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Patrick Connolly
Elastic impedance
Leading Edge (Tulsa, OK) (April 1999), 18(4):438, 440, 442, 444, 446, 448, 450, 452

Abstract:
It is now commonplace for 3-D data sets to be processed as partial offset volumes to exploit the AVO information in the data. However, there has been significant asymmetry in the way these volumes could be calibrated and inverted. The amplitudes of near-offset, or intercept, stacks relate to changes in acoustic impedance and can be tied to well logs using synthetics based on acoustic impedance (AI) or inverted, to some extent, back to AI using poststack inversion algorithms. However, there have been no simple analogous processes for far-offset stacks.

Index Terms/Descriptors:
Atlantic Ocean; AVO methods; body waves; data acquisition; data processing; density; elastic waves; Foinaven Field; Gulf of Mexico; impedance; mathematical methods; nonzero-offset data; North Atlantic; oil and gas fields; oil sands; P-waves; petroleum engineering; reservoir properties; S-waves; sedimentary rocks; seismic waves; stacking; three-dimensional models; volume; well-logging

Latitude & Longitude:
N18°00'00" - N30°04'00" and W98°00'00" - W80°30'00" (Search for maps and images at Alexandria Digital Library)

GeoRef, Copyright 2008, American Geological Institute. Reference includes data supplied by Society of Exploration Geophysicists, Tulsa, OK, United States