Origin of the high Pd/Pt ratio of the J-M Reef, Stillwater Complex Montana USA

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Abstract

The J-M Reef of the Stillwater Complex exhibits a high and consistent Pd/Pt ratio (~3.8). This ratio results from the equilibration of an immiscible sulfide liquid with a relatively high Pd/Pt silicate melt rather than an unusually Pd- and Pt-enriched parental melt. Numerical modeling suggests that the original silicate melt contained typical mantle-derived concentrations of Pd and Pt (~10–20 ppb Pd/Pt ~1). The partitioning of Pt and Pd between sulfide liquid and silicate melt alone cannot explain the consistently high Pd/Pt ratio across variable melt-to-sulfide mass ratios (R factors). Instead Pt-depletion caused by the early fractionation of Pt-alloy from S-undersaturated silicate magma likely established the high Pd/Pt signature. High Pd/Pt ratios can form through batch equilibration of sulfide liquid with silicate melt if partition coefficients are extremely high (>10⁶). Alternatively Pd enrichment may result from sulfide upgrading within the resident footwall mush under smaller partition coefficients (10⁴–10⁶) in this model the instantaneous R factors remain low (R ≈ 100–700). This limits the impact of Pt and Pd partitioning on sulfide composition and helps explain the Pd-enriched character of the J-M Reef.

Publication type Conference Paper
Publication Subtype Abstract or summary
Title Origin of the high Pd/Pt ratio of the J-M Reef, Stillwater Complex Montana USA
Volume II
Year Published 2025
Language English
Publisher Society for Geology Applied to Mineral Deposits
Contributing office(s) Geology, Minerals, Energy, and Geophysics Science Center
Description 4 p.
First page 603
Last page 606
Conference Title 18th SGA Biennial Meeting
Conference Location Golden, CO
Conference Date August 3-7, 2025
Country United States
State Montana
Other Geospatial J-M Reef Stillwater Complex
Additional publication details