“…This is supported by the heavy mineral assemblages, particularly glaucophane and lawsonite that represent a HP-LT (blueschist) metamorphic rock source. These minerals were probably derived from the Mekongga and Rumbia metamorphic complexes, in which blueschists are exposed (de Roever, 1950(de Roever, , 1956Helmers et al, 1989;Mawaleda et al, 2016Mawaleda et al, , 2018Wijbrans et al, 1994). Garnet could have been derived from a multitude of metamorphic rocks, as well as garnet-bearing peridotites reported in Central Sulawesi close to the Palu-Koro Fault and in the East Arm where they are associated with the ophiolite (Kadarusman & Parkinson, 2000;Parkinson, 1996).…”