New insights into the origin of the Evate apatite-iron oxide-carbonate deposit, Northeastern Mozambique, constrained by mineralogy, textures, thermochronometry, and fluid inclusions
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文摘

Evate deposit is interpreted as a magmatic deposit overprinted by low-T fluids

High-T minerals originated during Late-Ediacaran post-collisional cooling

Low-T hydrothermal overprint recorded by sulfate-rich brines

Reactivation indicated by Ordovician monazite

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