I am going to use the SEG Wiki open data (https://wiki.seg.org/wiki/Open_data) to learn more the processing. There is a 2D land data with Vibrator as the source named as "Poland 2D Vibroseis Line 001" (https://wiki.seg.org/wiki/2D_Vibroseis_Line_001). So, I read about vibroseis data processing and its difference with explosive source. There exists a sweep generated by vibrator and the uncorrelated trace (which is the field data, raw shots) is actually the convolution of this sweep with earth reflectivity. Then, this uncorrelated trace should be cross-correlated with the sweep to have the correlated trace, and this correlated trace goes to be processed, right?
My first question is that since the sweep length has a long length, what would be the length of field data (uncorrelated trace)? Shouldn't it be sweep length+listen time?
My second question is that how can we realize if the raw data is the correlated one or the uncorrelated one? The data I mention, Poland 2D Vibroseis Line 001, says that the source is vibroseis and the characteristics of the sweep is also given, but, the length of the data is 3 seconds. Should I do the cross-correlation of this data with the synthetic sweep generated by the given characteristics?! or it's already done?! The following is a picture of the first shot which I taught may be useful: