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Proposed criteria for recognizing intrastratal deformation features in marine high resolution seismic reflection profiles

Geo-Marine Letters

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Abstract

Intrastratal deformation of marine strata is ordinarily recorded in high-resolution seismic reflection profiles as acoustically transparent or "chaotic" intervals marked by hyperbolic echoes. Intrastratal deformation is easily confused with buried slump or slide deposits formed initially at the sea floor. Correct identification of intrastratal deformation depends on the presence of a warped continuously reflective layer overlying a chaotic/transparent layer. Decollement is the key criterion for identification in seismic reflection profiles. Other criteria include intrusive structures or faults rooted in a chaotic/transparent layer and thickening and thinning of a chaotic/transparent layer with transitions to reflective intervals.

Additional Publication Details

Publication type:
Article
Publication Subtype:
Journal Article
Title:
Proposed criteria for recognizing intrastratal deformation features in marine high resolution seismic reflection profiles
Series title:
Geo-Marine Letters
Volume
16
Issue:
4
Year Published:
1996
Language:
English
Larger Work Type:
Article
Larger Work Subtype:
Journal Article
First page:
305
Last page:
312
Number of Pages:
8