Micromorphological changes as an indicator of the transition from glacial to glaciofluvial quartz grains: Evidence from Svalbard
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DOI: 10.1016/j.sedgeo.2017.06.010
Abstract: Abstract The micromorphology of quartz grains in a sedimentary environment is determined by the transport mechanism and the nature of weathering. Both these aspects change during the transport history of grains. Thus important questions include… read more here.
Keywords: micromorphological features; transport; quartz grains; quartz ... See more keywords