Effect of material anisotropy on the onset of convective flow in three-dimensional fluid-saturated faults

DOI10.1023/A:1023283421049zbMath1107.86004OpenAlexW1548094752MaRDI QIDQ1402237

Chongbin Zhao, Ge Lin, Hans B. Muhlhaus, Bruce E. Hobbs, Alison Ord

Publication date: 20 August 2003

Published in: Mathematical Geology (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1023/a:1023283421049

zbMATH Keywords

analytical solutioncritical Rayleigh numberconvective instabilitymaterial anisotropythree-dimensional fault

Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) Stability and instability of geophysical and astrophysical flows (76E20)

Related Items (1)

Double diffusion-driven convective instability of three-dimensional fluid-saturated geological fault zones heated from below

This page was built for publication: Effect of material anisotropy on the onset of convective flow in three-dimensional fluid-saturated faults