Mineral assemblages record the intermediate and end products of magmatic, metamorphic, hydrothermal, and ore-forming processes, and they represent natural analogues to synthetic processes. For example, the alteration of ultramafic rocks (“listvenites”) is intimately linked to the geological processes responsible for the formation of both orogenic gold deposits and serpentinized nickel deposits (e.g., Kishida & Kerrich 1987, Böhlke 1989, Halls & Zhao 1995, Steinthorsdottir et al. 2022, Evans et al. 2023). Additionally, these processes mirror those of carbon capture and storage (e.g., Menzel et al. 2018, Steinthorsdottir et al. 2022)....
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