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Determining the degree to which continental deformation is continuous or discontinuous has proven dif cult to achieve with certainty in many areas One reason for the dif culty is that the short-term (decadescale) surface velocity eld measured with geodetic data usually appears continuous at large scales (kilometers to hundreds of kilometers) (Section 2105) This characteristic results because geodetic positioning techniques provide velocity estimates at speci c points in space, with the density of available points depending on the region and the scale of the investigation (Bos & Spakman, 2005) Most interpretation methods start with some interpolation of the geodetic data, with the nal resolution depending on the number and distribution of the available stations (Jackson, 2004) In addition, available information on fault slip rates is incomplete and those that are calculated over short timescales may not be representative of long-term slip rates (Meade & Hager, 2005; McCaffrey, 2005).

Collins, WJ (2002a) Hot orogens, tectonic switching, and creation of continental crust Geology 30, 535 8 Collins, WJ (2002b) Nature of extensional accretionary orogens Tectonics 21, doi:1029/2000TC001272 Collins, WJ & Sawyer, EW (1996) Pervasive granitoid magma transfer through the lower middle crust during non-coaxial compressional deformation J metam geol 14, 565 79 Collins, WJ, Van Kranendonk, MJ & Teyssier, C (1998) Partial convective overturn of Archaean crust in the east Pilbara Craton, Western Australia: driving mechanisms and tectonic implications J struct Geol 20, 1405 24 Condie, KC (1982a) Plate Tectonics and Crustal Evolution Pergamon Press, Oxford Condie, KC (1982b) Early and middle Proterozoic supracrustal successions and their tectonic settings Amer J Sci 282, 341 57 Condie, KC (1986) Geochemistry and tectonic setting of early Proterozoic supracrustal rocks in the southwestern United States J Geol 94, 845 64 Condie, KC.

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Vocabulary is important; shared vocabulary more so Words should mean things, and hopefully the same things to all participants When you use encryption, compression, or abbreviated codes in messages, the capability of an IDS or firewall to reason intelligently about the contents is lost This situation is not bad This statement should reinforce the notion that depending solely on IDS or firewall instances for systems security architecture is a flaw Do not implement your own cryptographic protocols or primitives Start with a single cryptographic family of primitives and use it everywhere until someone complains for performance or security reasons Consider the risk of implementation errors, and buy a.

If accurate long-term slip rates on all crustal faults were available, then the problem could be solved directly Furthermore, even though continental deformation is localized along faults over the long term, the steady-state motion of an elastic upper crust over the short-term contains little information about the rheology of the deforming material, so the importance of the faults in the overall mechanical behavior of the lithosphere is unclear This latter uncertainty clouds the issue of whether deformation along continental transforms is driven mostly by edge forces, basal tractions, or gravitational forces (Savage, 2000; Zatman, 2000; Hetland & Hager, 2004) (Section 853) Despite the dif culties involved in quantifying continental deformation, geoscientists have been able to.

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(1998) Episodic continental growth and supercontinents: a mantle avalanche connection Earth planet Sci Lett 163, 97 108 Condie, KC (2000) Episodic continental growth models: afterthoughts and extensions Tectonophysics 322, 153 62 Condie, KC (2005a) TTGs and adakites: are they both slab melts Lithos 80, 33 44 Condie, KC (2005b) Earth as an Evolving Planetary System Elsevier, Amsterdam Coney, PJ (1989) Structural aspects of suspect terranes and accretionary tectonics in western North America J struct Geol 11, 107 25 Coney, PJ & Harms, TA (1984) Cordilleran metamorphic core complexes: Cenozoic extensional relics of Mesozoic compression Geology 12, 550 4 Coney, PJ, Jones, PL & Monger, JWH (1980) Cordilleran suspect terranes Nature 288, 329 33 Conti, CM et al.

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