- 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...
Expand abstract - Publication status:
- Published
- Peer review status:
- Peer reviewed
- Version:
- Accepted Manuscript
- Files:
-
-
(pdf, 8.0MB)
-
- Publisher copy:
- 10.1017/S1431927618015568
-
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- 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
- Copyright holder:
- Microscopy Society of America
- Copyright date:
- 2019
- Notes:
- © Microscopy Society of America 2019. This is the accepted manuscript version of the article. The final version is available online from Cambridge University Press at: https://doi.org/10.1017/S1431927618015568
Journal article
Diamond anvil cell partitioning experiments for accretion and core formation: Testing the limitations of electron microprobe analysis
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