PDF COPY - Manuel berberian

314 BERBERIAN AND TCHALENK04. FAULTING AND THERMAL SPRING ACTIVITY4.1. GeneralTwo fault-breaks were associated with the earthquake: the first, termed hereSalmas Fault, occurred in a NW-SE direction at the southern edge of the Salma:~Plain; the second, termed Derik Fault, occurred in a NE-SE direction near the mountainvillage of Derik (Fig. 3). Maximum displacements on these faults faults were:Fig. 35. S. Asdvadzadzin (Derik). Only the apse of the small chapel survived the earthquake.