1986
DOI: 10.1193/1.1585311
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The Chile Earthquake of March 3, 1985—Introduction

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Cited by 13 publications
(3 citation statements)
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“…For all selected subduction earthquakes, there is a significant reduction in the potential for collapse in structural wall buildings from that in frame buildings. These results are consistent with the observed building response in 1985 Chile (Wyllie et al 1986, Wood 1991), 1985Mexico (Noreña et al 1989), 2007Peru (INDECI 2009, 2010 Chile (Lagos et al 2012, Wallace et al 2012, 2011 Great East Japan (Miyamoto et al 2012), and 2016Ecuador (GEER Association 2016.…”
Section: Results Of Evaluation Of I D For Subduction Earthquakes (Group Ii Ground Motions)supporting
confidence: 81%
See 1 more Smart Citation
“…For all selected subduction earthquakes, there is a significant reduction in the potential for collapse in structural wall buildings from that in frame buildings. These results are consistent with the observed building response in 1985 Chile (Wyllie et al 1986, Wood 1991), 1985Mexico (Noreña et al 1989), 2007Peru (INDECI 2009, 2010 Chile (Lagos et al 2012, Wallace et al 2012, 2011 Great East Japan (Miyamoto et al 2012), and 2016Ecuador (GEER Association 2016.…”
Section: Results Of Evaluation Of I D For Subduction Earthquakes (Group Ii Ground Motions)supporting
confidence: 81%
“…The selected accelerograms were recorded in locations where building damage occurred. These were the 1985 Chile earthquake (Wyllie et al 1986, Wood 1991, the 1994 Northridge earthquake (Holmes and Somers 1996), the 1995 Kobe earthquake (EERI 1995), the 1999 Chi-Chi earthquake (Uzarski and Arnold 2001), the 1999 Duzce earthquake (Anderson et al 2000), (INDECI 2009), the 1985 Mexico earthquake (Noreña et al 1989), the 2010 Maule earthquake (Lagos et al 2012, Wallace et al 2012, the 2011 Great East Japan earthquake (Miyamoto et al 2012), the 2011 Christchurch earthquake (Kam and Pampanin 2011), and the 2016 Ecuador earthquake (GEER Association 2016). The last accelerogram was not included in the previous study by Rodriguez (2015).…”
Section: Earthquake Ground Motionsmentioning
confidence: 99%
“…In reality, however, seismic site response is influenced not only by the local (i.e., 1-D) site conditions but also by the three-dimensional (3-D) environment, such as bedrock slope, geometry of the soft soil layers, and topographical irregularities. One of the main pieces of empirical evidence of 3-D amplification effects comes both from the concentration of structural damage near topographic irregularities (such as a hill, a ridge, a canyon, a cliff, or a slope) as observed during past and recent earthquakes (e.g., Wyllie andBolt 1986, Çelebi 1987) and instrumental data (e.g., Davis and West 1973), clearly indicating that surficial morphology and topography can affect the propagation of seismic motion, which, in turn, can lead to significantly modified levels of ground shaking because of scattering, diffraction, or trapping of waves.…”
Section: Introductionmentioning
confidence: 99%