The NASA InSight lander successfully placed a seismometer on the surface of Mars. Alongside, a hammering device was deployed that penetrated into the ground to attempt the first measurements of the planetary heat flow of Mars. The hammering of the heat probe generated repeated seismic signals that were registered by the seismometer. However, the broad frequency content of the seismic signals generated by the hammering extends beyond the Nyquist frequency governed by the seismometer's sampling rate of 100 samples per second. Here, we provide data that was reconstructed at a higher sampling rate of 2000 samples per second using a dedicated de-aliasing algorithm described in the accompanying article. This archive will be updated regularly with new data acquired on Mars. For a detailed data description and instructions on how to cite this dataset, please refer to the README file.

{"references": ["Sollberger, David et al. (2021). A reconstruction algorithm for temporally aliased seismic signals recorded by the InSight Mars lander. Earth and Space Science. 8(8). https://doi.org/10.1029/2020EA001234"]}