Doklady redepozice křídových sedimentů do uloženin spodního miocénu mezi Černou Horou a Závistí

نویسندگان

چکیده

Many boreholes have been drilled between Černá Hora town and Závist village to evaluate geohazards that may affect the construction of a new road. The core material from was studied for translucent heavy minerals microfossil content. Translucent mineral assemblages sands are often dominated by staurolite. Cyanite, tourmaline, rutile andalusite, typical Cenomanian sediments Moravia common. Relatively important share garnet (20–30 %) in two samples reflects most probably source Turonian sediments. Those granitoids Brno Massif, surrounding underlying sediments, very rare. Agglutinated foraminifera reworked or younger Cretaceous represent frequent microfossils. Single find Pleurostomella gr. alternans be only autochthonous element indicating Miocene age. Both microfossils correspond with those previously sites broader area including surroundings. Sediments characterised high susceptibility sliding, which particularly evident during rainfall totals spring 2006.

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ژورنال

عنوان ژورنال: Geologicke? vy?zkumy na Morave? a ve Slezsku v roce ...

سال: 2021

ISSN: ['1212-6209', '2336-4378']

DOI: https://doi.org/10.5817/gvms2021-15671