Fluid flow through a large vertical crack in the Earth's crust
- 10 February 1977
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 82 (5) , 929-932
- https://doi.org/10.1029/jb082i005p00929
Abstract
No abstract availableKeywords
This publication has 6 references indexed in Scilit:
- The effect of gradients in regional stress and magma pressure on the form of sheet intrusions in cross sectionJournal of Geophysical Research, 1976
- On the stability of open hydraulic fractures in the Earth's crustGeophysical Research Letters, 1975
- Fracture in rockReviews of Geophysics, 1975
- OCEANIC RIDGES, MAGMA FILLED CRACKS, AND MANTLE PLUMESGeofísica Internacional, 1973
- Velocity at which liquid-filled cracks move in the Earth's crust or in glaciersJournal of Geophysical Research, 1971
- Theory of water-filled crevasses in glaciers applied to vertical magma transport beneath oceanic ridgesJournal of Geophysical Research, 1971