Lower Miocene shallow water carbonates from soiuthern Apenniens (S Italy) are analysed in terms of rhodolith contents. Several rhodolith assemblges characterised a channelised area which was described according to the coralline algal associations. Paleoeoclogical analysis of these coralline algal assemblages was performed
Lower Oligocene, shallow-water carbonates of the Calcareniti di Castelgomberto Formation (Monti Beri...
There are few detailed studies on the evolution from the Oligocene to Miocene carbonate facies. This...
Shallow water carbonate rhodolith deposits constitute thick channelized sedimentary sequences in Ear...
Palaeoecological analysis of rhodolith successions in shallow water platform carbonates from the Sou...
Lower–Middle Miocene temperate marine carbonates occur in the Matese Mountains, Southern Apennines (...
Paleoecology of rhodolith accumulations in LOwer Miocene shallow water carbonates successions of Sou...
Paleoecological and paleoenvironmental analysis of rhodlith successions is presented. The studied su...
An integrated analysis of rhodolith assemblages and associated fossil traces (borings) found in hemi...
Lower Miocene carbonate sediments, known as “Calcari a Briozoi e Lithothamni ” (Bryozoan
The knowledge of re-sedimented rhodolith deposits has always lagged behind that of in situ deposits ...
Coralline red algae are common in Oligocene and Miocene marine shallow-water carbonate and silicicla...
During the Pliocene and Pleistocene, the Monte Cetona (Northern Apennines, central Italy) was part o...
During Aquitanian-Burdigalian times, temperate-type carbonate-siliciclastic successions were deposit...
During Aquitanian-Burdigalian times, temperate-type carbonate-siliciclastic successions were deposit...
During Aquitanian-Burdigalian times, temperate-type carbonate-siliciclastic successions were deposit...
Lower Oligocene, shallow-water carbonates of the Calcareniti di Castelgomberto Formation (Monti Beri...
There are few detailed studies on the evolution from the Oligocene to Miocene carbonate facies. This...
Shallow water carbonate rhodolith deposits constitute thick channelized sedimentary sequences in Ear...
Palaeoecological analysis of rhodolith successions in shallow water platform carbonates from the Sou...
Lower–Middle Miocene temperate marine carbonates occur in the Matese Mountains, Southern Apennines (...
Paleoecology of rhodolith accumulations in LOwer Miocene shallow water carbonates successions of Sou...
Paleoecological and paleoenvironmental analysis of rhodlith successions is presented. The studied su...
An integrated analysis of rhodolith assemblages and associated fossil traces (borings) found in hemi...
Lower Miocene carbonate sediments, known as “Calcari a Briozoi e Lithothamni ” (Bryozoan
The knowledge of re-sedimented rhodolith deposits has always lagged behind that of in situ deposits ...
Coralline red algae are common in Oligocene and Miocene marine shallow-water carbonate and silicicla...
During the Pliocene and Pleistocene, the Monte Cetona (Northern Apennines, central Italy) was part o...
During Aquitanian-Burdigalian times, temperate-type carbonate-siliciclastic successions were deposit...
During Aquitanian-Burdigalian times, temperate-type carbonate-siliciclastic successions were deposit...
During Aquitanian-Burdigalian times, temperate-type carbonate-siliciclastic successions were deposit...
Lower Oligocene, shallow-water carbonates of the Calcareniti di Castelgomberto Formation (Monti Beri...
There are few detailed studies on the evolution from the Oligocene to Miocene carbonate facies. This...
Shallow water carbonate rhodolith deposits constitute thick channelized sedimentary sequences in Ear...