Table 1. Basin ejecta thickness introduced within Faustini crater using Pike (1974) equation from Imbrium, Orientale, and Schrödinger

Basin source	D (km)	Mean TC Radius (km)	α (km)	Pike constant	Pike B-value	t (km)
Imbrium	1,321	372	3,794	0.033	3	0.012+0.025–0.008
Orientale	937	198.5	2,212	0.033	3	0.005+0.011–0.004
Schrödinger	326	55.5	411	0.033	3	0.005+0.007–0.003

D refers to basin diameters after Neumann et al. (2015); Mean TC radius is the mean transient crater Radius after Wieczorek & Phillips (1999) and Petro & Pieters (2004); α is the angular distance calculated using the spherical law of cosine, and t is the ejecta thickness.