A magmatic deposits is a type of ore deposit that forms when sulfide minerals crystallize in lenses or bands directly from magma.
Magmatic ore deposits are derived from accumulations of crystals of metal oxides, or immiscible sulfide, or oxide beverages that fashioned for the duration of the cooling and crystallization of magma, commonly with mafic to ultramafic compositions.
Magmatic ore deposits can be defined as the ones deposits which demonstrably owe their foundation and existence to the process of metamorphism and attendant deformation, no longer merely with the aid of reconstitution (as within the case of, say, kyanite/sillimanite/wollastonite deposits) but additionally thru “innovative” methods of transport.
A mineral deposit that is satisfactorily wealthy to be worked at a income is referred to as an ore deposit, and in an ore deposit the assemblage of ore minerals plus gangue is known as the ore.
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