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continental crust and upper mantle, respectively The results of these and other measurements (eg Ranalli & Murphy, 1987; Mackwell et al, 1998) suggest that within the oceanic lithosphere the upper brittle crust gives way to a region of high strength at a depth of 20 60 km, depending on the temperature gradient (Fig 226a) Below this depth the strength gradually decreases and grades into that of the asthenosphere Continental crust, however, is much thicker than oceanic crust, and at the temperatures of 400 700 C experienced in its lower layers the minerals are much weaker than the olivine found at these depths in the oceanic lithosphere Whereas the oceanic lithosphere behaves as a single rigid plate because of its high strength, the continental lithosphere does not (Sections 2105, 85) and typically is characterized by one or more layers of weakness at deep levels (Fig.

The data show two prominent bands of high strain rate along the eastern side of the Sierra Nevada and the western side of the Colorado Plateau These are the eastern California/central Nevada seismic belt and the Intermountain seismic belt, respectively (Fig 79) Focal mechanisms (Fig 710) indicate that the former accommodates both right lateral and normal displacements and the latter accommodates mostly normal motion..

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226b,c) Figure 226c,d shows two other experimentally determined strength curves for continental lithosphere that illustrate the potential effects of water on the strength of various layers These curves were calculated using rheologies for diabase and other crustal and mantle rocks, a strain rate of ( / ) = 10 15 s 1, a typical thermal gradient for continental crust with a surface heat ow of 60 mW m 2, and a crustal thickness of 40 km (Mackwell et al, 1998) The upper crust (0 15 km depth) is represented by wet quartz and Byerlee s (1978) frictional strength law (Section 2102), and the middle crust (15 30 km depth) by wet quartz and power-law creep (Section 2103) These and other postulated strength pro les commonly are used in thermomechanical models of continental deformation (Sections 766, 862, 1025).

When a JIT system is installed, management will find that it is inundated with paperwork stemming from its use of the time-honored picking system This is a method for tracking parts as they flow through a manufacturing facility that involves making a separate inventory entry at all key steps in the production process: when an item is received, when it is stored in the warehouse, when it is picked and sent to the manufacturing floor, when it moves from machine to machine, when it returns to the warehouse for storage, and when it is sold Because of the very large number of moves of very small quantities (and the large number of related transactions to record), a picking system is difficult to maintain in a JIT environment Instead, companies use the backflushing system.

Figure 18.4 Comparison of dynamic behaviour by FEA ( nite-element analysis) of a de ected diamond and silicon cantilever of identical geometry, when the de ection force is turned off. Inducing an oscillating characteristic, the diamond structure passes its quiescent position more than twice as fast as does the silicon one [61]. Reprinted with permission from Diamond and Related Materials, Diamond electro-mechanical micro devices technology and performance by E. Kohn, M. Adamschik, P. Schmid, S. Ertl and A. Fl ter, 10, 9 10. Copyright (2001) Elsevier o

As described in the preceding chapter, backflushing requires no data entry of any kind until a finished product is completed At that time, the total amount finished is entered into the computer system, which multiplies it by all of the components listed in the bill of materials for each produced item This yields a lengthy list of components that should have been used in the production process, and which is subtracted from the beginning inventory balance to arrive at the amount of inventory that should now be left on hand Backflushing is technically an elegant solution, because data entry only occurs once in the entire production process Given the large transaction volumes associated with JIT, this is an ideal solution to the problem However, some serious problems with backflushing must be corrected before it works properly They are as follows: Production reporting.