Abstract
Conduit flow and subaerial plume buoyancy models are combined to model
venusian volcanism under a range of conditions. Results are described
using case studies.
| Original language | English |
|---|---|
| Pages (from-to) | 1282 |
| Journal | 44th Lunar and Planetary Science Conference, held March 18-22, 2013 in The Woodlands, Texas |
| Volume | 44 |
| Publication status | Published - 1 Mar 2013 |
Cite this
- APA
- Author
- BIBTEX
- Harvard
- Standard
- RIS
- Vancouver