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Mapping the Moho beneath the Southern Urals with wide‐angle reflections

1998; American Geophysical Union; Volume: 25; Issue: 24 Linguagem: Inglês

10.1029/1998gl900107

1944-8007

R. Carbonell, D. Lecerf, M. Itzin, J. Gallart, Dennis Brown,

Geological and Geochemical Analysis

A stack of the wide‐angle reflection/refraction component of the URSEIS‐95 experiment provides the first well‐resolved imaged of the Moho beneath the southern Urals. The processing consisted of low pass filter (0–6 Hz), CMP sorting, and a NMO correction without stretch. The PmP phase, a very narrow band and low frequency (up to 6 Hz) wavelet, changes character from west to east along the transect. In the depth converted section, the Moho reaches a maximum depth of 53±2 km beneath the Magnitogorsk arc. Thickness estimates determined from high amplitudes at near critical distances also support a 53 km thick crust. A selective offset stack consisting of traces at 150–250 km offset indicate an undulating, irregular Moho, suggesting either strong lateral velocity variations or high topographic relief beneath the Magnitogorsk arc.