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16 Jul 2010: DENSI T Y. I00. ß. 200' Tf S. 250 -. 350 40 0 • z::::::::::::::. ::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::: ... 27 150 34.572 - 1.52 -2.01 0.49 1.0284421 1.0284568 147 11 29 200 34.637 - 1.73

19 Jul 2010: The layer was nominally 150 mm deep and was contained in a Perspex box of a 200 mm x 200 mm cross section. ... Again we used water/glycerine mix- tures which we introduced at the surface of a nominally 200 mm layer contained in the 200 mm x 200 mm

19 Jul 2010: IO]. Finally, in Section 4, we describe the eflects of cooling and crystallizing a gradient of sodium carbonate, fat which Pr = 7 and Le = 200.

15 Jul 2010: 0O ,. loo 200 300 400! 500 TIME(mins). Fig. 4. The bulk composition of the solution remaining in the tank is shown as a function of time for the above slope

16 Jul 2010: For each mineral fractionation densities have been calculated at 1,200 C (upper line) and at 1,400 C (lower line). ... Fig. 3 shows contours o f fractionation density at 1,200 C for each cotectic assemblage as a function of min- eral compositions.

6 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. ... 200 400 600 800 10000. 50. 100. 150. t (s). x N(t. )

16 Jul 2010: Plexiglas tank of internal dimensions 200 x 106. Two different experiments described in our ear- mmx •00 mm deep. ... which crystallization is taking place [Chen and Accordingly, we built a tank, 200 x 106 x •00 mm Turner, 1980].

30 Jun 2010: 442 H. E. Huppert and P. P. Linden. 220. 200. 160 l.

19 Jul 2010: Experimental studies of komatiite generation (Bickle et al.,1977) and thermal constraints (McKenzie, 1984) indicate depths of 200 km or greater.

19 Jul 2010: 2.1. Experimental techniques. The experiments were carried out in a cubical Perspex tank measuring 200 mm on eachside internally, which was insulated with a 90 mm thick polystyrene jacket (removable