1976•Lunar and Planetary Science Conference ProceedingsRequires access

Partitioning of chromium between silicate crystals and melts

J. S. Huebner, Bruce R. Lipin, L. B. Wiggins

Abstract

Experiments were performed determining the distribution of chromium between olivine, pyroxenes, and melt at oxygen fugacity values near those of lunar rocks for a wide range of bulk compositions. The range of values of D-Cr (wt% of Cr2O3 in crystals/Cr2O3 in melt) is 0.6-1.3 for olivine and 1.6-3.5 for pyroxene; this ratio shows no obvious dependence on any experimental parameter.

About this research paper

What this paper is about

Why it matters

OpenAlex reports 44 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

Key concepts: Olivine, Pyroxene, Mineral redox buffer, Silicate, Chromium, Mineralogy, Fugacity, Pigeonite