Tharsis‐radial graben systems as the surface manifestation of plume‐related dike intrusion complexes: Models and implications
- 1 August 2002
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 107 (E8) , 1-1-1-24
- https://doi.org/10.1029/2001je001593
Abstract
No abstract availableKeywords
This publication has 77 references indexed in Scilit:
- Surface deformation in volcanic rift zonesPublished by Elsevier ,2003
- Primary centers and secondary concentrations of tectonic activity through time in the western hemisphere of MarsJournal of Geophysical Research, 2001
- Evidence for episodicity in the magma supply to the large Tharsis volcanoesJournal of Geophysical Research, 2001
- An altitude‐normalized magnetic map of Mars and its interpretationGeophysical Research Letters, 2000
- Identification of a basaltic component on the Martian surface from Thermal Emission Spectrometer dataJournal of Geophysical Research, 2000
- Mantle convection and the dynamic geoid of MarsGeophysical Research Letters, 2000
- Thermal and mechanical aspects of magma emplacement in giant dike swarmsJournal of Geophysical Research, 1999
- Extension across Tempe Terra, Mars, from measurements of fault scarp widths and deformed cratersJournal of Geophysical Research, 1996
- The global distribution of giant radiating dike swarms on Venus: Implications for the global stress stateGeophysical Research Letters, 1994
- Evidence from magnetic fabric for the flow pattern of magma in the Mackenzie giant radiating dyke swarmNature, 1992