Micromorphology of Quartz Grain Surface as Indicator of Glacial Sedimentation Conditions: Evidence from the Protva River Basin

Author:

Alekseeva V. A.

Publisher

Springer Science and Business Media LLC

Subject

Economic Geology,Geochemistry and Petrology

Reference43 articles.

1. Alekseeva, V.A., Migration and Diagenetic Transformation of Quartz Grains and Their Paleogeographic Interpretation, Vestn. Mosk. Univ., Ser. 5: Geogr., 2003, no. 4, pp. 40–46.

2. Alekseeva, V.A., Micromorphology of Quartz Grain Surfaces as Indicator of Glacial Relief Formation Conditions (with Reference to the Middle Course of the Protva River), PhD (Geogr.) Dissertation, Moscow: Mosk. Gos. Univ., 2004.

3. Alekseeva, V.A. and Hounslow, M.W., Clastic Sediment Source Characterization Using Discrete and Included Magnetic Particles-Their Relationship to Conventional Petrographic Methods in Early Pleistocene Fluvial-Glacial Sediments, Upper Don River Basin (Russia), Phys. Chem. Earth, 2004, vol. 29, pp. 961–971.

4. Anan'eva, E.G., Litologo-mineralogicheskii analiz pri geomorfologicheskikh i paleogeograficheskikh issledovaniyakh, (Lithological-Mineralogical Analysis for Geomorphological and Paleogeographical Investigations) Smolensk: Smolen. Gumanit. Univ., 1998.

5. Artemova, N.L., Micromorphology of Loess-Type Sediments in Permafrost Area as an Indicator of Their Genesis, PhD (Geogr.) Dissertation, Moscow: Mosk. Gos. Univ., 1988.

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