Attenuation of Coda Waves in Hungary
Abstract Microearthquake codas from 19 shallow depth local events have been analysed in Hungary. We estimate coda attenuation Qc in the frequency range 6 to 24 Hz used Sato’s (1977) single scattering model for a coda window of 12.5±2.5 s beginning at twice the S-wave travel time. Travel times were b...
Ausführliche Beschreibung
Autor*in: |
Kiszely, M. [verfasserIn] |
---|
Format: |
E-Artikel |
---|---|
Sprache: |
Englisch |
Erschienen: |
2000 |
---|
Schlagwörter: |
---|
Anmerkung: |
© Akadémiai Kiadó 2000 |
---|
Übergeordnetes Werk: |
Enthalten in: Acta geodaetica et geophysica Hungarica - Budapest : Akad. Kiadó, 1997, 35(2000), 4 vom: Dez., Seite 465-473 |
---|---|
Übergeordnetes Werk: |
volume:35 ; year:2000 ; number:4 ; month:12 ; pages:465-473 |
Links: |
---|
DOI / URN: |
10.1007/BF03325634 |
---|
Katalog-ID: |
SPR037131869 |
---|
LEADER | 01000caa a22002652 4500 | ||
---|---|---|---|
001 | SPR037131869 | ||
003 | DE-627 | ||
005 | 20230328170043.0 | ||
007 | cr uuu---uuuuu | ||
008 | 201007s2000 xx |||||o 00| ||eng c | ||
024 | 7 | |a 10.1007/BF03325634 |2 doi | |
035 | |a (DE-627)SPR037131869 | ||
035 | |a (SPR)BF03325634-e | ||
040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
041 | |a eng | ||
100 | 1 | |a Kiszely, M. |e verfasserin |4 aut | |
245 | 1 | 0 | |a Attenuation of Coda Waves in Hungary |
264 | 1 | |c 2000 | |
336 | |a Text |b txt |2 rdacontent | ||
337 | |a Computermedien |b c |2 rdamedia | ||
338 | |a Online-Ressource |b cr |2 rdacarrier | ||
500 | |a © Akadémiai Kiadó 2000 | ||
520 | |a Abstract Microearthquake codas from 19 shallow depth local events have been analysed in Hungary. We estimate coda attenuation Qc in the frequency range 6 to 24 Hz used Sato’s (1977) single scattering model for a coda window of 12.5±2.5 s beginning at twice the S-wave travel time. Travel times were between 2–23 sec. The stations showed similar values of Qc which were about 400 at 6 Hz and about 1400 at 24 Hz. The Qc values in Hungary indicate moderate tectonic characteristic. | ||
650 | 4 | |a coda waves |7 (dpeaa)DE-He213 | |
650 | 4 | |a coda waves |7 (dpeaa)DE-He213 | |
650 | 4 | |a seismic quality factor |7 (dpeaa)DE-He213 | |
773 | 0 | 8 | |i Enthalten in |t Acta geodaetica et geophysica Hungarica |d Budapest : Akad. Kiadó, 1997 |g 35(2000), 4 vom: Dez., Seite 465-473 |w (DE-627)364470852 |w (DE-600)2110468-2 |x 1587-1037 |7 nnns |
773 | 1 | 8 | |g volume:35 |g year:2000 |g number:4 |g month:12 |g pages:465-473 |
856 | 4 | 0 | |u https://dx.doi.org/10.1007/BF03325634 |z lizenzpflichtig |3 Volltext |
912 | |a GBV_USEFLAG_A | ||
912 | |a SYSFLAG_A | ||
912 | |a GBV_SPRINGER | ||
912 | |a GBV_ILN_20 | ||
912 | |a GBV_ILN_22 | ||
912 | |a GBV_ILN_23 | ||
912 | |a GBV_ILN_24 | ||
912 | |a GBV_ILN_31 | ||
912 | |a GBV_ILN_39 | ||
912 | |a GBV_ILN_40 | ||
912 | |a GBV_ILN_60 | ||
912 | |a GBV_ILN_62 | ||
912 | |a GBV_ILN_65 | ||
912 | |a GBV_ILN_69 | ||
912 | |a GBV_ILN_70 | ||
912 | |a GBV_ILN_73 | ||
912 | |a GBV_ILN_74 | ||
912 | |a GBV_ILN_90 | ||
912 | |a GBV_ILN_95 | ||
912 | |a GBV_ILN_100 | ||
912 | |a GBV_ILN_105 | ||
912 | |a GBV_ILN_110 | ||
912 | |a GBV_ILN_120 | ||
912 | |a GBV_ILN_152 | ||
912 | |a GBV_ILN_161 | ||
912 | |a GBV_ILN_171 | ||
912 | |a GBV_ILN_187 | ||
912 | |a GBV_ILN_224 | ||
912 | |a GBV_ILN_250 | ||
912 | |a GBV_ILN_281 | ||
912 | |a GBV_ILN_285 | ||
912 | |a GBV_ILN_293 | ||
912 | |a GBV_ILN_370 | ||
912 | |a GBV_ILN_602 | ||
912 | |a GBV_ILN_702 | ||
951 | |a AR | ||
952 | |d 35 |j 2000 |e 4 |c 12 |h 465-473 |
author_variant |
m k mk |
---|---|
matchkey_str |
article:15871037:2000----::teutoocdwv |
hierarchy_sort_str |
2000 |
publishDate |
2000 |
allfields |
