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American Mineralogist; February 2008; v. 93; no. 2-3; p. 270-282; DOI: 10.2138/am.2008.2592
© 2008 Mineralogical Society of America
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Metamorphosed Ordovician Fe- and Mn-rich rocks in south-central Maine: From peri-Gondwanan deposition through Acadian metamorphism

David P. West, Jr.1,*, Martin G. Yates2, Christopher Gerbi2 and Nellie Q. Barnard1

1 Department of Geology, Middlebury College, Middlebury, Vermont 05753, U.S.A.
2 Department of Earth Sciences, University of Maine, Orono, Maine 04469, U.S.A.

Correspondence: * E-mail: dwest{at}middlebury.edu

The Wilson Cove Member of the Cushing Formation is a thin (up to 120 m thick) metamorphosed Fe- and Mn-rich unit exposed discontinuously over a distance of >75 km in southern Maine. Cathodoluminescence imaging of zircon grains from the unit reveal texturally isolated detrital cores surrounded by distinct metamorphic overgrowths. U-Pb SHRIMP core ages range from 463 to 2058 Ma with a strong peak in the Neoproterozoic-Early Cambrian. This distribution of ages is consistent with a peri-Gondwanan source region and a Middle to Late Ordovician depositional age. Zircon rims have an age of 373 ± 4 Ma, consistent with growth during late Acadian metamorphism. Whole-rock geochemistry reveals considerable major- and trace-element variability with generally elevated abundances of Fe2O3(t) (15–43 wt%), MnO (0.1–12.1 wt%), Ba (4–2503 ppm), and As (7–1161 ppm). Geochemical discrimination diagrams suggest the protoliths were mixtures of hydrothermal exhalatives and terrigenous clastic sediment, with these materials most likely having been deposited in a marine back-arc basin proximal to a peri-Gondwanan continental source region. Late Devonian low-pressure, amphibolite-facies metamorphism of these bulk compositions produced assemblages dominated by grunerite + garnet + biotite + quartz. These and other mineral assemblages found in the Wilson Cove unit in south-central Maine are consistent with peak metamorphic conditions of 550 to 600 °C and 3–4 kbar previously determined from nearby metapelites. Mineral assemblages, mineral modes, and mineral compositions in these Fe- and Mn-rich rocks are strongly influenced by whole-rock bulk compositional variability. In particular, the compositions of co-existing garnet and grunerite vary systematically as a function of whole-rock MnO concentration.

Key Words: Metamorphic petrology • analysis • chemical (rock) • analysis • chemical (mineral) • geochronology • ironstone • Maine






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