Abstract
Abstract The Precambrian supracrustal rocks of Finland were produced during four main evolutionary stages: (1) late Archaean (Pre-Svecokarelidic) greenstone-schist evolution on an unknown basement; (2) at least four cycles of early Proterozoic (Karelian) continental-epi/pericontinental sedimentation and volcanism on or next to the cratonized late Archaean basement; (3) early Proterozoic (Svecofennian) eugeosynclinal evolution west of, or in part, on the late Archaean basement and its cratonic cover; and (4) middle to late Proterozoic (Jotnia) continental sedimentation on the stabilized early Proterozoic (Post Svecokarelidic) basement.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Paper version not known
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
