Paleosesimic study of the Sudetic Marginal Fault at the locality Bílá Voda (Bohemian Massif)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985891%3A_____%2F11%3A00371132" target="_blank" >RIV/67985891:_____/11:00371132 - isvavai.cz</a>

Výsledek na webu

—

DOI - Digital Object Identifier

—

Jazyk výsledku

angličtina

Název v původním jazyce

Paleosesimic study of the Sudetic Marginal Fault at the locality Bílá Voda (Bohemian Massif)

Popis výsledku v původním jazyce

The study area is situated in the north-eastern part of the Bohemian Massif and comprises SE part of the Sudetic Marginal Fault zone (SMF) with pronounced mountain front, which borders the Sudeten Mts. Paleoseismological trenches at the locality of BíláVoda municipality performed across the SMF were carried out in order to study potential prehistoric morphogenic earthquakes responsible for the present-day morphology. Geomorphologic analysis and electrical resistivity tomography enabled to position thetrenches at suitable site. The trenches revealed prevailing strike-slip character of the late Quaternary faulting. Faulted deposits were dated by OSL and radiocarbon dating methods and the results are discussed here. At least four or five events creatinga surface rupture during late Quaternary (Holocene) were inferred. Due to strike-slip character, the horizontal displacement and the related slip-rate on the SMF is still under investigation. From the previous study, minimum magnitude M

Název v anglickém jazyce

Paleosesimic study of the Sudetic Marginal Fault at the locality Bílá Voda (Bohemian Massif)

Popis výsledku anglicky

The study area is situated in the north-eastern part of the Bohemian Massif and comprises SE part of the Sudetic Marginal Fault zone (SMF) with pronounced mountain front, which borders the Sudeten Mts. Paleoseismological trenches at the locality of BíláVoda municipality performed across the SMF were carried out in order to study potential prehistoric morphogenic earthquakes responsible for the present-day morphology. Geomorphologic analysis and electrical resistivity tomography enabled to position thetrenches at suitable site. The trenches revealed prevailing strike-slip character of the late Quaternary faulting. Faulted deposits were dated by OSL and radiocarbon dating methods and the results are discussed here. At least four or five events creatinga surface rupture during late Quaternary (Holocene) were inferred. Due to strike-slip character, the horizontal displacement and the related slip-rate on the SMF is still under investigation. From the previous study, minimum magnitude M

Druh

D - Stať ve sborníku

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

—

Projekt

<a href="/cs/project/GP205%2F08%2FP521" target="_blank" >GP205/08/P521: Projevy mladokvartérní tektoniky v zóně okrajového sudetského zlomu</a><br>

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2011

Kód důvěrnosti údajů

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

Název statě ve sborníku

Earthquake Geology and Geoarchaeology: Science, Society and Critical facilities. 2nd INQUA-IGCP-567 International Workshop on Active Tectonics, Earthquake Geology, Archaeology and Engineering

ISBN

978-960-466-093-3

ISSN

—

e-ISSN

—

Počet stran výsledku

4

Strana od-do

239-242

Název nakladatele

Natural Hazards Laboratory, National and Kapodistrian University of Athens

Místo vydání

Athens

Místo konání akce

Corinth

Datum konání akce

19. 9. 2011

Typ akce podle státní příslušnosti

WRD - Celosvětová akce

Kód UT WoS článku

—