Pre-Holocene joint fillings at Forsmark, Uppland, Sweden

Abstract
Subhorizontal joints filled with sediments were found at Forsmark in north-eastern Uppland, Sweden. The sediments are glacial in character and show varves, graded and current bedding, and clay laminae. The occurrence, structure and pollen frequency of the sediments imply a deposition during a Pre-Holocene age, possibly during Early or Middle Weichsel.

This publication has 0 references indexed in Scilit: