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Windley, BF (1984) The Evolving Continents, 2nd edn Wiley, London Wingate, MTD, Pisarevsky, SA & Evans, DAD (2002) Rodinia connections between Australia and Laurentia: no SWEAT, no AUSWUS Terra Nova 14, 121 8 Winter, JD (2001) An Introduction to Igneous and Metamorphic Petrology Prentice-Hall, New Jersey Wittlinger G et al (2004) Teleseismic imaging of subducting lithosphere and Moho offsets beneath western Tibet Earth planet Sci Lett 221, 117 30 Wolfenden, E et al (2004) Evolution of the northern Main Ethiopian rift: birth of a triple junction Earth planet Sci Lett 224, 213 28 Wolfenden, E et al (2005) Evolution of a volcanic rifted margin: southern Red Sea, Ethiopia Bull geol Soc Am 117, 846 64 Woodcock, NH & Fischer, M (1986) Strike-slip duplexes J struct Geol 8, 725 35 Woodcock, NH & Rickards, B.



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(2003) Transpressive duplex and ower structure: Dent Fault System, NW England J struct Geol 25, 1981 92 Woodhouse, JH & Dziewonski, AM (1984) Mapping the upper mantle: three dimensional modelling of Earth structure by inversion of seismic waveforms J geophys Res 89, 5953 86 Wyllie, PJ (1981) Plate tectonics and magma genesis Geol Rundsch 70, 128 53 Wyllie, PJ (1988) Magma genesis, plate tectonics and chemical differentiation of the Earth Rev Geophys 26, 370 404 Wyman DA & Kerrich, R (2002) Formation of Archean continental lithospheric roots: the role of mantle plumes Geology 30, 543 6 Xie, J et al (2004) Lateral variations of crustal seismic attenuation along the INDEPTH pro les in Tibet from Lg Q inversion J geophys Res 109, B10308, doi:101029/2004JB002988 Y ez, G & Cembrano, J (2004) Role of viscous plate coupling in the late Tertiary Andean tectonics J geophys.





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Res 109, B02407, doi:101029/2003JB002494 Yamazaki D & Karato, S-I (2001) Some mineral physics constraints on the rheology and geothermal structure of Earth s lower mantle American Mineralogist 86, 385 91 Yin, A & Harrison, TM (2000) Geologic evolution of the Himalayan Tibetan Orogen Annu Rev Earth planet Sci 28, 211 80 Yogodzinski, GM, Lees, JM Churikova, TG et al (2001) Geochemical evidence for the melting of subducting oceanic lithosphere at plate edges Nature 409, 500 4 Young, GM (1992) Late Proterozoic stratigraphy and the Canada Australia connection Geology 20, 215 18 Yuan, X et al (2000) Subduction and collision processes in the central Andes constrained by converted seismic phases Nature 408, 958 61..

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This differs from Prob. 19. The integrand is not analytic! 2i 22. cos z 0 1 cosh 2 by the first method 24. By linearity we can integrate the two terms separately. The integral of z is 0 by Theorem 1. The integral of 1/z is 2 i; see Example 5. . 26. z(t) t it 2 ( 1 t 1), z (t) 1 2it, z t it 2, so that

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sequences failed and were scraped off the downgoing plate, forming the Himalayan fold and thrust belt 2 Continental underthrusting The underthrusting, or subduction, of continental lithosphere beneath another continental plate is one of the most important mechanisms that accommodates convergence in zones of continental collision The rheology of the two plates and the degree of mechanical coupling between them control shortening and the evolution of stresses within the overriding plate In the Himalayan Tibetan orogen, the underthrusting of Indian continental lithosphere drives intra-plate shortening at the leading edge of the Indian plate and in Tibet, and, possibly, also farther north into Asia The resultant shortening has generated crust that is up to 70 80 km thick (Section 1045) and has contributed to the uplift and growth of the Tibetan Plateau Like its counterpart in the central Andes (Section 102.

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