File:Diabase dike (ophitic olivine tholeiite) (right) intruding gabbroic anorthosite to anorthositic gabbro (left) (anorthosite series, Duluth Complex, Mesoproterozoic, 1099 Ma; Merritt Creek West Skyline Parkway roadcut, Duluth, Minnesota,.jpg

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English: Diabase dike intruding gabbroic anorthosite to anorthositic gabbro in the Precambrian of Minnesota, USA. (geology hammer for scale)

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 on the left are gabbroic anorthosite to anorthositic gabbro, which are mafic, phaneritic (coarsely-crystalline), intrusive igneous rocks dominated calcium-rich plagioclase feldspar - CaAl2Si2O8 - calcium aluminosilicate.

The rocks on the right are part of a large, mafic igneous dike that intruded the anorthosites. The dike-anorthosite intrusive contact is subvertical below the handle of the geology hammer. Dikes are planar igneous intrusions that cut across country rocks. As such, they postdate the host rocks. This igneous dike is composed of diabase (microgabbro) - a more thorough lithologic designation is ophitic olivine tholeiite.

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@N05/22075326529/
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@N05/22075326529. It was reviewed on 19 June 2022 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

19 June 2022

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