科研之友
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摘要
The present article is a part of the implementation of the task for standardization of distinct types of the Upper Pleistocene - Holocene sediments in the Black Sea Basin. Detailed sedimentological analysis for the upper part of the core was carried out as the regressive-transgressive events were determined. It is proved that the lowest aragonite layer at the onset of the Black sea sapropel deposition is a result of redeposition of aragonate of chemical origin during the last regression.
- 出版日期2014
