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1 - 10 of 18 search results for katalk:za33 24 |u:www.itg.cam.ac.uk where 0 match all words and 18 match some words.
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  2. PII: 0022-0248(86)90410-0

    www.itg.cam.ac.uk/people/heh/Paper76.pdf
    19 Jul 2010: Trans. Geotherm.Res. 24 (1985) 25. Roy. Soc. London A310(1984) 511. [19] H.E.
  3. PII: 0012-821X(86)90188-3

    www.itg.cam.ac.uk/people/heh/Paper74.pdf
    15 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,
  4. Initial advance of long lava flows in open channels

    www.itg.cam.ac.uk/people/heh/Paper222.pdf
    27 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.
  5. 29 Apr 2010: we can make the approximation G(y) π y. Equation (2.24) then becomesπ. ... By dimensionalization of equation (3.24), we findthat the system is stable when.
  6. 16 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
  7. Dynamics of viscous grounding lines

    www.itg.cam.ac.uk/people/heh/Paper220.pdf
    6 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).
  8. Replenishment of Magma Chambers by Light Inputs

    www.itg.cam.ac.uk/people/heh/Paper70.pdf
    19 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.
  9. Flow and instability of thin films on a cylinder and sphere

    www.itg.cam.ac.uk/people/heh/Paper219.pdf
    6 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
  10. 19 Jul 2010: η1. )w2(0),. (24). (. 1. k2D3 D. )w1(0) η2. η1. (1.
  11. The Crystallization of Lava Lakes

    www.itg.cam.ac.uk/people/heh/Paper118.pdf
    19 Jul 2010: JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 98, NO. B9, PAGES 15,891-15,901, SEPTEMBER 10, 1993. The Crystallization of Lava Lakes. M. GRAE WORSTER AND HERBERT E. HUPPERT. Institute of Theoretical Geophysics, Department of Applied Mathematics and

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