Research paperStrain in an Archean greenstone belt of Minnesota
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Cited by (12)
Strain variations across the Proterozoic Penokean Orogen, USA and Canada
2018, Precambrian ResearchCitation Excerpt :Pillows in the Ely Greenstone are vertical and north-facing and contain calcite between pillows and in pillow-margin calcite veins. Twinning strains in both types of calcite preserve a layer-parallel shortening strain: ε1 is vertical and so is bedding (Fig. 7a; Table 1) and there is no twinning strain overprint (see also Bauer, 1985; Schultz-Ela and Hudleston, 1991). North-striking lamprophyre dikes that crosscut the Archean Saganaga tonalite (Goldich and Hedge, 1962) in the Wawa terrane in northern Minnesota (Fig. 1).
Constrains on vorticity and non-coaxial shear direction in Neoarchean L-S tectonites, an example from northern Minnesota, USA
2015, Precambrian ResearchCitation Excerpt :The Neoarchean (2.7–2.5 Ga) Wawa Subprovince forms a NE-trending belt of sub-greenschist- to greenschist-facies supracrustal rocks cut by multiple L-S tectonite packages marked by a well-developed metamorphic foliation (Fm) and elongation lineation (Le) (Fig. 1). The Wawa Subprovince has been further interpreted as a transpressional plate-margin recording dextral strike-slip shear (Hudleston et al., 1988; Schultz-Ela and Hudleston, 1991; Jirsa et al., 1992). This interpretation is highlighted as evidence for Archean plate-tectonic processes based on plate-tectonic models that require extensive strike-slip shear zones, with length ≥1200 km (Sleep, 1992).
Kinematics and timing of shear zone deformation in the western Coast Belt: Evidence for mid-Cretaceous orogen-parallel extension
2014, Journal of Structural GeologyCitation Excerpt :This can result in vertical lineations associated with horizontal shear sense indicators (Fossen and Tikoff, 1993). Such models cannot explain field observations of stretching lineations oriented between vertical, or down dip, and the shear direction (Schultz-Ela and Hudleston, 1991; Robin and Cruden, 1994; Goodwin and Williams, 1996; Dutton, 1997; Jones et al., 1997; Lin et al., 1998). Several updated models were developed to accommodate these observations (Robin and Cruden, 1994; Merle and Gapais, 1997; Jones et al., 1997; Jiang and Williams, 1998; Lin et al., 1998; Czeck and Hudleston, 2003).
Physical experiments of vertical transpression with localized nonvertical extrusion
2004, Journal of Structural GeologyTesting models for obliquely plunging lineations in transpression: A natural example and theoretical discussion
2003, Journal of Structural GeologyThree-dimensional reference deformations and strain facies
1999, Journal of Structural Geology