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separating the simulated encoded data according to source and/or receiver using a source or receiver separation algorithm ,resultingin simulated sequential source and/or receiver data
The change in the frequency of a wave , as a light wave or sound waveresultingfrom relative motion of the source and the receiver
the factorsinfluencingthe pattern of sources and receivers in a seismic survey
Doppler shiftsresultingfrom relative motion of the transmitter and receiver
In the drawing , fd+fd ' is the Doppler frequency due to the movements of the satellite and the receiverresultsfrom satellite movement and fd ' results from receiver movement
the perceived change in frequencyresultingfrom the relative movement of the source and receiver
Doppler - frequency shiftresultingfrom relative motion of source and receiver
New seismic source and streamer technologies and methodologieswill contributetowards resolving the source and receiver ghost effect in seismic data
The seismic rayoriginatesat seismic source s and travels to seismic receiver
emitted and received frequency(passive) caused byemitted and received frequency
Doppler frequency errors(passive) caused byDoppler frequency errors
a wave(passive) caused bya wave
the distortion(passive) caused bythe distortion
this signal(passive) caused bythis signal
some types of errors(passive) caused bysome types of errors
a delay , or moveoutcreatesa delay , or moveout
to Doppler and differential Doppler effects that are robust phenomena in many ASW scenariosleadsto Doppler and differential Doppler effects that are robust phenomena in many ASW scenarios
time dilation(passive) caused bytime dilation
to 0setto 0