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Like other Dreamweaver extensions, such as behaviors and commands, translators are HTML files with JavaScript. Translators have no user interface. Other than deciding when to invoke it, you have no parameters to set or options from which to choose. All the pertinent code is in a script located in the <head> of the translator, which, along with any necessary support routines, includes two essential JavaScript functions: getTranslatorInfo() and translateMarkup(). Any other Dreamweaver JavaScript API functions not specific to behaviors can be used in a translator as well.

Let Df)(c) denote the first j indices in the ordered set,



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The following code looks at each member of the array; if that option is the one in which the selectedIndex property is true, then the proper value is assigned to a variable:

In this section we briefly describe several variations on Reed-Solomon and BCH codes. More detail can be found in [220].





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Let us assume that three vectors of prices, costs, and bought and sold units (in contracts or shares) are given and have the same number of elements n: P = P(P1, . . ., Pi, . . ., Pn), C = C(C1, . . ., Ci, . . ., Cn), U = U(U1, . . ., Ui , . . ., Un). The bold font is used to denote vectors. Scalars are shown using the regular font. The elements of the vector P are all positive numbers. The elements of the vector C are all non-negative numbers. The elements of the vector U are all integer numbers. If Ui < 0, then |Ui| units are sold at time i. The vertical lines denote the absolute value of a number. If Ui > 0, then Ui units are bought at time i. If the Ui = 0, then no transaction is done at time i. The profit or loss (PL) is calculated: PL = k(P, U) (C, abs(U)) + kPn sum(U) Cn|sum(U)| (2.1)

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As for the discrete channel, the channel capacity C of a channel with input X and output Y is the maximum mutual information between X and Y , where the maximum is over all input distributions. In Example 1.10, the maximizing distribution is, in fact, the uniform distribution, P ( X = a ) = P ( X = -a) = so (1.40) is the capacity for the BAWGNC. In Example 1.11, the maximizing distribution is, in fact, the Gaussian distribution (since this maximizes the entropy of the output), so (1.41) is the capacity for the AWGNC.

IGRP and EIGRP are Cisco proprietary routing protocols. Although the details of the protocol behaviour have been published, no other vendor may implement IGRP or EIGRP. Therefore, their use is constrained to Cisco-only networks.

evidence of folding and faulting associated with dextral motion within a 10- to 20-km-wide zone along the C te d Ivoire Ghana marginal ridge (Edwards et al, 1997; Attoh et al, 2004) The folds display northeast-trending axes that are compatible with dextral motion The faults record both strike-slip and dip-slip (south-side down) displacements that appear to re ect at least two episodes of strike-slip deformation (Attoh et al, 2004) The rst involved a combination of strike-slip motion and extension on northeast-trending faults, leading to the formation of pull-apart basins (Section 82) The second involved strike-slip motion and folding, possibly as a result of a change in the direction of motion in the transform On the basis of these and other observations, it has been possible to reconstruct the large-scale evolution of the Ivory Coast Ghana margin Four main phases are illustrated diagrammatically in Fig 8.

17c f In phase 1 (Fig 817c) there is contact between two continents Strike-slip motion results in brittle deformation of the upper crust and ductile deformation at depth (Section 210), giving rise to pull-apart basins and rotated crustal blocks (Section 85) In phase 2 (Fig 817d), as rifting and crustal thinning accompany the formation of a divergent margin, the contact is between normal thickness continental lithosphere and thinner, stretched continental lithosphere The newly created rift basin experiences rapid sedimentation from the adjacent continent and subsidence associated with the crustal thinning (Section 773) The sediments are folded and faulted by the transform motion and blocks of material are uplifted (Basile & Allemand, 2002), forming scarps and marginal ridges (see also Section 62).

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