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www.itg.cam.ac.uk/people/heh/Paper146.pdf27 Apr 2006: L. J., et al., eds., Geology of continentalslopes: Society of Economic Paleontologists and Mineralogists Special Publi-cation 27, p. ... 69–93. Hungr, O., 1990, Mobility of rock avalanches: National Research Institute for EarthScience and Disaster -
GeoFluidMech_fin.tex typeset [1]
www.itg.cam.ac.uk/people/heh/Paper154.pdf9 Mar 2004: Geological Fluid Mechanics 17. mas, the origin of some economic ore deposits, such as platinum sulphides (Campbell,. Results that match 3 of 4 words
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www.itg.cam.ac.uk/people/heh/Paper235.pdf21 Dec 2012: Research is also conducted into the economics of CCS because cost is a major issue. ... 5. 3 Current Research Output at the University of Cambridge 63.1 The Policy and Economics of CCS. -
Ice blocks melting into a salinity gradient
www.itg.cam.ac.uk/people/heh/Paper35.pdf30 May 2006: Australian National University, Canberra. (Received 21 June 1979 and in revised form 21 November 1979). ... the final position of melt water origi- nating a t a specific depth. -
PII: 0012-821X(82)90155-8
www.itg.cam.ac.uk/people/heh/Paper45.pdf27 Apr 2006: J. Stewart Turner Research School of Earth Sciences. Australian National University, Canberra, A. ... fluid crystallized at the top and thus increased the height o f the " c h i m n e y ". Later examination o f the " c h i m n e -
Double-diffusive convection
www.itg.cam.ac.uk/people/heh/Paper42.pdf30 May 2006: I n the final section we attempt t o draw some general conclusions and suggest t h a t further progress will again depend on a close collaboration between fluid dynamicists ... Fluorescein dye, originally frozen into the ice, has been illuminated from -
Convection and particle entrainment driven by differential…
www.itg.cam.ac.uk/people/heh/Paper99.pdf30 May 2006: Research School of Earth Sciences, Australian National University, GPO Box 4, Canberra 2601, ACT, Australia. ... This conclusion is a clear consequence of the theoretical description below and is discussed further in the final section.
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