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J. Fluid Mech. (2001), vol. 440, pp. 359–380. Printed ...
www.itg.cam.ac.uk/people/heh/Paper160.pdf9 Mar 2004: Received 24 April 2000 and in revised form 7 December 2000). -
jb002019 1..16
www.itg.cam.ac.uk/people/heh/Paper176.pdf9 Mar 2004: are captured by Figure 4.[24] The calculations in Figure 4 illustrate that volcanic. -
J. Fluid Mech. (2002), vol. 472, pp. 333–371. c© ...
www.itg.cam.ac.uk/people/heh/Paper172.pdf9 Mar 2004: Sm =. 0. (ni=1. ψi(0) exp (2Viy))1/2. dy. (2.24). Recall thatn. ... 1 = 2/H0. (3.24)Hence from (3.16), by forming an expansion for ϕi, we find that. -
flm661.dvi
www.itg.cam.ac.uk/people/heh/Paper178.pdf9 Mar 2004: J. Fluid Mech. (2003), vol. 497, pp. 167–199. c 2003 Cambridge University PressDOI: 10.1017/S002211200300661X Printed in the United Kingdom. 167. Solidification and compositional convectionof a ternary alloy. By ANDREW F. THOMPSON†, HERBERT E. -
GeoFluidMech_fin.tex typeset [1]
www.itg.cam.ac.uk/people/heh/Paper154.pdf9 Mar 2004: which indicates that, at least initially,. s = (ΓT 4/3/L)t. (2.24). ... 24 H. E. Huppert. surface. The magma flows in conduits or dykes in a manner controlled by elastic, fluid.
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