We describe a new method to analyze the properties of plasma waves and apply it to observations made upstream from Mars by the Mars Atmosphere and Volatile EvolutioN (MAVEN) mission. The slow measurement cadence of most charged particle instrumentation has limited the application of analysis techniques based on correlations between particle and magnetic field measurements. We show that we can extend the frequency range of applicability for these techniques, for a subset of waves that remain nearly coherent over multiple wave periods, by subsampling velocity distribution function measurements and binning them by the wave phase. This technique enables the computation of correlations and transport ratios for plasma waves previously inaccessible to this technique at Mars. By computing the cross helicity, we find that most identified waves propagate upstream in the plasma frame. This supports the conclusions of previous studies but enables a clearer determination of the intrinsic wave mode and characteristics. The intrinsic properties of observed waves with frequencies close to the proton cyclotron frequency have little spatial variability but do have large temporal variations, likely due to seasonal changes in the hydrogen exosphere. In contrast, the predominant characteristics of waves at higher frequencies have less temporal variability but more spatial variability. We find several indications of the presence of multiple wave modes in the lower frequency wave observations, with unusual wave properties observed for propagation parallel to the magnetic field and for background magnetic fields nearly perpendicular to the solar wind flow. Plain Language Summary The interaction between the solar wind and planetary environments leads to the growth of a variety of plasma waves. These waves serve as a sensitive tracer of the physical interactions between the solar wind and local charged particle populations. Plasma waves reveal the conversion of energy between kinetic and electromagnetic forms, as well as mediating the exchange of energy between different particle populations. However, identifying the intrinsic characteristics of low-frequency plasma waves often proves quite challenging, because the solar wind sweeps them downstream, altering their properties as measured by an orbiting spacecraft. By combining magnetic field and charged particle data, one can remove some of the resulting ambiguities. However, the low cadence of many charged particle observations limits the applicability of such analyses. In this work, we describe a new technique to eke higher time resolution out of the charged particle measurements and apply it to observations from the Mars Atmosphere and Volatile EvolutioN (MAVEN) mission, opening a new window on the properties of plasma waves at Mars.