Ice-free intervals continuing into Marine Isotope Stage 3 at Sokli in the central area of the Fennoscandian glaciations

An unusually long and continuous Late Quaternary sedimentary sequence has been preserved in a sedimentary basin formed in the Sokli Carbonatite Massif in eastern-central Finnish Lapland. A nearly complete sediment recovery from the central Sokli basin combined with palynological results from sedimen...

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Bibliographic Details
Published in:Bulletin of the Geological Society of Finland
Main Authors: K.F. Helmens, P.W. Johansson, M.E. Räsänen, H. Alexanderson, K.O. Eskola
Format: Article in Journal/Newspaper
Language:English
Published: Geological Society of Finland 2007
Subjects:
Online Access:https://doi.org/10.17741/bgsf/79.1.002
https://doaj.org/article/f404f36c92b941819fda0506fddf2439