NIVNÍ ULOŽENINY DYJE U MICMANIC
Vol.11,(2004)
Abstract
Keywords:
Quaternary; flood plain; subfossil soil
80 cm thick subfossil soil developed within about 5 m thick overbank sediments of the Dyje River near Micmanice village. During the subsequent phase was a polygenetic pseudochernozem originated (depth 2,30 - 3,10 m, 2950 ± 140 years BP, Gd-30053).
Quaternary; flood plain; subfossil soil
References
Dornič, J.et al. (1984):Vysvětlivky k základní geologické mapě ČSSR 1:25000 34-132 Božice. - Ústř. Úst. geol. Praha.
Havlíček, P. - Smolíková , L. (1994): Vývoj jihomoravských niv (Evolution of south Moravian flood plains). Věst. Čes. geol. Úst., 69, 1, 23-40. Praha.