Planktonic Foraminifera And The Cretaceous-Tertiary Boundary In Central Delaware

Author(s)Jordan, R.R.
Date Accessioned2007-08-06T18:24:04Z
Date Available2007-08-06T18:24:04Z
Publication Date1962-02
AbstractThe uppermost Cretaceous and lowermost Tertiary planktonic Foraminifera obtained from cores taken in a deep well near Dover, Delaware are studied. The Cretaceous foraminifers are of the Heterohelix-Globotruncana assemblage and are probably of late Maescrichtian age. The Danian Globorotalia compressa - Globigerinoides daubjergensis zone lies immediately above. The Cretaceous-Tertiary boundary is at a depth of approximately 980 feet and lies within a gray, glauconitic silt.en
URLhttp://udspace.udel.edu/handle/19716/2796
Languageen_USen
PublisherNewark, DE: Delaware Geological Survey, University of Delawareen
Part of SeriesReport of Investigationsen
Part of Series5en
KeywordsPlanktonicen
KeywordsForaminiferaen
KeywordsCretaceous-Tertiaryen
KeywordsCentral Delawareen
TitlePlanktonic Foraminifera And The Cretaceous-Tertiary Boundary In Central Delawareen
TypeTechnical Reporten
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