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Geochemical
and textural variations in frontal dune sediments along the western coast of
Jutland, Denmark, were investigated in order to identify possible sediment
'provinces' and transport pathways. Four coastal sectors were identified on the
basis of geochemical composition. One sector is compositionally different from
the other three units, having higher concentrations of the trace elements Ni,
Cr, V, Sc, Zn, Pb, Ba, Zr and many rare earth elements. Dune sediments on this
section of coast also have higher Al2O3 to K2O
ratios and lower Al2O3 to Fe2O3
ratios, reflecting a lower content of feldspar and higher content of heavy
minerals. It is inferred that different, or additional, sediment source(s) have
supplied sediment to this section of coast. Alongshore trends were also
identified in the mean particle size and sorting of the frontal dunes, three
coastal units being identified, although there is no direct correspondence with
the observed geochemical differences. Frontal dune sediments in the middle
section are relatively coarser and less well-sorted than those to the north and
south, probably reflecting both the addition of beach nourishment material and
greater exposure to strong westerly winds, which are a capable of transporting a
wide range of particle sizes.
Publications Saye, S.E., Pye,
K. and Clemmensen, L.B. (2006) Development of a cliff-top dune indicated by particle size and
geochemical characteristics: Rubjerg Knude, Denmark. Sedimentology 53,
1-21. Saye, S.E. and Pye,
K.
(2006) Variations in chemical composition and particle size of dune
sediments along the west coast of Jutland, Denmark. Sedimentary Geology
183, 217-242. |
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