Consequences of viscous anisotropy in a deforming, two-phase aggregate. Why is porosity-band angle lowered by viscous anisotropy?

DOI10.1017/JFM.2015.592zbMath1382.76010arXiv1506.05286OpenAlexW2963783163WikidataQ57861604 ScholiaQ57861604MaRDI QIDQ2797040

Yasuko Takei, Richard F. Katz

Publication date: 30 March 2016

Published in: Journal of Fluid Mechanics (Search for Journal in Brave)

Full work available at URL: https://arxiv.org/abs/1506.05286

zbMATH Keywords

rheologynon-Newtonian flowsmagma and lava flow

Mathematics Subject Classification ID

Non-Newtonian fluids (76A05) Seismology (including tsunami modeling), earthquakes (86A15)

Related Items (1)

Granular dilatancy and non-local fluidity of partially molten rock

Cites Work

• Consequences of viscous anisotropy in a deforming, two-phase aggregate. Part 1. Governing equations and linearized analysis
• Consequences of viscous anisotropy in a deforming, two-phase aggregate. Part 2. Numerical solutions of the full equations

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