Verification of the shallow seismic crustal structure of the western Krun, Hory crystalline unit, Czech Republic

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F13%3A10172677" target="_blank" >RIV/00216208:11320/13:10172677 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1007/s11200-012-0215-6" target="_blank" >http://dx.doi.org/10.1007/s11200-012-0215-6</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1007/s11200-012-0215-6" target="_blank" >10.1007/s11200-012-0215-6</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Verification of the shallow seismic crustal structure of the western Krun, Hory crystalline unit, Czech Republic

Popis výsledku v původním jazyce

We analyze refraction measurements along a short profile in western Krun, hory crystalline unit. The profile passed close to the seismically active zone of NovA1/2 Kostel. The measurements were carried out to distances of about 15 km using quarry blastsnear the village of Horni Rozmyl, located at the eastern margin of the crystalline unit. Smoothed P-wave travel times were interpreted using the Wiechert-Herglotz method, which yielded a 1-D velocity model of the shallow crustal structure of the crystalline unit down to a depth of 1.7 km. The P-wave velocity of the model increases from about 4.0 km/s at the surface to 5.9 km/s at a depth of 1.7 km. The superficial velocities of our model are somewhat higher than the superficial velocities of the model that is routinely used for earthquake location in the region.

Název v anglickém jazyce

Verification of the shallow seismic crustal structure of the western Krun, Hory crystalline unit, Czech Republic

Popis výsledku anglicky

We analyze refraction measurements along a short profile in western Krun, hory crystalline unit. The profile passed close to the seismically active zone of NovA1/2 Kostel. The measurements were carried out to distances of about 15 km using quarry blastsnear the village of Horni Rozmyl, located at the eastern margin of the crystalline unit. Smoothed P-wave travel times were interpreted using the Wiechert-Herglotz method, which yielded a 1-D velocity model of the shallow crustal structure of the crystalline unit down to a depth of 1.7 km. The P-wave velocity of the model increases from about 4.0 km/s at the surface to 5.9 km/s at a depth of 1.7 km. The superficial velocities of our model are somewhat higher than the superficial velocities of the model that is routinely used for earthquake location in the region.

Druh

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

CEP obor

DC - Seismologie, vulkanologie a struktura Země

OECD FORD obor

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Projekt

—

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2013

Kód důvěrnosti údajů

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

Název periodika

Studia Geophysica et Geodaetica

ISSN

0039-3169

e-ISSN

—

Svazek periodika

57

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

13

Strana od-do

507-519

Kód UT WoS článku

000323315400009

EID výsledku v databázi Scopus

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