Spatial Analysis of Remote Sensing Data in Early Stage of a Seismo-tectonic Research

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985891%3A_____%2F15%3A00448143" target="_blank" >RIV/67985891:_____/15:00448143 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1007/978-3-319-09060-3_21" target="_blank" >http://dx.doi.org/10.1007/978-3-319-09060-3_21</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1007/978-3-319-09060-3_21" target="_blank" >10.1007/978-3-319-09060-3_21</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Spatial Analysis of Remote Sensing Data in Early Stage of a Seismo-tectonic Research

Popis výsledku v původním jazyce

In 1901, M4.7 earthquake hit the area of NE Bohemia, Czech Republic. The Hronov-Porici Fault (HPF) was found responsible for the event. Ongoing seismic monitoring proves the Hronov-Porici Fault Zone (HPFZ) is, in fact, the second most active area in theBohemian Massif. Despite importance of the area, the HPFZ has not been described reasonably. Up to the moment, neither length of the HPFZ nor exact locations of its south branch are clear. Vagueness in length of the HPFZ causes large uncertainty in seismic risk assessment of the area. Integrated approach based on geographic information systems and remote sensing was employed to delineate lineaments in the wider HPFZ area. NASA provided Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) data was evaluated. ASTER digital elevation model provided basic topographic characteristics (surface curvature, slope and drainage systems). Edge detecting process was employed to define lineaments. Recent seismic activity and GPS mon

Název v anglickém jazyce

Spatial Analysis of Remote Sensing Data in Early Stage of a Seismo-tectonic Research

Popis výsledku anglicky

In 1901, M4.7 earthquake hit the area of NE Bohemia, Czech Republic. The Hronov-Porici Fault (HPF) was found responsible for the event. Ongoing seismic monitoring proves the Hronov-Porici Fault Zone (HPFZ) is, in fact, the second most active area in theBohemian Massif. Despite importance of the area, the HPFZ has not been described reasonably. Up to the moment, neither length of the HPFZ nor exact locations of its south branch are clear. Vagueness in length of the HPFZ causes large uncertainty in seismic risk assessment of the area. Integrated approach based on geographic information systems and remote sensing was employed to delineate lineaments in the wider HPFZ area. NASA provided Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) data was evaluated. ASTER digital elevation model provided basic topographic characteristics (surface curvature, slope and drainage systems). Edge detecting process was employed to define lineaments. Recent seismic activity and GPS mon

Druh

D - Stať ve sborníku

CEP obor

DC - Seismologie, vulkanologie a struktura Země

OECD FORD obor

—

Projekt

<a href="/cs/project/GA205%2F09%2F1244" target="_blank" >GA205/09/1244: Charakter seismicity v oblasti Hronovsko-poříčského zlomu</a><br>

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2015

Kód důvěrnosti údajů

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

Název statě ve sborníku

Engineering Geology for Society and Territory.

ISBN

978-3-319-09059-7

ISSN

—

e-ISSN

—

Počet stran výsledku

5

Strana od-do

119-123

Název nakladatele

Springer

Místo vydání

Cham

Místo konání akce

Torino

Datum konání akce

15. 9. 2014

Typ akce podle státní příslušnosti

WRD - Celosvětová akce

Kód UT WoS článku

000359016200021