Dj. White et Rm. Clowes, SEISMIC ATTENUATION STRUCTURE BENEATH THE JUAN-DE-FUCA RIDGE FROM TOMOGRAPHIC INVERSION OF AMPLITUDES, J GEO R-SOL, 99(B2), 1994, pp. 3043-3056
Tomographic inversion of seismic amplitudes for attenuation structure
has been applied to first arrival amplitudes from a seismic refraction
profile across the Juan de Fuca Ridge to further constrain a velocity
structure previously obtained by travel time-velocity tomography and
to obtain a model for attenuation variations within the shallow crust.
Amplitude analysis has identified an additional boundary, defined by
a decrease in vertical velocity gradient, at approximately 2.0 km subb
ottom which was not required by the travel time data. This transition
zone likely represents the oceanic layer 2-layer 3 boundary. The analy
sis also identified zones of relatively high attenuation (Q(E) approxi
mately 20-100) at subbottom depths of 0.3-2.0 km beneath the ridge axi
s which correlate well with low-velocity zones (velocities reduced by
< 0.4 km/s) in the velocity model. The subaxial zone is interpreted as
a region of increased fracture porosity and/or permeability associate
d with axial hydrothermal circulation within the extrusives and sheete
d dike complex.