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How might flow regimes be expressed in solidified magma?
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Classroom Contents
Modelling Magma Movement: Unexpected Journeys in the Field and Lab
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- 1 Modelling magma movement: Unexpected journeys in the field and the lab
- 2 The Liverpool MAGMA Lab approach
- 3 Unexpected journey in the field..
- 4 Scaled analogue experiments
- 5 Dyke Geometry & surface deformation
- 6 Medusa - LaVision Laser System
- 7 Simple magma Analogue materials
- 8 Particle image velocimetry (PIV)
- 9 Dyke Flow velocity from PIV analysis
- 10 Silicon oil Dyke - 3 rpm
- 11 Scaling - Reynolds number (Re)
- 12 Scaling Results - Reynolds number
- 13 Unexpected journey in the Lab.. Newtonian fluid dyke at different Re
- 14 Newtonian fluid dykes - Flow regimes
- 15 Magma: A multiphase fluid
- 16 Crystal proportion and crystal shape
- 17 What about bubbly magma?
- 18 Modelling complex magma rheology
- 19 Another unexpected journey in the Lab... Magma analogues - were they shear thinning?
- 20 What about Reynolds number effects?
- 21 Drastically different flow regimes for dykes
- 22 How might flow regimes be expressed in solidified magma?
- 23 Sill geometry, strain rates and flow
- 24 Summary
- 25 Final thoughts and future directions
