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Miscellany

Discussion—Timing of regional deformation of the hill end trough

Page 109 | Published online: 01 Aug 2007

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D. I. A. Hood & D. W. Durney. (2002) Sequence and kinematics of multiple deformation around Taemas Bridge, Eastern Lachlan Fold Belt, New South Wales. Australian Journal of Earth Sciences 49:2, pages 291-309.
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R. A. Glen & J. J. Watkins. (1999) Implications of Middle Devonian deformation of the eastern part of the Hill End Trough, Lachlan Orogen, New South Wales. Australian Journal of Earth Sciences 46:1, pages 35-52.
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D. R. Gray, D. A. Foster & M. Bucher. (1997) Recognition and definition of orogenic events in the Lachlan Fold Belt. Australian Journal of Earth Sciences 44:4, pages 489-501.
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H. J. Harrington & R. J. Korsch. (1985) Late Permian to Cainozoic tectonics of the New England Orogen. Australian Journal of Earth Sciences 32:2, pages 181-203.
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K. A. W. Crook. (1978) Implications of a downward‐facing fold in the Bathurst granite contact aureole, Hill End Synclinorial Zone, New South Wales. Journal of the Geological Society of Australia 25:7-8, pages 467-471.
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C. McA. Powell & J. G. Jones. (1978) Reply: Timing of regional deformation in the Hill End Trough. Journal of the Geological Society of Australia 25:5-6, pages 362-364.
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Articles from other publishers (1)

Scott R. Paterson, Othmar T. Tobisch & Vince J. Morand. (1990) The influence of large ductile shear zones on the emplacement and deformation of the Wyangala Batholith, SE Australia. Journal of Structural Geology 12:5-6, pages 639-650.
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