“…Hence, the main state variable for elasticity is the velocity field, and the deformation gradient, entering in the elasticity constitutive assumptions, is determined solving a transport equation in terms of the velocity and the velocity gradient. A similar modelling approach for evolutionary models with finite viscoelasticity was implemented also in [3], which studies the Oldroyd-B model for a dilute polymeric fluid, in [8], which studies the motion of a class of incompressible heat-conducting viscoelastic rate-type fluids with stress-diffusion, in [4,12], which study problems in magnetoelasticity, in [20], which studies an evolutionary non-isothermal viscoelastic problem, and in [22], which studies the diffusion of a solvent in a saturated hyperelastic porous solid of viscoelastic Kelvin-Voigt type at large strains.…”