RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 20, ES6003, doi:10.2205/2020ES000714, 2020

Figure 2. A – Morphometric characteristics of glauconite grain: a – longitudinal section (the major axis), b – cross-section (intermediate axis); B – glauconite in the heavy subfraction of the in bottom sediments in the fraction 0.063 mm on the profile 5, at depth 15 m; C – glauconite in the light subfraction of the in bottom sediments in the fraction 0.063 mm on the profile 5, at depth 15 m; D – glauconite in heavy subfraction 0.355 mm fraction on profile 1, depth 15 m (yield of heavy subfraction 1.2%, glauconite content 35.7%, with its content in the light fraction 2.1%).

 
Citation: Krek A., M. Ulyanova (2020), Mineral tracers of the alongshore sediment transport (example from the South-Eastern Baltic Sea), Russ. J. Earth Sci., 20, ES6003, doi:10.2205/2020ES000714.
 

Copyright 2020 by the Geophysical Center RAS.