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W (1977) A model for the process of formation of the upper oceanic crust Geophys J Roy astr Soc 50, 149 83 Kieffer, B et al (2004) Flood and shield basalt from Ethiopia: magmas from the African superswell J Petrol 45, 793 834 Kilgour, B & Hatch, L (compilers) (2002) Magnetic Anomaly Images of the Australian Region [Digital Dataset] Geoscience Australia, Canberra Kincaid C & Grif ths RW (2003) Laboratory models of the thermal evolution of the mantle during rollback subduction Nature, 425, 58 62 King, SD (2005) Archean cratons and mantle dynamics Earth planet Sci Lett 234, 1 14 Kirby, SH, Engdahl, ER & Denlinger, R (1996) Intermediate depth intraslab earthquakes and arc volcanism as physical expressions of crustal and upper mantle metamorphism in subducting slabs In Bebout, GE et al (eds) Subduction: top to bottom Geophys Monogr Ser 96, pp 195 214.



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A comprehensive treatment of using discrete time in the context of CSP may be found in Roscoe s book (1998). We have adapted the approach presented there to fitwiththemodelingtoolsandtechniquesusedinthisbook.However,our approach is essentially the same and much credit is due to Roscoe for providing the first generally accessible introduction to this style of modeling time. It was explicitly stated in the introduction that the timed system we deal with are not real-time the senseof guaranteeing deadlines. The interested reader will in find that there is a vast literatureon the specification, verification and analysisof by real-time systems.A good starting point is a book edited Mathai Joseph which presents a number techniques with respect to the same case study (1996). of of One the techniques presented is TirnedCSP, which uses a dense continuous model of time in contrast to the discrete model we present. Continuous time is more expre sive but leads to difficulties in automated analysis.





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American Geophysical Union, Washington, DC Kirby, E et al (2002) Late Cenozoic evolution of the eastern margin of the Tibetan Plateau: inferences from 40Ar/39Ar and (U-Th)/He thermochronology Tectonics 21, 1001, doi:101029/ 2000TC001246 Kitada, K et al (2006) Distinct regional differences in crustal thickness along the axis of the Mariana Trough, inferred from gravity anomalies Geochem Geophys Geosyst 7, Q04011, doi:101029/2005GC001119..

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object looks like and from our sense of touch what the object feels like. When combining this evidence, our brain behaves just like an ideal Bayesian observer. Weak evidence is ignored; strong evidence is emphasized. When I am speaking to the Professor of English at a very noisy party, I will nd myself staring intently at her lips, because in this situation the evidence coming though my eyes is better than the evidence coming through my ears.

The hard reality is that millions of homeowners can t be saved and will lose their homes for a variety of reasons: they lost their jobs and can t afford even the lower payments; they they re too far underwater; the loan balance is above $729,750; or they don t live in the home Thus, we estimate that HASP, if it s very successful (and we think it will be), might help two to three million families avert foreclosure and another one to three million re nance into lower rates over the next few years This is a step in the right direction, but given that Credit Suisse estimated prior to HASP that there would be eight million foreclosures from 2009 to 2012,4 it is likely HASP will reduce the number of foreclosures by only 25 to 35 percent.

10. Symmetric when b 0, skew-symmetric when a 0, orthogonal when a 2 b 2 1. Eigenvalues a ib and a ib. Note that this section concerns real matrices. 12. Orthogonal, rotation about the z-axis through an angle . Eigenvalues 1 and cos i sin 14. Skew-symmetric, eigenvalues 0 and 18i

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