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magma supply are characterized by negative mantle Bouguer anomalies (MBAs) and the areas of thinned crust between them by positive MBAs (Lin et al, 1990) These latter areas include second order discontinuities in addition to transform faults Evidence for the focusing of magma supply at segment centers is less obvious on the fast-spreading East Paci c Rise, but discontinuities and variations in the size and width of the magma chamber correlate with segmentation (Toomey et al, 1990) These observations suggest that magma is emplaced at segment centers and migrates laterally along the ridge axis towards the segment ends Increasingly it has been recognized that on cooler slowspreading crust this can mean that segment ends are starved of magma and that parts of the crustal section consist of serpentinized mantle.



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The extension of oceanic crust at ridge crests can occur either by the intrusion of magma or by extensional faulting If ridge crests in the vicinity of transform faults are deprived of magma, amagmatic extension becomes more important Perhaps the most spectacular expression of this is the occurrence of major low-angle detachment faults (Ranero & Reston, 1999; MacLeod et al, 2002) (Section 73) on the inside corners of slow-spreading ridge transform intersections that give rise to large corrugated and striated domes of serpentinized peridotite and gabbro (Plate 61 between pp 244 and 245) These corrugated domes are exposed fault planes that deform the upper mantle and lower crust of oceanic lithosphere The corrugations parallel the spreading direction and indicate the direction of motion on the fault The offset on these faults is typically at least 10 15 km (Cann et al, 1997).





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These exposures are thought to result from processes involving extension, detachment faulting, and crustal exure that are similar to those that form metamorphic core complexes in zones of continental extension (Sections 73, 762, 773) For this reason the zones of exhumed peridotite at ridge transform intersections are referred to as oceanic core complexes Examples include the Atlantis Massif at the Mid-Atlantic Ridge Atlantis transform intersection (Plate 61 between pp 244 and 245) (Blackman et al, 1998; Schroeder & John, 2004; Karson et al, 2006) and along the Southeast Indian Ridge south of Australia (Baines et al, 2003; Okino et al, 2004) Figure 615 illustrates the along axis variation of oceanic crust for slow- and fast-spreading ridges as envisioned by Cannat et al (1995) and Sinton & Detrick (1992) respectively Indeed Cannat et al (1995) suggested.

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lie about that event (active); (ii) studies in which participants were shown a videotaped event and then asked to tell the truth or lie about that event (video); (iii) studies in which participants watched a staged event and then asked to tell the truth or lie about that event (staged); and (iv) studies in which participants were asked to tell a truthful or ctitious story about a previous negative experience in their life (memory) As mentioned before, CBCA was developed to evaluate statements from children in alleged sexual abuse cases Many authors still describe CBCA as a technique solely developed to evaluate statements made by children in sexual offence trials (Honts, 1994; Horowitz, Lamb, Esplin, Boychuk, Krispin, & Reiter-Lavery, 1997).

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Figure 2.21 Three classes of fault determined by the orientation of the principal stresses: (a) normal fault; (b) thrust fault; (c) strike-slip fault (after Angelier, 1994, with permission from Pergamon Press. Copyright Elsevier 1994).

When several people are working on a site, they can t just rely on the Web pages to speak for themselves. In any team collaboration, a great deal of organizational information needs to be communicated behind the scenes: who s working on what areas, the status of any given file, when the project is due, what modifications are needed, and so on. Dreamweaver includes a feature called Design Notes that is designed to facilitate team communication in a very flexible manner. Dreamweaver Design Notes are small files that, in a sense, attach themselves to the Web pages or objects they concern. A Design Note can be attached to any HTML page, graphic, or media file inserted into a page. Design Notes follow their corresponding file whenever that file is moved or renamed using the Dreamweaver Files panel; moreover, a Design Note is deleted if the file to

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