Chronology of Coastal Alluvial Deposits in The Ria de Coruña (NW Spain) Linked to the Upper Pleistocene Sea Level Regression
The Ria de Coruña (NW Spain) is a wide estuary recently formed by the flooding of the Mero fluvial valley lowlands during the last postglacial transgression. During the last glacial episode, with the sea level located more than 100 m below the current one, the final section of the Mero river and lat...
| Үндсэн зохиолчид: | , , |
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| Формат: | Өгүүллэг |
| Хэл сонгох: | English |
| Хэвлэсэн: |
MDPI AG
2022-10-01
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| Цуврал: | Applied Sciences |
| Нөхцлүүд: | |
| Онлайн хандалт: | https://www.mdpi.com/2076-3417/12/19/9982 |