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- W2057480518 abstract "Abyssal variations beneath the Baikal rift zone are revealed in an irregular seismic stratification of the crust, the presence of an intracrust waveguide and by the vast (> 200,000 km2) underlying area of anomalously low velocity (Pn = 7.6−7.8 km/sec) uppermost mantle. In its abyssal structure the Baikal rift is heterogeneous along the strike, with sharp changes in crustal thickness (35–50 km). Comparison of first-arrival seismic-velocity curves and also the respective velocity columns reveals the essential similarity of upper-mantle seismic cross-sections for all continental rift zones. The anomalous upper layer of the mantle (ca. 7.7 km/sec) is relatively thin (15-13 km) and can be linked with the mantle waveguide only locally." @default.
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- W2057480518 date "1978-01-01" @default.
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- W2057480518 title "Deep structure of the baikal and other continental rift zones from seismic data" @default.
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- W2057480518 doi "https://doi.org/10.1016/0040-1951(78)90219-6" @default.
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