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Diamond anvil cell partitioning experiments for accretion and core formation: Testing the limitations of electron microprobe analysis

Abstract:

Metal–silicate partitioning studies performed in high-pressure, laser-heated diamond anvil cells (DAC) are commonly used to explore element distribution during planetary-scale core–mantle differentiation. The small run-products contain suitable areas for analysis commonly less than tens of microns in diameter and a few microns thick. Because high spatial resolution is required, quantitative chemical analyses of the quenched phases is usually performed by electron probe microanalysis (EPMA). H...

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Publication status:
Published
Peer review status:
Peer reviewed
Version:
Accepted Manuscript

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Publisher copy:
10.1017/S1431927618015568

Authors


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Institution:
University of Oxford
Division:
MPLS Division
Department:
Earth Sciences
Role:
Author
ORCID:
0000-0002-6998-236X
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Grant:
Advanced Grant “ACCRETE”: 290568
Publisher:
Cambridge University Press Publisher's website
Journal:
Microscopy and Microanalysis Journal website
Volume:
25
Issue:
1
Pages:
1-10
Publication date:
2019-01-22
Acceptance date:
2018-11-02
DOI:
EISSN:
1435-8115
ISSN:
1431-9276
Pubs id:
pubs:937116
URN:
uri:27bab4ca-f71b-4378-b72f-05e9f0e46cbc
UUID:
uuid:27bab4ca-f71b-4378-b72f-05e9f0e46cbc
Local pid:
pubs:937116

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