Özet:

Conventionally, the data obtained from images and vibrations are assessed separately fort the blasts. A high speed video camera records the changes around the blast point from the beginning till the end of the blast period. Three component geophone records the seismic signals of the same blast. However, examining all the blast effects together makes us understand the complete occasion. The seismic signals which coincide with the images originated from the blasts are recorded with time delays when compared to the images. A kind of deconvolution is necessary to prevent this delay in time. Therefore, all the geological-way and delay effects are prevented which cause the elongation of the seismic signals and their asynchronization with the image data. There is one more problem between the blast images and the seismic signals of the same blast: Interference. Interference is a strengthening or weakening wave interaction created by the multi source systems. Deconvolution deducts both the asynchronization and interference effects from the seismic signals. In the presented study, synchronized image and seismic signal data are compared, blast occasions are correlated with each other, and productive suggestions are presented in the model applications

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