Constrains on vorticity and non-coaxial shear direction in Neoarchean L-S tectonites, an example from northern Minnesota, USA (vol 256, pg 189, 2015)
Precambrian Research(2015)
Abstract
•We examine microstructural fabrics in seven Neoarchean LS-tectonite samples.•We compare LS-tectonite microstructural fabrics to three monoclinic shear models.•We determine that non-coaxial shear direction is parallel to elongation lineation.•Non-coaxial shear direction is parallel to elongation despite varying lineation geographic orientation.
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Key words
Neoarchean,L-S tectonite,Vorticity analysis,Shear,Superior Craton,Vermilion District
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