Abstract
The paleovolcanic complex of the Albere area occurs entirely within the Canaveilles series (Cambrian) and apparently has been overturned. Observations on exposures of the complex along the route between Mas Claret and the Branca col made during the eastern Pyrenees field trip of the Societe Geologique de France are reported.
This content is PDF only. Please click on the PDF icon to access.
You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
