2012Geochimica et Cosmochimica ActaRequires access

Experimental evidence for the absence of iron isotope fractionation between metal and silicate liquids at 1GPa and 1250–1300°C and its cosmochemical consequences

Remco C. Hin, Max W. Schmidt, Bernard Bourdon

Open publisher page 71 citations

Abstract

This record does not include an abstract. Use the full-text link above if available.

About this research paper

What this paper is about

An abstract is not available in the OpenAlex record for this paper.

Why it matters

OpenAlex reports 71 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.

Key concepts: Silicate, Isotope fractionation, Fractionation, Equilibrium fractionation, Chondrite, Metal, Mass-independent fractionation, Meteorite

Related papers

Back to paper searchBrowse research topicsOriginal source
Experimental evidence for the absence of iron isotope fractionation between metal and silicate liquids at 1GPa and 1250–1300°C and its cosmochemical consequences — Research Paper | ScholarLens