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Continental transforms, like their oceanic counterparts (Section 421), are conservative plate boundaries where lithosphere is neither created nor destroyed and strike-slip deformation results in lateral displacements across the fault zone Strike-slip faults generally may occur at a variety of scales in virtually any tectonic setting Only transform faults represent plate boundaries In contrast to oceanic fracture zones, which are characterized by a relatively simple linear trough (Section 612), continental transforms exhibit a structural complexity that re ects differences in the thickness, composition, and pressure temperature pro le of oceanic and continental lithosphere (Sections 27, 2104) In the southwestern United States, for example, relative motion between the Paci c and North American plates is distributed across a zone that ranges from hundreds to a thousand kilometers wide (Fig 81) Similarly, in New Zealand (Fig 8.

Figure 1-10 shows how a web query pulls the Historical Mortgage Rate Report information from the Freddie Mac web site. Note that this report uses the http://www. freddiemac.com/pmms/pmms30.htm link at the Freddie Mac web site.

If you had your computer for a while before you bought FileMaker Pro, you probably also had one or more address or contacts files that you created in other programs address data recorded in an included contact manager such as the Mac OS X Address Book or Microsoft Outlook Express (Windows), for example. Rather than keep this information spread across a handful of programs, it s usually preferable to put all the data into one database or program. Unfortunately, most of us don t plan for (or count on) the difficulties encountered when trying to create one composite file from two or more separate address files. In particular, the various files are likely to contain different fields. This section discusses some simpleprocedures you can use

2), oblique convergence on the South Island has produced a >100-km-wide zone of deformation on the continental portion of the Paci c plate These diffuse, commonly asymmetric patterns generally re ect lateral contrasts in lithospheric strength and areas where continental lithosphere is especially weak (Section 862) In areas where continental lithosphere is relatively cool and strong, transforms tend to display narrow zones of deformation The Dead Sea Transform is an example of this latter type of system where deformation has localized into a zone that is only 20 40 km wide (Fig 83) In this chapter, the shallow (Section 82) and deep (Section 83) structure of continental transforms and major strike-slip faults is illustrated using examples from the southwestern US, New Zealand, the Middle East, and elsewhere Other topics include the evolution of transform continental margins (Section 8.

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Orphan st~at,es arid result,ing obsolet,e messages are detected with t,he version endtable nieclianism. 'This nirt,hod requires that, after recovering from a failure, a process notify ot.her processes by broadcasting a token. The token contains the version number t,hat,failed and t,he t,iniestamp of that version at the point, of restorat,ion. We do not, niake any assumption about the ordering of tokens among themselves or with respect, to the messages. We assunie that, tokens are delivered reliably. Every process maintains some information, called vtable, about other processes in its stable storage. In ufable of Pi, t,here is a record for every known version of processes that ended in a failure. If Pi has received a token about kt,h version of Pi, tlieri it keeps that, token's timest,amp in the corresponding record in vtable. The routirie inswt(i.rtable[j], h n ) insertasthe token in t>hatpart of the !table of Pi that fo keeps t,rack of Pj. A formal descript,ion of t,hc version end-table manipulation algorit'lirri is given in Figure 17.5.

4), the use of velocity elds to describe crustal motion (Section 85), and the mechanisms that control the localization and delocalization of strain during strike-slip faulting (Section 86) This latter subject, and the overall strength of large strike-slip faults (Section 87), are especially important for explaining how continental transforms accomplish large magnitudes of slip..

Listing 9-2: scraperlib.py (Part 2 of 13)

etting a graphic into your layout is one thing, but that s not the end of the story. At a minimum, you want to make sure the image fits in the layout.

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Summary