2018
DOI: 10.1016/j.soildyn.2018.01.032
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Ground motion processing and observations for the near-field accelerograms from the 2015 Gorkha, Nepal earthquake

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Cited by 3 publications
(2 citation statements)
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“…This is located at an epicentral distance of 155.1 km, but only at 42.7 km from the fault, and presented a PGA of 0.269 g. Moreover, the importance of the distance to the ruptured fault plane can also be observed in other earthquakes, or through the results of stochastic simulations [44]. This type of comparison was also carried out by another author for Nepal, in the context of the Gorkha earthquake (Mw = 7.8) that occurred on 25 April 2015 [96]. This means that the distance to the fault plane rupture seems to be a better choice, regarding accuracy issues, when selecting a GMPE to deal with high-magnitude earthquake events.…”
Section: Resultsmentioning
confidence: 79%
“…This is located at an epicentral distance of 155.1 km, but only at 42.7 km from the fault, and presented a PGA of 0.269 g. Moreover, the importance of the distance to the ruptured fault plane can also be observed in other earthquakes, or through the results of stochastic simulations [44]. This type of comparison was also carried out by another author for Nepal, in the context of the Gorkha earthquake (Mw = 7.8) that occurred on 25 April 2015 [96]. This means that the distance to the fault plane rupture seems to be a better choice, regarding accuracy issues, when selecting a GMPE to deal with high-magnitude earthquake events.…”
Section: Resultsmentioning
confidence: 79%
“…This method requires the zero-padded portion to obtain accurate velocity and displacement waveforms when integrating from zero. Consequently, it may need more analysis runtime for structural dynamic analysis [12].…”
Section: Introductionmentioning
confidence: 99%