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- W2166173669 abstract "Abstract Sandstone, mudstone, and minor chert and volcanogenic rocks east of the bends in the Alpine Fault between the Maruia River and Nelson Lakes have been progressively metamorphosed to greenschist facies schists and penetratively deformed during two distinct periods. Mesoscopic and probably macroscopic folding accompanied phase 1 regional metamorphism; phase 2 mesoscopic folding and minor recrystallisation is restricted to a 1–4 km wide zone adjacent to the Alpine Fault, where it obliterates phase 1 features and disturbs isotextural zones; it is related to fault movement. Phase 3 deformation is limited to kink folding and close-spaced shearing between the bends. At least two periods of movement are inferred on the fault. Up to 5 km of dextral movement are recorded on the Awatere Fault." @default.
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- W2166173669 date "1986-04-01" @default.
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- W2166173669 title "Schist structure east of the Alpine Fault bends, southeast Nelson, New Zealand" @default.
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- W2166173669 doi "https://doi.org/10.1080/00288306.1986.10427533" @default.
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