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As an example, heat determinations to own equilibrium magnetite\u2013quartz sets and magnetite\u2013pyroxene sets of Kiruna, El Laco, and you can Gr\u00e4ngesberg produce heat you to continuously surpass 600\u2009\u00b0C1,5. This is especially the instance for the enormous magnetite ores, in which so it overall chemically inert and refractory mineral would provide regional buffering in terms of blog post-depositional lso are-equilibration1. step 3 and you will 4 next either reflect the lower avoid of your own magmatic heat diversity, or secondary outcomes, such adjustment, as well as leaching and you will then lso are-rain from the heat less than eight hundred\u2009\u00b0C, which postdates an initial high-heat (magmatic) phase of development (Fig.\u00a05). Resource fields to own common hydrothermal and you can magmatic magnetites are shown for comparison39,forty five,46,47,51,69,70. Trials from the Bafq Exploration Region were accumulated in the Sechahun, Lakkeh Siah, Chadormalu, and you may Esfordi deposits42. The brand new Plio- to help you Pleistocene El Laco deposit falls under the young apatite-iron-oxide mineralizations one to define the brand new east higher Andes which can be separate regarding the Cretaceous apatite-iron-oxide ores of your very-entitled Chilean Metal Belt7,14,17,18.<\/p>\n