- Title
- Aenigmatite stability in silica-undersaturated rocks
- Creator
- Marsh, Julian S
- Date
- 1975
- Type
- text
- Type
- article
- Identifier
- http://hdl.handle.net/10962/132942
- Identifier
- vital:36911
- Identifier
- https://doi.org/10.1007/BF00373333
- Description
- Aenigmatite is common in many trachytes, phonolites and agpaitic nepheline syenites. Petrographic evidence suggests that the aenigmatite in these rocks arises by the reaction of Ti-magnetite with a peralkaline silica-undersaturated liquid, and it is postulated that a no-oxide field, where aenigmatite is stable, exists in alkaline undersaturated magmas.
- Format
- 10 pages, pdf
- Language
- English
- Relation
- Contributions to Mineralogy and Petrology, Marsh, J.S., 1975. Aenigmatite stability in silica-undersaturated rocks. Contributions to Mineralogy and Petrology, 50(2), pp.135-144., Contributions to Mineralogy and Petrology volume 50 number 2 135 144 1975 1432-0967
- Rights
- Springer
- Rights
- Use of this resource is governed by the terms and conditions of the SpringerLink Terms of Use Statement (https://link.springer.com/termsandconditions)
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Marsh, Julian (Goonie)(Prof)
RU Department of Geology
SDG 13. Climate Action
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