Add to ORKGWe present the revised stratigraphic setting of the late Quaternary deposits cropping out along the western coast of Sar-dinia (Italy). The height defined units have been dated using luminescence. © 2010 AIQUA - Associazione Italiana per lo Studio del Quaternario e EMMEVI - Servizio Congressi SPA
Two major synthems have been recognised along the coasts of Sardinia. The older one is composed of ...
The study area is located in NW Sardinia Island (Italy), Mediterranean Sea. Sardinia is considered s...
Although occupying a critical position at the center of the Mediterranean Sea, the Island of Sardini...
We present the revised stratigraphic setting of the late Quaternary deposits cropping out along the ...
Geochronological framework of Middle-Late Holocene coastal succession are usually based on radiocarb...
The Middle Pleistocene–Holocene Sardinian stratigraphy has been revised to identify the roles played...
Recent stratigraphic surveys and facies analyses have questioned long-held interpretations of the de...
The relict beach deposit of the Cala Mosca marine terrace is considered an important section of Mari...
The Upper Pleistocene succession of coastal deposits outcropping at San Giovanni di Sinis (west Sard...
The shallow-marine to coastal deposits of Alghero have been dated using the Optically Stimulated Lum...
For its relative stability during Quaternary (from the isotopic stage 5 about 125,000 years ago) and...
Capo S. Marco is the southernmost termination of the Sinis Peninsula in the northwestern border of t...
© 2020 John Wiley & Sons Ltd Precise dating of the activity of Late Pleistocene to Holocene neo-te...
A multi-disciplinary approach was performed to investigate two compound geosols included between win...
Two major synthems have been recognised along the coasts of Sardinia. The older one is composed of ...
The study area is located in NW Sardinia Island (Italy), Mediterranean Sea. Sardinia is considered s...
Although occupying a critical position at the center of the Mediterranean Sea, the Island of Sardini...
We present the revised stratigraphic setting of the late Quaternary deposits cropping out along the ...
Geochronological framework of Middle-Late Holocene coastal succession are usually based on radiocarb...
The Middle Pleistocene–Holocene Sardinian stratigraphy has been revised to identify the roles played...
Recent stratigraphic surveys and facies analyses have questioned long-held interpretations of the de...
The relict beach deposit of the Cala Mosca marine terrace is considered an important section of Mari...
The Upper Pleistocene succession of coastal deposits outcropping at San Giovanni di Sinis (west Sard...
The shallow-marine to coastal deposits of Alghero have been dated using the Optically Stimulated Lum...
For its relative stability during Quaternary (from the isotopic stage 5 about 125,000 years ago) and...
Capo S. Marco is the southernmost termination of the Sinis Peninsula in the northwestern border of t...
© 2020 John Wiley & Sons Ltd Precise dating of the activity of Late Pleistocene to Holocene neo-te...
A multi-disciplinary approach was performed to investigate two compound geosols included between win...
Two major synthems have been recognised along the coasts of Sardinia. The older one is composed of ...
The study area is located in NW Sardinia Island (Italy), Mediterranean Sea. Sardinia is considered s...
Although occupying a critical position at the center of the Mediterranean Sea, the Island of Sardini...