Pages that link to "Item:Q2269402"
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The following pages link to Effect of viscous dissipation on nonisothermal high-viscosity magma flow in a volcanic conduit (Q2269402):
Displaying 10 items.
- Dynamics of boundary layer formation in a volcano channel in a cavitating high-viscosity magma flow (Q369134) (← links)
- Magma flow in a volcanic conduit with account for nonequilibrium crystallization and heat exchange with surrounding rocks (Q665563) (← links)
- In memory of Aleksei Alekseevich Barmin (Q665604) (← links)
- Two-dimensional models of magma flows in a volcanic conduit taking the magma compressibility and thermal effects into account (Q736076) (← links)
- Eruption dynamics of high-viscosity gas-saturated magmas (Q1317825) (← links)
- Effect of crystallization, heat exchange, and viscous dissipation on the dynamics of extrusive eruptions (Q2446201) (← links)
- Two-dimensional simulations of magma ascent in volcanic conduits (Q4267567) (← links)
- Expansion dynamics of volatile-supersaturated liquids and bulk viscosity of bubbly magmas (Q4549886) (← links)
- The effects of temperature-dependent viscosity on flow in a cooled channel with application to basaltic fissure eruptions (Q4892842) (← links)
- Disrupt the upper or the lower conduit? The dual role of gas exsolution in the conduits of persistently active volcanoes (Q5078921) (← links)
