The effect of gradients in regional stress and magma pressure on the form of sheet intrusions in cross section
- 10 February 1976
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 81 (5) , 975-984
- https://doi.org/10.1029/jb081i005p00975
Abstract
No abstract availableKeywords
This publication has 14 references indexed in Scilit:
- Mechanics of growth of some laccolithic intrusions in the Henry mountains, Utah, II: Bending and failure of overburden layers and sill formationPublished by Elsevier ,2003
- Mechanics of growth of some laccolithic intrusions in the Henry mountains, Utah, I: Field observations, Gilbert's model, physical properties and flow of the magmaPublished by Elsevier ,2003
- The Form and Growth of Fingered Sheet IntrusionsGSA Bulletin, 1975
- Derivation and evaluation of a mechanical model for sheet intrusionsTectonophysics, 1973
- Theory of water-filled crevasses in glaciers applied to vertical magma transport beneath oceanic ridgesJournal of Geophysical Research, 1971
- Rheology of Basalt in the Melting RangeJournal of Petrology, 1969
- Depth and spacing of tension cracksJournal of Geophysical Research, 1961
- FracturePublished by Springer Nature ,1958
- XVII.—The Dynamics of Sheet IntrusionProceedings of the Royal Society of Edinburgh, 1939
- Igneous geology of the Spanish Peaks region, ColoradoGSA Bulletin, 1936