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A GRADUAL DROWNING OF THE SOUTHWESTERN BLACK SEA SHELF: EVIDENCE FOR A PROGRESSIVE RATHER THAN ABRUPT HOLOCENE RECONNECTION WITH THE EASTERN MEDITERRANEAN SEA THROUGH THE MARMARA SEA GATEWAY (2007)
The major conclusion that is drawn from the study of core samples is that the SW Black Sea shelf wastransgressed by no later than 10 ka, and that the outer and middle shelf of Black Sea has been under water ever since.
Reference:
Quaternary International 167-168 (2007) 19-34
Quaternary International 167-168 (2007) 19-34
Organization:
Department of Earth Sciences, Memorial University of Newfoundland, St. John's, NF, Canada A1B 3X5
Turkey
Department of Earth Sciences, Memorial University of Newfoundland, St. John's, NF, Canada A1B 3X5
Turkey
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