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- W2041651623 abstract "Abstract A relation between low‐angle shear zones and folds is established in the dynamically deformed Otago Schist. These events occurred during the Cretaceous towards the close of the Rangitata Orogeny (D3–4). Prominent low‐angle north‐dipping shears are often subparallel to F3 axial planes. South‐dipping mesoshears are present as an antithetic set. Thrusting was initiated on the shear zones after F3 folding, accompanying continued regional compression. In western sections, two sequential F3 fold subphases are distinguished, but to the east the earlier phase is weakly preserved. The existence of two post‐S2 folding events, and dominance of north‐dipping shears, is important in relation to potential sites of gold mineralisation. Structural factors influencing the development of dilation sites associated with gently dipping macroshears include the F3 axial plane geometry, variations in fold intensity, and lithology‐shear strength control. The lack of widespread low‐angle macro‐shears is believed to be due..." @default.
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- W2041651623 date "1991-12-01" @default.
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- W2041651623 title "Low‐angle shear zones in Central Otago, New Zealand—their regional extent and economic significance" @default.
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- W2041651623 doi "https://doi.org/10.1080/00288306.1991.9514486" @default.
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