Abstract
Mazin and Singh comment that the peaks in the Fourier-transformed spectroscopic maps of Fe(Se,Te) are not related to the quasi-particle-interference (QPI) but may be Bragg peaks associated with chalcogen lattice and possible surface reconstruction which would be triggered by surface-induced spin-density wave. We show that the peaks are too broad to be assigned as Bragg peaks and are consistent with QPI.
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