10.1007/BF03325634 doi (DE-627)SPR037131869 (SPR)BF03325634-e DE-627 ger DE-627 rakwb eng Kiszely, M. verfasserin aut Attenuation of Coda Waves in Hungary 2000 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Akadémiai Kiadó 2000 Abstract Microearthquake codas from 19 shallow depth local events have been analysed in Hungary. We estimate coda attenuation Qc in the frequency range 6 to 24 Hz used Sato’s (1977) single scattering model for a coda window of 12.5±2.5 s beginning at twice the S-wave travel time. Travel times were between 2–23 sec. The stations showed similar values of Qc which were about 400 at 6 Hz and about 1400 at 24 Hz. The Qc values in Hungary indicate moderate tectonic characteristic. coda waves (dpeaa)DE-He213 coda waves (dpeaa)DE-He213 seismic quality factor (dpeaa)DE-He213 Enthalten in Acta geodaetica et geophysica Hungarica Budapest : Akad. Kiadó, 1997 35(2000), 4 vom: Dez., Seite 465-473 (DE-627)364470852 (DE-600)2110468-2 1587-1037 nnns volume:35 year:2000 number:4 month:12 pages:465-473 https://dx.doi.org/10.1007/BF03325634 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 35 2000 4 12 465-473 |
spelling |
10.1007/BF03325634 doi (DE-627)SPR037131869 (SPR)BF03325634-e DE-627 ger DE-627 rakwb eng Kiszely, M. verfasserin aut Attenuation of Coda Waves in Hungary 2000 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Akadémiai Kiadó 2000 Abstract Microearthquake codas from 19 shallow depth local events have been analysed in Hungary. We estimate coda attenuation Qc in the frequency range 6 to 24 Hz used Sato’s (1977) single scattering model for a coda window of 12.5±2.5 s beginning at twice the S-wave travel time. Travel times were between 2–23 sec. The stations showed similar values of Qc which were about 400 at 6 Hz and about 1400 at 24 Hz. The Qc values in Hungary indicate moderate tectonic characteristic. coda waves (dpeaa)DE-He213 coda waves (dpeaa)DE-He213 seismic quality factor (dpeaa)DE-He213 Enthalten in Acta geodaetica et geophysica Hungarica Budapest : Akad. Kiadó, 1997 35(2000), 4 vom: Dez., Seite 465-473 (DE-627)364470852 (DE-600)2110468-2 1587-1037 nnns volume:35 year:2000 number:4 month:12 pages:465-473 https://dx.doi.org/10.1007/BF03325634 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 35 2000 4 12 465-473 |
allfields_unstemmed |
10.1007/BF03325634 doi (DE-627)SPR037131869 (SPR)BF03325634-e DE-627 ger DE-627 rakwb eng Kiszely, M. verfasserin aut Attenuation of Coda Waves in Hungary 2000 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Akadémiai Kiadó 2000 Abstract Microearthquake codas from 19 shallow depth local events have been analysed in Hungary. We estimate coda attenuation Qc in the frequency range 6 to 24 Hz used Sato’s (1977) single scattering model for a coda window of 12.5±2.5 s beginning at twice the S-wave travel time. Travel times were between 2–23 sec. The stations showed similar values of Qc which were about 400 at 6 Hz and about 1400 at 24 Hz. The Qc values in Hungary indicate moderate tectonic characteristic. coda waves (dpeaa)DE-He213 coda waves (dpeaa)DE-He213 seismic quality factor (dpeaa)DE-He213 Enthalten in Acta geodaetica et geophysica Hungarica Budapest : Akad. Kiadó, 1997 35(2000), 4 vom: Dez., Seite 465-473 (DE-627)364470852 (DE-600)2110468-2 1587-1037 nnns volume:35 year:2000 number:4 month:12 pages:465-473 https://dx.doi.org/10.1007/BF03325634 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 35 2000 4 12 465-473 |
allfieldsGer |
10.1007/BF03325634 doi (DE-627)SPR037131869 (SPR)BF03325634-e DE-627 ger DE-627 rakwb eng Kiszely, M. verfasserin aut Attenuation of Coda Waves in Hungary 2000 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Akadémiai Kiadó 2000 Abstract Microearthquake codas from 19 shallow depth local events have been analysed in Hungary. We estimate coda attenuation Qc in the frequency range 6 to 24 Hz used Sato’s (1977) single scattering model for a coda window of 12.5±2.5 s beginning at twice the S-wave travel time. Travel times were between 2–23 sec. The stations showed similar values of Qc which were about 400 at 6 Hz and about 1400 at 24 Hz. The Qc values in Hungary indicate moderate tectonic characteristic. coda waves (dpeaa)DE-He213 coda waves (dpeaa)DE-He213 seismic quality factor (dpeaa)DE-He213 Enthalten in Acta geodaetica et geophysica Hungarica Budapest : Akad. Kiadó, 1997 35(2000), 4 vom: Dez., Seite 465-473 (DE-627)364470852 (DE-600)2110468-2 1587-1037 nnns volume:35 year:2000 number:4 month:12 pages:465-473 https://dx.doi.org/10.1007/BF03325634 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 35 2000 4 12 465-473 |
