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 |
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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 |