JOURNAL OF METAMORPHIC GEOLOGY, 2000 SEP, V18, N5.

   1.1 Ralser, S.
         Microstructural constraints on the timing of Proterozoic
       deformation in central New Mexico.                           
       pp. 457-466
       
   1.2 Miler, JA; Cartwright, I.
         Distinguishing between seafloor alteration and fluid flow
       during subduction using stable isotope geochemistry:
       examples from Tethyan ophiolites in the Western Alps.        
       pp. 467-482
       
   1.3 Onen, AP; Hall, R.
         Sub-ophiolite metamorphic rocks from NW Anatolia, Turkey.  
         pp. 483-495
         
   1.4 White, RW; Powell, R; Holland, TJB; Worley, BA.
         The effect of TiO2 and Fe2O3 on metapelitic assemblages at
       greenschist and amphibolite facies conditions: mineral
       equilibria calculations in the system
       K2O-FeO-MgO-Al2O3-SiO2-H2O-TiO2-Fe2O3.                       
       pp. 497-511
       
   1.5 Liogys, VA; Jenkins, DM.
         Hornblende geothermometry of amphibolite layers of the
       Popple Hill gneiss, north-west Adirondack Lowlands, New
       York, USA.                                     
       pp. 513-530
       
   1.6 Arkai, P; Mata, MP; Giorgetti, G; Peacor, DR; and others.
         Comparison of diagenetic and low-grade metamorphic
       evolution of chlorite in associated metapelites and
       metabasites: an integrated TEM and XRD study.                
       pp. 531-550
       
   1.7 Cooke, RA; O'Brien, PJ; Carswell, DA.
         Garnet zoning and the identification of equilibrium
       mineral compositions in high-pressure-temperature granulites
       from the Moldanubian Zone, Austria.                         
       pp.  551-569
       
   1.8 Stephenson, BJ; Waters, DJ; Searle, MP.
         Inverted metamorphism and the main central thrust: field
       relations and thermobarometric constraints from the Kishtwar
       Window, NW Indian Himalaya.                                  
       pp.  571-590
       
   1.9 Spiess, R; Bertolo, B; Borghi, A; Chinellato, M; and others.
         Microtextures of opaque inclusions: their use as
       indicators for hiatuses during garnet porphyroblast growth.  
       pp. 591-603