Geology Of The Fall Zone In Delaware
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Date
1972-03
Authors
Journal Title
Journal ISSN
Volume Title
Publisher
Newark, DE: Delaware Geological Survey, University of Delaware
Abstract
The complex geologic framework of the Fall Zone in Delaware is primarily caused by diverse structural features present in the crystalline basement rocks that have exerted a considerable influence on the distribution of the overlying sediments of the Coastal Plain.
Description
Keywords
crystalline basement complex, overlying sediments, horst-graben structures, Fall Zone in Delaware