Nature, provenance and relationships of early miocene palaeovalley fills, northern Adana Basin, Turkey: Their significance for sediment-bypassing on a carbonate shelf
Atıf İçin Kopyala
DERMAN A. S., Gurbuz K.
TURKISH JOURNAL OF EARTH SCIENCES, cilt.16, sa.2, ss.179-209, 2007 (SCI-Expanded)
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Yayın Türü:
Makale / Tam Makale
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Cilt numarası:
16
Sayı:
2
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Basım Tarihi:
2007
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Dergi Adı:
TURKISH JOURNAL OF EARTH SCIENCES
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Derginin Tarandığı İndeksler:
Science Citation Index Expanded (SCI-EXPANDED), Scopus, TR DİZİN (ULAKBİM)
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Sayfa Sayıları:
ss.179-209
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Çukurova Üniversitesi Adresli:
Evet
Özet
The Gildirli Formation is the oldest Neogene rock unit in the Adana Basin and was formed prior to the regionally extensive Early Miocene marine transgression. These coarse clastic red-beds provide important evidence about the causes and early phases of filling in this large trough, because the Gildirli Formation sediments fill an irregular palaeotopography carved out of Palaeozoic and Mesozoic basement rocks.