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11 - 20 of 37 search results for KaKaoTalk:vb20 200 |u:www.itg.cam.ac.uk where 0 match all words and 37 match some words.

  1. Results that match 1 of 2 words

  2. Solidification of an alloy cooled from above Part 2. Non-equilibrium…

    www.itg.cam.ac.uk/people/grae/10.pdf
    1 Jun 2006: 4. 0. Tc W). - 4. 0 200 400 600 800. ... Part 2 347. Equilibrium. t (min). 200 400 600 800. t (min).

  3. PII: 0012-821X(82)90155-8

    www.itg.cam.ac.uk/people/heh/Paper45.pdf
    27 Apr 2006: Fluid Mech. 33 (1968) 183-200. 16 H.E. H u p p e r t and P.F.

  4. Solidification of leads: Theory, experiment,and field observations J. …

    www.itg.cam.ac.uk/people/grae/43.pdf
    26 Apr 2006: 1125WETTLAUFER ET AL.: SOLIDIFICATION OF LEADS. profile was taken after the buoy had reached the oceanic tem-perature, and each subsequent profile is separated by 200 min.A quantitative analysis of ... The initial profile was taken after the buoy had

  5. The growth and structure of double-diffusive cells adjacent to a…

    www.itg.cam.ac.uk/people/heh/Paper183.pdf
    5 May 2006: Perspex, 1.1 cm thick, with internal lengths and depths of 50 cm 30 cm, 200 cm 22.3 cm and 232.5 cm 40 cm.

  6. jc001173 1..12

    www.itg.cam.ac.uk/people/grae/57.pdf
    26 Apr 2006: thickness around day 200 is due toflushing of surface melt water through an artificial bore holeand the creation of a false bottom.

  7. The Generation of Granitic Magmas by Intrusion of Basalt ...

    www.itg.cam.ac.uk/people/heh/Paper83.pdf
    15 Sep 2006: 400. 300. 200. a). BS. 100 2O0 300. TIME (yre). S! ... 100. 400. b). 100 200. TIME (yre). 300 4OO. FIG 5 Variations of (a) temperature, and (b) thickness of the silicic magma layer with time for a 500 m thick sillemplaced

  8. doi:10.1016/j.jcp.2005.12.002

    www.itg.cam.ac.uk/people/grae/74.pdf
    12 Jun 2006: We then adapt our code to the configurationof Worster [1]. Since analytical results are obtained in a semi-infinite domain, we impose a very large aspectratio w/h = 200 and choose

  9. The stability of a large gas bubble rising through liquid

    www.itg.cam.ac.uk/people/heh/Paper81.pdf
    30 May 2006: 1. oo 1.712 1.26 1.42 1.10 1.24. 13.61 1.200 0.79 1.06 1.

  10. The fluid dynamics of a basaltic magma chamber replenished by influx…

    www.itg.cam.ac.uk/people/heh/Paper39.pdf
    18 Sep 2006: In t h e case o f olivine, the best available estimate of L is 200 cal g m - 1 (Bottinga a n d Richet 1978), a n d ... 3. 100. o. z 200. I 0 I 0 0 I 0 0 0.

  11. Multiple coexisting states of liquid rope coiling

    www.itg.cam.ac.uk/people/heh/Paper194.pdf
    17 May 2006: Liquid rope coiling 289. 0.6. 0.8. 1.0. 0.8. 1.0. 100 200 500 1000 2000 5000.

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