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for a single dipping plane interface
DEPARTMENT OF GEOPHYSICS STANFORD UNIVERSITY, STANFORD, CALIFORNIA
Abstract
A relation is derived for correcting dT/d
for a single dipping interface under a seismic array:
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is the computed azimuth,
' is the observed azimuth,
is the azimuth of the normal to the tilted interface, and (
T/
)' is the observed quantity. The relation is explicitly independent of the dip and the velocities of the media on either side of the interface. This article has been cited by other articles:
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J. HAVSKOV and E. R. KANASEWICH Determination of the dip and strike of the Moho from array analysis Bulletin of the Seismological Society of America, October 1, 1978; 68(5): 1415 - 1419. [Abstract] [PDF] |
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D. W. SIMPSON, R. F. MEREU, and D. W. KING An array study of P-wave velocities in the upper mantle transition zone beneath northeastern Australia Bulletin of the Seismological Society of America, December 1, 1974; 64(6): 1757 - 1788. [Abstract] [PDF] |
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A. QAMAR Revised velocities in the Earth's core Bulletin of the Seismological Society of America, June 1, 1973; 63(3): 1073 - 1105. [Abstract] [PDF] |
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