Fig. 3From: Full, constrained and stochastic source inversions support evidence for volumetric changes during the Basel earthquake sequenceFull moment tensor solutions for event 113. a Full moment tensor solution using both P and S waves. Inversion of 3 s long, 3 component displacement records of 5 stations filtered between 0.5 and 3 Hz. b Full moment tensor solution using only P waves on the vertical components filtered between 2 and 6 Hz. Both solutions return similar source decompositionBack to article page