Add to ORKGThe new Sheet “557” Cagliari (CARG Project) produced a map of the Quaternary Syntems, however the results of the new radiometric datings were not exhaustive and sometimes contradictory. The groups working on continental and marine areas reached different conclusions on the chronology of the deposits: some coastal deposits have been included in the subsynthem of Cala Mosca (Tyrrhenian) although we should refer them to the Holocene. However, the distribution of the Tyrrhenian deposits was reduced and the Is Arenas beach ridge grouped within the Holocene. We report the elements supporting a Holocene age for the coastal deposits
The timing of the colonization of Sardinia by mammalian fauna and anatomically modern humans (AMH) i...
Multiproxy analysis composed of biostratigraphy and pollen analysis allowed reconstructing the palae...
) We report the evolutionary model of the coastal plain of Cagliari and the continental relatively l...
The new Sheet “557” Cagliari (CARG Project) produced a map of the Quaternary Syntems, however the r...
The Middle Pleistocene–Holocene Sardinian stratigraphy has been revised to identify the roles played...
In this research, we studied the marine flood risk of the Cagliari plain in relation to the depresse...
For its relative stability during Quaternary (from the isotopic stage 5 about 125,000 years ago) and...
Two major synthems have been recognised along the coasts of Sardinia. The older one is composed of ...
The shallow-marine to coastal deposits of Alghero have been dated using the Optically Stimulated Lum...
Capo S. Marco is the southernmost termination of the Sinis Peninsula in the northwestern border of t...
In 2005, the National Geological Survey of Italy released the new sheet, 557 Cagliari (1:50.000 scal...
The Upper Pleistocene succession of coastal deposits outcropping at San Giovanni di Sinis (west Sard...
We provide new data on relative sea-level change from the late Holocene for two locations in the cen...
We provide new data on relative sea-level change from the late Holocene for two locations in the cen...
The timing of the colonization of Sardinia by mammalian fauna and anatomically modern humans (AMH) i...
Multiproxy analysis composed of biostratigraphy and pollen analysis allowed reconstructing the palae...
) We report the evolutionary model of the coastal plain of Cagliari and the continental relatively l...
The new Sheet “557” Cagliari (CARG Project) produced a map of the Quaternary Syntems, however the r...
The Middle Pleistocene–Holocene Sardinian stratigraphy has been revised to identify the roles played...
In this research, we studied the marine flood risk of the Cagliari plain in relation to the depresse...
For its relative stability during Quaternary (from the isotopic stage 5 about 125,000 years ago) and...
Two major synthems have been recognised along the coasts of Sardinia. The older one is composed of ...
The shallow-marine to coastal deposits of Alghero have been dated using the Optically Stimulated Lum...
Capo S. Marco is the southernmost termination of the Sinis Peninsula in the northwestern border of t...
In 2005, the National Geological Survey of Italy released the new sheet, 557 Cagliari (1:50.000 scal...
The Upper Pleistocene succession of coastal deposits outcropping at San Giovanni di Sinis (west Sard...
We provide new data on relative sea-level change from the late Holocene for two locations in the cen...
We provide new data on relative sea-level change from the late Holocene for two locations in the cen...
The timing of the colonization of Sardinia by mammalian fauna and anatomically modern humans (AMH) i...
Multiproxy analysis composed of biostratigraphy and pollen analysis allowed reconstructing the palae...
) We report the evolutionary model of the coastal plain of Cagliari and the continental relatively l...