Simultane interpretation geophysikalischer messdatensysteme

Summary After general definitions in1 and deducing a special method in2, it will be shown in3 on a simple concrete example the effectiveness of the simultaneous interpretation of two series of data belonging two different geophysical methods, namely, it can be determined in the simultaneous way deep values, too, although both methods, separately, are not capable under the given conditions even for estimation of the great order of the deep. In4 there are some conclusions; above all it is emphasized for any geophysical method the necessity and importance of the general applicable form of the interpretation procedures.