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Measurements of seismic anisotropy (Section 2.1.8) and the results of mineral physics experiments have been used to infer creep mechanisms and ow patterns in the mantle (Karato, 1998; Park & Levin, 2002; Bystricky, 2003). The deformation of mantle minerals, including olivine, by dislocation creep results in either a preferred orientation of crystal lattices or a preferred orientation of mineral shapes. This alignment affects how fast seismic waves propagate in different directions. Measurements of this directionality and other properties potentially allow investigators to image areas of the mantle that are deforming by dislocation creep (Section 2.10.3) and to determine whether the ow is mostly vertical or mostly horizontal. However, these interpretations are complicated by factors such as temperature, grain size, the presence of water and partial melt, and the amount of strain (Hirth & Kohlstedt, 2003; Faul et al., 2004). Most authors view power-law (or dislocation) creep as the dominant deformation mechanism in the upper mantle. Experiments on olivine, structural evidence in mantle-derived nodules, and the presence of seismic anisotropy suggest that power-law creep occurs to a depth of at least 200 km. These results contrast with many studies of post-glacial isostatic rebound (Section 2.11.5), which tend to favor a diffusion creep mechanism for ow in the upper mantle. Karato & Wu (1993) resolved this apparent discrepancy by suggesting that a transition from power-law creep to diffusion creep occurs with depth in the upper mantle. Diffusion creep may become increasingly prominent with depth as pressure and temperature increase and stress differences decrease. A source of potential uncertainty in studies of mantle rheology

Figure 8-13 compares how styles are rendered in Dreamweaver s Design view, Internet Explorer, and Mozilla Firefox. Although the various renderings are mostly the same, notice the subtle difference between how the Keyboard style is rendered in Dreamweaver (far left) and in either browser. The various styles may be rendered quite a bit differently in other browsers and other browser versions. Two of the physical style tags bold and italic are controlled by a Preferences setting. Although you can use the <b> and <i> tags to style text, it is considered better practice to use the equivalent logical tags, <strong> and <em>. Dreamweaver enables you to specify which tags to use via the Use <strong> And <em> In Place Of <b> And <i> option in the General category of Preferences. If this option is checked (the default), <strong> and <em> tags are used to code bold or italic text, respectively; if the option is clear, <b> and <i> tags are used. To actually apply bold or italic formatting, select the text and click the Bold or Italic button on the Property inspector s HTML tab, or use the keyboard shortcuts (Ctrl+B [Command+B] and Ctrl+I [Command+I], respectively). Buttons for bold, italic, strong, and emphasis are also available in the Text category of the Insert panel.

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1. Make sure that you have added InContext Editing editable regions to any section of the page you want to repeat. 2. Select the outermost section of the element you want to repeat in the Tag Selector or in Code view.

Stopping your losses Write down the conditions Ulysses: Untie me Don t you dare! Let s hear it from the experts Keeping your pro ts

One of the major advantages of using named anchors is the almost instantaneous response the viewer receives when they click them. The browser only needs to scroll to the particular place in the document because the entire page is loaded. For long text documents, this capability is an invaluable time-saver. Once you have placed a named anchor or all of them at once in your document, you can link to these anchors. Follow these steps to create a link to a named anchor in the same document: 1. Select the text or image that you want to designate as a link. 2. In the Link text box of the Property Inspector, type a hash mark, #, followed by the exact anchor name. For example:

Proof Let c = (ci, . . . ,c,) be a codeword and let p ( x ) be a polynomial of degree < k that maps to the codeword: p(xj) = c j for all x j in the support set of the code. Let g(x) = Q M ( x , p(x)). We will show that g ( x ) is identically 0, which will imply that (Y - P ( x ) >Q M ~ Y ,) . ~ Write SM(C)= m i m2 . . .m,. The polynomial Q M ( x y) has a zero of order , m j at (Xj, C j ) (by the definition of Q M ) . By Lemma 7.18, (x - xj)mj Q M ( x , ( x ) ) , for p j = 1,2, . . . , n. Thus g(x) = Q M ( x , p ( x ) ) is divisible by the product

JavaScript code for the onclick attribute is contained directly in the value of the attribute because the code is only one line a separate function is not necessary.

P1: JYS WY022-33 WY022/Pfaffenberger WY022/Pfaffenberger-v3.cls June 9, 2004 15:11