As remnants of past oceanic lithosphere, ophiolites could potentially record the life cycles of ocean basins from their rift-drift and seafloor spreading to subduction initiation and terminal closure (Dilek & Furnes, 2011Xu et al., 2020;Vannucchi et al., 2020). Different types of ophiolites formed in various tectonic environments, such as ocean-continent-transition (OCT), mid-ocean-ridges (MOR), and supra-subduction-zone settings (SSZ; Dilek & Furnes, 2014 and references therein), are believed to represent different