Biga Yarımadası'nda Asimetrik Havza Gelişimi ve Yapı İlişkisine Bir Örnek: Yapıldak Dere Havzası
In the east of the Strait of Çanakkale, the dominant direction of which is SW-NE with some lineation-caused bends, river basins have developed on various of lithological features giving rise to selective erosion. In these basins, lithological diversity became effective on basin forms and dreinage de...
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Format: | Article |
Language: | English |
Published: |
Çanakkale Onsekiz Mart University
2008-04-01
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Series: | Çanakkale Araştırmaları Türk Yıllığı |
Online Access: | http://canakkalearastirmalari.comu.edu.tr/images/form/dosya/dosya_533805.pdf |