Deux soubassements paleozoiques differents et non correlables stratigraphiquement sont
juxtaposes dans la coupole de Karacahisar. Le double accident tectonique qui les separe actuellement s'amortit
lateralement dans la couverture mesozoique commune qui les recouvre. Le rapprochement tectonique de ces
deux series paleozoiques differentes serait du au jeu d'un accident anterieur ä la transgression mesozoique.
Karacahisar kubbesi içinde, aralarında stratigrafik ilişki bulunmayan ve birbirinden farklı iki
Paleozoyik taban yan yana bulunmaktadır. Bunları ayırmakta olan çift tektonik hat, her iki Paleozoyik tabanın ortak
örtüsünü oluşturan Mesozoyik içinde yanal olarak sönmektedir. Bu farklı iki serinin tektonik yolla yan yana gelişi
Mesozoyik transgresyonundan önceki bir olaya bağlıdır.
Primary Language | Turkish |
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Subjects | Engineering |
Journal Section | Articles |
Authors | |
Publication Date | July 1, 1978 |
Published in Issue | Year 1978 Volume: 90 Issue: 90 |
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