We investigate numerically some thermo-mechanical conditions for the development of crustal scale diapirism and convection in a heterogeneous continental crust independently from the action of regional tectonics. Here, we consider a hot crust where convection is generated below a melting front, with unmolten and partially molten domains of specific temperature and strain-rate dependent power-law rheologies. We take advantage of the VOF (Volume Of Fluid) method to capture the coalescence and separation of deformable inclusions in the partially molten domain. The inclusions, of several hundred meters in size, are more or less dense and more or less viscous with respect to the ambient medium (they also behave with a power-law rheology). We restrict our study to a 20 Myr time scale, during which gravitational dynamics may dominate over lateral tectonics and lithospheric thermal reequilibration. The motion of these inclusions during the development of gravitational instabilities allows to define distinct flow regimes that depend on two Rayleigh numbers denoted RaUM and RaPM, for the unmolten and partially molten rock properties, respectively. A ’suspension’ regime occurs at high RaUM and high RaPM, in which most of the light compositional heterogeneities remain entrained in the convective cells. In contrast at low RaUM and high RaPM, a ’layering’ regime is characterized by merging of the light inclusions as floating clusters below the rigid upper crustal lid. This regime occurs occurs in association with a sharp viscosity gradient at upper-to-middle crust transitional depths. In these two regimes, the dense inclusions accumulate at the bottom of the partially molten zone. Finally at moderate RaPM, a ’diapiric’ regime reflects the segregation of the heavy and the light inclusions, respectively downward and upward, without global convection. These numerical experiments lead to a first order evaluation of the physical parameters required for the segregation of deformable inclusions of variable densities and convection, in a partially molten crust, and provide insights on the conditions for the development of migmatite domes. Geological data indicate that these processes likely occur in a large number of settings from Archean to Phanerozoic times, and contribute to the differentiation of the continental crust.