Zonation and faciality of loessic deposits in Lithology and stratigraphy of loess and paleosols.

Auteur :
KES, A. S.

Description :
The deposit facies resulted from the sorting of silt during transportation and sedimentation. The farther is the source, the finer is the soil texture. Soil formation processes reflect the zonal climate (zonation) and other natural environmental conditions. (DLO).


Type de document :
Monographie

Source :
, p. 105-111, Références bibliographiques : 7 réf.

Date :
1984

Editeur :
Pays édition : Hongrie, Budapest, Hungarian Academy of Sciences, Geographical Research Institut