Placer platinum-group minerals in the Shetland ophiolite complex derived from anomalously enriched podiform chromitites

Abstract

Highly anomalous platinum-group element (PGE) concentrations in the podiform chromitites at the Cliff and Harold's Grave localities in the Shetland ophiolite complex have been well documented previously. The focus of this study is alluvial platinum-group minerals (PGM) located in small streams that drain from the PGE-rich chromitites. The placer PGM assemblage at Cliff is dominated by Pt-arsenides (64%) and Pd-antimonides (17%), with less irarsite–hollingworthite (11%) and minor Pd-sulfides, Pt–Pd–Cu and Pt–Fe alloys and laurite. Gold also occurs with the PGM. Alluvial PGM have average sizes of 20 µm × 60 µm, with sperrylite the largest grain identified at 110 µm in diameter, matching the range reported for the primary PGM in the source rocks. The placer assemblage contains more Pt-bearing and less Pd-bearing PGM compared with the rocks. The more resistant sperrylite and irarsite–hollingworthite grains which are often euhedral become more rounded further downstream whereas the less resistant Pd-antimonides which are commonly subhedral may become striated and etched. Less stable phases such as Pt- and Pd-oxides and other Ni-Cu-bearing phases located in the rocks (i.e. Ru-pentlandite, PtCu, Pd–Cu alloy) are absent in the placer assemblage. Also the scarce PGM (PdHg, Rh- and Ir-Sb) and Os in the rocks are absent. At Harold's Grave only three alluvial PGM (laurite, Ir, Os) and Au were recovered reflecting the limited release of IPGM from chromite grains in the rocks. In this cold climate with high rainfall, where erosion dominates over weathering, the PGM appear to have been derived directly from the erosion of the adjacent PGE-rich source rocks and there is little evidence of in situ growth of any newly formed PGM. Only the presence of dendritic pure Au and Pd-, Cu-bearing Au covers on the surface of primary minerals may indicate some local reprecipitation of these metals in the surficial conditions.

Introduction to the Special Issue dedicated to the work and memory of Professor Hazel Margaret Prichard (1954–2017)

“…Prichard et al . (2018 b ) also discuss the Shetland ophiolite, concentrating on the variety of placer platinum-group minerals (PGM) derived from the Cliff, and also the Harold's Grave, localities. Ophiolite-derived PGM are also described by Barkov et al .…”

“…The locality described in the O'Driscoll et al article (Cliff ) is the classic area where Hazel discovered such anomalously high Pt and Pd enrichments, compared to other ophiolitic chromitites worldwide, and adds additional support to Hazel's original and novel interpretation for a metasomatic origin for these enrichments. Prichard et al (2018b) also discuss the Shetland ophiolite, concentrating on the variety of placer platinum-group minerals (PGM) derived from the Cliff, and also the Harold's Grave, localities. Ophiolite-derived PGM are also described by Barkov et al (2018) and Cabri and Aiglsperger (2018).…”