PROVENANCE OF MIOCENE SUBMARINE FANS IN THE NORTHERN ADANA BASIN, SOUTHERN TURKEY - A TEST OF DISCRIMINANT FUNCTION-ANALYSIS

GURBUZ K., KELLING G.

GEOLOGICAL JOURNAL, cilt.28, ss.277-293, 1993 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 28
  • Basım Tarihi: 1993
  • Doi Numarası: 10.1002/gj.3350280307
  • Dergi Adı: GEOLOGICAL JOURNAL
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.277-293
  • Çukurova Üniversitesi Adresli: Hayır

Özet

The provenance of the deep marine clastics of the Cingoz Formation, which were deposited contemporaneously during the Miocene as two small neighbouring submarine fans (western and eastern fans) in the northern part pf Basin, has been studied by: (1) thin section petrography; (2) the use of the ternary discriminant diagrams (Q-F-L, Qm-F-ss) of Dickinson et al. (1983); and (3) the use of discriminant function analysis (DFA) techniques.