Alessandro Morbidelli has kindly consulted me on this topic. He said:
"The late veneer on Mars is approximately equivalent to that of the Earth, from the abundance of highly siderophile elements in its mantle-derived rocks. So it is about 0.5% of Mars mass. The late veneer is carried mostly by the planetesimals left-over from the terrestrial planet formation period."
His words are illustrated by Figure 17 from this recent work by his team:
Nesvorný, David; Roig, Fernando V.; Vokrouhlický, David; Bottke, William F.; Marchi, Simone; Morbidelli, Alessandro; Deienno, Rogerio. (2023)
"Early bombardment of the moon: Connecting the lunar crater record to the
terrestrial planet formation"
Icarus, Vol. 399, article id. 115545.