turkey

TEMİZEL İ., ARSLAN M.

TURKISH JOURNAL OF EARTH SCIENCES, cilt.18, sa.1, ss.29-53, 2009 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 18 Sayı: 1
  • Basım Tarihi: 2009
  • Dergi Adı: TURKISH JOURNAL OF EARTH SCIENCES
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus, TR DİZİN (ULAKBİM)
  • Sayfa Sayıları: ss.29-53
  • Anahtar Kelimeler: calc-alkaline volcanics, crystal fractionation, mineral chemistry, Tertiary volcanism, eastern Pontides, Turkey, GEOCHEMICAL TRENDS, CONTINENTAL-CRUST, ISOTOPIC EVIDENCE, PULUR COMPLEX, ARC, EVOLUTION, MANTLE, ROCKS, SUBDUCTION, PETROGENESIS
  • Karadeniz Teknik Üniversitesi Adresli: Evet

Özet

Post-collisional Tertiary volcanic rocks in the Ulubey (Ordu) area at the western edge of the eastern Pontides palaeo-arc are divided into four suites. The Yenisayaca basalt (TB) contains plagioclase (An(61-83)), clinopyroxene (Wo(42-44) En(39-41) Fs(15-18)) and olivine phenocrysts and titanomagnetite microphenocrysts, whereas the Catal Tepe and Elekcioglu Tepe suite (CES), Islk Tepe suite (ITS) and andesite/trachyandesite suite (ATS) rocks include plagioclase (An(23-78)), clinopyroxene (Wo(27-48) En(37-55) Fs(11-26)), hornblende (Mg#=0.63-0.76), biotite (Mg#=0.63-0.82), sanidine phenocrysts and titanomagnetite and apatite microphenocrysts.