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        Publicly Available
    
                
        
        
            
            
                
            
            
            
            
            
            
        
    
    
    Atomic-resolution transmission electron microscope evidence for the mechanism by which chlorite weathers to 1:1 semi-regular chlorite-vermiculite
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        Jillian F. Banfield
        
 and Takashi Murakami 
                            Published/Copyright:
                            
                                November 13, 2015
                            
                        
                    
                
            
  Received: 1997-3-28
 
 
  Accepted: 1997-10-13
 
 
  Published Online: 2015-11-13
 
 
  Published in Print: 1998-3-1
 
© 2015 by Walter de Gruyter Berlin/Boston
Articles in the same Issue
- Reversed determination of the reaction: Phlogopite + quartz = enstatite + potassium feldspar + H2O in the ranges 750–875 °C and 2–12 kbar at low H2O activity with concentrated KCl solutions
 - Phase relations in the system MgO-NaCl-H2O: The dehydroxylation of brucite in the presence of NaCl-H2O fluids
 - Experimental determination of the reaction: Magnesite + enstatite = forsterite + CO2 in the ranges 6–25 kbar and 700–1100 °
 - An experimental study of the pressure-temperature stability of MgMgAl-pumpellyite in the system MgO-Al2O3-SiO2-H2O
 - Off-center hot spots: Double thermocouple determination of the thermal gradient in a 1.27 cm (1/2 in.) CaF2 piston-cylinder furnace assembly
 - Viscosity data for hydrous peraluminous granitic melts: Comparison with a metaluminous model
 - Sr-bearing zoisite and epidote in ultra-high pressure (UHP) metamorphic rocks from the Su-Lu province, eastern China: An important Sr reservoir under UHP conditions
 - Replacement of primary monazite by apatite-allanite-epidote coronas in an amphibolite facies granite gneiss from the eastern Alps
 - The chemical composition of REE-Y-Th-U-rich accessory minerals in peraluminous granites of the Erzgebirge-Fichtelgebirge region, Germany, Part I: The monazite-(Ce)-brabantite solid solution series
 - Chemical microstructure of Franciscan jadeite from Pacheco Pass, California
 - Effects of Mg-Fe2+ substitution in calcite-structure carbonates: Thermoelastic properties
 - High-pressure single-crystal X-ray diffraction and infrared spectroscopic studies of the C2/m-P21/m phase transition in cummingtonite
 - Full multiple scattering calculations of the X-ray absorption near edge structure at the magnesium K-edge in pyroxene
 - Interpretation of XPS Mn(2p) spectra of Mn oxyhydroxides and constraints on the mechanism of MnO2 precipitation
 - Reactions of aqueous Au1+ sulfide species with pyrite as a function of pH and temperature
 - Mineralogy of the Louvres Merovingian garnet cloisonné jewelry: Origins of the gems of the first kings of France
 - Temperature dependence of the OH⁻ absorption in SiO2 glass and melt to 1975 K
 - High-temperature multi-nuclear NMR investigation of analcime
 - Atomic-resolution transmission electron microscope evidence for the mechanism by which chlorite weathers to 1:1 semi-regular chlorite-vermiculite
 - Structure and formation mechanism of low-angle grain boundaries in chlorite
 - Stacking disorder and polytypism in enargite and luzonite
 - Relationships between microstructure and composition in enargite and luzonite
 - Description and crystal structure of Yvonite, Cu(AsO3OH)2H2O
 - Georgeericksenite, Na6CaMg(IO3)6(CrO4)2(H2O)12, a new mineral from Oficina Chacabuco, Chile: Description and crystal structure
 - LETTER. Crystal structure of a new spinelloid with the wadsleyite structure in the system Fe2SiO4-Fe3O4 and implications for the Earth’s mantle
 - Heat capacity and thermodynamic properties for coesite and jadeite, reexamination of the quartz-coesite equilibrium boundary
 
Articles in the same Issue
- Reversed determination of the reaction: Phlogopite + quartz = enstatite + potassium feldspar + H2O in the ranges 750–875 °C and 2–12 kbar at low H2O activity with concentrated KCl solutions
 - Phase relations in the system MgO-NaCl-H2O: The dehydroxylation of brucite in the presence of NaCl-H2O fluids
 - Experimental determination of the reaction: Magnesite + enstatite = forsterite + CO2 in the ranges 6–25 kbar and 700–1100 °
 - An experimental study of the pressure-temperature stability of MgMgAl-pumpellyite in the system MgO-Al2O3-SiO2-H2O
 - Off-center hot spots: Double thermocouple determination of the thermal gradient in a 1.27 cm (1/2 in.) CaF2 piston-cylinder furnace assembly
 - Viscosity data for hydrous peraluminous granitic melts: Comparison with a metaluminous model
 - Sr-bearing zoisite and epidote in ultra-high pressure (UHP) metamorphic rocks from the Su-Lu province, eastern China: An important Sr reservoir under UHP conditions
 - Replacement of primary monazite by apatite-allanite-epidote coronas in an amphibolite facies granite gneiss from the eastern Alps
 - The chemical composition of REE-Y-Th-U-rich accessory minerals in peraluminous granites of the Erzgebirge-Fichtelgebirge region, Germany, Part I: The monazite-(Ce)-brabantite solid solution series
 - Chemical microstructure of Franciscan jadeite from Pacheco Pass, California
 - Effects of Mg-Fe2+ substitution in calcite-structure carbonates: Thermoelastic properties
 - High-pressure single-crystal X-ray diffraction and infrared spectroscopic studies of the C2/m-P21/m phase transition in cummingtonite
 - Full multiple scattering calculations of the X-ray absorption near edge structure at the magnesium K-edge in pyroxene
 - Interpretation of XPS Mn(2p) spectra of Mn oxyhydroxides and constraints on the mechanism of MnO2 precipitation
 - Reactions of aqueous Au1+ sulfide species with pyrite as a function of pH and temperature
 - Mineralogy of the Louvres Merovingian garnet cloisonné jewelry: Origins of the gems of the first kings of France
 - Temperature dependence of the OH⁻ absorption in SiO2 glass and melt to 1975 K
 - High-temperature multi-nuclear NMR investigation of analcime
 - Atomic-resolution transmission electron microscope evidence for the mechanism by which chlorite weathers to 1:1 semi-regular chlorite-vermiculite
 - Structure and formation mechanism of low-angle grain boundaries in chlorite
 - Stacking disorder and polytypism in enargite and luzonite
 - Relationships between microstructure and composition in enargite and luzonite
 - Description and crystal structure of Yvonite, Cu(AsO3OH)2H2O
 - Georgeericksenite, Na6CaMg(IO3)6(CrO4)2(H2O)12, a new mineral from Oficina Chacabuco, Chile: Description and crystal structure
 - LETTER. Crystal structure of a new spinelloid with the wadsleyite structure in the system Fe2SiO4-Fe3O4 and implications for the Earth’s mantle
 - Heat capacity and thermodynamic properties for coesite and jadeite, reexamination of the quartz-coesite equilibrium boundary