Diamonds, dunites, and metasomatic rocks formed by melt/rock reaction in craton roots
Reactions of depleted, reduced peridotite with oxidised volatile-rich melts can explain several contentious rock assemblages sampled by kimberlites from the metasomatised zone at the base of the lithosphere, according to high pressure laboratory experiments.
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Nature Portfolio
2022-11-01
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| Series: | Communications Earth & Environment |
| Online Access: | https://doi.org/10.1038/s43247-022-00630-3 |
| _version_ | 1811207611774664704 |
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| author | Zsanett Pintér Stephen F. Foley Gregory M. Yaxley |
| author_facet | Zsanett Pintér Stephen F. Foley Gregory M. Yaxley |
| author_sort | Zsanett Pintér |
| collection | DOAJ |
| description | Reactions of depleted, reduced peridotite with oxidised volatile-rich melts can explain several contentious rock assemblages sampled by kimberlites from the metasomatised zone at the base of the lithosphere, according to high pressure laboratory experiments. |
| first_indexed | 2024-04-12T04:07:27Z |
| format | Article |
| id | doaj.art-7668b14cdcec4059b86b75926a3e0655 |
| institution | Directory Open Access Journal |
| issn | 2662-4435 |
| language | English |
| last_indexed | 2024-04-12T04:07:27Z |
| publishDate | 2022-11-01 |
| publisher | Nature Portfolio |
| record_format | Article |
| series | Communications Earth & Environment |
| spelling | doaj.art-7668b14cdcec4059b86b75926a3e06552022-12-22T03:48:35ZengNature PortfolioCommunications Earth & Environment2662-44352022-11-01311810.1038/s43247-022-00630-3Diamonds, dunites, and metasomatic rocks formed by melt/rock reaction in craton rootsZsanett Pintér0Stephen F. Foley1Gregory M. Yaxley2School of Natural Sciences and ARC Centre of Excellence for Core to Crust Fluid Systems, Macquarie UniversitySchool of Natural Sciences and ARC Centre of Excellence for Core to Crust Fluid Systems, Macquarie UniversityResearch School of Earth Sciences, Australian National UniversityReactions of depleted, reduced peridotite with oxidised volatile-rich melts can explain several contentious rock assemblages sampled by kimberlites from the metasomatised zone at the base of the lithosphere, according to high pressure laboratory experiments.https://doi.org/10.1038/s43247-022-00630-3 |
| spellingShingle | Zsanett Pintér Stephen F. Foley Gregory M. Yaxley Diamonds, dunites, and metasomatic rocks formed by melt/rock reaction in craton roots Communications Earth & Environment |
| title | Diamonds, dunites, and metasomatic rocks formed by melt/rock reaction in craton roots |
| title_full | Diamonds, dunites, and metasomatic rocks formed by melt/rock reaction in craton roots |
| title_fullStr | Diamonds, dunites, and metasomatic rocks formed by melt/rock reaction in craton roots |
| title_full_unstemmed | Diamonds, dunites, and metasomatic rocks formed by melt/rock reaction in craton roots |
| title_short | Diamonds, dunites, and metasomatic rocks formed by melt/rock reaction in craton roots |
| title_sort | diamonds dunites and metasomatic rocks formed by melt rock reaction in craton roots |
| url | https://doi.org/10.1038/s43247-022-00630-3 |
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