A revision of metallographic cooling rate curves for chondrites
New metallographic cooling rate curves for the chondritic meteorites are calculated. On the basis of these curves, estimated cooling rates for the chondrites are twice as fast as those determined using the Wood (1967) curves. This change in estimated rates derives from the use of the most recent Fe-Ni phase diagram and the use of more accurate computational techniques. The new cooling rate curves can be applied to meteorites with P contents in the metal phase less than 0.01 wt%. They should be applied with some caution to meteorites, such as the unequilibrated ordinary chondrites, where the metal grains may not have equilibrated above approximately 850K, or to metallic phases which contain P in quantities greater than 0.01 wt% and/or phosphides.