Abstract
Crystals constitute potential sources of information on magmatic timescales, conditions, and processes. One could say that the ecology of crystals in magmas is very rich, including phenocrysts, microlites, xenocrysts, and antecrysts, to name just a few types. A recent reassessment of thermodynamic equilibrium between crystals in the Bishop Tuff has concluded to the reliability of temperature estimates based on Fe-Ti oxides.
Keywords : Rhyolitic magma; crystals; thermodynamic equilibrium; pre-eruptive temperatures; Fe-Ti oxides
Received: 2013-1-2
Accepted: 2013-1-3
Published Online: 2015-3-7
Published in Print: 2013-4-1
© 2015 by Walter de Gruyter Berlin/Boston
You are currently not able to access this content.
You are currently not able to access this content.
Articles in the same Issue
- Highlight and Breakthrough. A fresh look at crystals in the Bishop Tuff
- Actinides in Geology, Energy, and the Environment. Remobilization of U and REE and the formation of secondary minerals in oxidized U deposits
- Actinides in Geology, Energy, and the Environment. Revision of the symmetry and the crystal structure of čejkaite, Na4(UO2)(CO3)3
- Characterization of ferric arsenate-sulfate compounds: Implications for arsenic control in refractory gold processing residues
- Crystal structure and chemistry of skarn-associated bismuthian vesuvianite
- Transformation of graphite to lonsdaleite and diamond in the Goalpara ureilite directly observed by TEM
- Quartz nanocrystals in the 2.48 Ga Dales Gorge banded iron formation of Hamersley, Western Australia: Evidence for a change from submarine to subaerial volcanism at the end of the Archean
- Synthesis and characterization of amphiboles along the tremolite–glaucophane join
- Elasticity of franklinite and trends for transition-metal oxide spinels
- Redox systematics of martian magmas with implications for magnetite stability
- Hydrogen incorporation and the oxidation state of iron in ringwoodite: A spectroscopic study
- Hydrous ringwoodite to 5 K and 35 GPa: Multiple hydrogen bonding sites resolved with FTIR spectroscopy
- Calibration of zircon as a Raman spectroscopic pressure sensor to high temperatures and application to water-silicate melt systems
- Computational study of the elastic behavior of the 2M1 muscovite-paragonite series
- Vanadium L2,3 XANES experiments and first-principles multielectron calculations: Impact of second-nearest neighboring cations on vanadium-bearing fresnoites
- A time-resolved X-ray diffraction study of Cs exchange into hexagonal H-birnessite
- Grain-boundary diffusion rates inferred from grain-size variations of quartz in metacherts from a contact aureole
- On the use of unpolarized infrared spectroscopy for quantitative analysis of absorbing species in birefringent crystals
- A computational model of cation ordering in the magnesioferrite-qandilite (MgFe2O4- Mg2TiO4) solid solution and its potential application to titanomagnetite (Fe3O4-Fe2TiO4)
- 3T-phlogopite from Kasenyi kamafugite (SW Uganda): EPMA, XPS, FTIR, and SCXRD study
- Revision of the crystal structure and chemical formula of haiweeite, Ca(UO2)2(Si5O12)(OH)2·6H2O
- Cation arrangement in the octahedral and tetrahedral sheets of cis-vacant polymorph of dioctahedral 2:1 phyllosilicates by quantum mechanical calculations
- High-pressure phase transitions of Fe3–xTixO4 solid solution up to 60 GPa correlated with electronic spin transition
- Hydrogen incorporation in crystalline zircon: Insight from ab initio calculations
- The vibrational features of hydroxylapatite and type A carbonated apatite: A first principle contribution
- STEM investigation of exsolution lamellae and “c” reflections in Ca-rich dolomite from the Platteville Formation, western Wisconsin
- Karenwebberite, Na(Fe2+,Mn2+)PO4, a new member of the triphylite group from the Malpensata pegmatite, Lecco Province, Italy
- The crystal structure of ramdohrite, Pb5.9Fe0.1Mn0.1In0.1Cd0.2Ag2.8Sb10.8S24: A new refinement
