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ing an outer transition zone made up of a hot, mostly solidi ed crust with small amounts of interstitial melts and an inner zone of crystal mush with suf cient melt for it to behave as a very viscous uid A melt lens only develops in fast-spreading ridges where there is a suf ciently high rate of magma supply for it to persist at the top of the mush zone (Fig 611a) This lens may extend for tens of kilometers along the ridge crest, but is only 1 2 km wide and tens or hundreds of meters in thickness Slow-spreading ridges are assumed to have an insuf cient rate of magma supply for a melt lens to develop (Fig 611b) and that eruptions only occur when there are periodic in uxes of magma from the mantle.

y itself, the Connected Limited Device Configuration (CLDC) is not enough of a platform on which to build applications. Although the CLDC comes with a library of classes that adds the basic features that applications require, those classes are unsupported and are meant to be used as examples only. The Mobile Information Device Profile (MIDP), on the other hand, is a complete and supported foundation for application development. In this chapter, we will look at the first MIDP implementation: the MIDP Early Access Release.

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The purpose of this chapter is to review recent progress in the various areas of modelling applicable to the Design Pathway in effect a hierarchy of methods Then, in 7, interrelationships between the various methods will be explored together with.

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1. Place your cursor where you d like your textarea to appear. 2. From the Spry or Forms categories of the Insert panel, choose Spry Validation Textarea. 3. If your Dreamweaver Preferences are set to display the accessibility attributes for form fields, the Input Form Accessibility Attributes dialog is displayed; click OK after you ve completed the appropriate fields. 4. If your cursor is not within a <form> tag, Dreamweaver asks if you d like to add one; click Yes. 5. In the Spry Textarea Property inspector (see Figure 17-19), choose whether the field should be required by setting or clearing the Required checkbox.

Example 16.5 [2] Maximum likelihooddecoding. We now consider application of these principles to error correction, demonstratingthe idea with the (7,4,3) Hamming code having parity check matrix

Such a model is consistent with the seismic data from ocean ridges and petrologic observations which require magma to have been modi ed by fractionation within the crust, which could not occur in a large, well-mixed chamber It also explains why less fractionation occurs in the volcanic rocks of slow-spreading ridges A problem with this model, however, is that it is not apparent how the layered gabbros of layer 3 might develop Subsequent work by Singh et al (1998), involving further processing of the seismic re ection data obtained by Detrick et al (1993a) near to 14 S on the East Paci c Rise, was speci cally targeted at identifying any along-axis variations in the seismic properties and thickness of the melt lens Their results suggest that only short, 2 4 km lengths of the melt lens contain pure melt capable of erupting to form the upper crust.

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Minimal Polynomial M-(x) = x Mo(x) = x + 1 2 Ml(X1 = ( x - a ) 3 x - a ) ( x - a 4 ) = x 3 + x + 1 ( M 3 ( x ) = ( x - a ) ( x - a S ) ( x - a6) = x3 + x 2 + 1 .