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26 Mar 2023: Stokes at 200: a celebration ofthe remarkable achievementsof Sir George Gabriel Stokestwo hundred years after hisbirthSilvana S. ... This article is part of the theme issue ‘Stokes at 200(Part 1)’.

26 Mar 2023: Stokes at 200 (part 2)Silvana S. S. Cardoso1,2, Julyan H. E. ... This article is part of the theme issue ‘Stokes at 200(part 2)’.

20 Jan 2023: Sparks, R.S.J. and Huppert, H.E. (1984) "Igneous Petrology: Old magma chambers replenished by new ideas", Nature 312, 200. ... Cryst. Growth 200, 287-296.

27 Apr 2006: The mean volume fraction 4,. 0 I I,,,, I0 100 200 300 400 500. ... whoseheight h ‘ H. Substituting. 0 0 100 200 300 500 M0 M= p0AH (A.4).

9 Feb 2004: 1. Two different experimental channels were used: omeasuring 100 cm long, 15 cm wide and 10 cm deep; andother measuring 200 cm long, 20 cm wide and 25 cm deIn both ... 9 3.0 10.0 30.0 289.5 0.150 1.333 326.2 244.8A22 9 3.0 8.0 24.0 200.0 0.173 1.383

26 Mar 2023: Phil. Trans.R.Soc.A 378:20190515.http://dx.doi.org/10.1098/rsta.2019.0515. Accepted: 31 March 2020. One contribution of 14 to a theme issue ‘Stokesat 200 (Part ... This article is part of the theme issue ‘Stokes at 200(Part 1)’.

26 Mar 2023: Phil. Trans.R.Soc.A 378: 20190531.http://dx.doi.org/10.1098/rsta.2019.0531. Accepted: 19 June 2020. One contribution of 13 to a theme issue ‘Stokesat 200 (part ... This article is part of the theme issue ‘Stokes at 200(part 2)’.

9 Mar 2004: 288 B.J. Spencer, H.E. Huppert / Journal of Crystal Growth 200 (1999) 287—296. ... B.J. Spencer, H.E. Huppert / Journal of Crystal Growth 200 (1999) 287—296 291.

9 Mar 2004: The mushy layer starts to grow more slowlythan predicted by the theory after about 200 minutes. ... This is likely to be an indirectconsequence of the brine expulsion which begins at about 200 minutes, as shown infigure 6.

1 Feb 2008: 10 12 14 16 18 200. 5. 10. 15. 20. 12.9 12.95 13 13.050.

24 Apr 2014: Reservoir. 25 cm. Glycerineax. q. 200 cm. FIGURE 5. Schematic of the experimental Hele-Shaw cell. ... Colour online) Sequence of photographs showing the progression of experimentB at dimensional times (a) t = 20 s, (b) 100 s and (c) 200 s.

9 Mar 2004: a)35. 30. 25. 20. 15. 100 100 200 300 400 500.

14 May 2008: Solidification of ammonium chloride 473. 0–15 –10 –5 5 10 15 200.

2 Apr 2007: 184 E. L. Thompson and H. E. Huppert. 2 4 6 8 10 12 14 16 18 200.

23 Dec 2021: 1.15,. a2/5 ,. a>. 1.15. Lub. eet. al. (200. 5). Dry. ... t (s)0 5 10 15. t (s). 200. 400. 600(a) (b).

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

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).

9 Mar 2004: 700. 600. 500. 400. 300. 200. 1000 20 40 60 80 100 120. ... R8. R9. 600. 500. 400. 300. 200. 100. 0 20 40 6050 70.

5 May 2006: 0 20 40 60 80 100 120. 500400300200100. 0–100–200. 200300. 1000. ... 0 20 40 60 80 100 120. –100–200–300. Time (s)Time (s).

11 Oct 2006: 1992). The typical grid has 200 intervals over [0, xN (t)] and a time step of0.04. ... 2 4 6 8 10 12 14 16 18 200.

5 May 2006: pulses, 512 µs in duration and anacquisition width of 200 kHz was used. ... In our velocity imaging experiments the echo time TE was 10.3 ms, while theobservation time was 200 ms.

4 Jun 2009: relative density,rises as a buoyant plume through the approximately 200 metre thick formation beforeit is ultimately stopped by the Nordland shale, a relatively impermeable cap rock atthe top of the ... 2007)clearly show that the dynamics of the plume

26 Mar 2023: During the July 12, 2003 to July 13, 2003 paroxysmal dome collapse of Soufrière Hills volcano, more than 200  106 m3 of hot pyroclastic material entered the ocean. ... The predictive model gives an impact velocity of ui68 m.s1, with  200.

9 Oct 2015: 5. rsta.royalsocietypublishing.orgPhil.Trans.R.Soc.A373:20140166. dayhour week month. 300. 200. 100. buoy. ancy. flux.

1 Jun 2006: I I I. I I I I 0 200 400 600 800. ... about half a year (hi = 200 cm and T / = 1016 "C).

20 Jun 2007: This allows one. to interpret the seismically isotropic top 100 - 200 km thick layer of the inner core [11, 12].

