“…This process is known as “spinodal decomposition.” For the Liesegang patterning, it has been interpreted as a discrete scenario of competing dynamics between spin‐flip (i.e., reaction) and spin‐exchange (i.e., diffusion) (Antal et al., 1999), evolving toward the final stationary pattern. It is worth noting that this category of generalized approach has gained significant success in diverse disciplines, including those involving morphogenesis in a system of natural materials (Arguello, Gumulya, et al., 2022; Arguello, Labanda, et al., 2022; Arguello et al., 2023; Christoph et al., 1999; Cooper, 2012; Nakouzi & Sultan, 2011), and those focusing on digital pattern recognition in for example, (Bertozzi et al., 2007; Theljani et al., 2020), due to the striking similarity in the essential force‐flux interactions of thermodynamic nature. Here, the concept of phase separation is employed for interpretation and parameter inversion of the rhythmically banded and spotted patterns of East Kimberley Zebra rocks, which can be extended to the general classification of Mississippi Valley Type deposits (L’Heureux, 2013; Kelka et al., 2017).…”