Open AccessSand analysis as a method of estimating bedrock compositions in Greenland. Illustrated by fluvial sands from the Fiskenæsset region
Author(s) -
Feiko Kalsbeek,
M Ghisler,
Bent Thomsen
Publication year - 1974
Publication title -
bulletin
Language(s) - English
Resource type - Journals
eISSN - 2597-2936
pISSN - 0105-3507
DOI - 10.34194/bullggu.v111.6652
Subject(s) - geology , bedrock , geochemistry , sedimentary rock , chemical composition , metamorphic rock , fluvial , gneiss , biotite , mineralogy , pyroxene , grain size , parent rock , geomorphology , weathering , olivine , paleontology , chemistry , structural basin , quartz , organic chemistry
Mineralogical and chemical composition, heavy and opaque mineral content and grain size distribution of the sands show that they mainly consist of locally derived material. Glacially transported material has little influence on the composition of the sands. By comparing sands of various grain sizes, it is shown that the sedimentary processes do not appreciably change the composition of the sands, except that biotite is largely winnowed out. Thus, the sands are suitable for a regional study of the composition of the country rocks and for prospecting. Estimates are made of the average mineralogical and chemical composition of the area and the abundance of the different rock types. The amount of hypersthene gives an impression of the metamorphic grade of the rocks, and the average chemical composition of the high-grade rocks in the northern part of the area is the same as that of the lower grade rocks in the southern part.