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- W1966795767 abstract "Many large outcrops of deformed Archean metavolcanics display a plethora of small-scale structures. Detailed study shows that much of the structural complexity is caused by heterogeneous deformation and associated shear-sense reversals on individual material surfaces. This situation contrasts with ideal band models in which such shear-sense reversals simplify rather than complicate the final structural pattern. Two generations of E-W band structures occur in schistose metavolcanics at the Aubelle Mine. The first structures are short limbs of Z-shaped buckle folds and akin to dextral kink bands, the second structures resemble sinistral shear bands but contain relics of Z-shaped folds. The emplacement and deformation of three sets of subvertical veins (V1, V2, V3) is compatible with the band-structure development and associated local reversal of shear sense in the horizontal plane. V1 and V3 are oblique to all other structures, but V2 is parallel to the band boundaries and is boudinaged in many places. The dilatant V2 was emplaced while the axis of instantaneous bulk shortening was within 45° of the dextral bands. Oblique deformation of the dextral bands led to boudinage of V2 and ultimately to extension fracturing of metavolcanics and emplacement of V3." @default.
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- W1966795767 date "1991-01-01" @default.
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- W1966795767 title "Metre-scale band structures and associated veins in Archean metavolcanics: Aubelle gold mine, central Canada" @default.
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- W1966795767 doi "https://doi.org/10.1016/0191-8141(91)90086-x" @default.
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