The role of dust source area and pedogenesis in three loess-palaeosol sections from North Bulgaria: A mineral magnetic study

Author:

Avramov V. I.,Jordanova D.,Hoffmann V.,Roesler W.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference43 articles.

1. Balescu S., Lamothe M., Mercier N., Huot S., Balteanu D., Billard A. and Hus J., 2003. Luminescence chronology of Pleistocene loess deposits from Romania: testing methods of age correction for anomalous fading in alkali feldspar. Quaternary Geochronology, 22, 967–973.

2. Balsam W., Ji J. and Chen J., 2004. Climatic interpretation of the Luochuan and Lingtai loess sections, based on changing iron oxide mineralogy and magnetic susceptibility. Earth Planet. Sci. Lett., 223, 335–348.

3. Bronger A. and Heinkele Th., 1989. Micromorphology and genesis of palaeosols in the Luochuan loess section, China: pedostratigraphic and environmental implications. Geoderma, 45, 123–143.

4. Christova R., 2003. Biostratigraphical analysis and paleoecological conditions in the Bulgarian Black sea Zone during the Quaternary. Annales of the Institute of Oceanology, Bulg. Acad. Sci., 4, 36–41.

5. Cornell R. and Schwertmann U., 1996. The Iron Oxides. Structure, Properties, Reactions, Occurrence and Uses. VCH Verlagsgesellschaft, Weinheim, Germany.

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