Andrei Panin
Biographic Data
| ID | 7516730 |
|---|---|
| NAME | Andrei Panin |
| GIVEN NAMES | Andrei |
| FAMILY NAME | Panin |
| SIGNATURE | PANIN A |
| VERIFIED | No |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 1 |
| AUTHOR COUNT | 3 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2015 |
| LATEST PUBLICATION YEAR | 2025 |
| H-INDEX | 1 |
Radiocarbon dating of the end of the latest Caspian Sea overflow through the Manych Depression (southeastern European Plain)
The Manych Depression is a relatively narrow elongated depression of tectonic origin, connecting the Caspian and Azov-Black Sea basins. The Caspian Sea repeatedly discharged its waters through this depression into the Black Sea and further into the Mediterranean Sea during the Quaternary period. The last discharge occurred in MIS 2 when the Khvalynian transgression waters exceeded the drainage divide between those two basins. The geochronology of…
Pleistocene stratigraphy of the Vychegda River basin, European North-East
Climatic fluctuations reflected in the evolution of fluvial systems of Central-Eastern Europe (60–8 ka cal BP)
Radiocarbon dating of the end of the latest Caspian Sea overflow through the Manych Depression (southeastern European Plain)
The Manych Depression is a relatively narrow elongated depression of tectonic origin, connecting the Caspian and Azov-Black Sea basins. The Caspian Sea repeatedly discharged its waters through this depression into the Black Sea and further into the Mediterranean Sea during the Quaternary period. The last discharge occurred in MIS 2 when the Khvalynian transgression waters exceeded the drainage divide between those two basins. The geochronology of…
Climatic fluctuations reflected in the evolution of fluvial systems of Central-Eastern Europe (60–8 ka cal BP)
Pleistocene stratigraphy of the Vychegda River basin, European North-East
Radiocarbon dating of the end of the latest Caspian Sea overflow through the Manych Depression (southeastern European Plain)
The Manych Depression is a relatively narrow elongated depression of tectonic origin, connecting the Caspian and Azov-Black Sea basins. The Caspian Sea repeatedly discharged its waters through this depression into the Black Sea and further into the Mediterranean Sea during the Quaternary period. The last discharge occurred in MIS 2 when the Khvalynian transgression waters exceeded the drainage divide between those two basins. The geochronology of…
Geology (3 works) · Paleontology (3 works) · Archaeology and ancient environmental studies (2 works) · Geography (2 works) · Geology and Paleoclimatology Research (2 works) · Geomorphology (2 works) · Glacial period (2 works) · Marine and environmental studies (2 works) · Oceanography (2 works) · Physical geography (2 works)