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.
Primary Language | English |
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Subjects | Engineering |
Journal Section | Articles |
Authors | |
Publication Date | December 1, 1997 |
Published in Issue | Year 1997 Volume: 119 Issue: 119 |
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