Geology Of The Fall Zone In Delaware
| Author(s) | Spoljaric, N. | |
| Date Accessioned | 2008-03-19T18:49:52Z | |
| Date Available | 2008-03-19T18:49:52Z | |
| Publication Date | 1972-03 | |
| 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. | en_US |
| Sponsor | Water Resources Center, University of Delaware, Newark, Delaware | en_US |
| URL | http://udspace.udel.edu/handle/19716/3115 | |
| Language | en_US | en_US |
| Publisher | Newark, DE: Delaware Geological Survey, University of Delaware | en_US |
| Part of Series | Report of Investigations | en_US |
| Part of Series | 19 | en_US |
| Keywords | crystalline basement complex | en_US |
| Keywords | overlying sediments | en_US |
| Keywords | horst-graben structures | en_US |
| Keywords | Fall Zone in Delaware | en_US |
| Title | Geology Of The Fall Zone In Delaware | en_US |
| Type | Technical Report | en_US |