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be a "partial" sequence, starting at the beginning of r, but extending only through nmax branches. (The tilde is used to represent partial sequences.) Each ri consists of n symbols, so we can also write this as a vector of nnmm elements From among the sequences in X,the optimal receiver chooses the ii(i) which maximizes

See Figure 5.2 for the facts in working memory and how they are inferred using forward chaining. In the end, the expert system recommends that the user buy Countrywide Financial and Bank of America stock. Let us now look at a backward chaining example. We will rst state our hypothesis: short American Airlines. In backward chaining, we nd evidence to either support or refute this hypothesis. In addition, we will assume the following initial facts:

m : difference observed between the unknown mass and the standard; mc : correction to make up for the error due to the off-centering of the mass; B : correction of thrust from the air.

Fresh/exhaust air dampers: a ( f,e ) = pd (a 0( f,e ) - 90) + 90 ( pd0 pd 1) Recirculating air damper: a r = (1 - pd ) (a 0 r - 90) + 90 ( pd0 pd 1)

Sinha, MC et al (1998) Magmatic processes at slow spreading ridges: implications of the RAMESSES experiment at 57 45 N on the Mid-Atlantic ridge Geophys J Int 135, 731 45 Sinton, JM & Detrick, RS (1992) Mid-ocean ridge magma chambers J geophys Res 97, 197 216 Sisson, TW & Bronto, S (1998) Evidence for pressure-release melting beneath magmatic arcs from basalt at Galunggung, Indonesia Nature 391, 833 86 Sleep, NH (1975) Formation of oceanic crust: some thermal constraints J geophys Res 80, 4037 42 Sleep, NH (2003) Survival of Archean cratonal lithosphere J geophys Res 108, 2302, doi:101029/2001JB000169 Sleep, NH (2005) Evolution of continental lithosphere Annu Rev Earth planet Sci 33, 369 93 Smelov, AP & Beryozkin, VI (1993) Retrograded eclogites in the Olekma granite greenstone region, Aldan Shield Precambrian Res 62, 419 30 Smith, AG.

(1999) Gondwana: its shape, size and position from Cambrian to Triassic times J African Earth Sci 28, 71 97 Smith, AG & Hallam, A (1970) The t of the southern continents Nature 225, 139 44 Smith, AG & Pickering, KT (2003) Oceanic gateways as a critical factor to initiate icehouse Earth J Geol Soc London 160, 337 40 Smith, AG, Smith, DG & Funnell, BM (1994) Atlas of Mesozoic and Cenozoic coastlines Cambridge University Press, Cambridge Smith, DE et al (1985) Global plate motion results from satellite laser ranging (abstract) EOS Trans Amer Geophys Un 66, 848 Smith, DK & Cann, JR (1993) Building the crust at the MidAtlantic Ridge Nature 365, 707 15 Smith, M & Mosley, P (1993) Crustal heterogeneity and basement in uence on the development of the Kenya rift, East Africa Tectonics 12, 591 606.

0 0 5 10 15 0 5 10 15 Temperature (K) (a) Temperature (K) (b) 10

Smith, WHF & Sandwell, DT (1997) Global sea oor topography from satellite altimetry and ship depth soundings Science 277, 1957 62 Smithies, RH (2000) The Archean tonalite tondhjemite granodiorite (TTG) series is not an analogue of Cenozoic adakite Earth planet Sci Lett 182, 115 25 Smithson, SB & Brown, SK (1977) A model for the lower continental crust Earth planet Sci Lett 35, 134 44 Snider, A (1858) La Cr ation et ses Myst res D voil s Frank and Dentu, Paris Snow, JK & Wernicke, B (2000) Cenozoic tectonism in the central Basin and Range: magnitude, rate, and distribution of upper crustal strain Amer J Sci 300, 659 719 Sobolev, SV & Babeyko, AY (2005) What drives orogeny in the Andes Geology 33, 671 20 Sobolev, SV et al (2005) Thermo-mechanical model of the Dead Sea transform Earth planet.

Sci Lett 238, 78 95 Solomon, M (1990) Subduction, arc reversal, and the origin of porphyry copper-gold deposits in island arcs Geology 18, 630 3 Solomon, SC, Sleep, NH & Richardson, RM (1975) On the forces driving plate tectonics: inferences from absolute plate.