Abstract
Knowledge of volatile cycling is vital to understanding the evolution of the planet and the life it supports. Although it has been gradually accepted that the mantle is a vast storehouse of H2O and other volatiles, the impact of coexisting volatiles on the thermal stabilities of OH and the lattice of the host mineral is still poorly understood. Phlogopite is one of the few hydrous minerals capable of carrying both water and halogens into the mantle. Previous observations from both experiments and textural relationships in natural samples have indicated that F-rich phlogopite can be stable under ultrahigh-temperature conditions. Here, the impact of F on the thermal stability of phlogopite was investigated via XRD, Raman, and IR spectroscopy from room temperature to 1000 to 1200 °C. Based on the experimental results from F-poor and F-rich natural phlogopites, we show that about 4 wt% F can increase the breakdown temperature of phlogopite by 100 °C under ambient pressure. The impact mechanism mainly involves preventing OH and lattice softening at high temperatures. This study reveals the links between F and the behavior of OH and phlogopite lattice, which is important for constraining volatile cycling, as well as the role of F in the physical and chemical properties of the upper mantle.
Funding statement: Can Rao and Suwen Qiu are thanked for the analysis of F using EPMA. Associate editor Daniel Harlov is thanked for his extensive editing of the manuscript. This work is supported by the National Natural Science Foundation of China (41972038), the Zhejiang Province Natural Science Foundation of China (LY18D020001), and the Fundamental Research Funds for the Central Universities (K20210168).
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Articles in the same Issue
- Ab initio study of the structure and relative stability of MgSiO4H2 polymorphs at high pressures and temperatures
- Thermal conductivity of single-crystal brucite at high pressures: Implications for thermal anomaly in the shallow lower mantle
- Magmatic volatiles and platinum-group element mineralization in the Stillwater layered intrusion, U.S.A
- Impact of fluorine on the thermal stability of phlogopite
- Ferrous hydroxychlorides hibbingite [γ-Fe2(OH)3Cl] and parahibbingite [β-Fe2(OH)3Cl] as a concealed sink of Cl and H2O in ultrabasic and granitic systems
- Chukochenite, (Li0.5Al0.5)Al2O4, a new lithium oxyspinel mineral from the Xianghualing skarn, Hunan Province, China
- Ground-truthing the pyrite trace element proxy in modern euxinic settings
- Interplay between fluid circulation and Alpine metamorphism in the Monte Rosa whiteschist from white mica and quartz in situ oxygen isotope analysis by SIMS
- Atomic-scale structure and non-stoichiometry of meteoritic hibonite: A transmission electron microscope study
- Synthesis, structure, and single-crystal elasticity of Al-bearing superhydrous phase B
- Specific roles of sodium for the formation process of manganese-substituted octacalcium phosphate
- Oxygen isotope heterogeneity of olivine crystals in orogenic peridotites from Songshugou, North Qinling Orogen: Petrogenesis and geodynamic implications
- Effects of arsenic on the distribution and mode of occurrence of gold during fluid-pyrite interaction: A case study of pyrite from the Qiucun gold deposit, China
- Xuite, Ca3Fe2[(Al,Fe)O3(OH)]3, a new mineral of the garnet group: Implications for the wide occurrence of nanominerals
- Raman spectroscopy-based screening of zircon for reliable water content and oxygen isotope measurements
- Halogen (F, Cl, Br, I) contents in silt and clay fractions of a Cambisol from a temperate forest
- Resolving sub-micrometer-scale zonation of trace elements in quartz using TOF-SIMS
- Hexagonal magnetite in Algoma-type banded iron formations of the ca. 2.52 Ga Baizhiyan Formation, North China: Evidence for a green rust precursor?
- Presentation of the Dana Medal of the Mineralogical Society of America for 2021 to Sergey Krivovichev
- Acceptance of the Dana Medal of the Mineralogical Society of America for 2021
- Presentation of the 2021 MSA Distinguished Public Service Medal to Denton Ebel
- Acceptance of the Distinguished Public Service Medal of the Mineralogical Society of America for 2021
- Presentation of the Mineralogical Society of America Award for 2021 to Chenguang Sun
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Articles in the same Issue
- Ab initio study of the structure and relative stability of MgSiO4H2 polymorphs at high pressures and temperatures
- Thermal conductivity of single-crystal brucite at high pressures: Implications for thermal anomaly in the shallow lower mantle
- Magmatic volatiles and platinum-group element mineralization in the Stillwater layered intrusion, U.S.A
- Impact of fluorine on the thermal stability of phlogopite
- Ferrous hydroxychlorides hibbingite [γ-Fe2(OH)3Cl] and parahibbingite [β-Fe2(OH)3Cl] as a concealed sink of Cl and H2O in ultrabasic and granitic systems
- Chukochenite, (Li0.5Al0.5)Al2O4, a new lithium oxyspinel mineral from the Xianghualing skarn, Hunan Province, China
- Ground-truthing the pyrite trace element proxy in modern euxinic settings
- Interplay between fluid circulation and Alpine metamorphism in the Monte Rosa whiteschist from white mica and quartz in situ oxygen isotope analysis by SIMS
- Atomic-scale structure and non-stoichiometry of meteoritic hibonite: A transmission electron microscope study
- Synthesis, structure, and single-crystal elasticity of Al-bearing superhydrous phase B
- Specific roles of sodium for the formation process of manganese-substituted octacalcium phosphate
- Oxygen isotope heterogeneity of olivine crystals in orogenic peridotites from Songshugou, North Qinling Orogen: Petrogenesis and geodynamic implications
- Effects of arsenic on the distribution and mode of occurrence of gold during fluid-pyrite interaction: A case study of pyrite from the Qiucun gold deposit, China
- Xuite, Ca3Fe2[(Al,Fe)O3(OH)]3, a new mineral of the garnet group: Implications for the wide occurrence of nanominerals
- Raman spectroscopy-based screening of zircon for reliable water content and oxygen isotope measurements
- Halogen (F, Cl, Br, I) contents in silt and clay fractions of a Cambisol from a temperate forest
- Resolving sub-micrometer-scale zonation of trace elements in quartz using TOF-SIMS
- Hexagonal magnetite in Algoma-type banded iron formations of the ca. 2.52 Ga Baizhiyan Formation, North China: Evidence for a green rust precursor?
- Presentation of the Dana Medal of the Mineralogical Society of America for 2021 to Sergey Krivovichev
- Acceptance of the Dana Medal of the Mineralogical Society of America for 2021
- Presentation of the 2021 MSA Distinguished Public Service Medal to Denton Ebel
- Acceptance of the Distinguished Public Service Medal of the Mineralogical Society of America for 2021
- Presentation of the Mineralogical Society of America Award for 2021 to Chenguang Sun
- Acceptance of the Mineralogical Society of America Award for 2021
- Presentation of the 2021 Roebling Medal of the Mineralogical Society of America to George Rossman
- Acceptance of the 2021 Roebling Medal of the Mineralogical Society of America