Die Entstehung der Kohlenlagerstaetten zwischen Divriği und Oltu haengt zusammen mit der beginnenden Abtragung des Taurus, in dessen nördlicher Vortiefe sie sich bildeten. Mit Hilfe von Fossilien und Pollen liess sich eine kontinuierliche Sedimentation vom obersten Oligozaen bis zum Helvet nachweisen.
Divriği ile Oltu arasındaki kömür yataklarının teşekkülü, Toroslar'ın aşınmaya başlaması ile ilgili olup, kömür yatakları Toroslar'ın kuzey önçukurunda meydana gelmişlerdir. Fosil ve polenler yardımıyla en Üst Oligosenden Helvesiene kadar devamlı bir sedimantasyonun vukua geldiği ispatlanmıştır.
Primary Language | Turkish |
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Subjects | Engineering |
Journal Section | Articles |
Authors | |
Publication Date | May 1, 1965 |
Published in Issue | Year 1965 Volume: 64 Issue: 64 |
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