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How thin is a thin bed? An alternative perspective

Hongliu Zeng
How thin is a thin bed? An alternative perspective
Leading Edge (Tulsa, OK) (October 2009) 28 (10): 1192-1197

Abstract

The resolution limit of seismic data is a complex issue that involves not only wavelet frequency, phase characters, and data quality (S/N), but also criteria on how to measure resolvability. In his classic 1973 paper "How thin is a thin bed?", Widess discussed the effect of bed thickness on re-flection character and timing using a symmetrical wavelet and suggested that lambda /8 be the resolution limit, or the minimum distance at which a composite waveform stabilized as the derivative of the waveform from an individual reflection. However, this definition has more theoretical than practical impact because of the difficulties in judging waveform stabilization. A more workable and widely accepted definition of resolution limit corresponds to Rayleigh's criterion of peak-to-trough separation at lambda /4 (Kallweit and Wood, 1982). This point is also a "tuning point", at which composite amplitude reaches a maximum if an opposite-polarity (at top and bottom) thin bed is involved.


ISSN: 1070-485X
EISSN: 1938-3789
Serial Title: Leading Edge (Tulsa, OK)
Serial Volume: 28
Serial Issue: 10
Title: How thin is a thin bed? An alternative perspective
Author(s): Zeng, Hongliu
Affiliation: Bureau of Economic Geology, Austin, TX, United States
Pages: 1192-1197
Published: 200910
Text Language: English
Publisher: Society of Exploration Geophysicists, Tulsa, OK, United States
References: 7
Accession Number: 2009-095185
Categories: Economic geology, geology of energy sourcesApplied geophysics
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus.
N18°00'00" - N30°04'00", W98°00'00" - W80°30'00"
N29°00'00" - N33°00'00", W94°04'60" - W89°00'00"
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Reference includes data from GeoScienceWorld, Alexandria, VA, United States. Reference includes data supplied by Society of Exploration Geophysicists, Tulsa, OK, United States
Update Code: 200951

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