Chemical interdiffusion of dacite and rhyolite: anhydrous measurements at 1 atm and 10 kbar, application of transition state theory, and diffusion in zoned magma chambers-Reference-Cited by-同舟云学术

Chemical interdiffusion of dacite and rhyolite: anhydrous measurements at 1 atm and 10 kbar, application of transition state theory, and diffusion in zoned magma chambers

Published:1990-07 Issue:4 Volume:104 Page:407-423
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contr. Mineral. and Petrol.

Author:

Baker Don R.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/BF01575619.pdf

Reference61 articles.

1. Rev Mineral;DE Anderson,1981

2. Angell CA, Cheeseman PA, Tamaddon S (1983) Water-like transport property anomalies in liquid silicates investigated at high T and P by computer simulation techniques. Bull Mineral 106:87–97

3. Baker DR (1989) Tracer versus trace element diffusion: Diffusional decoupling of Sr concentration from Sr isotope composition. Geochim Cosmichim Acta 53:3015–3023

4. Baker DR, Watson EB (1988) Diffusion of major and trace elements in compositionally complex Cl- and F-bearing silicate melts. J Non-Cryst Solids 102:62–70

5. Bence AE, Albee AL (1968) Empirical correction factors for the electron microanalysis of silicates and oxides. J Geol 76:382–403

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