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It is possible to associate with each sliced value vi a reliability zj, which indicatesthe quality of the decision. The reliabilities are ordered such that zj > z j if the ith symbol is more reliable - capable of producing better decisions -than the j t h symbol. If the channel is AWGN, then zi = IriI E R can be used as the reliability measure, since the absolute log likelihood ratio

dance Geochem Geophys Geosyst 5, Q12012, doi:101029/ 2004GC000793 Oldow, JS (2003) Active transtensional boundary zone between the western Great Basin and Sierra Nevada block, western US Cordillera Geology 31, 1033 6 Oliver, J (1982) Tracing surface features to great depths: a powerful means for exploring the deep crust Tectonophysics 81, 257 72 Oliver, J & Isacks, B (1967) Deep earthquake zones, anomalous structures in the upper mantle, and the lithosphere J geophys Res 72, 4259 75 Opdyke, ND & Channel, JET (1996) Magnetic Stratigraphy Academic Press, San Diego Opdyke, ND, Burckle, LH & Todd, A (1974) The extension of the magnetic time scale in sediments of the central Paci c Ocean Earth planet Sci Lett 22, 300 6 Opdyke, ND et al (1966) Palaeomagnetic study of Antarctic deep sea cores Science 154, 349 57 Oreskes, N.

The matrix structure found in many organizations discourages strong staff commitment to individual projects. With a matrix system, project staff are drawn out of functional departments and assigned to projects on an as-needed basis. They are temporary visitors who stay with a project long enough to carry out their technical tasks; when the tasks are completed, they leave. In addition, they may be applying their expertise to several projects simultaneously, further attenuating their commitment to any single project. The reward system in a matrix structure does not encourage project staff to put in long hours on projects. Why should they work extra hours for an undertaking in which they have no personal stake What will their extra effort earn them other than a pat on the head and a nice letter of thanks written by the project manager and sent to their functional boss Under these organizationally rooted circumstances, it is hardly surprising to encounter a reluctance on the part of project staff to commit extra time to projects.

(1999) The Rejection of Continental Drift: theory and method in American earth science Oxford University Press, New York Oreskes, N (2001) (ed) Plate Tectonics: an insider s history of the modern theory of the Earth Westview press, Boulder, CO Orowan, E (1965) Convection in a non-Newtonian mantle, continental drift, and mountain building Phil Trans Roy Soc Lond A 258, 284 313 Owens, TJ & Zandt, G (1997) Implications of crustal property variations for models of Tibetan plateau evolution Nature 387, 37 43 Ozacar, AA & Zandt, G (2004) Crustal seismic anisotropy in central Tibet: implications for deformational style and ow in the crust Geophys Res Lett 31, L23601, doi:101029/ 2004GL021096 zalaybey, S & Savage, MK (1995) Shear-wave splitting beneath western United States in relation to plate tectonics J geophys Res 100, 18 135 49 Packham, GH & Falvey, DA.

We do this by sending the IM_SETDATA message. The SendMessage() parameters, in the order shown, are the handle to the ink control window; the message constant IM_SETDATA; the length of the data in bytes, as reported by the control when we saved the data; and the address of the buffer containing the saved inking data, cast to the type LPARAM.

j =1

If, for any reason, you need to interrupt the Live Data connection process, click the stop button on the Live Data toolbar. The stop button remains active only while Dreamweaver is transitioning into Live Data view.

(1971) An hypothesis for the formation of marginal seas in the Western Paci c Tectonophysics 11, 79 110 Pakiser, LC (1963) Structure of the crust and upper mantle in the western United States J geophys Res 68, 5747 56 Pancha, A, Anderson, JG & Kreemer, C (2006) Comparison of seismic and geodetic scalar moment rates across the Basin and Range Province Bull seis Soc Am 96, 11 32 Panien, M, Schreurs, G & P ffner, A (2005) Sandbox experiments on basin inversion: testing the in uence of basin orientation and basin ll J struct Geol 27, 433 45 Panning, M & Romanowicz, B (2004) Inferences on ow at the base of Earth s mantle based on seismic anisotropy Science 303, 351 3 Pardo-Casas, F & Molnar, P (1987) Relative motion of the Nazca (Farallon) and South American plates since Late Cretaceous time Tectonics 6, 233 48.