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flm145.dvi
www.itg.cam.ac.uk/people/heh/Paper197.pdf11 Oct 2006: t. θ. 5 10 15 20 25 3010–4. 10–3. 10–2. 10–1. ... 374 M. Ungarish and H. E. Huppert. t0 4 8 12 16 20 24. -
doi:10.1098/rsta.2006.1803
www.itg.cam.ac.uk/people/heh/Paper196.pdf11 Oct 2006: Statistical studies of the globaldatabase suggest that for volcanism more than 2000 years ago, only 20% of largemagnitude explosive eruptions have been recognized. ... The historiccatalogue, and in particular the 20 year period of analysis in this study, -
The fluid dynamics of a basaltic magma chamber replenished by influx…
www.itg.cam.ac.uk/people/heh/Paper39.pdf18 Sep 2006: 0010-7999/80/0075/0279/$02.20. 280 H.E. H u p p e r t and R.S.J. ... of between 10 and 20, and similar magmas involved to those compositions in Table 2, the results of our quantitative calculations are directly applicable. -
The Generation of Granitic Magmas by Intrusion of Basalt ...
www.itg.cam.ac.uk/people/heh/Paper83.pdf15 Sep 2006: 2 Department of Earth Sciences, Downing Street, Cambridge CB2 3EQ. (Received 20 July 1987; revised typescript accepted 14 January 1988). ... This temperature profile is governed by the diffusion equation. 36 326— = , —y (20). -
Under consideration for publication in J. Fluid Mech. 1 ...
www.itg.cam.ac.uk/people/heh/jfm50.pdf28 Jul 2006: 5. 50% most cited (/yr) 21( 0.6) 21( 0.8) 20( 1.3) 6( 1.2). ... 1970-1975 1975-1980 1980-1985 1985-1990 1990-1995 1995-2000 2000-2005 2005-2010. 0. 10. 20. -
On Howards technique for perturbing neutral solutions of the…
www.itg.cam.ac.uk/people/heh/Paper14.pdf30 May 2006: a 3 ) ( 2 ) - (0 < 01 < 1) (2.20 c). ... 2 1 ) ; part of (2.20); and part of (2.17) [and none of (2.16)]. -
Flow and Reactions in Permeable Rocks. By O. M. P HILLIPS .…
www.itg.cam.ac.uk/people/heh/Paper106.pdf30 May 2006: I found only one obvious error. I n Section 6.6 the angle q5 is used in the text, while it is depicted as 8 in figure 6.20 ; and qi -
The slumping of gravity currents
www.itg.cam.ac.uk/people/heh/Paper32.pdf30 May 2006: 0 20 40 60 80 100 120 140 160. t (9 FIGURE 2. ... 796 H. E. Huppert and J. E. Simpson. 0 10 20 30 40 50 60 70. -
Lee waves in a stratified flow Part 3. Semi-elliptical obstacle
www.itg.cam.ac.uk/people/heh/Paper8.pdf30 May 2006: BLANCH, G. 1964 Mathieu Functions, chapter 20 in Handbook of Mathematical Functions (edited by M. -
Gravity-driven flows in porous layers
www.itg.cam.ac.uk/people/heh/Paper125.pdf30 May 2006: Huppert and A. W. Woods. 0 20 40 60 80 100. ... Gravity-driven flows in porous layers 61. 100. 80. 20. FIGURE 4.
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