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PII: 0022-0248(86)90410-0
www.itg.cam.ac.uk/people/heh/Paper76.pdf19 Jul 2010: Trans. Geotherm.Res. 24 (1985) 25. Roy. Soc. London A310(1984) 511. [19] H.E. -
PII: 0012-821X(86)90188-3
www.itg.cam.ac.uk/people/heh/Paper74.pdf15 Jul 2010: After 24 hours the fluid at the surface and floor had reached compositions of about 17 wt.% and 25 wt.% NaNO, respectively. ... Volcanol. Geotherm. Res. 24, 25-54, 1985. J.S. Turner, Buoyancy Effects in Fluids, Cambridge Uni- versity Press, Cambridge, -
Initial advance of long lava flows in open channels
www.itg.cam.ac.uk/people/heh/Paper222.pdf27 Aug 2010: However, variations in fountain height in episode 4, asplotted in figure 1.24 of Wolfe et al. ... the night of 24–25 July 1983,when the flow front divided into two parallel lobes. -
Thermohaline Steps Induced By Melting of the Erebus Glacier Tongue
www.itg.cam.ac.uk/people/heh/Paper44.pdf16 Jul 2010: Geophys. Res., 79, 1792-1797, 1974. Gebhart, B., and J. C. Molendorf, A new density relationship for pure and saline water, Deep Sea Res., 24(9), 831-848, 1977. ... Glaciol., 24, 259-271, 1979. Tressler, W. L., and A.M. Ommundsen, Seasonal oceanographic -
Dynamics of viscous grounding lines
www.itg.cam.ac.uk/people/heh/Paper220.pdf6 May 2010: H. t+. q. x= 0 (2.24). to form the nonlinear diffusion equation. ... f (ξ ) dξ = 1, (3.24). to the leading-order front solution (3.21). -
Replenishment of Magma Chambers by Light Inputs
www.itg.cam.ac.uk/people/heh/Paper70.pdf19 Jul 2010: Petrol., 24, 133-165, 1983. Eichelberger, J. C., Vesiculation of mafic magma during replenish- ment of silicic magma reservoirs, Nature, 288, 446-450, 1980. -
Flow and instability of thin films on a cylinder and sphere
www.itg.cam.ac.uk/people/heh/Paper219.pdf6 May 2010: where representative valuesof ρ = 1.4 kg m3, g = 9.8 m s2, γ = 78 mN m1 and R = 0.24 m were fixed. ... and R = 0.24 m. Wavelengths were estimated by dividing the circumference of the leading edgeof the flow at the onset of instability by the number of -
Gravitational and buckling instabilities of a rheologically layered…
www.itg.cam.ac.uk/people/heh/Paper169.pdf19 Jul 2010: η1. )w2(0),. (24). (. 1. k2D3 D. )w1(0) η2. η1. (1. -
The effect of confining impermeable boundaries on gravity currents in …
www.itg.cam.ac.uk/people/heh/Paper221.pdf6 May 2010: Sd 75 0.24. V 1 20 200 V a 44 0.20 V 2 60 100 V b 75 0.25V 3 40 150 V 4 40 62. -
Double-Diffusive Convection Due to Crystallization in Magmas
www.itg.cam.ac.uk/people/heh/Paper59.pdf16 Jul 2010: nly. 24 HUPPERT & SPARKS. compositional film is to substitute the film thickness into the compositional Rayleigh number, which can be re-expressed as. ... 24. I. A. -.:---n;o • • Pl AA GIOCl A S E.
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