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Journal ArticleDOI

The effect of sulfur on the partitioning of Ni and other first-row transition elements between olivine and silicate melt

J. Tuff, +1 more
- 01 Nov 2010 - 
- Vol. 74, Iss: 21, pp 6180-6205
TLDR
In this paper, the effect of sulfur dissolved as sulfide (S2−) in silicate melts on the activity coefficients of NiO and some other oxides of divalent cations (Ca, Cr, Mn, Fe and Co) has been determined from olivine/melt partitioning experiments at 1400°C in six melt compositions in the system CaO-MgO-Al2O3-SiO2 (CMAS), and in derivatives of these compositions at 1370°C, obtained from the six CMAS compositions by substituting Fe for M
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This article is published in Geochimica et Cosmochimica Acta.The article was published on 2010-11-01. It has received 25 citations till now. The article focuses on the topics: Silicate & Incompatible element.

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Citations
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Journal ArticleDOI

Partitioning of platinum-group elements and Au between sulfide liquid and basalt and the origins of mantle-crust fractionation of the chalcophile elements

TL;DR: In this paper, the authors present direct experimental measurements of D PGE sul, based on in situ microanalysis of the sulfide and silicate melt, with values ranging from ∼4.5 × 105 (Ru) to ∼2.3 × 106 (Ir, Pt) and they use their new set of partition coefficients to develop a fully constrained model of PGE behavior during melting which accurately predicts the abundances of PME in mantle-derived magmas and their restites, including mid-ocean ridge basalts, continental picrites, and the parental magmas
Journal ArticleDOI

The Temperature and Pressure Dependence of Nickel Partitioning between Olivine and Silicate Melt

TL;DR: In this article, the authors measured Ni partitioning between olivine and melt, D^(ol/liq)_(Ni), in experiments on mid-ocean ridge basalt (MORB) encapsulated in Olivine at pressures from 1 atm to 3·0 GPa and temperatures from 1400 to 1550°C.
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Trace element mineral/melt partitioning for basaltic and basaltic andesitic melts: An experimental and laser ICP-MS study with application to the oxidation state of mantle source regions

TL;DR: In this article, the trace element partition coefficients for a large number of trace elements, in the various minerals present in basaltic rocks, and under diverse conditions, particularly of variable fO2.
Journal ArticleDOI

Prediction of metal–silicate partition coefficients for siderophile elements: An update and assessment of PT conditions for metal–silicate equilibrium during accretion of the Earth

TL;DR: In this paper, the behavior of the moderately siderophile elements Ni and Co was compared using several approaches, each of which results in the same conclusion for Ni and co. The main difference between the current result and several other recent modeling efforts is that Mn, V, and Cr are hosted in deep mantle phases as well as the core.
Journal ArticleDOI

Evaporation of moderately volatile elements from silicate melts: experiments and theory

TL;DR: In this paper, a series of experiments in which silicate liquids are evaporated in one-atmosphere (1-atm) gas-mixing furnaces under controlled f O 2 s, from the Fe-“FeO” buffer (iron-wustite, IW) to air (10 -0.68 bars), bracketing the range of most magmatic rocks.
References
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Journal ArticleDOI

Revised effective ionic radii and systematic studies of interatomic distances in halides and chalcogenides

TL;DR: The effective ionic radii of Shannon & Prewitt [Acta Cryst. (1969), B25, 925-945] are revised to include more unusual oxidation states and coordinations as mentioned in this paper.
Journal ArticleDOI

Olivine-Liquid Equilibrium

TL;DR: In this paper, a number of experiments have been conducted in order to study the equilibria between olivine and basaltic liquids and to try and understand the conditions under which OIVINE will crystallize.
Journal ArticleDOI

A Compilation of New and Published Major and Trace Element Data for NIST SRM 610 and NIST SRM 612 Glass Reference Materials

TL;DR: In this article, the authors present a compilation of trace element data from approximately sixty published works for NIST SRM 611 and NISTSRM 613 and provide useful new working values for these reference materials.
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Reference Samples for Electron Microprobe Analysis

TL;DR: In this paper, chemical analyses of twenty-six minerals, four natural glasses, and one synthetic glass were presented for use as microprobe reference samples, and details of sample preparation were described and homogeneity of the samples has been tested by the homogeneity index.
Journal ArticleDOI

GeoReM: A New Geochemical Database for Reference Materials and Isotopic Standards

TL;DR: GeoReM as mentioned in this paper is a relational database for reference materials and isotopic standards of geochemical and mineralogical interest, which contains published analytical and compilation values (major and trace element concentrations, radiogenic and stable isotope ratios), important metadata about the analytical values, such as uncertainty, uncertainty type, method and laboratory.
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