File:Gabbroic anorthosite to anorthositic gabbro (anorthosite series, Duluth Complex, Mesoproterozoic, 1099 Ma; Merritt Creek West Skyline Parkway roadcut, Duluth, Minnesota, USA) 1.jpg

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English: Gabbroic anorthosite to anorthositic gabbro in the Precambrian of Minnesota, USA.

This is part of the widespread Duluth Complex, a ~1.1 billion year old suite of igneous rocks in northeastern Minnesota that is associated with volcanism in the Lake Superior segment of the ancient Mid-Continent Rift System.

These grayish-colored rocks are gabbroic anorthosite to anorthositic gabbro, which are mafic, phaneritic (coarsely-crystalline), intrusive igneous rocks dominated calcium-rich plagioclase feldspar - CaAl2Si2O8 - calcium aluminosilicate. The light gray-colored crystals are the plagioclase - their composition (An70) is on the border between labradorite plagioclase and bytownite plagioclase. The dark-colored material between the plagioclase crystals is principally a mix of olivine and augite pyroxene.

Gabbroic anorthosite is slightly more plagioclase rich than anorthositic gabbro.

Geologic unit & age: anorthosite series, Duluth Complex, late Mesoproterozoic, 1099 Ma

Locality: Merritt Creek West outcrop - roadcut along the northern & northwestern side of Skyline Parkway, Duluth, northeastern Minnesota, USA (46° 45’ 41.23” North, 92° 09’ 38.58” West)
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Source https://www.flickr.com/photos/47445767@N05/22262061155/
Author James St. John

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This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/22262061155. It was reviewed on 9 October 2020 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

9 October 2020

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current05:57, 9 October 2020Thumbnail for version as of 05:57, 9 October 20203,357 × 2,658 (3.33 MB)Ser Amantio di Nicolao (talk | contribs)Uploaded a work by James St. John from https://www.flickr.com/photos/47445767@N05/22262061155/ with UploadWizard

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