allfieldsSound |
10.1007/BF03325634 doi (DE-627)SPR037131869 (SPR)BF03325634-e DE-627 ger DE-627 rakwb eng Kiszely, M. verfasserin aut Attenuation of Coda Waves in Hungary 2000 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Akadémiai Kiadó 2000 Abstract Microearthquake codas from 19 shallow depth local events have been analysed in Hungary. We estimate coda attenuation Qc in the frequency range 6 to 24 Hz used Sato’s (1977) single scattering model for a coda window of 12.5±2.5 s beginning at twice the S-wave travel time. Travel times were between 2–23 sec. The stations showed similar values of Qc which were about 400 at 6 Hz and about 1400 at 24 Hz. The Qc values in Hungary indicate moderate tectonic characteristic. coda waves (dpeaa)DE-He213 coda waves (dpeaa)DE-He213 seismic quality factor (dpeaa)DE-He213 Enthalten in Acta geodaetica et geophysica Hungarica Budapest : Akad. Kiadó, 1997 35(2000), 4 vom: Dez., Seite 465-473 (DE-627)364470852 (DE-600)2110468-2 1587-1037 nnns volume:35 year:2000 number:4 month:12 pages:465-473 https://dx.doi.org/10.1007/BF03325634 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 35 2000 4 12 465-473 |
language |
English |
source |
Enthalten in Acta geodaetica et geophysica Hungarica 35(2000), 4 vom: Dez., Seite 465-473 volume:35 year:2000 number:4 month:12 pages:465-473 |
sourceStr |
Enthalten in Acta geodaetica et geophysica Hungarica 35(2000), 4 vom: Dez., Seite 465-473 volume:35 year:2000 number:4 month:12 pages:465-473 |
format_phy_str_mv |
Article |
institution |
findex.gbv.de |
topic_facet |
coda waves seismic quality factor |
isfreeaccess_bool |
false |
container_title |
Acta geodaetica et geophysica Hungarica |
authorswithroles_txt_mv |
Kiszely, M. @@aut@@ |
publishDateDaySort_date |
2000-12-01T00:00:00Z |
hierarchy_top_id |
364470852 |
id |
SPR037131869 |
language_de |
englisch |
fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR037131869</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230328170043.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201007s2000 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/BF03325634</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR037131869</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)BF03325634-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Kiszely, M.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Attenuation of Coda Waves in Hungary</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2000</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Akadémiai Kiadó 2000</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Microearthquake codas from 19 shallow depth local events have been analysed in Hungary. We estimate coda attenuation Qc in the frequency range 6 to 24 Hz used Sato’s (1977) single scattering model for a coda window of 12.5±2.5 s beginning at twice the S-wave travel time. Travel times were between 2–23 sec. The stations showed similar values of Qc which were about 400 at 6 Hz and about 1400 at 24 Hz. The Qc values in Hungary indicate moderate tectonic characteristic.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">coda waves</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">coda waves</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">seismic quality factor</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Acta geodaetica et geophysica Hungarica</subfield><subfield code="d">Budapest : Akad. Kiadó, 1997</subfield><subfield code="g">35(2000), 4 vom: Dez., Seite 465-473</subfield><subfield code="w">(DE-627)364470852</subfield><subfield code="w">(DE-600)2110468-2</subfield><subfield code="x">1587-1037</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:35</subfield><subfield code="g">year:2000</subfield><subfield code="g">number:4</subfield><subfield code="g">month:12</subfield><subfield