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Published by way of the yankee Geophysical Union as a part of the Geodynamics Series
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83, 4975-4987, 1978. , 11, 1251-1254, 1984. , Continentaldelaminationand the ColoradoPlateau,J. Lyon-Caen,H. andP. ,84, 7561-7571, 1979. , Gravityanomalies andtheflexureof thelithosphere HimalayaandGangabasin,Tectonics, 4, 513-538, 1985. in the Karakoram,Pakistan,J. , Comparisonof the uppermantleshearwave 15085, 1995. -S. -Y. Sun, The tectonicevolution andtectonicimplications, Geophys. J. R. ,86, 727749, 1986. C. 415-476,1989. L. V. J. L. J. Fitch, and P. A. Lukk, Evidencefor a high-velocity slabassociated with intermediate depthearthquake beneathTibet: Sourcecharacthe Hindu Kushseismiczone,J.
D. , Velocity structureof the Pamir-HinduKush seismic reflection evidence for continentalunderthrusting region: Possible evidence of subducted crust,d. Geophys. beneathsouthernTibet, Nature, 366, 557-559, 1993. , 87, 945-959, 1982. P. , The closingof Tethysandthe tectonicsof the Himalaya,Geol. Am. , 98, 678-701, 1987. , C. Hawkesworth,J. Liu, N. Rogers,S. V. Calsteren,Timing of Tibetan uplift constrainedby analysisof vocanicrocks,Nature, 364, 50-54, 1993. K. -Y. , Suite 103, Seabrook,MD 20706. S.
Qiangtang Block LB. B. •+ *' LB2 - MCT1 (d) MCT1 - QB1 (e) QB2 - QB1 (f) Fig. 1. Observeddifferentialresiduals (a) - (f) and eventlocations(g). The crosses represent possitivedifferentialresiduals. DIFFERENTIAL RESIDUALS 27 1924; Powell and Conaghan, 1973; Barazangi and Ni, 1993]. The cold downwellingsshould exhibit anoma1982],which causedthe uplift of the TibetanPlateau. The louslyhigh seismicvelocities. Whetheror not thereis a penetrationof the Indian lithosphereis believedto have lateralchangein the seismicvelocitiesacrossthe plateau reached to at least north-central Tibet.