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ro = 11. We compute the metric to each state at time t = 1 by finding the (Hamming) distance between ro and the possible transmitted sequence co along the branches of the first stage of the trellis. Since state 0 was known to be the initial state, we end up with only two paths, with path metrics 2 and 0, as shown here:

To add a new file type, click the Add (+) button above the Extensions list and enter the file extension including the period in the field displayed at the bottom of the list. For multiple file extensions, separate each extension with a space, as shown here:

If you print your own graphics, consider using a can of clear acrylic spray (clear-coat spray paint) to coat them before applying them to your portable. This will help prevent smudging and ensure longevity.

reproducibility (R): precision under reproducibility conditions where test results are obtained with the same method on identical tests items in different laboratories with different operators using different equipment. Other characteristics of the method (e.g., linearity, robustness, etc.) can also contain some interesting information to assess the uncertainty. The ISO/CEI 17025 norm provides that the validation data can be used to evaluate the uncertainty of the measurement result:

The scope of a parameter is the process or composite in which it is defined. Parameter substit~tion creates a new process with each occurrence of the parameter replaced by the a r ~ ~ m evalue. This is simply macro expansion. nt Substitu~ng parameters in the example results in the following equivalent the definition.

Not only does the new Live view render CSS stylings with great fidelity, Dreamweaver CS4 has also enhanced the way CSS rules are created, modified, and applied. To achieve a smoother workflow, the Property inspector has been split into two tabs, one for HTML properties and the other for CSS. Place your cursor anywhere on the page in Design or Code view, and the CSS tab of the Property inspector displays the relevant CSS rule, as shown in Figure 1-5. Dreamweaver no longer creates styles automatically instead, the designer is presented with a targeted selector, which can be made less specific, if desired. The revised New CSS Rule dialog box with its plain language selector description is a great learning tool for better understanding the complexities of CSS. Modifying textrelated properties with the Dreamweaver CS4 Property inspector is now much faster and more consistent, which will make it easier for Web designers to follow best practices when styling their sites.

exceed those observed in narrow continental rifts (Section 72) The Basin and Range example thus shows that continental lithosphere may be highly extended without rupturing to form a new ocean basin This pattern is characteristic of rifts that form in relatively thin, hot, and weak continental lithosphere Here, the key features that distinguish wide rifts from their narrow rift counterparts are illustrated using the Basin and Range and the Aegean Sea provinces as examples: 1 Broadly distributed deformation The Basin and Range Province is bounded on the west by the greater San Andreas Fault system and Sierra Nevada Great Valley microplate and on the east by the Colorado Plateau (Figs 78, 79) Both the Sierra and the Plateau record comparatively low heat ow values (40 60 mW m 2) and virtually no Cenozoic extensional deformation (Sass et al, 1994; Bennett et al, 2003).

A lot of the startup code for a Windows CE application is identical to that of Win32 (see Tables 1.1 and 1.2). Here s one notable exception, depicted in this code excerpt from WinMain():

In between these two rigid blocks Cenozoic deformation has resulted in a broad zone of linear, north-trending mountain ranges of approximately uniform size and spacing across thousands of square kilometers The mountain ranges are about 15 20 km wide, spaced approximately 30 km apart, and are elevated 15 km above the adjacent sedimentary basins Most are delimited on one side by a major range-bounding normal fault Some strike-slip faulting also is present In the northern part of the province (latitude 40 N) roughly 20 25 basin-range pairs occur across 750 km The present day deformation eld of the Basin and Range is revealed by patterns of seismicity (Figs 78, 710) and horizontal velocity estimates (Fig 711) derived from continuous GPS data (Section 58) (Bennett et al, 2003).