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Second, because they deal with intangibles and are hard to get a handle on, they tend to be lled with uncertainty Given the smaller size of typical information age projects and their high degree of uncertainty, the need for rigid formality in their management is generally low; therefore, in most such cases, heavy formality is undesirable Nevertheless, this call for exibility on information age projects should not be used as an excuse for poor planning and control..

We use the term reconstruction of events to represent any activity within an application that records historical or transactional events for later audit or replay. Systems that implement this architectural goal support the concept of system memory. The system can remember its past from application startup or from some safe system state up to the point of failure or error. The goal of event reconstruction through comprehensive auditing appears in many forms in applications.

Substituting the sequence of S - 1 zeros into Ci gives Ci = 0; proceeding forward from that index shows that all the Cis are 0, so that C = 0. 0 Based on our transform interpretation, we have the following definition (construction) for a Reed-Solomon code: A Reed-Solomon code can be obtained by selecting as codewords all vectors whose transforms have S - 1 = 2t consecutive zeros. That is, a vector c is a codeword in a code with minimum distance 2t 1 if its transform C = F[c] has a consecutive sequence of 2t zeros (where the sequence of zeros starts from some fixed index in the transform vector). This definition of the code can be used to establish another encoding mechanism for Reed-Solomon codes. Given a message sequence m = (mo, l , . . . ,mk-I), form the m vector

P1: JYS WY022-18 WY022/Pfaffenberger WY022/Pfaffenberger-v3.cls June 8, 2004 14:58

The link tag does not result in any visible text being rendered, but can be used by user agents to provide additional navigation or other user-interface tools. Another important use of the link tag is to provide alternate content for search engines. For example, the following link references a French version of the current document (chapter10.html):

package com.aboutobjects.pitfalls; import import import import import import import java.math.BigDecimal; java.text.DecimalFormat; java.text.ParseException; java.text.ParsePosition; java.text.SimpleDateFormat; java.util.ArrayList; java.util.Date;

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Conrad discontinuity, but this is not globally developed By contrast, the layering of the majority of oceanic crust is well de ned into three distinct layers However, the nature of these layers, in particular layers 2 and 3, may change quite markedly with depth 2 Thickness The thickness of continental crust averages 40 km but is quite variable, thinning to only a few kilometers beneath rifts and thickening to up to 80 km beneath young mountain belts Most oceanic crust has a remarkably constant thickness of about 7 km, although layer 1, the sedimentary layer, increases in thickness towards ocean margins that are not characterized by ocean trenches Differences in the thickness and the creep strength (Section 2104) of continental crust make the lower crust of continental regions much more likely to deform pervasively than in the lower layers of oceanic crust (Section 2105) 3 Age.

Continental crust is as at least as old as 40 Ga, the age of the oldest rocks yet discovered (Section 111) On a very broad scale the oldest crust consists of Precambrian cratons or shield areas that are surrounded by younger orogenic belts, both active and inactive Oceanic crust, however, is nowhere older than 180 Ma, and progressively increases in age outwards from oceanic ridges (Section 41) Oceans are consequently viewed as essentially transient features of the Earth s surface About 50% of the surface area of the present day ocean oor has been created during the last 65 Ma, implying that 30% of the solid Earth s surface has been created during the most recent 15% of geologic time 4 Tectonic activity Continental crust may be extensively folded and faulted and preserves evidence of being subjected to multiple tectonic events.

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Oceanic crust, however, appears to be much more stable and has suffered relatively little deformation except at plate margins 5 Igneous activity There are very few active volcanoes on the great majority of the continental crust The only major locations of activity are mountain belts of Andean type (Section 98) The activity within the oceans is very much greater Ocean ridges and island arcs.