entrant fluid phase, a continuous melting as predicted by the KTHNY theory and, in some
cases, waterlike anomalies. In this paper, we employ Langevin Dynamics simulations of a
ramp-like core-softened fluid that have two characteristic length scales and all the features
mentioned above. Analyzing the fluid phase of this system, Bordin and Barbosa (2018)
reported the existence of two waterlike anomalous region. Now, we revisit this problem …