Synchronous development of type 2 and Type 3 fold interference patterns: evidence for recumbent sheath folds in the Allendale Area, Broken Hill, NSW, Australia

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Forbes, C J
Betts, P
Lister, Gordon

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Pergamon-Elsevier Ltd

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Synchronous development of Type 2 and Type 3 fold interference patterns occur in the poly-deformed Broken Hill Inlier. The interference patterns have resulted from the superposition of recumbent F2 folds and ∼N-S-oriented upright F3 folds. The synchrono

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Journal of Structural Geology

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