1887

Abstract

Measurements of seismic Q proliferate in the geophysics literature. Laboratory tests on highly confined matrix, large scale in situ estimation of Q from geothermal areas and from earthquake coda, and more recent measurements in and above anisotropic fractured hydrocarbon reservoirs from walkaway VSP using multi-azimuth sources, give an assortment of seismic Q from a multitude of depths and rock types.

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/content/papers/10.3997/2214-4609.201405184
2005-06-13
2024-12-05
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/content/papers/10.3997/2214-4609.201405184
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