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11 - 20 of 28 search results for TALK:PC53 20 |u:www.itg.cam.ac.uk where 0 match all words and 28 match some words.

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  2. doi: 10.1098/rspa.2009.0434 published online 13 January 2010Proc. R.…

    www.itg.cam.ac.uk/people/grae/92.pdf
    14 Apr 2010: 800. 1000. 1200. time (kyr). 0 5 10 15 20 25 30 35 40 45. ... m. 2 s–. 1 ). heig. ht (. m). 0 10 20 30 40 500.8.

  3. Dynamics of viscous grounding lines

    www.itg.cam.ac.uk/people/heh/Paper220.pdf
    6 May 2010: H 1. H0=. g′. 8ν(t t0) (2.20). from which H (x, t) can be determined as. ... x. h. 0.05 0.10 0.15 0.20. 0.1. 0.2. 0.3. 0.4. 0.5.

  4. SOME EFFECTS OF VISCOSITY ON THE DYNAMICS OF REPLENISHED MAGMA…

    www.itg.cam.ac.uk/people/heh/Paper60.pdf
    16 Jul 2010: 5O. 2O. (cm • s-') 5. 2. 1. 0.5. 0.2 o 20 40 60 80. ... Fig.7. Experiment 3.3a. Convective overturning produced by crystallization, with a viscosity ratio of 20.

  5. http://journals.cambridge.org Downloaded: 16 Jul 2010 IP address:…

    www.itg.cam.ac.uk/people/heh/Paper68.pdf
    16 Jul 2010: http://journals.cambridge.org Downloaded: 16 Jul 2010 IP address: 131.111.18.65. Geol. Mag. 122 (5), 1985, pp. 555-568. Primed in Great Britain 555. Postcumulus processes in layered intrusions. C. K E R R , f D. P. M c K E N Z I E , & S. R. T A I T.

  6. Density changes during the fractional crystallization of basaltic…

    www.itg.cam.ac.uk/people/heh/Paper56.pdf
    16 Jul 2010: 009 2 1,400 1.46 2.845 2.838 003 2 1,400 1.60 2.931 2.967 Synthetic 3 1,39J 1.20 2.671 2.660. ... density. Troctolite 30 70 - - 2.64-2.69 Norite - 65 - 35 2.59-2.61 Olivine gabbro 10 55 35 - 2.62-2.65 Gabbronorite - 55 25 20

  7. Gravitational and buckling instabilities of a rheologically layered…

    www.itg.cam.ac.uk/people/heh/Paper169.pdf
    19 Jul 2010: Boundary conditions defined in eqs (7)–(13) are represented inthe form. w1(h1) = 0, Dw1(h1) = 0, (20)(D2 k2 4γ k. ... 18) for the upper layer withconditions defined in either eqs (20) and (22)–(26) or eqs (21)–(26) make up a boundary value problem

  8. Double-Diffusive Convection Due to Crystallization in Magmas

    www.itg.cam.ac.uk/people/heh/Paper59.pdf
    16 Jul 2010: nal u. se o. nly. 14 HUPPERT & SPARKS. Figure 1 shows the experiment 20 minutes after the introduction of the KN03 layer. ... Doublediffusive layering occurs in the K2C03 solution, seen here 20 minutes after the experiment began.

  9. On heating a stable salinity gradient from below

    www.itg.cam.ac.uk/people/heh/Paper31.pdf
    30 Jun 2010: 8C. 60. z 40. 20. On heating a stable satinity gradient from below. ( ... 60. 50. 40. 30. 20. 10. 0-. T. A - - - - - -. 0 10. 20. FIQ. UR. E. 6. A. set. of. tem.

  10. Flow and instability of thin films on a cylinder and sphere

    www.itg.cam.ac.uk/people/heh/Paper219.pdf
    6 May 2010: Bo ρgA3/2/γ R, (2.20)which is expressed in terms of input parameters that do not vary in time.

  11. Komatiites I: Eruption and Flow by HERBERT E. HUPPERT1 ...

    www.itg.cam.ac.uk/people/heh/Paper66.pdf
    19 Jul 2010: 2700 kg m3. 10-20 MPa. 1. INTRODUCTION. Komatiite lavas were erupted predominantly during the Archaean. ... 1). 1 0 0. 0-1-. 15 20 25MgO CONTENTf/o). F I G.

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