Quartz dissolution associated with magnesium silicate hydrate cement precipitation
<p>Quartz has been replaced by magnesium silicate hydrate cement at the Feragen ultramafic body in south-east Norway. This occurs in deformed and recrystallized quartz grains deposited as glacial till covering part of the ultramafic body. Where the ultramafic body is exposed, weathering leads...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2021-02-01
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| Series: | Solid Earth |
| Online Access: | https://se.copernicus.org/articles/12/389/2021/se-12-389-2021.pdf |