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25 Jan 2007: are similar to those derived in P a r t 1 (equations (3.19) and (3.20)), though they now involve the variable 8, and, as mentioned earlier, q5i is no ... Solidijcation of an alloy cooled from above. Part 2. 20. 15.

25 Jan 2007: Huppert. To cooler. - I 20 cm l o - 10 cm I 1 Scale. ... A. - 0. -10. T ("C). -20. -30. 100. Source. E D B, n C D.

16 Jan 2007: 0 10 20 30. c, (wt Yo) FIQURE 10. The non-dimensional growth rates A4, A, and A, (determined by Worster 1986) with. ... 20. 15 - v. 3 l 0 - fi 5 -. - -. X I I I I I. 0 10 20 30 40 50.

25 Jan 2007: T, = -20 "C c, = 9.37%. 1. H 01 = -h,(AC)f = 2.40 x 10-4K, s-'. ... 0.04 - (b) -. 0.01. 0 5 10 15 20 25 0 5 10 15 20 25.

25 Jan 2007: which satisfies (2.17b) if B ( z ) = exp ( - 4 V z ) , (2.20). ... This justifies the use of the long-time solutions (2.20) and (2.21) in the geological context.

25 Jan 2007: 45. 20 30 40 0 10 20 30 40 0 10 I (min) t (min). ... Melting the roof of a chamber. Finally, (18) and (20) can be written J D.

16 Jan 2007: 1.40. • 1.3o >,. 1.20. 1.10 I 6 0 5 0 4 0 3 0 2 0 10. ... 149. 1.32 /. 1.31 /. 1. 3 0 /. Eo 1 2 9 /. /. _., / 1. 2 8 1.27. /. 1 2 6 / i , = / • 20 ; 0 35 4'0.

13 Nov 2007: Received 20 November 2006; accepted 11 July 2007; published online 2 October 2007. ... For Ls= 0.20 m / s and = 0.4 it is reduced to 0.08 s.

23 Apr 2007: Received 15 November 2005; accepted 9 January 2007; published online 20 April 2007. ... Thewidely accepted reason for this scaling relationship is theconstant ratio of shear stress and normal stress.20.

22 Mar 2007: Thus Layer 8 hasreflection amplitudes that are systematically some 20%higher than those of the other layers. ... 1 1 sigma(kg/m3) (kg/m3) (Pa s). 420–610 1020 20 3.0–5.0105 4106.