Experimental Partitioning of Trace Elements into Schreibersite with Applications to IIG Iron Meteorites

Author(s)

Nancy L. Chabot and Rachel H. Cueva, Johns Hopkins University Applied Physics Laboratory, Laurel, MD, 20723; Andrew W. Beck Department of Petroleum Engineering & Geology, Marietta College, Marietta, OH, 45750; Richard D. Ash Department of Geology, University of Maryland, College Park, MD, 20742

Publication Year

2020

Journal

Meteoritics and Planetary Science

DOI

10.1111/maps.13462

Description

Abstract

Some of the defining characteristics of the IIG iron meteorite group are their high bulk P contents and massive, coarse schreibersite, which have been calculated to make up roughly 11–14 wt% of each specimen. In this study, we produced two datasets to investigate the formation of schreibersites in IIG irons: measurements of trace elements in the IIG iron meteorite Twannberg and experimental determinations of trace element partitioning into schreibersite. The schreibersite-bearing experiments were conducted with schreibersite in equilibrium with a P-rich melt and with bulk Ni contents ranging from 0–40 wt%. The partitioning behavior for the 20 elements measured in this study did not vary with Ni content. Comparison of the Twannberg measurements with the experimental results required a correction factor to account for the fact that the experiments were conducted in a simplified system that did not contain a solid metal phase. Previously determined solid metal/P-rich melt partition coefficients were applied to infer schreibersite/solid metal partitioning behavior from the experiments, and once this correction was applied, the two datasets showed broad similarities between the schreibersite/solid metal distribution of elements. However, there were also differences noted, in particular between the Ni and P contents of the solid metal relative to the schreibersite inferred from the experiments compared to that measured in the Twannberg sample. These differences support previous interpretations that subsolidus schreibersite evolution has strongly influenced the Ni and P content now present in the solid metal phase of IIG irons. Quantitative attempts to match the IIG solid metal composition to that of late-stage IIAB irons through subsolidus schreibersite growth were not successful, but qualitatively, this study corroborates the striking similarities between the IIAB and IIG groups, which are highly suggestive of a possible genetic link between the groups as has been previously proposed.

Files

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tables2020-03-16.pdf

All Tables

table_1_twannberg_tablev2.docx

Table1

table_3_weighted_averagesv3.docx

Table 3

table_2_experimentsv22019-11-05.docx

Table 2

table_s2_initial_composition_table.docx

Table S2

table_s1_twannberg_data_comparison_tablev2.docx

Table S1

table_s4_previous_data_table.docx

Table S4

table_s3_feni2p_tablev3.docx

Table S3

fig1_twannberg.tif

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Fig. S2

figs1_fe2p.tif

Fig. S1

fe2p.psd

Fig. S1 - photoshop format

fe3p.psd

Fig. 2 - photoshop format

twannberg.psd

Fig. 1 - photoshop format

Uploaded by nchabot on March 16, 2020, 5:19 p.m.
Last modified March 16, 2020, 5:36 p.m.