Open AccessSeismic structure of the upper mantle beneath the United States by three‐dimensional inversion of body wave arrival times
Author(s) -
Romanowicz Barbara A.
Publication year - 1979
Publication title -
geophysical journal of the royal astronomical society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.302
H-Index - 168
eISSN - 1365-246X
pISSN - 0016-8009
DOI - 10.1111/j.1365-246x.1979.tb04790.x
Subject(s) - geology , classification of discontinuities , seismology , inversion (geology) , mantle (geology) , azimuth , geodesy , geophysics , low velocity zone , geometry , tectonics , lithosphere , mathematical analysis , mathematics
Summary. Teleseismic P and S arrival times to North American stations are obtained from the ISC bulletins for the 10‐yr period 1964–73, and relative travel‐time delays are calculated with respect to standard tables. Station anomalies as well as variations of the delays with azimuth and epicentral distance from station are analysed, and the location of the velocity anomalies responsible for them is discussed. Inversion of the P delays to infer upper mantle velocity structure down to a depth of 700 km is obtained using three‐dimensional blocks, as proposed by Aki, Christofferson & Husebye. Three layers can be resolved in this depth range. It is found that the heterogeneities responsible for the travel‐time delays are primarily located in the first 250 km of the upper mantle, and that they correlate with surface features. Significant heterogeneities subsist to depths of at least 700 km and their broad scale pattern also correlates with the surface features: in the third layer (500 to 700 km depth) there is an increase of velocity from the West to the East of the United States, while the second layer (250 to 450 km depth) exhibits a reversed pattern. A tentative interpretation of these deeper anomalies is made, as being due mainly to topography of the major upper mantle discontinuities, near 400 and 650 km depth.