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Flash movies require the same basic parameters as their Shockwave counterparts and Flash movies have a few additional optional ones as well. As it does for Shockwave files, Dreamweaver sets almost all the attributes for Flash movies through the Property Inspector. The major difference is that several more parameters are available. To set or modify the attributes for a Flash file, follow these steps: 1. After your Flash movie has been inserted in the Document window, make sure it s selected. Dreamweaver automatically inserts the correct dimensions for your Flash movie. 2. Set any attributes in the Property Inspector as needed for your Flash movie. ( Refer to the previous descriptions of these attributes in the section Specifying Shockwave Properties. ) In addition, you can also set the parameters described in Table 23-2.



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void gcd(int a, int b, int &g, int & s , int &t);

The number of victims and the amount of information recovered indicated the relative ease with which Lukamba was able to commit his frauds With the personal information he obtained, he conducted full account takeovers that allowed him to transfer funds; change billing addresses, e-mail addresses and telephone numbers for the accounts; and have additional credit cards sent to him He was also able to conduct application fraud using the victims information to open new accounts A major challenge in investigating Internet fraud is that victims, suspects and witnesses can be in multiple jurisdictions However, Internet frauds can be resolved successfully if the investigators use a combination of computer research, traditional investigative tools and interjurisdictional law enforcement cooperation This case required an inordinate amount of resources, time and labor to investigate.





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There are several compile-time solutions to stack overflow problems. StackGuard implements a Sentinel-based overflow protection solution. StackGuard uses a compiler extension that adds stack-bounds checks to the generated code. Function calls, in code compiled with StackGuard, are modified to first insert a sentinel word called a canary onto the stack before the return address. All exploits that use sequential writing of bytes to write down the user stack until the return address is overrun must first cross the canary value. The canary is chosen at random to prevent attacks that guess the canary. Before the function returns, the canary is checked and if modified, the program terminates. StackGuard will not protect against attacks that can skip over the canary word. Such exploits are believed to be very difficult to construct.

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The G function expresses an average logarithmic increment or decrement of the account associated with one trade, as the number of trades goes to infinity. Whether this will be an increment or a decrement depends on the parameters from the right side of Equation (4.12). Now consider the function G as a continuous function of a single independent variable b and write G = G(b). All other parameters, such as pw, pl, Aw, Al, M, are fixed. The higher the value of G the faster the account grows. This function may have a maximum in the interval of b satisfying the conditions (4.07) and/or (4.08). If it does have a maximum G* at some point b*, then the first derivative dG/db must be equal to zero at point b*. This can be written as dG/db(b*) = 0. A calculus exercise gives the expression for the derivative: dG/db = pw (Aw /M )(M/(M + bAw )) pl (Al /M )(M /(M bAl)) = pw Aw /(M + bAw ) pl Al /(M bAl )

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transition zone between the shelf edge and the Lofoten basin is 50 150 km wide, includes an abrupt lateral gradient in crustal thinning, and is covered by layers of volcanic material that display shallow seaward dipping re ectors (Fig 732a) The 50 150 km width of this zone is typical of many rifted margins, although in some cases where there is extreme thinning the zone may be several hundred kilometers wide Crustal relief in this region is related to faulted blocks that delineate uplifted highs In the Lofoten example, the continent ocean boundary occurs landward of magnetic anomaly 24B (53 56 Ma) and normal ocean crust occurs seaward of magnetic anomaly 23 (Fig 731b) Crustal thinning is indicated by variations in Moho depth The Moho reaches a maximum depth of 26 km beneath the continental shelf and 11 12 km beneath the Lofoten basin.

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