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Statements

Subject Item
n2:RIV%2F67985530%3A_____%2F11%3A00372604%21RIV12-MZP-67985530
rdf:type
n4:Vysledek skos:Concept
dcterms:description
The latest international seismic refraction experiment in the Central Europe SUDETES 2003 covered also the territory of the northern part of the Bohemian Massif. The profile S01 follows the SW-NE axis of the Eger/Ohře Rift in Northwestern Bohemia. The dictinct first arrivals of Pg waves were used to derive a 2-D tomographic velocity model with an optimum lateral resolution. The innovative DRTG method was applied in iterative mode to minimize linearized errors of tomographic inversion. The iteration process yielded a fine-grid velocity model with a required level of RMS travel-time fit and the model rouhgness. The time residuals were assessed at single grid depth levels and used to derive the statistical lateral resolution of %22lens-shaped%22 velocity anomalies: for the 95% confidence level and 5% anomalies, one can resolve their lateral sizes from 15 to 40 km at the depths from 0 to 20 km. The latest international seismic refraction experiment in the Central Europe SUDETES 2003 covered also the territory of the northern part of the Bohemian Massif. The profile S01 follows the SW-NE axis of the Eger/Ohře Rift in Northwestern Bohemia. The dictinct first arrivals of Pg waves were used to derive a 2-D tomographic velocity model with an optimum lateral resolution. The innovative DRTG method was applied in iterative mode to minimize linearized errors of tomographic inversion. The iteration process yielded a fine-grid velocity model with a required level of RMS travel-time fit and the model rouhgness. The time residuals were assessed at single grid depth levels and used to derive the statistical lateral resolution of %22lens-shaped%22 velocity anomalies: for the 95% confidence level and 5% anomalies, one can resolve their lateral sizes from 15 to 40 km at the depths from 0 to 20 km.
dcterms:title
Upper crustal structure of the northern part of the Bohemian ­Massif in ­rel­ation­ t­o geological, potential field data and new deep seismic data (Eger/Ohře Rift, Central Europe) Upper crustal structure of the northern part of the Bohemian ­Massif in ­rel­ation­ t­o geological, potential field data and new deep seismic data (Eger/Ohře Rift, Central Europe)
skos:prefLabel
Upper crustal structure of the northern part of the Bohemian ­Massif in ­rel­ation­ t­o geological, potential field data and new deep seismic data (Eger/Ohře Rift, Central Europe) Upper crustal structure of the northern part of the Bohemian ­Massif in ­rel­ation­ t­o geological, potential field data and new deep seismic data (Eger/Ohře Rift, Central Europe)
skos:notation
RIV/67985530:_____/11:00372604!RIV12-MZP-67985530
n4:predkladatel
n5:ico%3A67985530
n6:aktivita
n9:P n9:Z n9:I
n6:aktivity
I, P(1M0554), P(IAA300460602), P(SB/630/3/02), Z(AV0Z30120515), Z(MZP0002579801)
n6:cisloPeriodika
1
n6:dodaniDat
n12:2012
n6:domaciTvurceVysledku
n16:1424408 n16:5126649
n6:druhVysledku
n11:J
n6:duvernostUdaju
n13:S
n6:entitaPredkladatele
n10:predkladatel
n6:idSjednocenehoVysledku
236965
n6:idVysledku
RIV/67985530:_____/11:00372604
n6:jazykVysledku
n19:eng
n6:klicovaSlova
upper crustal structure; Bohemian Massif; Eger/Ohře Rift; Saxothuringian Zone; Teplá-Barrandian Unit; Moldanubian Zone
n6:klicoveSlovo
n7:Saxothuringian%20Zone n7:Bohemian%20Massif n7:Tepl%C3%A1-Barrandian%20Unit n7:Eger%2FOh%C5%99e%20Rift n7:Moldanubian%20Zone n7:upper%20crustal%20structure
n6:kodStatuVydavatele
DE - Spolková republika Německo
n6:kontrolniKodProRIV
[BC5ABCBF24EC]
n6:nazevZdroje
Zeitschrift für geologische Wissenschaften
n6:obor
n17:DC
n6:pocetDomacichTvurcuVysledku
2
n6:pocetTvurcuVysledku
4
n6:projekt
n14:SB%2F630%2F3%2F02 n14:1M0554 n14:IAA300460602
n6:rokUplatneniVysledku
n12:2011
n6:svazekPeriodika
39
n6:tvurceVysledku
Mlčoch, B. Novotný, Miroslav Mrlina, Jan Skácelová, Z.
n6:zamer
n18:AV0Z30120515 n18:MZP0002579801
s:issn
0303-4534
s:numberOfPages
18