Geomorphological and archaeological indicators of sea level change over the last 2 000 years on the Croatian shoreline between Poreč and Split (CROSBI ID 33415)
Prilog u knjizi | izvorni znanstveni rad
Podaci o odgovornosti
Faivre, Sanja
engleski
Geomorphological and archaeological indicators of sea level change over the last 2 000 years on the Croatian shoreline between Poreč and Split
The northern Adriatic, particularly the Kvarner and Istria area, undoubtedly had a phase of stabilisation in the 1st and 2nd centuries AD and later a sea level rise probably of the eustatic origin. The importance of that rise over the last 2000 years, confirmed also in the other western Mediterranean regions, is about 50 cm. The regional tectonic subsidence could be the reason for the absence of a fossil and even recent tidal notch in the north Dalmatian area between Zadar and Split.
sea-level, tidal notch, Croatia
nije evidentirano
nije evidentirano
nije evidentirano
nije evidentirano
nije evidentirano
nije evidentirano
Podaci o prilogu
69-72.
objavljeno
Podaci o knjizi
Adria 2006, Field trip Guide Book
Menichetti, Marco ; Mencucci, Daniela
Urbino: Istituto scienze della Terra ; University of Urbino
2006.
0-000-00000-0000