Skip to Main Content

Abstract

The reflections from beds below the unconformity surface terminate abruptly at various eroded portions of the profile. The chaotic reflection pattern immediately above the unconformity is possibly due to the disorder of the reflecting surfaces. The reflections being fragmentary and of low amplitude suggest that the strata were deposited in variable settings of relatively high energy. The depressed parts of the unconformity surface could be channels of various depths.

You do not currently have access to this chapter.

Figures & Tables

Contents

GeoRef

References

Related

Citing Books via

Close Modal
This Feature Is Available To Subscribers Only

Sign In or Create an Account

Close Modal
Close Modal