Geochemistry Of The Mafic Rocks, Delaware Piedmont And Adjacent Pennsylvania And Maryland: Confirmation Of Arc Affinity

Author(s)Plank, M.O.
Author(s)Srogi, L.A.
Author(s)Schenck, W.S.
Author(s)Plank, T.A.
Date Accessioned2007-08-07T17:55:31Z
Date Available2007-08-07T17:55:31Z
Publication Date2001
AbstractGeochemical data from Ordovician and Silurian mafic rocks in the Wilmington Complex in Delaware, the James Run Formation in Cecil County, Maryland, and the Wissahickon Formation in Delaware and Pennsylvania were collected in conjunction with preparation of a new geologic map of the Delaware-Pennsylvania Piedmont. Although concentrations of most elements may have been disrupted by metamorphism, the more stable high field strength elements, including the rare earth elements (REE), are consistent within mapped lithodemic units and are compared to modern basaltic magmas from relatively well known tectonomagmatic environments.en
URLhttp://udspace.udel.edu/handle/19716/2814
Languageen_USen
PublisherNewark, DE: Delaware Geological Survey, University of Delawareen
Part of SeriesReport of Investigationsen
Part of Series60en
KeywordsGeochemistryen
KeywordsMafic Rocksen
KeywordsDelaware Piedmonten
KeywordsPennsylvaniaen
KeywordsMarylanden
KeywordsArc Affinityen
TitleGeochemistry Of The Mafic Rocks, Delaware Piedmont And Adjacent Pennsylvania And Maryland: Confirmation Of Arc Affinityen
TypeTechnical Reporten
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