Refraction and CDP Reflection Shallow Seismics for Detection of Low Amplitude Faults

P146 REFRACTION AND CDP REFLECTION SHALLOW SEISMICS FOR DETECTION OF LOW AMPLITUDE FAULTS Abstract 1 The inversion of travel time curves of refracted waves by a method of homogeneous functions allows to compute seismic cross sections comparable with respect to resolution with cross sections obtained by a reflection CDP (Common Deep Point) method. The integration of seismic methods in a structure of a method of refracted waves and CDP method was applied for research of the rocky basis of Kursk Atomic Power Station (KAPS). The purpose of researches was detection of low amplitude faults. Sets of faults detected in CDP