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: | Oleg Safonov, Valentina Butvina, Evgenii Limanov |
---|---|
Format: | Article |
Language: | English |
Published: |
MDPI AG
2019-11-01
|
Series: | Minerals |
Subjects: | |
Online Access: | https://www.mdpi.com/2075-163X/9/11/685 |
Similar Items
-
METASOMATIC AND MAGMATIC PROCESSES IN THE MANTLE LITHOSPHERE OF THE BIREKTE TERRAIN OF THE SIBERIAN CRATON AND THEIR EFFECT ON THE LITHOSPHERE EVOLUTION
by: Lidia V. Solov’eva, et al.
Published: (2015-10-01) -
The influence of mantle metasomatism on the oxidation state of the lithospheric mantle
by: Creighton, Steven
Published: (2009) -
Boron Isotopic Composition of the Subcontinental Lithospheric Mantle
Published: (2014) -
Composition Heterogeneity of Xenoliths of Mantle Peridotites from Alkaline Basalts of the Sverre Volcano, the Svalbard Archipelago
by: Dmitriy S. Ashikhmin, et al.
Published: (2019-10-01) -
CO2, carbonate-rich melts, and brines in the mantle
by: Maria-Luce Frezzotti, et al.
Published: (2014-09-01)