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A Strong-Motion Network in the Lower Rhine Embayment (SeFoNiB), Germany

2007; Seismological Society of America; Volume: 78; Issue: 5 Linguagem: Inglês

10.1785/gssrl.78.5.502

1938-2057

K.-G. Hinzen, Claus Fleischer,

Seismic Waves and Analysis

Research Article| September 01, 2007 A Strong-Motion Network in the Lower Rhine Embayment (SeFoNiB), Germany Klaus-G. Hinzen; Klaus-G. Hinzen Earthquake Geology Division Institute for Geology and Mineralogy Cologne University Vinzenz-Pallotti-St. 26 51429 Bergisch Gladbach, Germany hinzen@uni-koeln.de (K.-G. H.) Search for other works by this author on: GSW Google Scholar C. Fleischer C. Fleischer Earthquake Geology Division Institute for Geology and Mineralogy Cologne University Vinzenz-Pallotti-St. 26 51429 Bergisch Gladbach, Germany hinzen@uni-koeln.de (K.-G. H.) Search for other works by this author on: GSW Google Scholar Seismological Research Letters (2007) 78 (5): 502–511. https://doi.org/10.1785/gssrl.78.5.502 Article history first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Klaus-G. Hinzen, C. Fleischer; A Strong-Motion Network in the Lower Rhine Embayment (SeFoNiB), Germany. Seismological Research Letters 2007;; 78 (5): 502–511. doi: https://doi.org/10.1785/gssrl.78.5.502 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietySeismological Research Letters Search Advanced Search More than 20 damaging earthquakes have happened in the past 300 years in the Lower Rhine Embayment (LRE), a young sedimentary basin with typical intraplate seismicity (Hinzen and Reamer forthcoming). The most recent damaging earthquakes were those of Alsdorf, 22 July 2002 (M 4.3; Hinzen 2005) and Roermond, 13 April 1992 (M 5.4; Camelbeeck et al. 1994). The latter had a hypocentral depth of more than 15 km and a sedimentary cover of more than 1 km in the source area. These conditions helped to constrain the damages to a moderate level of approximately... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.