A comparison of proxies for seismic site conditions and amplification for the large urban area of Santiago de Chile
Situated in an active tectonic region, Santiago de Chile, the countryś capital with more than six million inhabitants, faces tremendous earthquake hazard. Macroseismic data for the 1985 Valparaiso and the 2010 Maule events show large variations in the distribution of damage to buildings within short...
Ausführliche Beschreibung
Autor*in: |
Pilz, Marco [verfasserIn] Zschau, Jochen [betreuer] |
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Hochschulschrift: |
Potsdam, Universität Potsdam, Diss., 2011 |
Format: |
E-Book |
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Sprache: |
Englisch |
Erschienen: |
Potsdam: Universitätsbibliothek der Universität Potsdam ; 2010 |
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Formangabe: |
Hochschulschrift |
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Umfang: |
Online-Ressource |
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Links: |
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DOI / URN: |
urn:nbn:de:kobv:517-opus-52961 |
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Katalog-ID: |
667957928 |
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245 | 1 | 0 | |a A comparison of proxies for seismic site conditions and amplification for the large urban area of Santiago de Chile |c Marco Pilz. Betreuer: Jochen Zschau |
246 | 1 | |i Nebentitel |a Ein Vergleich seismischer Parameter für die Standort- und Verstärkungsabschätzung im Stadtgebiet von Santiago de Chile | |
246 | 3 | 3 | |a Ein Vergleich seismischer Parameter für die Standort- und Verstärkungsabschätzung im Stadtgebiet von Santiago de Chile |
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520 | |a Situated in an active tectonic region, Santiago de Chile, the countryś capital with more than six million inhabitants, faces tremendous earthquake hazard. Macroseismic data for the 1985 Valparaiso and the 2010 Maule events show large variations in the distribution of damage to buildings within short distances indicating strong influence of local sediments and the shape of the sediment-bedrock interface on ground motion. Therefore, a temporary seismic network was installed in the urban area for recording earthquake activity, and a study was carried out aiming to estimate site amplification derived from earthquake data and ambient noise. The analysis of earthquake data shows significant dependence on the local geological structure with regards to amplitude and duration. Moreover, the analysis of noise spectral ratios shows that they can provide a lower bound in amplitude for site amplification and, since no variability in terms of time and amplitude is observed, that it is possible to map the fundamental resonance frequency of the soil for a 26 km x 12 km area in the northern part of the Santiago de Chile basin... | ||
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11,O09 dnb 1014619106 DE-101 urn:nbn:de:kobv:517-opus-52961 urn (DE-627)667957928 (DE-599)DNB1014619106 (OCoLC)838127660 DE-627 ger DE-627 rakwb eng XA-DE-BB a OCLC 550 a DNB 16,13 ssgn Pilz, Marco verfasserin aut A comparison of proxies for seismic site conditions and amplification for the large urban area of Santiago de Chile Marco Pilz. Betreuer: Jochen Zschau Nebentitel Ein Vergleich seismischer Parameter für die Standort- und Verstärkungsabschätzung im Stadtgebiet von Santiago de Chile Ein Vergleich seismischer Parameter für die Standort- und Verstärkungsabschätzung im Stadtgebiet von Santiago de Chile Potsdam Universitätsbibliothek der Universität Potsdam 2010 Online-Ressource Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Potsdam, Universität Potsdam, Diss., 2011 Situated in an active tectonic region, Santiago de Chile, the countryś capital with more than six million inhabitants, faces tremendous earthquake hazard. Macroseismic data for the 1985 Valparaiso and the 2010 Maule events show large variations in the distribution of damage to buildings within short distances indicating strong influence of local sediments and the shape of the sediment-bedrock interface on ground motion. Therefore, a temporary seismic network was installed in the urban area for recording earthquake activity, and a study was carried out aiming to estimate site amplification derived from earthquake data and ambient noise. The analysis of earthquake data shows significant dependence on the local geological structure with regards to amplitude and duration. Moreover, the analysis of noise spectral ratios shows that they can provide a lower bound in amplitude for site amplification and, since no variability in terms of time and amplitude is observed, that it is possible to map the fundamental resonance frequency of the soil for a 26 km x 12 km area in the northern part of the Santiago de Chile basin... Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Zschau, Jochen betreuer oth Potsdam uvp http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 Resolving-System Volltext http://d-nb.info/1014619106/34 Langzeitarchivierung Nationalbibliothek Volltext http://opus.kobv.de/ubp/volltexte/2011/5296 Verlag kostenfrei Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GEO SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 BO 045F a 20 01 0084 1268153591 x 08-09-11 21 01 0046 1268162248 z 08-09-11 22 01 0018 1268170461 SUBolrd xu 08-09-11 23 01 0830 1268177652 olr-d x 08-09-11 30 01 0104 1268184152 z 08-09-11 40 01 0007 1268192627 ksn 26-03-12 60 01 0705 1268201383 OLRD z 08-09-11 63 01 3401 1595741860 ORD x 21-01-16 70 01 0089 1268218499 zdo 08-09-11 105 01 0841 1596554983 z 21-01-16 110 01 3110 1268209686 x 08-09-11 132 01 0959 1498076939 OLR-DISS x 12-08-14 151 01 0546 3594156710 OLR-ODISS z 13-02-20 161 01 0960 1597522570 ORD x 28-01-16 293 01 3293 1597983462 ORD xf 28-01-16 370 01 4370 1268212091 x 08-09-11 20 01 0084 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 21 01 0046 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 22 01 0018 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 23 01 0830 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 30 01 0104 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 40 01 0007 http://webdoc.sub.gwdg.de/ebook/dissts/Potsdam/Pilz2010.pdf LF 60 01 0705 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 LF 70 01 0089 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 105 01 0841 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 110 01 3110 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 132 01 0959 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 161 01 0960 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 293 01 3293 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 370 01 4370 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 40 00 DE-7 00 (DE-627)623604957 TOH 700 Erdbebenwirkungen und Erdbeben-Engineering {Geophysik} 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2011-09-08:10:35:52 40 01 0007 2011-12 9 v |
spelling |
11,O09 dnb 1014619106 DE-101 urn:nbn:de:kobv:517-opus-52961 urn (DE-627)667957928 (DE-599)DNB1014619106 (OCoLC)838127660 DE-627 ger DE-627 rakwb eng XA-DE-BB a OCLC 550 a DNB 16,13 ssgn Pilz, Marco verfasserin aut A comparison of proxies for seismic site conditions and amplification for the large urban area of Santiago de Chile Marco Pilz. Betreuer: Jochen Zschau Nebentitel Ein Vergleich seismischer Parameter für die Standort- und Verstärkungsabschätzung im Stadtgebiet von Santiago de Chile Ein Vergleich seismischer Parameter für die Standort- und Verstärkungsabschätzung im Stadtgebiet von Santiago de Chile Potsdam Universitätsbibliothek der Universität Potsdam 2010 Online-Ressource Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Potsdam, Universität Potsdam, Diss., 2011 Situated in an active tectonic region, Santiago de Chile, the countryś capital with more than six million inhabitants, faces tremendous earthquake hazard. Macroseismic data for the 1985 Valparaiso and the 2010 Maule events show large variations in the distribution of damage to buildings within short distances indicating strong influence of local sediments and the shape of the sediment-bedrock interface on ground motion. Therefore, a temporary seismic network was installed in the urban area for recording earthquake activity, and a study was carried out aiming to estimate site amplification derived from earthquake data and ambient noise. The analysis of earthquake data shows significant dependence on the local geological structure with regards to amplitude and duration. Moreover, the analysis of noise spectral ratios shows that they can provide a lower bound in amplitude for site amplification and, since no variability in terms of time and amplitude is observed, that it is possible to map the fundamental resonance frequency of the soil for a 26 km x 12 km area in the northern part of the Santiago de Chile basin... Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Zschau, Jochen betreuer oth Potsdam uvp http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 Resolving-System Volltext http://d-nb.info/1014619106/34 Langzeitarchivierung Nationalbibliothek Volltext http://opus.kobv.de/ubp/volltexte/2011/5296 Verlag kostenfrei Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GEO SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 BO 045F a 20 01 0084 1268153591 x 08-09-11 21 01 0046 1268162248 z 08-09-11 22 01 0018 1268170461 SUBolrd xu 08-09-11 23 01 0830 1268177652 olr-d x 08-09-11 30 01 0104 1268184152 z 08-09-11 40 01 0007 1268192627 ksn 26-03-12 60 01 0705 1268201383 OLRD z 08-09-11 63 01 3401 1595741860 ORD x 21-01-16 70 01 0089 1268218499 zdo 08-09-11 105 01 0841 1596554983 z 21-01-16 110 01 3110 1268209686 x 08-09-11 132 01 0959 1498076939 OLR-DISS x 12-08-14 151 01 0546 3594156710 OLR-ODISS z 13-02-20 161 01 0960 1597522570 ORD x 28-01-16 293 01 3293 1597983462 ORD xf 28-01-16 370 01 4370 1268212091 x 08-09-11 20 01 0084 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 21 01 0046 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 22 01 0018 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 23 01 0830 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 30 01 0104 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 40 01 0007 http://webdoc.sub.gwdg.de/ebook/dissts/Potsdam/Pilz2010.pdf LF 60 01 0705 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 LF 70 01 0089 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 105 01 0841 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 110 01 3110 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 132 01 0959 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 161 01 0960 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 293 01 3293 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 370 01 4370 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 40 00 DE-7 00 (DE-627)623604957 TOH 700 Erdbebenwirkungen und Erdbeben-Engineering {Geophysik} 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2011-09-08:10:35:52 40 01 0007 2011-12 9 v |
allfields_unstemmed |
11,O09 dnb 1014619106 DE-101 urn:nbn:de:kobv:517-opus-52961 urn (DE-627)667957928 (DE-599)DNB1014619106 (OCoLC)838127660 DE-627 ger DE-627 rakwb eng XA-DE-BB a OCLC 550 a DNB 16,13 ssgn Pilz, Marco verfasserin aut A comparison of proxies for seismic site conditions and amplification for the large urban area of Santiago de Chile Marco Pilz. Betreuer: Jochen Zschau Nebentitel Ein Vergleich seismischer Parameter für die Standort- und Verstärkungsabschätzung im Stadtgebiet von Santiago de Chile Ein Vergleich seismischer Parameter für die Standort- und Verstärkungsabschätzung im Stadtgebiet von Santiago de Chile Potsdam Universitätsbibliothek der Universität Potsdam 2010 Online-Ressource Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Potsdam, Universität Potsdam, Diss., 2011 Situated in an active tectonic region, Santiago de Chile, the countryś capital with more than six million inhabitants, faces tremendous earthquake hazard. Macroseismic data for the 1985 Valparaiso and the 2010 Maule events show large variations in the distribution of damage to buildings within short distances indicating strong influence of local sediments and the shape of the sediment-bedrock interface on ground motion. Therefore, a temporary seismic network was installed in the urban area for recording earthquake activity, and a study was carried out aiming to estimate site amplification derived from earthquake data and ambient noise. The analysis of earthquake data shows significant dependence on the local geological structure with regards to amplitude and duration. Moreover, the analysis of noise spectral ratios shows that they can provide a lower bound in amplitude for site amplification and, since no variability in terms of time and amplitude is observed, that it is possible to map the fundamental resonance frequency of the soil for a 26 km x 12 km area in the northern part of the Santiago de Chile basin... Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Zschau, Jochen betreuer oth Potsdam uvp http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 Resolving-System Volltext http://d-nb.info/1014619106/34 Langzeitarchivierung Nationalbibliothek Volltext http://opus.kobv.de/ubp/volltexte/2011/5296 Verlag kostenfrei Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GEO SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 BO 045F a 20 01 0084 1268153591 x 08-09-11 21 01 0046 1268162248 z 08-09-11 22 01 0018 1268170461 SUBolrd xu 08-09-11 23 01 0830 1268177652 olr-d x 08-09-11 30 01 0104 1268184152 z 08-09-11 40 01 0007 1268192627 ksn 26-03-12 60 01 0705 1268201383 OLRD z 08-09-11 63 01 3401 1595741860 ORD x 21-01-16 70 01 0089 1268218499 zdo 08-09-11 105 01 0841 1596554983 z 21-01-16 110 01 3110 1268209686 x 08-09-11 132 01 0959 1498076939 OLR-DISS x 12-08-14 151 01 0546 3594156710 OLR-ODISS z 13-02-20 161 01 0960 1597522570 ORD x 28-01-16 293 01 3293 1597983462 ORD xf 28-01-16 370 01 4370 1268212091 x 08-09-11 20 