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Hydrogen in Feldspars and Related Silicates

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Feldspars and their Reactions

Part of the book series: NATO ASI Series ((ASIC,volume 421))

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Abstract

The importance of trace quantities of hydrogen in feldspars in determining the rates of intra-crystalline transport processes was suggested by several early experimental studies of Al-Si order-disorder in feldspars and oxygen isotope exchange between feldspars and water. With the aid of modern experimental and analytical techniques, it has been possible to distinguish solid-state from solutioncontrolled processes in hydrothermal experiments, and to confirm the conclusions of earlier studies. The identities of the hydrogen-bearing species which enhances diffusion processes and of the oxygentransporting species have however remained controversial.

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Authors and Affiliations

  1. Department of Geology and Geophysics, University of Edinburgh, Edinburgh, EH9 3JW, Scotland

    Colin M. Graham & Stephen C. Elphick

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  1. Colin M. Graham
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  2. Stephen C. Elphick
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  1. Department of Geology and Geophysics, The University of Edinburgh, Edinburgh, UK

    Ian Parsons

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Graham, C.M., Elphick, S.C. (1994). Hydrogen in Feldspars and Related Silicates. In: Parsons, I. (eds) Feldspars and their Reactions. NATO ASI Series, vol 421. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-1106-5_10

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  • DOI: https://doi.org/10.1007/978-94-011-1106-5_10

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  • Print ISBN: 978-94-010-4483-7

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