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- W2033401966 abstract "Abstract Phosphate Hill is a small inlier of Ordovician rocks enclosed in an envelope of ?Lower Devonian quartzose sandstones and shales. Lithological layering (S 0) within the Ordovician inlier shows tight B 1 folds with a second group of folds (B 2) superimposed. The orientation and shape of these B 2 folds are highly variable. The overall structure of the area falls naturally into two subareas: Subarea 1 comprises sub‐horizontal east‐west B 1 folds which are overturned to the north and show slides on their lower limbs; B 2 folds in this subarea are small‐scale features. Subarea 2 is dominated by B 2 folds and contains a large S‐shaped B 2 fold in its eastern part. The variability of axial orientation characteristic of B 2 folds is believed to be caused by the combined effects of two factors: The variation of the imposed strain field (relative to S 0 ), owing to the inherent characteristics of an incipient shear‐zone style of strain. 2. The internal rotation of S 0 relatively to externally imposed axes ..." @default.
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- W2033401966 date "1977-06-01" @default.
- W2033401966 modified "2023-09-26" @default.
- W2033401966 title "The structure of a small complexly‐deformed area within Ordovician rocks near Mansfield, Victoria" @default.
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- W2033401966 doi "https://doi.org/10.1080/00167617708728983" @default.
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