01 0084 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 21 01 0046 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 22 01 0018 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 23 01 0830 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 30 01 0104 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 40 01 0007 http://webdoc.sub.gwdg.de/ebook/dissts/Potsdam/Pilz2010.pdf LF 60 01 0705 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 LF 70 01 0089 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 105 01 0841 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 110 01 3110 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 132 01 0959 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 161 01 0960 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 293 01 3293 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 370 01 4370 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 40 00 DE-7 00 (DE-627)623604957 TOH 700 Erdbebenwirkungen und Erdbeben-Engineering {Geophysik} 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2011-09-08:10:35:52 40 01 0007 2011-12 9 v |
allfieldsGer |
11,O09 dnb 1014619106 DE-101 urn:nbn:de:kobv:517-opus-52961 urn (DE-627)667957928 (DE-599)DNB1014619106 (OCoLC)838127660 DE-627 ger DE-627 rakwb eng XA-DE-BB a OCLC 550 a DNB 16,13 ssgn Pilz, Marco verfasserin aut A comparison of proxies for seismic site conditions and amplification for the large urban area of Santiago de Chile Marco Pilz. Betreuer: Jochen Zschau Nebentitel Ein Vergleich seismischer Parameter für die Standort- und Verstärkungsabschätzung im Stadtgebiet von Santiago de Chile Ein Vergleich seismischer Parameter für die Standort- und Verstärkungsabschätzung im Stadtgebiet von Santiago de Chile Potsdam Universitätsbibliothek der Universität Potsdam 2010 Online-Ressource Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Potsdam, Universität Potsdam, Diss., 2011 Situated in an active tectonic region, Santiago de Chile, the countryś capital with more than six million inhabitants, faces tremendous earthquake hazard. Macroseismic data for the 1985 Valparaiso and the 2010 Maule events show large variations in the distribution of damage to buildings within short distances indicating strong influence of local sediments and the shape of the sediment-bedrock interface on ground motion. Therefore, a temporary seismic network was installed in the urban area for recording earthquake activity, and a study was carried out aiming to estimate site amplification derived from earthquake data and ambient noise. The analysis of earthquake data shows significant dependence on the local geological structure with regards to amplitude and duration. Moreover, the analysis of noise spectral ratios shows that they can provide a lower bound in amplitude for site amplification and, since no variability in terms of time and amplitude is observed, that it is possible to map the fundamental resonance frequency of the soil for a 26 km x 12 km area in the northern part of the Santiago de Chile basin... Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Zschau, Jochen betreuer oth Potsdam uvp http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 Resolving-System Volltext http://d-nb.info/1014619106/34 Langzeitarchivierung Nationalbibliothek Volltext http://opus.kobv.de/ubp/volltexte/2011/5296 Verlag kostenfrei Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GEO SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 BO 045F a 20 01 0084 1268153591 x 08-09-11 21 01 0046 1268162248 z 08-09-11 22 01 0018 1268170461 SUBolrd xu 08-09-11 23 01 0830 1268177652 olr-d x 08-09-11 30 01 0104 1268184152 z 08-09-11 40 01 0007 1268192627 ksn 26-03-12 60 01 0705 1268201383 OLRD z 08-09-11 63 01 3401 1595741860 ORD x 21-01-16 70 01 0089 1268218499 zdo 08-09-11 105 01 0841 1596554983 z 21-01-16 110 01 3110 1268209686 x 08-09-11 132 01 0959 1498076939 OLR-DISS x 12-08-14 151 01 0546 3594156710 OLR-ODISS z 13-02-20 161 01 0960 1597522570 ORD x 28-01-16 293 01 3293 1597983462 ORD xf 28-01-16 370 01 4370 1268212091 x 08-09-11 20 01 0084 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 21 01 0046 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 22 01 0018 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 23 01 0830 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 30 01 0104 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 40 01 0007 http://webdoc.sub.gwdg.de/ebook/dissts/Potsdam/Pilz2010.pdf LF 60 01 0705 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 LF 70 01 0089 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 105 01 0841 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 110 01 3110 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 132 01 0959 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 161 01 0960 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 293 01 3293 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 370 01 4370 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 40 00 DE-7 00 (DE-627)623604957 TOH 700 Erdbebenwirkungen und Erdbeben-Engineering {Geophysik} 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2011-09-08:10:35:52 40 01 0007 2011-12 9 v |
allfieldsSound |
11,O09 dnb 1014619106 DE-101 urn:nbn:de:kobv:517-opus-52961 urn (DE-627)667957928 (DE-599)DNB1014619106 (OCoLC)838127660 DE-627 ger DE-627 rakwb eng XA-DE-BB a OCLC 550 a DNB 16,13 ssgn Pilz, Marco verfasserin aut A comparison of proxies for seismic site conditions and amplification for the large urban area of Santiago de Chile Marco Pilz. Betreuer: Jochen Zschau Nebentitel Ein Vergleich seismischer Parameter für die Standort- und Verstärkungsabschätzung im Stadtgebiet von Santiago de Chile Ein Vergleich seismischer Parameter für die Standort- und Verstärkungsabschätzung im Stadtgebiet von Santiago de Chile Potsdam Universitätsbibliothek der Universität Potsdam 2010 Online-Ressource Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Potsdam, Universität Potsdam, Diss., 2011 Situated in an active tectonic region, Santiago de Chile, the countryś capital with more than six million inhabitants, faces tremendous earthquake hazard. Macroseismic data for the 1985 Valparaiso and the 2010 Maule events show large variations in the distribution of damage to buildings within short distances indicating strong influence of local sediments and the shape of the sediment-bedrock interface on ground motion. Therefore, a temporary seismic network was installed in the urban area for recording earthquake activity, and a study was carried out aiming to estimate site amplification derived from earthquake data and ambient noise. The analysis of earthquake data shows significant dependence on the local geological structure with regards to amplitude and duration. Moreover, the analysis of noise spectral ratios shows that they can provide a lower bound in amplitude for site amplification and, since no variability in terms of time and amplitude is observed, that it is possible to map the fundamental resonance frequency of the soil for a 26 km x 12 km area in the northern part of the Santiago de Chile basin... Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Zschau, Jochen betreuer oth Potsdam uvp http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 Resolving-System Volltext http://d-nb.info/1014619106/34 Langzeitarchivierung Nationalbibliothek Volltext http://opus.kobv.de/ubp/volltexte/2011/5296 Verlag kostenfrei Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GEO SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 BO 045F a 20 01 0084 1268153591 x 08-09-11 21 01 0046 1268162248 z 08-09-11 22 01 0018 1268170461 SUBolrd xu 08-09-11 23 01 0830 1268177652 olr-d x 08-09-11 30 01 0104 1268184152 z 08-09-11 40 01 0007 1268192627 ksn 26-03-12 60 01 0705 1268201383 OLRD z 08-09-11 63 01 3401 1595741860 ORD x 21-01-16 70 01 0089 1268218499 zdo 08-09-11 105 01 0841 1596554983 z 21-01-16 110 01 3110 1268209686 x 08-09-11 132 01 0959 1498076939 OLR-DISS x 12-08-14 151 01 0546 3594156710 OLR-ODISS z 13-02-20 161 01 0960 1597522570 ORD x 28-01-16 293 01 3293 1597983462 ORD xf 28-01-16 370 01 4370 1268212091 x 08-09-11 20 01 0084 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 21 01 0046 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 22 01 0018 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 23 01 0830 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 30 01 0104 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 40 01 0007 http://webdoc.sub.gwdg.de/ebook/dissts/Potsdam/Pilz2010.pdf LF 60 01 0705 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 LF 70 01 0089 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 105 01 0841 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 110 01 3110 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 132 01 0959 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 161 01 0960 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 293 01 3293 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 370 01 4370 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-52961 40 00 DE-7 00 (DE-627)623604957 TOH 700 Erdbebenwirkungen und Erdbeben-Engineering {Geophysik} 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2011-09-08:10:35:52 40 01 0007 2011-12 9 v |
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Pilz, Marco |
