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The Generation of Granitic Magmas by Intrusion of Basalt ...
www.itg.cam.ac.uk/people/heh/Paper83.pdf15 Sep 2006: Finally (1) and (4) can be written. d r b 4/3 _,d t b b I b b - b •. Equations (8)-(l 1) describe the heat transfer and melting process ... a). 50 100. b). 100. c). 50 100. TIME (yrs). F I G. -
The effects of capillary forces on the axisymmetric propagation ...
www.itg.cam.ac.uk/people/heh/Paper243.pdf12 Apr 2013: ηN =[. 2π 1. 0. f0. s[ B f (y), z]yd zd y. ... s0( f B) B f (33a)and. F( f B) 2. 4(2 ) ( f B)3 , (33b). -
The growth of compositionally stratified solid above a horizontal…
www.itg.cam.ac.uk/people/heh/Paper86.pdf25 Jan 2007: Lines of constant density. B. B. FIGURE 1. Phase diagram of a binary alloy. ... b ) Variation of solid composition, 1-4, with depth in the solid, h. -
flm412.dvi
www.itg.cam.ac.uk/people/heh/Paper174.pdf9 Mar 2004: Inthe liquid layer. B = B, C = C. (5.1). In the primary mushy layer. ... B =B. χ, C =. C. χ. (5.2). In the secondary mushy layer. -
flm483.dvi
www.itg.cam.ac.uk/people/heh/Paper186.pdf5 Jan 2006: ρs AH, φg =. mg. ρgAH, φl = 1 (φs φg), (1.1a, b, c). ... a) Ballotini in water, (b) KNO3 in solution,(c) KNO3 ballotini in solution. -
J. Fluid Mech. (1998), vol. 359, pp. 109–142. Printed ...
www.itg.cam.ac.uk/people/heh/Paper141.pdf9 Mar 2004: b). W. g. U. U = (1 – n5/2) 2. s = &(n) =s1/2. ... agreement with independent measurementsof the pump throughput, as shown on figure 4(b). -
The fluid dynamics of a basaltic magma chamber replenished by influx…
www.itg.cam.ac.uk/people/heh/Paper39.pdf18 Sep 2006: Sparks: The Fluid Dynamics of a Basaltic M a g m a C h a m b e r. ... The crystals begin to settle, leading to a concentration which increases towards the b o t t o m. -
PII: 0377-0273(82)90062-2
www.itg.cam.ac.uk/people/heh/Paper48.pdf27 Apr 2006: o c k e d b y r u b b l e a n d previous- ly c o o l e d lava. ... p a n d s t o f o r m t h e r u b b l y surface. -
Sedimentation and entrainment in dense layers of suspended particles…
www.itg.cam.ac.uk/people/heh/Paper124.pdf30 May 2006: D = au3,/B, (10). 274 H. E. Huppert, J. S. Turner and M. ... of the layer. Hence. where B, is the buoyancy flux at the origin. -
PII: 0198-0149(81)90135-7
www.itg.cam.ac.uk/people/heh/Paper41.pdf26 Sep 2011: Southeast o f it, a smaller hill, casually n am ed " W e b b ' s F o o t " , was discovered in echo soundings taken during the experiment. ... s B u m p " and " W e b b ' s F o o t " is shown in Fig. -
Komatiites II: Experimental and Theoretical Investigations of…
www.itg.cam.ac.uk/people/heh/Paper69.pdf19 Jul 2010: S. T U R N E R ET AL. T A B L E 1. ... B. Relatedfigures. 3, 4, 5, 6. A2. A2, A3. A2. 11, 12B1.B2.
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