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One of the most prominent of these zones is the Tintina Fault, which now forms the boundary between the accreted terranes to the west and ancestral North America to the east This fault is a major lithospheric-scale structure that may record several hundred kilometers of dextral displacement since the Paleocene (Clowes et al, 2005) Other major strike-slip displacements are more speculative For example, some paleomagnetic data suggest that, from 90 Ma to 50 Ma, many of the terranes in southeast Alaska and British Columbia were displaced several thousand kilometers northward parallel to the margin from a latitude near present day Baja, California (Umhoefer, 1987; Irving et al, 1996) This interpretation is known as the Baja British Columbia or Baja BC hypothesis.

However, the great magnitude of the postulated displacements has been disputed mainly because the faults along which the terranes may have moved great distances have not been found (eg Cowan et al, 1997) Many correlations of stratigraphy and structures across faults suggest that the displacements are much less than those indicated by some paleomagnetic data Numerous attempts to resolve these con icting observations have been proposed, including: (i) tests of the paleomagnetic data using other types of data (Housen & Beck, 1999; Keppie & Dostal, 2001); (ii) determining reasons why strike-slip faults that record large translations are unlikely to be preserved (Umhoefer, 2000); and (iii) evaluating alternative correlations of units across terranes (Johnston, 2001) It seems probable that only through an interdisciplinary approach that combines paleomagnetic data, plate motions, paleontologic data, and geologic evidence will the history of large-magnitude terrane translation in western North America be resolved..

Where a large number of data are available, one can improve the accuracy of the regression equation by choosing a polynomial with a high order In theory, it is possible to have a polynomial that ts every point in the sample if the order of the polynomial is exactly one less than the total number of sample data A high-order polynomial, however, is not always desirable Besides being more complicated, the large number of associated in exion points would cause numerical problems (eg instability or even divergence) while the set of model equations, formed by coupling the high-order polynomial (representing one component model) with equations for other components, is solved numerically in the simulation process Ahigh order also presents problems to the process of evaluation of the coef cients.

The alphabet of a process is the set of actions in which it c m engage. P + S extends the alphabet of the process P with the actions in the set S.

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Telephone modem Ethernet (local area network) Integrated Services Digital Network Basic Rate Interface (ISDN BRI) Cable modem Asymmetric Digital Subscriber Line (ADSL) Vireless local area network (IEEE 802.11)

Since the data have to be raised to a high power in the calculation and hence the value of the coef cient would be extremely small or large, accuracy of the coef cients so evaluated would be low because rounding-off errors that arise during the calculation process would become signi cant The polynomial regression method can be extended and applied to derive models for systems that involve more than one in uencing variable In this case, one dependent variable is expressed as a function of a number of independent variables.

P1: KPE WY022-28

1. Select the text or position your cursor where you want the new text color to begin. 2. Choose Format Color to open the Colors dialog box. 3. In the Macintosh color picker, the list of available pickers is displayed across the top of the dialog like a toolbar, and each particular interface s options are shown below as they are selected. Choose a color picker by clicking on its icon in the top toolbar, and create the color you want in the rest of the dialog below. (The number and type of color pickers vary from system to system, depending on the version of the operating system and whether you ve added any third-party color pickers.) 4. When you ve found the desired color, click OK.

For the case of two independent variables, where each independent variable can appear up to the second order, the expression, which is a bi-quadratic equation, will be as follows: z( x , y) = (a0 + a1 x + a2 x 2 ) (b0 + b1 y + b2 y 2 ) z = c0 + c1 x + c2 x 2 + c3 y + c4 y 2 + c5 xy + c6 x 2 y + c7 xy 2 + c8 x 2 y 2 (45).

Client-Side versus Server-Side Scripting 257 Client-side scripting 257 Server-side scripting 257 Setting the Default Scripting Language 258 Including a Script 259 Calling an External Script 259 Triggering Scripts with Events 260 Hiding Scripts from Older Browsers 264 Summary 265.

To convert back again, TTime provides a constructor overload that takes a string as parameter: