From 68210d4e55e4f5fca658c7002c13ab5ac5abd7a1 Mon Sep 17 00:00:00 2001 From: LanaTodorovic93 Date: Mon, 10 Mar 2025 09:51:48 +0100 Subject: [PATCH] Update max shaking info. --- Europe/Serbia/20101103_M5.52_Kraljevo/README.md | 2 +- 1 file changed, 1 insertion(+), 1 deletion(-) diff --git a/Europe/Serbia/20101103_M5.52_Kraljevo/README.md b/Europe/Serbia/20101103_M5.52_Kraljevo/README.md index 2a22ac5..68447ef 100644 --- a/Europe/Serbia/20101103_M5.52_Kraljevo/README.md +++ b/Europe/Serbia/20101103_M5.52_Kraljevo/README.md @@ -36,7 +36,7 @@ The `2010 Serbia earthquake` struck on November 3, 2010, at 01:56 local time, ju ## Estimated and observed ground shaking -The folder [OpenQuake_gmfs](./OpenQuake_gmfs/) contains the input files required to generate ground motion fields, considering different rupture solutions and conditioning the ground shaking to the recording stations for the event, where available. The figures below present an example of the results, illustrating the median ground motion fields with and without conditioning. These results are based on the rupture and ground motion model that demonstrates the lowest nominal bias. The maximum recorded Peak Ground Acceleration (PGA) was [insert value here], observed at [insert location here]. If no seismic station data were available for the event, the generated ground motion fields are shown without conditioning to recording stations, as illustrated in the figures. +The folder [OpenQuake_gmfs](./OpenQuake_gmfs/) contains the input files required to generate ground motion fields, considering different rupture solutions and conditioning the ground shaking to the recording stations for the event, where available. The figures below present an example of the results, illustrating the median ground motion fields with and without conditioning. These results are based on the rupture and ground motion model that demonstrates the lowest nominal bias. The maximum recorded Peak Ground Acceleration (PGA) was 0.164 g, observed in Cacak. If no seismic station data were available for the event, the generated ground motion fields are shown without conditioning to recording stations, as illustrated in the figures.