Accreted forearc, continental, and oceanic rocks of Maryland’s Eastern Piedmont: The Potomac terrane, Baltimore terrane, and Baltimore Mafic Complex-Reference-Cited by-同舟云学术

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Accreted forearc, continental, and oceanic rocks of Maryland’s Eastern Piedmont: The Potomac terrane, Baltimore terrane, and Baltimore Mafic Complex

Published:2020 Issue: Volume: Page:21-41
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Container-title:Geology Field Trips in and around the U.S. Capital
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Geological Society of America

Reference91 articles.

1. The discordant Doe Run thrust: Implications for stratigraphy and structure in the Glenarm Supergroup, southeastern Pennsylvania Piedmont;Alcock;Geological Society of America Bulletin,1994

2. SHRIMP and conventional U-Pb ages of Ordovician granites and tonalites in the central Appalachian Piedmont: Implications for Paleozoic tectonic events;Aleinikoff;American Journal of Science,2002

3. Deciphering multiple Mesoproterozoic and Paleozoic events recorded in zircon and titanite from the Baltimore Gneiss, Maryland: SEM imaging, SHRIMP U-Pb geochronology, and EMP analysis;Aleinikoff,2004

4. The problem of the anorthosites;Bowen;The Journal of Geology,1917

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