30 May 2006: 200. n 150 W. 50. 1 I I I I 0 20 40 60 80. ... R. Lister. 60 I n g'. (cm s-3 Expt Theory 42 21 11 0 - -. 0 - A. 0. I - - - 9 - - - --.__ I 100 I 150 I 200.

5 Jan 2006: 3. 4. 5. 6. 100 200 300 400 500. a(cm). t (min). ... b). 1. 2. 3. 4. 5. 0 50 100 150 200 250 300.

21 Oct 2011: 10 15 200. 0.2. 0.4. 0.6. 0.8. 1.0. (h/. d i)/. ... 250. 200. 150. 100. 50. 0. 400. AD. – A. W (. cm2 ). t (s). 300. 200. 100. 0.4 0.8 1.2. t (s).

25 Jan 2007: 4. 0. Tc W). - 4. 0 200 400 600 800. ... Part 2 347. Equilibrium. t (min). 200 400 600 800. t (min).

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.

26 Mar 2023: 1. IntroductionAccurate simulations of lava emplacement are vital for lava flow forecasting, assessing volcanic hazard, and designing barriers or other mitigation methods. Lava often flows over topography as rough brecciated basaltic flows known as a

27 Apr 2006: 0 0. c) loo. 50 100 150 200. TIME (yrs). 50 100 150 200. ... 100. 8O. 60. 40. 20. O " '. ". ' ". " ' -. 0 50 100 150 200. TIME (yrs) Fig.

23 Dec 2021: exp3 Glycerin 209 0.28 20 5.2 5106exp4 Glycerin 200 0.08 35 5.6 1107.

26 Mar 2023: J. Fluid Mech. (2019), vol. 876, pp. 912–938. c Cambridge University Press 2019doi:10.1017/jfm.2019.588. 912. Interaction of viscous free-surfaceflows with topography. Edward M. Hinton1,2,†, Andrew J. Hogg3 and Herbert E. Huppert2. 1BP Institute

30 May 2006: initial volume fraction 5 YO of 200 pm-diameter sand and initial height of 20 m, for which us = 2 cm sP1 and gh = 0.81 m s -. The dynamics of ... 400. cl. 200. Y I I I L 0 50 100 150 200.

9 Mar 2004: τc = (γ/U)3, (3.6). which is around 200 s for our experiments. ... 0.4. – 0.6. 80. 60. 40. 20. 0 50 100 150 200. –

30 May 2006: h. 5 200 - 9. ( b ) 400. 34 4 34 5 34 6 34 1 34 4 34 5 34 6 34 7 S ( % a ) S ( % O ). B I L t<h ... 100 0.0026 0.0061 0.0083 0.0184 150 0.0035 0.0077 0.0092 0.0198 200 0.0041 0.0088 00101 0.0210.

30 May 2006: J. F u i d Xech. (19761, VOZ. 78, part 4? pp. 821-854 Printed in Great Britain. 82 1. Nonlinear double-diffusive convection By H E R B E R T E. H U P P E R T A N D D A N I E L R. MOORE. Department of Applied Mathematics and Theoretical Physics,

5 May 2006: Convection in reactive porous media 111. 100 200 300 400 500 600 700 8000. ... 50 100 150 200 250 3000. 0.5. 1.0. 1.5. 2.0. 2.5.

24 Aug 2012: The elastic sheets and the salt solution were containedinside an acrylic rectangular tank of dimensions 200 20 25 cm, with an opaque base.

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].

25 Jan 2007: I I I. I I I I 0 200 400 600 800. ... about half a year (hi = 200 cm and T / = 1016 "C).

9 Mar 2004: Each new time step rN (t) is updated using(12). Typically, we used 200 y-intervals and a time step of 0.002, but the convergenceand resolution (accurate to at least ... 4.2. H = 1. 0 50 100 150 200. –uN. Figure 14.

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. )

26 Apr 2006: Journal of Crystal Growth 205 (1999) 427}440. The interaction between a particle and an advancingsolidi"cation front. A.W. Rempel, M.G. Worster. Department of Applied Mathematics and Theoretical Physics, Institute of Theoretical Geophysics,

27 Apr 2006: 0 0. c) loo. 50 100 150 200. TIME (yrs). 50 100 150 200. ... 100. 8O. 60. 40. 20. O " '. ". ' ". " ' -. 0 50 100 150 200. TIME (yrs) Fig.

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

8 Jun 2012: Adjacent to the Sleipner field,this sandstone formation is 200–300 m thick [Chadwicket al., 2004] (Figure 1). ... The highestintrareservoir mudstone is 5 m thick, although the ultimateseal is the Nordland Shale, which is 200 m thick [Zweigelet al., 2000

9 Mar 2004: 100 m abovethe valley floor on the southern margins of the depres-sion, more than 200 m above the eastern slope of GuaneGuane Hill (12 km west of the source area,