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Abstract: ESC General Assembly, Montpellier, 2010
Programme: 906
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Zecchinon L., Claverie P., Collins T., D'amico S., Delille D., Feller G., Georlette D., Gratia E., Hoyoux A., Meuwis M.A. & 1.a.l. (2001). Did psychrophilic enzymes really win the challenge? Extremophiles, 5, 313–321.
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Jouzel J., Waelbroeck C., Malaize B., Bender M., Petit J.R., Stievenard M., Barkov N.I., Barnola J.M., King T., Kotlyakov V.M., Lipenkov V, Lorius C., Raynaud D., Ritz C. & Sowers T. (1996). Climatic interpretation of the recently extended Vostok ice records. Climate dynamics, 12, 513–521.
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Zhang Yang, Ritsema Jeroen, Thorne Michael S, . (2009). Modeling the ratios of SKKS and SKS amplitudes with ultra-low velocity zones at the core-mantle boundary
. Geophysical Research Letters, 36(19), L19303–.
Abstract: Between 105115° degrees, the SKS waveform is complicated by the formation of SPdKS, a wave that has segments of P diffraction along the core mantle boundary. While previous studies have primarily focused on the move-out of SPdKS from SKS, we analyze the concomitant reduction of the SKS amplitude. Long-period SKKS/SKS amplitude ratios present a coherent global pattern. SKKS/SKS is relatively large in North and South American recordings of deep Tonga-Fiji earthquakes but PREM-like in European recordings of earthquakes in South America and North American recordings of earthquakes in Indonesia. Modeling of SKKS/SKS indicate that Ultra-Low Velocity Zones (ULVZs), layers at the base of the mantle with a thickness of about 1020 km and a shear velocity reduction between 2030%, are required to explain high SKKS/SKS ratios and the early move-out of SPdKS.
Keywords: core-mantle boundary, SKS waves, amplitudes, 0545 Modeling, 7203 Body waves, 7208 Mantle,
Programme: 133
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Philippe H. (1993). Etude de la robustesse des phylogénies moléculaires..
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