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Figure 34-8: Dreamweaver s main editing window can show the code view, the design (visual) view, or both.





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A limitation of asking an open-ended question is that people may have beliefs about cues to deception that do not occur to them when they are asked such a question For this reason, many researchers ask participants to complete questionnaires that contain closed questions In a typical closed question method questionnaire, cues are listed and participants are asked to indicate their belief about the relationship between the cue (eg, eye contact ) and deception using rating scales for their answers with headings such as: much more when lying , more when lying , slightly more when lying , no difference , slightly more when telling the truth , more when telling the truth , and much more when telling the truth .

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pressure studies have shown that olivine, the dominant mineral in mantle peridotite, undergoes transformations to the spinel structure at the pressure/temperature conditions at 410 km depth and then to perovskite plus magnesiow stite at 660 km (Table 2.4) (Helffrich & Wood, 2001). Within subducting lithosphere, where the temperature at these depths is colder than in normal mantle, the depths at which these discontinuities occur are displaced exactly as predicted by thermal modeling and high-pressure experiments (Section 9.5). This lends excellent support to the hypothesis that the upper and lower bounds of the transition zone are de ned by phase transformations. The other components of mantle peridotite, pyroxene and garnet, also undergo phase changes in this depth range but they are gradual and do not produce discontinuities in the variation of seismic velocity with depth. Pyroxene transforms into the garnet structure at pressures corresponding to 350 500 km depth; at about 580 km depth Ca-perovskite begins to exsolve from the garnet, and at 660 750 km the remaining garnet dissolves in the perovskite phase derived from the transformation of olivine. Thus the lower mantle mostly consists of phases with perovskite structure.

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