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Pilz, Marco ddc a ddc 550 ssgn 16,13 A comparison of proxies for seismic site conditions and amplification for the large urban area of Santiago de Chile |
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550 - Earth sciences |
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a OCLC 550 a DNB 16,13 ssgn A comparison of proxies for seismic site conditions and amplification for the large urban area of Santiago de Chile Marco Pilz. Betreuer: Jochen Zschau |
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A comparison of proxies for seismic site conditions and amplification for the large urban area of Santiago de Chile Marco Pilz. Betreuer: Jochen Zschau |
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a comparison of proxies for seismic site conditions and amplification for the large urban area of santiago de chile |
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A comparison of proxies for seismic site conditions and amplification for the large urban area of Santiago de Chile |
abstract |
Situated in an active tectonic region, Santiago de Chile, the countryś capital with more than six million inhabitants, faces tremendous earthquake hazard. Macroseismic data for the 1985 Valparaiso and the 2010 Maule events show large variations in the distribution of damage to buildings within short distances indicating strong influence of local sediments and the shape of the sediment-bedrock interface on ground motion. Therefore, a temporary seismic network was installed in the urban area for recording earthquake activity, and a study was carried out aiming to estimate site amplification derived from earthquake data and ambient noise. The analysis of earthquake data shows significant dependence on the local geological structure with regards to amplitude and duration. Moreover, the analysis of noise spectral ratios shows that they can provide a lower bound in amplitude for site amplification and, since no variability in terms of time and amplitude is observed, that it is possible to map the fundamental resonance frequency of the soil for a 26 km x 12 km area in the northern part of the Santiago de Chile basin... |
abstractGer |
Situated in an active tectonic region, Santiago de Chile, the countryś capital with more than six million inhabitants, faces tremendous earthquake hazard. Macroseismic data for the 1985 Valparaiso and the 2010 Maule events show large variations in the distribution of damage to buildings within short distances indicating strong influence of local sediments and the shape of the sediment-bedrock interface on ground motion. Therefore, a temporary seismic network was installed in the urban area for recording earthquake activity, and a study was carried out aiming to estimate site amplification derived from earthquake data and ambient noise. The analysis of earthquake data shows significant dependence on the local geological structure with regards to amplitude and duration. Moreover, the analysis of noise spectral ratios shows that they can provide a lower bound in amplitude for site amplification and, since no variability in terms of time and amplitude is observed, that it is possible to map the fundamental resonance frequency of the soil for a 26 km x 12 km area in the northern part of the Santiago de Chile basin... |
abstract_unstemmed |
Situated in an active tectonic region, Santiago de Chile, the countryś capital with more than six million inhabitants, faces tremendous earthquake hazard. Macroseismic data for the 1985 Valparaiso and the 2010 Maule events show large variations in the distribution of damage to buildings within short distances indicating strong influence of local sediments and the shape of the sediment-bedrock interface on ground motion. Therefore, a temporary seismic network was installed in the urban area for recording earthquake activity, and a study was carried out aiming to estimate site amplification derived from earthquake data and ambient noise. The analysis of earthquake data shows significant dependence on the local geological structure with regards to amplitude and duration. Moreover, the analysis of noise spectral ratios shows that they can provide a lower bound in amplitude for site amplification and, since no variability in terms of time and amplitude is observed, that it is possible to map the fundamental resonance frequency of the soil for a 26 km x 12 km area in the northern part of the Santiago de Chile basin... |
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A comparison of proxies for seismic site conditions and amplification for the large urban area of Santiago de Chile |
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