Plestocenní fluviální řerasy řeky Svratky - faciální studium a provenience

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F07%3A00020461" target="_blank" >RIV/00216224:14310/07:00020461 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Pleistocene fluvial terraces of the Svratka river - facies and provenance study

Popis výsledku v původním jazyce

The middle course of the Svratka river flows through the geologically and geomorphologically complex area around the Brno city. This area underwent dynamic development during the Quaternary. Terrace system along the river course developed, witnessing thealternating incision and deposition phases during the last 1 Ma. The Quaternary uplift of the area can be deduced from the incision record of the river system. Sea level changes are assumed to have played negligible role (distance to the coastline, lowriver gradient). Three successive river terraces (Pleistocene) were studied within the terrace staircase, the highest of which is about 60 m and the lowest about 15 m above the present river. Preservation of the river deposits is mostly fragmentary. Themiddle terrace (ca. 40 m above the present river) is the best preserved one (with largest lateral extent and thickness). The terrace sediments are composed of fluvial gravels and sands. Architectural components within the outcrops were de

Název v anglickém jazyce

Pleistocene fluvial terraces of the Svratka river - facies and provenance study

Popis výsledku anglicky

The middle course of the Svratka river flows through the geologically and geomorphologically complex area around the Brno city. This area underwent dynamic development during the Quaternary. Terrace system along the river course developed, witnessing thealternating incision and deposition phases during the last 1 Ma. The Quaternary uplift of the area can be deduced from the incision record of the river system. Sea level changes are assumed to have played negligible role (distance to the coastline, lowriver gradient). Three successive river terraces (Pleistocene) were studied within the terrace staircase, the highest of which is about 60 m and the lowest about 15 m above the present river. Preservation of the river deposits is mostly fragmentary. Themiddle terrace (ca. 40 m above the present river) is the best preserved one (with largest lateral extent and thickness). The terrace sediments are composed of fluvial gravels and sands. Architectural components within the outcrops were de

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

<a href="/cs/project/GA205%2F06%2F1024" target="_blank" >GA205/06/1024: Geomorfologie údolí střední Svratky - kvartérní vývoj a environmentální aspekty</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2007

Kód důvěrnosti údajů

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

Název periodika

GeoAlp

ISSN

1824-7741

e-ISSN

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Svazek periodika

4/2004

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

AT - Rakouská republika

Počet stran výsledku

1

Strana od-do

70-70

Kód UT WoS článku

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EID výsledku v databázi Scopus

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