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Johnson, 2002) This motion created a zone of active deformation that stretches 3000 km north of the Himalayan mountain chain (Fig 1013) Global Positioning System (GPS) measurements show that India is moving to the northeast at a rate of some 35 38 mm a 1 relative to Siberia (Larson et al, 1999; Chen et al, 2000; Shen et al, 2000; Wang et al, 2001) This rate is considerably slower than the long-term rates of 45 50 mm a 1 estimated from global plate motion models (DeMets et al, 1994), which is typical of the short-term interseismic strain rates measured using geodetic data (eg Section 85).



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The geodetic data suggest that deformation within the Tibetan Plateau and its margins absorbs more than 90% of the relative motion between the India and Eurasia plates, with most centered on a 50-km-wide region of southern Tibet (Wang et al, 2001) Internal shortening of the plateau accounts for more than onethird of the total convergence An additional component of shortening is accommodated north of the Tibetan Plateau in Pamir, Tien Shan, Qilian Shan, and elsewhere, although the rates are not well known in these areas South of the Kunlun Fault (Fig 1013), the surface velocity eld shows that the Tibetan Plateau is extruding eastward relative to both India and Asia (Fig 1016) This motion, where slices of crust move laterally out of the way of colliding plates by slip on strike-slip faults, is termed lateral escape.

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The movement also involves the rotation of material around a curved belt in Myanmar called the eastern Himalayan syntaxis The term syntaxis refers to the abrupt changes in trend that occur on either side of the Himalaya in Myanmar and Pakistan where mountain ranges strike at nearly right angles to the trend of the Himalaya East of the plateau, North China and South China are moving to the east-southeast at rates of 2 8 mm a 1 and 6 11 mm a 1 relative to stable Eurasia, respectively A GPS velocity pro le across the Tibetan Plateau (Fig 1016a) is mostly linear parallel to the predicted direction of the India Eurasia collision (N21 E), except for a high gradient across the Himalaya at the southern end of the plateau (Wang et al, 2001).

This mostly linear trend suggests that the shortening across the plateau is broadly distributed; otherwise signi cant deviations across individual fault zones would be expected However, this generally continuous style of deformation appears to be restricted mostly to the plateau itself Rigid block-like motion appears to characterize regions to the north and northeast of the plateau, including the.

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You can also select a single cell by pressing the Ctrl (Command) key and clicking once in the cell, or you can select the rightmost <td> tag in the Tag selector.

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InDesign imports many file formats. If your graphics program s format is not one of the ones listed here, chances are it can save as or export to one. In the following list, the text in monofont and parentheses is the filename extension common for these files on PCs. The file formats InDesign imports include: n BMP: The native Windows bitmap format (.bmp, .dib). n EPS: The Encapsulated PostScript file format favored by professional publishers. A variant is called DCS, a color-separated variant whose full name is Desktop Color Separation (.eps, .dcs). n Flash animation: For use in interactive documents, InDesign supports this Adobeowned, cross-platform format (.swf). 32 covers the use of multimedia elements in more detail. n GIF: The Graphics Interchange Format common in Web documents (.gif). n JPEG: The Joint Photographic Expert Group compressed bitmap format often used on the Web (.jpg or .jpeg). n Illustrator: The native format in Adobe Illustrator 5.5 through CS4 is similar to EPS (.ai). n PCX: The PC Paintbrush format that was very popular in DOS programs and early version of Windows; other formats have now largely supplanted it (.pcx, .rle). n PDF: The Portable Document Format that is a variant of PostScript (as EPS is) and is used for Web-, network-, and CD-based documents. InDesign CS4 supports PDF versions 1.3 through 1.8 (the formats used in Acrobat 4 through 9) (.pdf).

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