Pages that link to "Item:Q665563"
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The following pages link to Magma flow in a volcanic conduit with account for nonequilibrium crystallization and heat exchange with surrounding rocks (Q665563):
Displaying 15 items.
- Dynamics of boundary layer formation in a volcano channel in a cavitating high-viscosity magma flow (Q369134) (← links)
- Two-dimensional models of magma flows in a volcanic conduit taking the magma compressibility and thermal effects into account (Q736076) (← links)
- Gasified magma flow in a volcanic conduit (Q811281) (← links)
- Simulation of the transition processes in the volcanic eruption of high-viscosity gas-saturated magmas (Q1375289) (← links)
- Viscosity models for silicate melts (Q1775657) (← links)
- Time-dependent crystallization in magma chambers and lava lakes cooled from above: the role of convection and kinetics on nonlinear dynamics of binary systems (Q1948949) (← links)
- Equidecomposable magmas (Q2217775) (← links)
- Effect of viscous dissipation on nonisothermal high-viscosity magma flow in a volcanic conduit (Q2269402) (← links)
- A study of magma flows in the case of non-equilibrium diffusion of water in the melt (Q2379168) (← links)
- Non-isothermal lava flows over a conical surface (Q2387895) (← links)
- Effect of crystallization, heat exchange, and viscous dissipation on the dynamics of extrusive eruptions (Q2446201) (← links)
- Magma flow through elastic-walled dikes (Q2501823) (← links)
- Two-dimensional simulations of magma ascent in volcanic conduits (Q4267567) (← links)
- One‐dimensional, time‐dependent, homogeneous, two‐phase flow in volcanic conduits (Q4865797) (← links)
- Disrupt the upper or the lower conduit? The dual role of gas exsolution in the conduits of persistently active volcanoes (Q5078921) (← links)
