SEDIMENTÁRNĚ-GEOLOGICKÉ STUDIUM VYBRANÝCH KVARTÉRNÍCH SEDIMENTŮ V OKOLÍ BRNĚNSKÉ PŘEHRADY
Author(s) -
Marek Mikulík,
Slavomı́r Nehyba,
František Hubatka
Publication year - 2012
Publication title -
geologické výzkumy na moravě a ve slezsku
Language(s) - English
Resource type - Journals
eISSN - 2336-4378
pISSN - 1212-6209
DOI - 10.5817/gvms2012-1-2-030
Subject(s) - geology , colluvium , loess , outcrop , facies , fluvial , quaternary , sedimentary rock , sediment , geomorphology , geochemistry , pleistocene , sedimentary structures , aeolian processes , paleontology , alluvium , structural basin
Outcrops of Quaternary deposits are lining banks of the Brno dam. One of them is situated on the left bank ~ 250 m NW of the Osada pier. The sedimentary profile of Pleistocene deposits is composed of fluvial deposits of the Paleo – Svratka River covered by colluvial and eolian (loess) deposits. Alternation of various facies and various grain-size fractions reveals alternation of more or less arid conditions and also evolution of the surrounding landscape.
Accelerating Research
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom
Address
John Eccles HouseRobert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom