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|Title:||Magmatic sulfide ore deposits|
|Authors:||Barnes, Stephen J.|
Holwell, David A.
Le Vaillant, Margaux
|Publisher:||Mineralogical Society of America|
|Citation:||Elements, 2017, 13 (2), pp. 89–95|
|Abstract:||Magmatic sulfide ore deposits are products of natural smelting: concentration of elements from silicate magmas (slags) by immiscible sulfide liquid (matte). Deposits occupy a spectrum from accumulated pools of matte within small igneous intrusions or lava flows, forming orebodies mined primarily for Ni and Cu, to stratiform layers of weakly disseminated sulfides, mined for platinum group elements, within large mafic-ultramafic intrusions. One of the world’s most valuable deposits, the Platreef in the Bushveld Complex in South Africa, has aspects of both of these end members. Natural matte compositions vary widely between and within deposits, controlled largely by the relative volumes of matte and slag that interact with one another.|
|Rights:||Copyright © 2016, Mineralogical Society of America. Deposited with reference to the publisher’s open access archiving policy.|
|Description:||The file associated with this record is under a 12 month embargo from publication in accordance with the publisher's self-archiving policy. The full text may be available through the publisher links provided above.|
|Appears in Collections:||Published Articles, Dept. of Geology|
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|Barnes et al Elements accepted.pdf||Post-review (final submitted author manuscript)||826.95 kB||Adobe PDF||View/Open|
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