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(2004) Seismic stratigraphic record of transpression and uplift on the Romanche transform margin, offshore Ghana Tectonophysics 378, 1 16 Atwater, T (1970) Implications of plate tectonics for the Cenozoic tectonic evolution of Western North America Bull geol Soc Am 81, 3513 36 Atwater, T (1989) Plate tectonic history of the northeast Paci c and western North America In Winterer, EL, Hussong, DM & Decker, RW (eds) The Eastern Paci c and Hawaii The Geology of North America N, pp 21 72 Geological Society of America, Boulder, CO Audley-Charles, MG (2004) Ocean trench blocked and obliterated by Banda forearc collision with Australian proximal continental slope Tectonophysics 389, 65 79 Audoine, E, Savage, MK & Gledhill, K (2004) Anisotropic structure under a back arc spreading region, the Taupo Volcanic Zone, New Zealand J geophys Res 109, B11305, doi:101029/ 2003JB002932 Auzende, J-M et al.

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(1989) Direct observation of a section through slow-spreading oceanic crust Nature 337, 726 9 Axen, GJ (2004) Mechanics of low-angle normal faults In Karner, GD et al (eds) Rheology and Deformation of the Lithosphere at Continental Margins, pp 46 91 Columbia University Press, New York Axen, GJ & Bartley, JM (1997) Field test of rolling hinges: existence, mechanical types, and implications for extensional tectonics J geophys Res 102, 20515 37 Aydin, A & Page, BM (1984) Diverse Pliocene Quaternary tectonics in a transform environment, San Francisco Bay region, California Bull geol Soc Am 95, 1303 17 Ayele, A, Stuart, GW & Kendall, J-M (2004) Insights into rifting from shear-wave splitting and receiver functions: an example from Ethiopia Geophys J Int 157, 354 62 Babeyko, AY & Sobolev, SV.

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R2 is the same value as X. Thus, the outcome of a sequence of two XORs using the same value produces the original value. To see this feature of the XOR in ...

other. The FDA did not give any guidance on organizing clinical trials or compiling an application. As Bob Temple, the associate director of medical policy, wrote in a textbook he coauthored in 1995, There was, in fact, an explicit concern that too much participation by FDA staff in the development process would leave the Agency unable to be appropriately neutral and analytical when the resulting data were submitted as part of an NDA. By the same token, the agency did not get all those phone calls from Congress. Bill Vodra said that when he was associate chief counsel in the late 1970s, a drug company wouldn t have a congressional strategy as part of drug development. Things slowly changed, in part spurred by the constant complaints that the FDA was taking too long to approve new drugs. Agency officials decided that during the trial process, neutrality did not have to mean silence. If there were standards for safety and efficacy that new drugs needed to meet, and if the FDA had recommendations on how to meet those standards, then telling the drug companies what those standards and recommendations were would not be some sort of unethical collusion that would cause

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(2005) Quantifying different modes of the late Cenozoic shortening in the central Andes Geology 33, 621 4 Babeyko, AY et al (2002) Numerical models of the crustal scale convection and partial melting beneath the Altiplano Puna plateau Earth planet Sci Lett 199, 373 88 Baby, P et al (1992) Geometry and kinematic evolution of passive roof duplexes deduced from cross section balancing: example from the foreland thrust system of the southern Bolivian Subandean Zone Tectonics 11, 523 36..

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The generalized morphology of an island arc system is shown in Fig. 9.3, although not all components are present in every system. Proceeding from the oceanward side of the system, a exural bulge about 500 m high occurs between 100 and 200 km from the trench. The forearc region comprises the trench itself, the accretionary prism, and the forearc basin. The accretionary prism is constructed of thrust slices of trench ll ( ysch) sediments and possibly oceanic crust sediments that have been scraped off the downgoing slab by the leading edge of the overriding plate. The forearc basin is a region of tranquil, at-bedded sedimentation between the accretionary prism and island arc. The island arc is made up of an outer sedimentary arc and an inner magmatic arc. The sedimentary arc comprises coralline and volcaniclastic sediments underlain by volcanic rocks older than those found in the magmatic arc. This volcanic substrate may represent the initial site of volcanism as the relatively cool oceanic plate began its descent. As the cold plate extended further into the asthenosphere the position of igneous activity moved backwards to its steady state location now represented by the magmatic arc. Processes contributing to the formation of the island arcs are discussed in Section 9.8 and 9.9. The island arc and remnant arc (backarc ridge), rst recognized by Vening Meinesz (1951), enclose a

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