We present here the results of detailed mapping, lithofacies analysis and stratigraphy of the Neogene James Ross Island Volcanic Group (Antarctic Peninsula) in the Cerro Santa Marta area (northwest of James Ross Island), in order to give constraints on the evolution of a glaciated volcanic island. Our field results included recognition and interpretation of seventeen volcanic and glacial lithofacies, together with their vertical and lateral arrangements,supported by four new unspiked K?Ar ages. This allowed us to conclude that the construction of the volcanic pile in this area took place during two main eruptive stages (Eruptive Stages 1 and 2), separated from the Cretaceous bedrock and from each other by two major glacial unconformities (U...
The Neogene geological record in the James Ross Island region (northern Antarctic Peninsula) is domi...
Basaltic volcanism in the James Ross Island region has been persistent over the last 6 million years...
Knowledge of the thickness, extent and basal thermal conditions of ice cover on Antarctica during pa...
The northern Antarctic Peninsula region has undergone ~10 m.y. of eruptive activity by basaltic volc...
The northern Antarctic Peninsula region has undergone ~10 m.y. of eruptive activity by basaltic volc...
The northern Antarctic Peninsula region has undergone similar to 10 m.y. of eruptive activity by bas...
Summary The Neogene geological record in the James Ross Island region (northern Antarctic Peninsula)...
Considerable controversy exists concerning the stability of the Antarctic Ice Sheet during the Neoge...
International audienceBasaltic volcanism in the James Ross Island region has been persistent over th...
International audienceBasaltic volcanism in the James Ross Island region has been persistent over th...
International audienceBasaltic volcanism in the James Ross Island region has been persistent over th...
International audienceBasaltic volcanism in the James Ross Island region has been persistent over th...
International audienceBasaltic volcanism in the James Ross Island region has been persistent over th...
Basaltic volcanism in the James Ross Island region has been persistent over the last 6 million years...
Basaltic volcanism in the James Ross Island region has been persistent over the last 6 million years...
The Neogene geological record in the James Ross Island region (northern Antarctic Peninsula) is domi...
Basaltic volcanism in the James Ross Island region has been persistent over the last 6 million years...
Knowledge of the thickness, extent and basal thermal conditions of ice cover on Antarctica during pa...
The northern Antarctic Peninsula region has undergone ~10 m.y. of eruptive activity by basaltic volc...
The northern Antarctic Peninsula region has undergone ~10 m.y. of eruptive activity by basaltic volc...
The northern Antarctic Peninsula region has undergone similar to 10 m.y. of eruptive activity by bas...
Summary The Neogene geological record in the James Ross Island region (northern Antarctic Peninsula)...
Considerable controversy exists concerning the stability of the Antarctic Ice Sheet during the Neoge...
International audienceBasaltic volcanism in the James Ross Island region has been persistent over th...
International audienceBasaltic volcanism in the James Ross Island region has been persistent over th...
International audienceBasaltic volcanism in the James Ross Island region has been persistent over th...
International audienceBasaltic volcanism in the James Ross Island region has been persistent over th...
International audienceBasaltic volcanism in the James Ross Island region has been persistent over th...
Basaltic volcanism in the James Ross Island region has been persistent over the last 6 million years...
Basaltic volcanism in the James Ross Island region has been persistent over the last 6 million years...
The Neogene geological record in the James Ross Island region (northern Antarctic Peninsula) is domi...
Basaltic volcanism in the James Ross Island region has been persistent over the last 6 million years...
Knowledge of the thickness, extent and basal thermal conditions of ice cover on Antarctica during pa...