In this study the ostracoda fauna of the Upper Miocene-Pliocene sedimentary units have been considered
aspects. According to ostracoda fauna-the Neogene sequence of the region has been deposited in different environments
ranging gradually from shallow marine through littoral and Lagoon to lacustrine within short intervals resulting
from continuous lowering of the sea-level.
Birincil Dil | İngilizce |
---|---|
Konular | Mühendislik |
Bölüm | Makaleler |
Yazarlar | |
Yayımlanma Tarihi | 1 Aralık 1997 |
Yayımlandığı Sayı | Yıl 1997 Cilt: 119 Sayı: 119 |
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