『Abstract
The absence of Ce anomaly and significant positive correlation
between Ce and Fe in the weathering profiles and sedimentary carbonate
rocks of the Baltic Shield with an age of 2.8-2.1 Ga indicate
that Fe3+ was the main form of Fe migration in the
Archean-Paleoproterozoic exogenous environments in the Baltic
Shield. The Ce distribution was mainly controlled by hydrogen
index rather than redox conditions.』
Introduction
Materials and methods
The REE distribution in the Ar-Pr exogenous objects of the Baltic
Shield
Weathering profile
Sedimentary carbonates
Mobility of cerium and iron in the early Precambrian supergene
zone of the Baltic Shield
Conclusions
Acknowledgments
References