Lower Carboniferous Goniatites from Moravice Formation, Nízký Jeseník Mts. (Moravo-Silesian Unit of the Czech Massif)

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15310%2F06%3A00010013" target="_blank" >RIV/61989592:15310/06:00010013 - isvavai.cz</a>

Result on the web

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DOI - Digital Object Identifier

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Result language

čeština

Original language name

Lower Carboniferous Goniatites from Moravice Formation, Nízký Jeseník Mts. (Moravo-Silesian Unit of the Czech Massif)

Original language description

Lower Carboniferous sediments developed in the Culm facies are common in the eastern edge of the Bohemian Massif (in the Nízký Jeseník Mts. and Drahany Upland). The oldest lithostratigraphical unit of the Nízký Jeseník Culm is the Andělská Hora Formation(gradded bedding of the clay/silt-shales rhytmites with positions of conglomerates). A younger formation is the Horní Benešov Fm. (uniform massive bedding of greywackes with thin-bedded rhytmites of silts). The Moravice Formation was defined by Patteisky in 1929. It is a complex of Lower Carboniferous deep water siliciclastic deposits, which contains black shales and conglomerates, greywackes or laminites of greywackes and silts or clays (Zapletal - Dvořák - Kumpera 1989). The overlying Hradec-KyjoviceFm. contains greywackes (in the lower part) and clay/silt rhytmites with fine grained greywackes (in the upper part). In environs of Ostrava city, the hradec-Kyjovice Formation shows the character of transition from flysch into molasse o

Czech name

Lower Carboniferous Goniatites from Moravice Formation, Nízký Jeseník Mts. (Moravo-Silesian Unit of the Czech Massif)

Czech description

Lower Carboniferous sediments developed in the Culm facies are common in the eastern edge of the Bohemian Massif (in the Nízký Jeseník Mts. and Drahany Upland). The oldest lithostratigraphical unit of the Nízký Jeseník Culm is the Andělská Hora Formation(gradded bedding of the clay/silt-shales rhytmites with positions of conglomerates). A younger formation is the Horní Benešov Fm. (uniform massive bedding of greywackes with thin-bedded rhytmites of silts). The Moravice Formation was defined by Patteisky in 1929. It is a complex of Lower Carboniferous deep water siliciclastic deposits, which contains black shales and conglomerates, greywackes or laminites of greywackes and silts or clays (Zapletal - Dvořák - Kumpera 1989). The overlying Hradec-KyjoviceFm. contains greywackes (in the lower part) and clay/silt rhytmites with fine grained greywackes (in the upper part). In environs of Ostrava city, the hradec-Kyjovice Formation shows the character of transition from flysch into molasse o

Type

D - Article in proceedings

CEP classification

DB - Geology and mineralogy

OECD FORD branch

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Project

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Continuities

S - Specificky vyzkum na vysokych skolach

Publication year

2006

Confidentiality

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Article name in the collection

Scripta Facultatis scientiarum naturalium Universitatis Masarykianae Brunensis, Geology

ISBN

80-210-4097-1

ISSN

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e-ISSN

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Number of pages

104

Pages from-to

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Publisher name

Masarykova univerzita

Place of publication

Brno

Event location

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Event date

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Type of event by nationality

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UT code for WoS article

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