code="g">pages:465-473</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://dx.doi.org/10.1007/BF03325634</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_SPRINGER</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_39</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_69</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_74</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_90</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_100</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_120</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_152</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_161</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_171</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_187</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_224</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_250</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_281</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_285</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_293</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_702</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">35</subfield><subfield code="j">2000</subfield><subfield code="e">4</subfield><subfield code="c">12</subfield><subfield code="h">465-473</subfield></datafield></record></collection>
|
author |
Kiszely, M. |
spellingShingle |
Kiszely, M. misc coda waves misc seismic quality factor Attenuation of Coda Waves in Hungary |
authorStr |
Kiszely, M. |
ppnlink_with_tag_str_mv |
@@773@@(DE-627)364470852 |
format |
electronic Article |
delete_txt_mv |
keep |
author_role |
aut |
collection |
springer |
remote_str |
true |
illustrated |
Not Illustrated |
issn |
1587-1037 |
topic_title |
Attenuation of Coda Waves in Hungary coda waves (dpeaa)DE-He213 seismic quality factor (dpeaa)DE-He213 |
topic |
misc coda waves misc seismic quality factor |
topic_unstemmed |
misc coda waves misc seismic quality factor |
topic_browse |
misc coda waves misc seismic quality factor |
format_facet |
Elektronische Aufsätze Aufsätze Elektronische Ressource |
format_main_str_mv |
Text Zeitschrift/Artikel |
carriertype_str_mv |
cr |
hierarchy_parent_title |
Acta geodaetica et geophysica Hungarica |
hierarchy_parent_id |
364470852 |
hierarchy_top_title |
Acta geodaetica et geophysica Hungarica |
isfreeaccess_txt |
false |
familylinks_str_mv |
(DE-627)364470852 (DE-600)2110468-2 |
title |
Attenuation of Coda Waves in Hungary |
ctrlnum |
(DE-627)SPR037131869 (SPR)BF03325634-e |
title_full |
Attenuation of Coda Waves in Hungary |
author_sort |
Kiszely, M. |
journal |
Acta geodaetica et geophysica Hungarica |
journalStr |
Acta geodaetica et geophysica Hungarica |
lang_code |
eng |
isOA_bool |
false |
recordtype |
marc |
publishDateSort |
2000 |
contenttype_str_mv |
txt |
container_start_page |
465 |
author_browse |
Kiszely, M. |
container_volume |
35 |
format_se |
Elektronische Aufsätze |
author-letter |
Kiszely, M. |
doi_str_mv |
10.1007/BF03325634 |
title_sort |
attenuation of coda waves in hungary |
title_auth |
Attenuation of Coda Waves in Hungary |
abstract |
Abstract Microearthquake codas from 19 shallow depth local events have been analysed in Hungary. We estimate coda attenuation Qc in the frequency range 6 to 24 Hz used Sato’s (1977) single scattering model for a coda window of 12.5±2.5 s beginning at twice the S-wave travel time. Travel times were between 2–23 sec. The stations showed similar values of Qc which were about 400 at 6 Hz and about 1400 at 24 Hz. The Qc values in Hungary indicate moderate tectonic characteristic. © Akadémiai Kiadó 2000 |
abstractGer |
Abstract Microearthquake codas from 19 shallow depth local events have been analysed in Hungary. We estimate coda attenuation Qc in the frequency range 6 to 24 Hz used Sato’s (1977) single scattering model for a coda window of 12.5±2.5 s beginning at twice the S-wave travel time. Travel times were between 2–23 sec. The stations showed similar values of Qc which were about 400 at 6 Hz and about 1400 at 24 Hz. The Qc values in Hungary indicate moderate tectonic characteristic. © Akadémiai Kiadó 2000 |
abstract_unstemmed |
