Phlogopite-Forming Reactions as Indicators of Metasomatism in the Lithospheric Mantle
Phlogopite is widely accepted as a major mineral indicator of the modal metasomatism in the upper mantle within a very wide P−T range. The paper reviews data on various phlogopite-forming reactions in upper-mantle peridotites. The review includes both descriptions of naturally occurring re...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
MDPI AG
2019-11-01
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| Series: | Minerals |
| Subjects: | |
| Online Access: | https://www.mdpi.com/2075-163X/9/11/685 |