Abstract
A quartz-granite conglomerate found in the Ammarnäs Complex, Västerbotten, is described. The conglomerate is considered to be intraformational and may represent an original river bed.
Geologiska Föreningen i Stockholm Förhandlingar
Volume 85, 1964 - Issue 4
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Nappe units along the Caledonian margin in central Scandinavia (Grong-Olden to Nasafjallet) : definition, distinction criteria and tectonic evolution
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