In materials science, sintering and melting are fundamentally different thermal processes.
Sintering fuses powder particles below their melting point. The material never becomes fully liquid. For lunar regolith - a mix of crystalline minerals and glass - bonding occurs primarily through viscous flow and partial liquid-phase mechanisms. The glassy fraction softens and pulls particles together, producing a dense, controlled microstructure. Sintering onset for regolith occurs around 1,180°C.
Melting heats past the melting point into a full liquid pool - a melt pool - that solidifies into a glass-ceramic mass. For regolith, full melt occurs above 1,360°C. The result is a vitrified material: hard, but brittle, with residual thermal stresses from rapid cooling.
The gap between these two thresholds is only about 180°C. Most laser processing of regolith lands in the melting regime because staying inside that narrow sintering window requires precise control. The peer-reviewed literature - Balla et al. (2012), ESA's PAVER program (Ginés-Palomares et al., 2023), and the MOONRISE project (Linke et al., 2022) - consistently reports melt pools, glassy phases, and full liquefaction.
That's fine for some applications. Not for all of them.