- Static disorders of atoms and experimental determination of Debye temperature in pyrope: Low- and high-temperature single-crystal X-ray diffraction study—Discussion
- Static disorders of atoms and experimental determination of Debye temperature in pyrope: Low- and high-temperature single-crystal X-ray diffraction study—Reply
Keywords for this article
Rhyolitic magma;
crystals;
thermodynamic equilibrium;
pre-eruptive temperatures;
Fe-Ti oxides
Articles in the same Issue
- Highlight and Breakthrough. A fresh look at crystals in the Bishop Tuff
- Actinides in Geology, Energy, and the Environment. Remobilization of U and REE and the formation of secondary minerals in oxidized U deposits
- Actinides in Geology, Energy, and the Environment. Revision of the symmetry and the crystal structure of čejkaite, Na4(UO2)(CO3)3
- Characterization of ferric arsenate-sulfate compounds: Implications for arsenic control in refractory gold processing residues
- Crystal structure and chemistry of skarn-associated bismuthian vesuvianite
- Transformation of graphite to lonsdaleite and diamond in the Goalpara ureilite directly observed by TEM
- Quartz nanocrystals in the 2.48 Ga Dales Gorge banded iron formation of Hamersley, Western Australia: Evidence for a change from submarine to subaerial volcanism at the end of the Archean
- Synthesis and characterization of amphiboles along the tremolite–glaucophane join
- Elasticity of franklinite and trends for transition-metal oxide spinels
- Redox systematics of martian magmas with implications for magnetite stability
- Hydrogen incorporation and the oxidation state of iron in ringwoodite: A spectroscopic study
- Hydrous ringwoodite to 5 K and 35 GPa: Multiple hydrogen bonding sites resolved with FTIR spectroscopy
- Calibration of zircon as a Raman spectroscopic pressure sensor to high temperatures and application to water-silicate melt systems
- Computational study of the elastic behavior of the 2M1 muscovite-paragonite series
- Vanadium L2,3 XANES experiments and first-principles multielectron calculations: Impact of second-nearest neighboring cations on vanadium-bearing fresnoites
- A time-resolved X-ray diffraction study of Cs exchange into hexagonal H-birnessite
- Grain-boundary diffusion rates inferred from grain-size variations of quartz in metacherts from a contact aureole
- On the use of unpolarized infrared spectroscopy for quantitative analysis of absorbing species in birefringent crystals
- A computational model of cation ordering in the magnesioferrite-qandilite (MgFe2O4- Mg2TiO4) solid solution and its potential application to titanomagnetite (Fe3O4-Fe2TiO4)
- 3T-phlogopite from Kasenyi kamafugite (SW Uganda): EPMA, XPS, FTIR, and SCXRD study
- Revision of the crystal structure and chemical formula of haiweeite, Ca(UO2)2(Si5O12)(OH)2·6H2O
- Cation arrangement in the octahedral and tetrahedral sheets of cis-vacant polymorph of dioctahedral 2:1 phyllosilicates by quantum mechanical calculations
- High-pressure phase transitions of Fe3–xTixO4 solid solution up to 60 GPa correlated with electronic spin transition
- Hydrogen incorporation in crystalline zircon: Insight from ab initio calculations
- The vibrational features of hydroxylapatite and type A carbonated apatite: A first principle contribution
- STEM investigation of exsolution lamellae and “c” reflections in Ca-rich dolomite from the Platteville Formation, western Wisconsin
- Karenwebberite, Na(Fe2+,Mn2+)PO4, a new member of the triphylite group from the Malpensata pegmatite, Lecco Province, Italy
- The crystal structure of ramdohrite, Pb5.9Fe0.1Mn0.1In0.1Cd0.2Ag2.8Sb10.8S24: A new refinement
- Static disorders of atoms and experimental determination of Debye temperature in pyrope: Low- and high-temperature single-crystal X-ray diffraction study—Discussion
- Static disorders of atoms and experimental determination of Debye temperature in pyrope: Low- and high-temperature single-crystal X-ray diffraction study—Reply