Viscosities in the system albite - anorthite.

D. Cranmer; D. R. Uhlmann

doi:10.1029/JB086iB09p07951

Viscosities in the system albite - anorthite.

D. Cranmer, D. R. Uhlmann

Research output: Contribution to journal › Article › peer-review

44 Scopus citations

Abstract

The viscosities of several compositions were measured from 800o to 1600oC. The logeta vs 1/T show continuous curvature for all compositions. The viscosity-T relations have a crossover so that at approx 750oC, viscosity increases with An content.-K.A.R.

Original language	English (US)
Pages (from-to)	7951-7956
Number of pages	6
Journal	Journal of Geophysical Research
Volume	86
Issue number	B9
DOIs	https://doi.org/10.1029/JB086iB09p07951
State	Published - Jan 1 1981
Externally published	Yes

ASJC Scopus subject areas

Geophysics
Forestry
Oceanography
Aquatic Science
Ecology
Water Science and Technology
Soil Science
Geochemistry and Petrology
Earth-Surface Processes
Atmospheric Science
Earth and Planetary Sciences (miscellaneous)
Space and Planetary Science
Palaeontology

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title = "Viscosities in the system albite - anorthite.",

abstract = "The viscosities of several compositions were measured from 800o to 1600oC. The logeta vs 1/T show continuous curvature for all compositions. The viscosity-T relations have a crossover so that at approx 750oC, viscosity increases with An content.-K.A.R.",

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year = "1981",

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AU - Uhlmann, D. R.

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AB - The viscosities of several compositions were measured from 800o to 1600oC. The logeta vs 1/T show continuous curvature for all compositions. The viscosity-T relations have a crossover so that at approx 750oC, viscosity increases with An content.-K.A.R.

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Viscosities in the system albite - anorthite.

Abstract

ASJC Scopus subject areas

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