Article
Publicly Available
Timing and mechanisms of carbon isotope exchange in granulite-facies calc-silicate boudins, Rauer Group, East Antarctica
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Ian Cartwright
Published/Copyright:
November 13, 2015
Received: 1996-3-26
Accepted: 1996-12-9
Published Online: 2015-11-13
Published in Print: 1997-3-1
© 2015 by Walter de Gruyter Berlin/Boston
Articles in the same Issue
- Review: Theory of displacive phase transitions in minerals
- Single-crystal compression and crystal structure of clinopyroxene up to 10 GPa
- K in clinopyroxene at high pressure and temperature: An experimental study
- Crystal structure of monoclinic hydrous wadsleyite [β-(Mg,Fe)2SiO4]
- Natural kalsilite, KAlSiO4, with P31c symmetry: Crystal structure and twinning
- Al, Si, and Mg occupancies in tetrahedrally and octahedrally coordinated sites in synthetic aluminous tremolite
- Site occupancies in synthetic monoclinic amphiboles: Rietveld structure refinement and infrared spectroscopy of (nickel, magnesium, cobalt)-richterite
- Transformation of mackinawite to greigite: An in situ X-ray powder diffraction and transmission electron microscope study
- Cathodoluminescence of meteoritic and synthetic forsterite at 296 and 77 K using TEM
- Cl incorporation into successively zoned amphiboles from the Ramnes cauldron, Norway
- Multi-site order-disorder kinetics in crystalline solids: A generalized formulation
- Redox conditions in piston-cylinder apparatus: The different behavior of boron nitride and unfired pyrophyllite assemblies
- A new garnet-orthopyroxene thermometer based on reversed Al2O3 solubility in FeO-Al2O3-SiO2 orthopyroxene
- Melting experiments on komatiite analog compositions at 5 GPa
- Degassing of alkalic basalts
- Phase relations among smectite, R1 illite-smectite, and illite
- Timing and mechanisms of carbon isotope exchange in granulite-facies calc-silicate boudins, Rauer Group, East Antarctica
- Changes in the crystal structure of tsaregorodtsevite [N(CH3)4][Si2(Si0.5Al0.5)O6]2 on heating
- Surite: Its Structure and Properties
- Terranovaite from Antarctica: A new ‘pentasil’ zeolite
Articles in the same Issue
- Review: Theory of displacive phase transitions in minerals
- Single-crystal compression and crystal structure of clinopyroxene up to 10 GPa
- K in clinopyroxene at high pressure and temperature: An experimental study
- Crystal structure of monoclinic hydrous wadsleyite [β-(Mg,Fe)2SiO4]
- Natural kalsilite, KAlSiO4, with P31c symmetry: Crystal structure and twinning
- Al, Si, and Mg occupancies in tetrahedrally and octahedrally coordinated sites in synthetic aluminous tremolite
- Site occupancies in synthetic monoclinic amphiboles: Rietveld structure refinement and infrared spectroscopy of (nickel, magnesium, cobalt)-richterite
- Transformation of mackinawite to greigite: An in situ X-ray powder diffraction and transmission electron microscope study
- Cathodoluminescence of meteoritic and synthetic forsterite at 296 and 77 K using TEM
- Cl incorporation into successively zoned amphiboles from the Ramnes cauldron, Norway
- Multi-site order-disorder kinetics in crystalline solids: A generalized formulation
- Redox conditions in piston-cylinder apparatus: The different behavior of boron nitride and unfired pyrophyllite assemblies
- A new garnet-orthopyroxene thermometer based on reversed Al2O3 solubility in FeO-Al2O3-SiO2 orthopyroxene
- Melting experiments on komatiite analog compositions at 5 GPa
- Degassing of alkalic basalts
- Phase relations among smectite, R1 illite-smectite, and illite
- Timing and mechanisms of carbon isotope exchange in granulite-facies calc-silicate boudins, Rauer Group, East Antarctica
- Changes in the crystal structure of tsaregorodtsevite [N(CH3)4][Si2(Si0.5Al0.5)O6]2 on heating
- Surite: Its Structure and Properties
- Terranovaite from Antarctica: A new ‘pentasil’ zeolite