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On the significance of argon release from biotite and amphibole during sup 40 Ar/ sup 39 Ar vacuum heating

Journal Article · · Geochimica et Cosmochimica Acta; (USA)
The nature of Ar release from biotite and amphibole is addressed via vacuum-heating experiments followed by measurements of {sup 40}Ar loss and unit cell parameters and scanning electron microscope observations of the heated specimens. {sup 40}Ar diffusion during hydrothermal heating was previously reported for the studied biotite and amphibole specimens allowing direct comparison to the Ar loss kinetics from vacuum heating. The results demonstrate conclusively that volume diffusion is not the mechanism controlling Ar loss during normal {sup 40}Ar/{sup 39}Ar measurements. These hydrous minerals also suffer weight loss and irreversible structural changes in the range 600 to 800{degree}C. Moreover, biotite suffers morphological modifications dramatically expressed by splitting along the basal cleavage. A few experiments on muscovite suggest similar weight loss and splitting effects. The behavior of these minerals has important implications for the interpretation of {sup 40}Ar/{sup 39}Ar step-heating data. The Ar-loss kinetics of {sup 40}Ar/{sup 39}Ar experiments cannot be used to calculate diffusion coefficients and it is inappropriate to estimate closure temperatures from such data. The morphological changes will not permit the meaningful resolution of fossil Ar gradients which may have been present in the initial grains.
OSTI ID:
5207234
Journal Information:
Geochimica et Cosmochimica Acta; (USA), Journal Name: Geochimica et Cosmochimica Acta; (USA) Vol. 52:10; ISSN GCACA; ISSN 0016-7037
Country of Publication:
United States
Language:
English