Example for major and trace element enrichment in marine source rock from Turkey: Akkuyu formation (Middle Taurus) Deni•zel kaynak kayalarda ana ve i•z element zengi• nlesmeleri•ne türki•ye'den bi•r örnek: Akkuyu formasyonu (Orta Toroslar)

Koca D., SARI A., Koç S., YAVUZ PEHLİVANLI B., Koralay D. B.

Journal of the Faculty of Engineering and Architecture of Gazi University, cilt.25, sa.2, ss.243-256, 2010 (SCI-Expanded) identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 25 Sayı: 2
  • Basım Tarihi: 2010
  • Dergi Adı: Journal of the Faculty of Engineering and Architecture of Gazi University
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus, TR DİZİN (ULAKBİM)
  • Sayfa Sayıları: ss.243-256
  • Anahtar Kelimeler: Akkuyu formation, Anoxic environment, Element enrichment, Middle Taurus
  • Yozgat Bozok Üniversitesi Adresli: Evet

Özet

Akkuyu Formation which occurs at Antalya region in Middle Taurus has carbonate lithology and 1.92 wt% average of Corg. The values of Corg are 6.4 times more elevated than the source rock average value accepted for carbonates (0.3 wt%). 9 major elements and 38 traces elements are investigated on the carbonate samples of Akkuyu Formation which are rich in organic matter. Determined major and trace elements are compared with average of carbonates and shales, also with Peru Margin sediments, Namibian Margin (Africa) sediments, Cenomanian/Turonian Demerara Rise sediments, Cenomanian/Turonian Gubbio sediments, and Mediterranean and Black Sea sapropels which is accumulated under anoxic conditions. The considerable element enrichment in Akkuyu Formation are in Rb, U, Ba, Cu, Ni, Cr, As, V, Zn, Sb, Co, Mo, Cd. Element intervals of major elements, Na, Ti, K, P, Si, Fe and Mg, of Akkuyu Formation which change between 0.003 and 1.70, are lower than that of upwelling sediments, sapropels, Cenomanian/Turonian (C/T) black shale samples.