We have compiled the trace element concentrations in pyrrhotite, pentlandite, chalcopyrite,
and pyrite from magmatic Ni-Cu-PGE ore deposits with the aim of understanding their …

In the present paper, we have compiled data on 565 layered and differentiated igneous
intrusions globally, documenting their (i) location,(ii) age,(iii) size,(iv) geotectonic setting,(v) …

Magmatic systems play a crucial role in enriching the crust with volatiles and elements that
reside primarily within the Earth's mantle, including economically important metals like …

Much of the world's supply of battery metals and platinum group elements (PGE) comes from
sulphide ore bodies formed in ancient sub-volcanic magma plumbing systems. Research on …

A common feature of the mineralised chonolith intrusions of the Norilsk-Talnakh camp is the
presence of globular disseminated Ni–Cu–Fe sulphide ores, particularly well developed …

Ore forming processes involve the redistribution of heat, mass and momentum by a wide
range of processes operating at different time and length scales. The fastest process at any …

Magmatic sulfide deposits are generated by extraordinary accumulations of immiscible
sulfide liquids in ultramafic-mafic magmas. While their associated geochemical and …

Much of the value of magmatic Ni-Cu-PGE sulfide orebodies is contained within massive or
semi-massive ores that show a wide variety of textural relationships to included or adjacent …

Pentlandite is the dominant Ni-hosting ore mineral in most magmatic sulfide deposits and
has conventionally been interpreted as being entirely generated by solid-state exsolution …

Magmatic sulfide ore deposits are products of natural smelting: concentration of immiscible
sulfide liquid ('matte'), enriched in chalcophile elements, derived from silicate magmas …