Electronic Supplement to
Reassessing the Rupture Process of the 2009 L’Aquila Earthquake (M_w 6.3) on the Paganica Fault and Investigating the Possibility of Coseismic Motion on Secondary Faults

by Julien Balestra and Bertrand Delouis

Table S5. Computed Surface Displacements from Model 1-SF

GPS Station	D. East* (cm)	D. North* (cm)	D. Up* (cm)	Station RMS†
PAGA	−3.25	−2.7	−8.52	0.066
INFN	5.68	6.05	1.72	0.121
CADO	−8.13	6.57	−16.47	0.0031

* D. East, D. North, and D. Up are the displacements toward the east, north, and up (vertical), respectively.

† Station RMS is the normalized root mean square value for the individual station. RMS = √[Σ_j=1,3 (O_j–C_j)²/Σ_j=1,3 O_j²], in which 3 is the number of components, O_j and C_j are observed and computed values for the jth component.

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