“…The first analysis of highly radioactive samples collected in premises below the burned-through reactor's base plate showed that fuel fragments and molten corium reacted with concrete and serpentinite and formed a highly radioactive silicate melt (called silicate-rich corium or "Chernobyl lava"). Three main sources of "lava" were observed during visual inspections of the destroyed reactor and related dose rate measurements (Borovoi et al, 1990;Kiselev et al, 1992;Pazukhin, 1994). EPMA, XRD, Raman spectroscopy, and FIBassisted TEM of inclusions extracted from silicate matrices of Chernobyl "lava" and "pumice" showed the presence of U-Zr-O solid solutions of various crystalline structures, UOx (relicts of a fuel pellet), metallic inclusions, and uranium-rich artificial zircon (Zr 1x U x )SiO 4 (Anderson et al, 1993;Trotabas et al, 1993;Burakov, 2020).…”