@ARTICLE{Chlebowski_Roman_Mineralogical_1991,
 author={Chlebowski, Roman},
 volume={vol. 12},
 number={No 2},
 journal={Polish Polar Research},
 pages={215—222},
 howpublished={online},
 year={1991},
 publisher={Polish Academy of Sciences},
 publisher={Committee on Polar Research},
 abstract={Heavy minerals in sandur deposits from the forefield of the Renard Glacier were investigated. They are concentrated only in fractions below 0.1 mm in diameter. Composition and preservation of heavy minerals indicate very high dynamic in the sedimentary environment. Most resistant minerals as zircon and tourmaline predominate and are strongly crumbled. They probably may serve as mineral indicators of sandur deposits. If distinguished regularities are confirmed in forefield in other Spitsbergen sandurs, then contemporary and Pleistocene sandur deposits could be compared. No mineralogie differentiation of intra- and extramorainal sandurs was noted.},
 type={Article},
 title={Mineralogical description of sandur deposits from the forefield of the Renard Glacier (Wedel Jarlsberg Land, Spitsbergen) on the ground of heavy minerals},
 URL={http://ochroma.man.poznan.pl/Content/111127/PDF-MASTER/1991-2_215-222.pdf},
 keywords={Arctic, Spitsbergen, mineralogy, sandur deposits},
}