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Table 3 Characteristics of the earthquakes for which focal mechanism was determined

From: Seismicity induced during the development of the Rittershoffen geothermal field, France

PeriodOrigin timeEasting (m)Northing (m)Depth (m TVD MSL)MlvNPOLDip (°)Strike (°)Rake (°)
Thermal stimulation2013-04-25 01:59:332,447,7821,010,27219600.315
Thermal stimulation2013-04-25 03:38:002,447,6491,010,38019010.236
Hydraulic stimulation2013-06-27 23:25:592,447,6361,010,37219930.691480199− 3
Hydraulic stimulation2013-06-28 01:45:442,447,6241,010,31218600.5412802023
July burst2013-07-02 04:53:522,448,2431,010,44820231.21148729− 10
July burst2013-07-02 05:11:182,448,1131,010,47314801.311281188− 5
GRT-2 drilling2014-05-26 13:33:252,448,4951,010,58715170.011887200− 9
GRT-2 drilling2014-05-26 14:18:292,448,4561,010,53216561.0231802839
  1. The column NPOL gives the number of P-wave polarities used to determine the focal mechanism. The focal plane angles follow the standard convention (Aki and Richards 1980)