Contributions to Mineralogy and Petrology , 2004, V 146, N 6, February.

   Can metamorphic reactions proceed faster than bulk strain?  
   Ethan F. Baxter, Donald J. DePaolo  
   pp. 657 - 670  
   
   Microstructural evolution and grain boundary structure during 
   static recrystallization in synthetic polycrystals of Sodium 
   Chloride containing saturated brine   
   Oliver Schenk, Janos L. Urai  
   pp. 671 - 682
   
   Oxygen isotope exchange and disequilibrium between calcite 
   and tremolite in the absence and presence of an experimental 
   C–O–H fluid   
   Y.-F. Zheng, M. Satir, P. Metz  
   pp. 683 - 695 
   
   Multi-stage metasomatism of diamondiferous eclogite 
   xenoliths from the Udachnaya kimberlite pipe, Yakutia, Siberia  
   Kula C. Misra, Mahesh Anand, Lawrence A. Taylor, et al.  
   pp. 696 - 714    
        
   Nature and timing of magma interactions before, during, 
   and after the caldera-forming eruption of Volcan Ceboruco, 
   Mexico 
   Darren G. Chertkoff, James E. Gardner  
   pp. 715 - 735  
   
  Mobility of metamorphic fluids inferred from infrared 
  microspectroscopy on natural fluid inclusions:
  the example of Tinos Island, Greece 
  Vincent Famin, Satoru Nakashima, Laurent Jolivet, et al.  
  pp. 736 - 749  
        
  Oxidized sulfur-rich mafic magma at Mount 
  Pinatubo, Philippines  
  J. C. M. de Hoog, K. H. Hattori, R. P. Hoblitt  
  pp. 750 - 761  
        
  Thermodynamic analysis of the system 
  Na 2O-K 2O-CaO-Al 2O 3-SiO 2-H 2O-F 2O -1: 
  Stability of fluorine-bearing minerals in felsic 
  igneous suites  
  David Dolejs, Don R. Baker  
  pp. 762 - 778  
   
  Erratum 
  The ‘Profile’ method of calculating the composition
  of solid in magma fractionation, and its application
  to an alkaline volcano  
  Wallace H. MacLean  
  p. 779