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Table 2 The acceleration (g) and displacement (cm) were recorded in different earthquake stations [28]

From: The displacement mechanism of the cracked rock – a seismic design and prediction study using XFEM and ANNs

Station

Distance (km) to the epicenter

Acceleration (g) peak

Displacement (cm)

90°

360°

90°

360°

Town Hall Siteia Lasithi Crete

NOA/RUB/GEOFON Karpathos Greece

13.6

91.2

-0.0894

0.0108

-0.3432

-0.0187

0.1953

-0.0268

0.7744

0.5171

4.4096

-0.5099

-2.1362

-0.7366

Irakleio Crete Greece

108.5

0.0121

-0.0279

-0.0245

0.3477

0.7502

-0.7249

Sivas Crete Greece

133.0

0.0031

0.0077

0.0057

0.2532

0.2642

0.3047

Thera Santorini Greece

154.7

0.0064

0.0122

0.0112

0.136

0.4889

-0.3152

Mandraki Nisyros Greece

176.0

-0.0044

0.0075

0.0045

-0.2067

-0.3386

0.3301

Town Hall Rhodes Rhodes Island

226.1

0.0032

0.0054

0.0052

-0.2145

0.451

0.4385