Abstract
Almost the whole of the western edge of the landmass of Scandinavia is occupied by a 1700-km belt of deformed and sometimes metamorphosed rocks on which in the west lie a few isolated masses of relatively undeformed and completely unmetamorphosed Old Red Sandstone....
Cite
CITATION STYLE
APA
Nicholson, R. (1974). The Scandinavian Caledonides. In The Ocean Basins and Margins (pp. 161–203). Springer US. https://doi.org/10.1007/978-1-4684-3033-2_6
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