rdlc data matrix

rdlc data matrix

rdlc data matrix

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3 MIAS is directed by Michael Brady and includes the Universities of Oxford, Manchester, King s College, London, University College, London, and Imperial College of Science, Technology and Medicine, London. It is supported by EPSRC and MRC.

PET-CT cameras are presently con gured as sequential gantries, also called in-line cameras, with a shared patient bed, or pallet (see Fig. 9-9). The advantage of this con guration as discussed at the introduction of the chapter is the consistent positioning of the patient between the acquisitions which reduces the risk of misregistration of the images. In addition the CT data can be used for attenuation correction of the PET images. Attenuation correction using CT data is discussed in 8. The CT scanner is usually placed closer to the patient. The CT scan is acquired in its entirety prior to acquiring the PET scan (Fig. 9-10), although the order of acquisition of the studies can be reversed.

upward along the vertical edges. Move/Copy each edge separately. The edges should be snapped to the intersection point of projected arc 3 and the vertical edge. Use the diagram as reference. These copied projected edges will be used as guides to snap to projected arc 4.

100 km; and second, that a more ef cient mechanism than conduction operates below this depth whereby heat is transferred at a much lower thermal gradient. These processes can be distinguished by considering the variation in heat ow over the Earth s surface in conjunction with the variation in content of radioactive minerals of different crustal types. Heat ow generally decreases with the age of the crust (Sclater et al., 1980). Within the oceans heat ow decreases from the ocean ridges to the anking basins and it has been shown (Section 6.4) that this cooling correlates with a progressive thickening of the oceanic lithosphere and an increase in water depth. Similarly, the heat ow of backarc basins (Section 9.10) decreases with age, with the presently active basins exhibiting the greatest heat ow. Within continental regions the heat ow generally decreases with increasing time since the last tectonic event. Consequently, Precambrian shields are characterized by the lowest heat ow and young mountain belts by the highest. The representation of the global pattern of heat ow is dif cult because the density of the observations is highly variable so that the location of contours can be greatly biased by only a small number of measurements. Chapman & Pollack (1975) overcame the problem of limited observations in some areas by predicting the heat ow in those areas on the basis of the correlation of heat ow with the age of the oceanic lithosphere and the age of the last tectonic event to affect continental crust. In Fig. 12.3 their results are presented by a spherical harmonic analysis of the

Table 3-19 (continued)

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Check standard Monitoring standards have to be used to implement these techniques A provisional definition of monitoring standards may be measuring instrument, material measure, or product, whose function is to generate or achieve the value of a quantity in a stable way in time These standards are used at regular intervals to ensure a statistical control of the measurement processes Several examples illustrate this concept A frequent measurement in a laboratory is the measurement of direct current In order to monitor the digital voltmeters, or the automatic measurement sequences, a voltage reference can be used; it can be introduced on different measurement benches to monitor them (by the connection of the reference tension generator to a channel of a channel scanner) These techniques are applied in the field of dimensional metrology It is possible to associate one check standard , or even several, to each measurement bench.

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