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  2. Static and flowing regions in granular collapses down…

    www.itg.cam.ac.uk/people/heh/Paper208.pdf
    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.
  3. Tuesday Informal Lunch Seminars

    www.itg.cam.ac.uk/seminars/tue_1.10/mich_2007.html
    9 Oct 2007: 20 November. No seminar. 27 November. Jessica Irving. (ITG). Inner core anisotropy.
  4. jf000701 1..3

    www.itg.cam.ac.uk/people/grae/79.pdf
    10 Jul 2007: mm/a is approximately 20 mW/m2, and thebasal heat flux that corresponds to freezing at 15 mm/a is220 mW/m2.
  5. arXiv:physics/0211069v1 [physics.geo-ph] 15 Nov 2002

    www.itg.cam.ac.uk/people/aa/Preprint1.pdf
    20 Jun 2007: depths 1400 - 1600 km. Structural and chemical heterogeneity [20] has been suggested to occur. ... 20] van der Hilst, R. and Karason, H., 1999. Compositional heterogeneity in the bottom.
  6. 8 May 2007: h. t+. 8g sin β. 15νh2. h. z= 0. (2.20). The effect of confining boundaries on viscous gravity currents 499. ... 10. 20(a) (b). t/(v/ga). 103 104 105. t/(v/ga). z N /. (V/a. )1/2. 10. 100. z N /. (V4 s. in3 β.
  7. flm466.dvi

    www.itg.cam.ac.uk/people/heh/Paper202.pdf
    8 May 2007: 6000. 0. 2. 4. 6. 8. 10. 0 20 40 60 80 100. ... 250. 300. 2 8 10t (min). 20 1.2 17.6 0.421 0.8 4.2 0.422 1.2 17.6 0.02. #
  8. 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.
  9. flm456.dvi

    www.itg.cam.ac.uk/people/heh/Paper200.pdf
    2 Apr 2007: The experiments werecarried out using cylinders and rectangular tanks 30 to 60 cm tall, and cover aspectratios between 0.5 and 20, where the aspect ratio is defined as the ratio ... 6. 4. 2. 0 5 10 15 20. Hei. ght (. cm). Horizontal distance (cm). XY. XY.
  10. doi:10.1016/j.epsl.2006.12.013

    www.itg.cam.ac.uk/people/heh/Paper203.pdf
    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.
  11. Tuesday Informal Lunch Seminars

    www.itg.cam.ac.uk/seminars/tue_1.10/lent_2007.html
    30 Jan 2007: 20 February. John Rudge. (ITG/Bullard). Solitary waves and melt migration in the mantle.

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