Seismic analysis of the differential compaction of reef and off-reef sediments

Abstract

Seismic and well-log control across two closely spaced, yet morphologically different Leduc Formation reef complexes was analyzed. On the basis of these data, the compaction of reef and offreef sediments is shown to be a function of depth of burial, rate of burial, time, and lithology. The initial heights of these reefs and the thickness of the encasing shales are estimated. These estimates are based on the premise that the burial histories as well of the two example reefs are similar.

Department(s)

Geosciences and Geological and Petroleum Engineering

Document Type

Article - Conference proceedings

Document Version

Citation

File Type

text

Language(s)

English

Rights

© 2023 Society of Exploration Geophysicists, All rights reserved.

Publication Date

01 Jan 1989

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