They reported that small positioning errors in the placement of sources and receivers can easily create discrepancies larger than the apparent reciprocity discrepancy. They also reported that theoretically reciprocal experiments may actually be less reciprocal than presumably nonreciprocal experiments. Geometrical complexity within the earth does not diminish the applicability of the principle of linearity. Likewise, geometrical complexity does not reduce the applicability of reciprocity. Reciprocity does not apply to sound waves in the presence of wind.
Sound goes slower upwind than downwind.
But this effect of wind is much less than the mundane irregularities of field work. Just the weakening of echoes with time leaves noises that are not reciprocal. Henceforth we will presume that reciprocity is generally applicable to the analysis of reflection seismic data.