Young sediments in the shelf
areas in the sea of Marmara have some faunal signs of Mediterranean
transgression, Flandrian, developed following the Vürm period. The evolution of
locally tectonic-controlled foraminifera paleobiofacies formed as a result of
this transgression 7.5-3.5 thousand years before present in the triple junction
between entrance of Bosphorus in Northern Marmara Shelf-Mouth of Golden
Horn-Üsküdar indicates that Mediterranean-Black Sea connection in late
Quaternary was accomplished over Bosphorus as a result of
tectonic-transgression association.
Primary Language | English |
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Subjects | Engineering |
Journal Section | Articles |
Authors | |
Publication Date | January 1, 1998 |
Published in Issue | Year 1998 Volume: 120 Issue: 120 |
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