Temperature gradients in the upper layers of the Earth's crust due to convective water flows

DOI10.1029/JZ067i009p03449zbMath0122.23406MaRDI QIDQ5734355

I. G. Donaldson

Publication date: 1962

Published in: Journal of Geophysical Research (Search for Journal in Brave)

zbMATH Keywords

astronomy, astrophysics, geophysics

Related Items (3)

The effect of conducting bounding plates on the onset of Horton-Rogers-Lapwood convection ⋮ Effects of medium thermoelasticity on high Rayleigh number steady-state heat transfer and mineralization in deformable fluid-saturated porous media heated from below ⋮ The onset of convection in porous layers with multiple horizontal partitions

This page was built for publication: Temperature gradients in the upper layers of the Earth's crust due to convective water flows