Abstract Microearthquake codas from 19 shallow depth local events have been analysed in Hungary. We estimate coda attenuation Qc in the frequency range 6 to 24 Hz used Sato’s (1977) single scattering model for a coda window of 12.5±2.5 s beginning at twice the S-wave travel time. Travel times were between 2–23 sec. The stations showed similar values of Qc which were about 400 at 6 Hz and about 1400 at 24 Hz. The Qc values in Hungary indicate moderate tectonic characteristic. © Akadémiai Kiadó 2000 |
collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 |
container_issue |
4 |
title_short |
Attenuation of Coda Waves in Hungary |
url |
https://dx.doi.org/10.1007/BF03325634 |
remote_bool |
true |
ppnlink |
364470852 |
mediatype_str_mv |
c |
isOA_txt |
false |
hochschulschrift_bool |
false |
doi_str |
10.1007/BF03325634 |
up_date |
2024-07-03T21:18:12.127Z |
_version_ |
1803594227649609728 |
fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR037131869</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230328170043.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201007s2000 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/BF03325634</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR037131869</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)BF03325634-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Kiszely, M.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Attenuation of Coda Waves in Hungary</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2000</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Akadémiai Kiadó 2000</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Microearthquake codas from 19 shallow depth local events have been analysed in Hungary. We estimate coda attenuation Qc in the frequency range 6 to 24 Hz used Sato’s (1977) single scattering model for a coda window of 12.5±2.5 s beginning at twice the S-wave travel time. Travel times were between 2–23 sec. The stations showed similar values of Qc which were about 400 at 6 Hz and about 1400 at 24 Hz. The Qc values in Hungary indicate moderate tectonic characteristic.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">coda waves</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">coda waves</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">seismic quality factor</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Acta geodaetica et geophysica Hungarica</subfield><subfield code="d">Budapest : Akad. Kiadó, 1997</subfield><subfield code="g">35(2000), 4 vom: Dez., Seite 465-473</subfield><subfield code="w">(DE-627)364470852</subfield><subfield code="w">(DE-600)2110468-2</subfield><subfield code="x">1587-1037</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:35</subfield><subfield code="g">year:2000</subfield><subfield code="g">number:4</subfield><subfield code="g">month:12</subfield><subfield code="g">pages:465-473</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://dx.doi.org/10.1007/BF03325634</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_SPRINGER</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_39</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_69</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_74</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_90</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_100</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_120</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_152</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_161</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_171</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_187</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_224</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_250</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_281</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_285</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_293</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_702</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">35</subfield><subfield code="j">2000</subfield><subfield code="e">4</subfield><subfield code="c">12</subfield><subfield code="h">465-473</subfield></datafield></record></collection>
|
score |
7.401726 |