Chalcophile and siderophile elements in mantle rocks: Trace elements controlled by trace minerals

JP Lorand, A Luguet - Reviews in Mineralogy and …, 2016 - pubs.geoscienceworld.org
BACKGROUND Rocks from the Earth's mantle occur in a wide range of geologic settings (1)
as peridotite massifs, now referred to as orogenic peridotites;(2) as spinel-(rarely garnet) …

Distribution and processing of highly siderophile elements in cratonic mantle lithosphere

S Aulbach, JE Mungall… - Reviews in Mineralogy …, 2016 - pubs.geoscienceworld.org
Cratonic lithospheric mantle is composed of predominantly refractory materials that formed
at higher mantle potential temperatures (TP) than recorded in non-cratonic peridotites. It also …

The crystal/melt partitioning of V during mantle melting as a function of oxygen fugacity compared with some other elements (Al, P, Ca, Sc, Ti, Cr, Fe, Ga, Y, Zr and Nb)

G Mallmann, HSC O'Neill - Journal of Petrology, 2009 - academic.oup.com
Vanadium exists in multiple valence states in silicate and oxide systems, namely V2+, V3+,
V4+ and V5+. This special characteristic has been exploited in several ways to estimate the …

Partitioning of platinum-group elements (PGE) and chalcogens (Se, Te, As, Sb, Bi) between monosulfide-solid solution (MSS), intermediate solid solution (ISS) and …

Y Liu, J Brenan - Geochimica et Cosmochimica Acta, 2015 - Elsevier
In order to better understand the behavior of highly siderophile elements (HSEs: Os, Ir, Ru,
Rh, Pt, Pd, Au, Re), Ag, Pb and chalcogens (As, Se, Sb, Te and Bi) during the solidification of …

Interpreting ages from Re–Os isotopes in peridotites

RL Rudnick, RJ Walker - Lithos, 2009 - Elsevier
Since the first application of the 187Re–187Os isotope system to determine the timing of
melt extraction from peridotites twenty years ago, a plethora of studies have demonstrated its …

Rhodium, gold and other highly siderophile elements in orogenic peridotites and peridotite xenoliths

M Fischer-Gödde, H Becker, F Wombacher - Chemical Geology, 2011 - Elsevier
The concentrations of Rh, Au and other highly siderophile elements (HSE: Re, Os, Ir, Ru, Pt,
Rh, Pd and Au), and 187Os/188Os isotope ratios have been determined for samples from …

The role of late sulfide saturation in the formation of a Cu-and Au-rich magma: insights from the platinum group element geochemistry of Niuatahi–Motutahi lavas …

JW Park, IH Campbell, J Kim, JW Moon - Journal of Petrology, 2015 - academic.oup.com
Magmas enriched in Cu and Au are likely to be the most prospective for magmatic–
hydrothermal deposits of these metals. However, the mechanism that leads to the formation …

Experimental results on fractionation of the highly siderophile elements (HSE) at variable pressures and temperatures during planetary and magmatic differentiation

JM Brenan, NR Bennett… - Reviews in Mineralogy …, 2016 - pubs.geoscienceworld.org
The platinum-group elements (PGEs; Os, Ir, Ru, Rh, Pt, Pd), along with rhenium and gold,
are grouped together as the highly siderophile elements (HSEs), defined by their extreme …

Hotspot volcanism and highly siderophile elements

JMD Day - Chemical Geology, 2013 - Elsevier
Hotspot volcanic rocks are formed under conditions that differ from conventional plate
tectonic boundary magmatic processes and are compositionally distinct from mid-oceanic …

Experiments and models bearing on the role of chromite as a collector of platinum group minerals by local reduction

CS Finnigan, JM Brenan, JE Mungall… - Journal of …, 2008 - academic.oup.com
Chromite is widely recognized to act as a collector for platinum group elements (PGE), which
tend to be observed as discrete grains of platinum group minerals included within magmatic …