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. 2020 May 6;10:7636. doi: 10.1038/s41598-020-64560-w

Table 1.

Seismological properties of the case studies (USGS).

Name Bam Earthquake Sichuan-Gansu border earthquake Elazig earthquake Banepa earthquake
Country Iran China Turkey Nepal
Regional geology Alluvial fans and argillaceous sandstones Precambrian granitic rocks, sandstone and limestone Anatolian Metamorphic Massifs and Basalt

Basement rock, gneiss, quartzite, phyllite

and limestone

Time (UTC) 01:56:52 09:49:17 02:32:34 06:15:22
Date 26 December 2003 5 August 2008 8 March 2010 25 April 2015
Magnitude 6.6 6.2 6.1 6.1
Depth (USGS) (km) 8.5 6 12 10
Latitude, Longitude

28.995°N

58.311°E

32.756°N

105.494°E

38.864°N

39.986°E

27.628°N

85.540°E

Mercalli intensity scale IX (Violent) VII (Very Strong) VIII (Severe) VII (Very Strong)
Name of the Fault The Bam Fault The Longman Shan Fault The East Anatolian fault The Gorkha fault
Fault Plate Solution Strike-slip Thrust Strike-slip Strike-slip
Reasons for the earthquake Combination of a small component of reverse-motion and strike-slip motion on the fault As the Indian plate moves northward, it collides with Eurasian plate and continues moving forward into China Displacement of left-lateral and right-lateral strike-slip on a northeast and northwest striking slip of the Anatolian fault Collision of Indo-Australian and Asian plates