Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4674426 | GeoResJ | 2016 | 12 Pages |
Abstract
Finally, comparing the reconstructed local sea level history during the late Holocene with the available sea level curves produced by glacio-hydro-isostastic models, a yo-yoing land motion with a period of about 4500 years and amplitude of about 2 m can be inferred for the eastern coast of Salento peninsula.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Atmospheric Science
Authors
P. Sansò, F. Gianfreda, G. Leucci, G. Mastronuzzi,