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Published 1993 | Published
Journal Article Open

The relationship between stable isotope diffusion, zonation and thermometry: a case study from the Adirondack Mountains, NY

Abstract

Retrograde diffusion is recognized as an important factor in the stable isotope geochemistry of slowly cooled rocks. However, it has never been demonstrated by micro-analysis that natural minerals are zoned with respect to stable isotopes in a way consistent with closed system interdiffusion during cooling.

Additional Information

© 1993 American Geophysical Union.

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