Temperature gradients in the upper layers of the Earth's crust due to convective water flows
- 1 August 1962
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 67 (9), 3449-3459
- https://doi.org/10.1029/jz067i009p03449
Abstract
No abstract availableKeywords
This publication has 2 references indexed in Scilit:
- Steady state free thermal convection of liquid in a saturated permeable mediumJournal of Fluid Mechanics, 1957
- Convection of a fluid in a porous mediumMathematical Proceedings of the Cambridge Philosophical Society, 1948