BENTHIC FORAMINIFERA (HOLOCENE) PALEOBIOFACIES OF BOSPHORUS (GOLDEN HORN - SARAYBURNU - ÜSKÜDAR): A NEW APPROACH TO MEDITERRANEAN-BLACK SEA WATERWAY
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 bef...
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| Format: | Article |
| Language: | English |
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General Directorate of Mineral Research and Exploration
1998-01-01
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| Series: | Bulletin of the Mineral Research and Exploration |
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| Online Access: | http://dergipark.gov.tr/bulletinofmre/issue/3939/444704?publisher=mta |