2023-02-142023-02-141980-01-10https://repository.tcu.edu/handle/116099117/57140Article focused on comparing elemental retentivity between samples from the Allende and Murchison stones when heated to high temperatures. Concludes that the broad differences demonstrates vastly different compositions.Prior written permission from TCU Special Collections required to use any document or photograph.MeteoriteAllende (Mexico)Abee stoneKrymkaTieschitzMurchison (Victoria, Australia)Enstatite chondriteAchondriteCarbonaceous chondriteArsenicCopperRubidiumAntimonyGeochimica et Cosmochimica ActaThermal Metamorphism of Primitive Meteorites - X. Additional Trace Elements in Allende (C3V) heated to 1400 CDocument