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the subordinate CA that leads to a mutually trusted CA. Each entity (such as a user or host) owns a cryptographic public-key and private-key pair. The public key is embedded in a certificate that holds the entity s distinguished name and can be transmitted over the network. The private key is normally encrypted with a password and stored locally on the user s hard drive. Neither the private key nor the password used to encrypt it is ever transmitted over the network. The protocol depends on the secrecy of the private key.

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n Page: This option lets you specify a specific page in a selected document. If you select this option, InDesign provides a Page field in which you specify the page number to open in the selected document, as well as the Zoom Setting pop-up menu, which lets you select how the page is displayed. (Options are Fixed, meaning at the default size in Adobe Reader; Fit View; Fit in Window; Fit Width; Fit Height; Fit Visible; and Inherit Zoom, which uses the current zoom setting in Adobe Reader.) n Text Anchor: This option lets you specify a specific piece of text in the selected document. This would be the selected text. n URL: This is a Web page address (the official name is Uniform Resource Locator), as shown in the New Hyperlink dialog box in Figure 32.2. If you select this option, InDesign displays the URL field in which you type the Web address.

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sqlite3_create_function(), sqlite3_create_collation(), and sqlite3_set_authorizer() and to ATTACH all associated databases as soon as a new database connection is created and before any statements are prepared.

I generally set up my pages with a body font-size of 62.5 percent. This has the effect of making 1 em equal to 10 points and it makes it easier for me to set sizes using ems, but thinking in points. For example, my standard text size is 11 points, which translates quite easily into 1.1 ems. When applied to a page with an image dimensioned by ems, the graphic is reduced in size by a little more than a third. In this example scenario, this is acceptable because I want the image to scale with clarity, as shown in Figure 7-5.

include thinning by delamination or tectonic erosion driven by convective ow in the mantle (Section 1025) At scales smaller than that of the transects shown in Fig 1033b and c, the structure of ancient accretionary orogens provides a record of the processes involved in terrane accretion, including subduction and the formation of crustal-scale wedges For example, seismic re ection data collected across the Appalachian orogen in Newfoundland provide an image (Fig 1034) of an Ordovician-Devonian collisional zone that resulted when several exotic terranes accreted onto the margin of Laurentia (Hall et al, 1998; van der Velden et al, 2004) Prior to the collision, thick sequences of sedimentary rock were deposited on a passive continental margin located outboard of the craton These sequences record the stretching, thinning and eventual rupture (Sections 72, 7.

If you paste the Fireworks rollover code manually into a Dreamweaver HTML document, take care to merge the existing <head> and <body> code with the Fireworks rollover code. And remember: An HTML document can have only one <head> and one <body> tag!

7) of Proterozoic continental lithosphere as the Iapetus Ocean opened during the Late Proterozoic and Early Cambrian This rifting event was followed by a series of terrane collisions and accretionary cycles that formed the Paleozoic orogenies of the Appalachian Mountains (Section 1154) Many of the accreted terranes, such as Meguma and Avalonia, were microcontinents and composite terranes rifted from northwestern Gondwana during the Early Ordovician (Section 1155, Fig 1124a) The seismic re ection data (Fig 1034b) show prominent re ectivity at deep levels of the Appalachian crust that taper westward and merge with a well-de ned Moho (van der Velden et al, 2004) The shape and character of these re ections suggest that they mark the location of an old Ordovician Devonian subduction zone A similar feature occurs beneath the Canadian Shield (Fig 11.

reaction 1 + 2 -+ 3f4, the transition rate per unit volume is Rfi =(Afi 1' /RT, where T is the time interval and R the volume, and

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