Mid to late Paleozoic shortening pulses in the Lachlan Orogen, southeastern Australia: a review

References

• Alder, J. D., Bembrick, C., Hartung-Kagi, B., Mullard, B., Pratt, D. A., Scott, J., & Shaw, R. D. (1998). A re-assessment of the petroleum potential of the Darling Basin: A discovery 2000 initiative. Australian Petroleum Production & Exploration Association Journal, 38, 278–310.
   Google Scholar
• Allen, R. L. (1992). Reconstruction of the tectonic, volcanic, and sedimentary setting of strongly deformed Zn–Cu massive sulphide deposits at Benambra, Victoria. Economic Geology, 87, 825–854.
   Web of Science ®Google Scholar
• Alonso, J. L. (1989). Fold reactivation involving angular unconformable sequences: Theoretical analysis and natural examples from the Cantabrian Zone (Northwest Spain). Tectonophysics, 170, 57–77.
   Web of Science ®Google Scholar
• Ashley, P. M., Brown, P. F., Franklin, B. J., Ray, A. S., & Scheibner, E. (1979). Field and geochemical characteristics of the Coolac Ophiolite suite and its possible origin in a marginal sea. Journal of the Geological Society of Australia, 26, 45–60.
   Google Scholar
• Beauchamp, W. (2004). Superposed folding resulting from inversion of a synrift accommodation zone, Atlas Mountains, Morocco. In K. R. McClay (Ed.). Thrust tectonics and hydrocarbon systems (pp. 635–646). Tulsa, USA: American Association of Petroleum Geologists, Memoir, 82.
   Google Scholar
• Belousova, E. A., Jiménez, J. M. G., Graham, I., Griffin, W. L., O'Reilly, S. Y., Pearson, N., … Talavera, C. (2015). The enigma of crustal zircons in upper-mantle rocks: Clues from the Tumut ophiolite, southeast Australia. Geology, 43, 119–122.
   Web of Science ®Google Scholar
• Bembrick, C. (1997). A re-appraisal of the Darling Basin Devonian sequence. Quarterly Notes Geological Survey of New South Wales, 105, 16.
   Google Scholar
• Bierlein, F. P., Arne, D. C., Keay, S. M., & McNaughton, N. J. (2001). Timing relationships between felsic magmatism and mineralisation in the central Victorian gold province, Southeast Australia. Australian Journal of Earth Sciences, 48, 883–899.
   Web of Science ®Google Scholar
• Bierlein, F. P., Foster, D. A., Gray, D. R., & Davidson, G. J. (2005). Timing of orogenic gold mineralisation in northeastern Tasmania: Implications for the tectonic and metallogenetic evolution of Palaeozoic SE Australia. Mineralium Deposita, 39, 890–903.
   Web of Science ®Google Scholar
• Black, L. P. (2005). SHRIMP U–Pb zircon ages obtained during 2004/05 for the NSW Geological Survey. Sydney, NSW: Geological Survey of New South Wales, Geological Survey File, GS2005/745.
   Google Scholar
• Black, L.P. (2006). SHRIMP U-Pb zircon ages obtained during 2005/06 for NSW Geological Survey projects. Sydney, NSW: Geological Survey of New South Wales, Geological Survey File, GS2006/821.
   Google Scholar
• Black, L. P., McClenaghan, M. P., Korsch, R. J., Everard, J. L., & Foudoulis, C. (2005). Significance of Devonian–Carboniferous igneous activity in Tasmania as derived from U–Pb SHRIMP dating of zircon. Australian Journal of Earth Sciences, 52, 807–829.
   Web of Science ®Google Scholar
• Bodorkos, S., Blevin, P. L., Eastlake, M. A., Downes, P. M., Campbell, L. M., Gilmore, P. J., … Trigg, S. J. (2015). New SHRIMP U–Pb zircon ages from the central and eastern Lachlan Orogen, New South Wales: July 2013–June 2014 (pp. 158). Canberra, ACT: Geoscience Australia, Record GS2015/0002. Maitland, NSW: Geological Survey of New South Wales, Record 2015/02. Retrieved from http://dx.doi.org/10.11636/Record.2015.002
   Google Scholar
• Bodorkos, S., Blevin, P.L., Simpson, C. J., Gilmore, P. J., Glen, R. A., Greenfield, J. E., … Quinn, C. D. (2013). New SHRIMP U–Pb zircon ages from the Lachlan, Thomson and Delamerian orogens, New South Wales: July 2009–June 2010 (pp. 124). Canberra, ACT: Geoscience Australia Record, 2013/29. Maitland, NSW: Geological Survey of New South Wales Report, GS2013/0427.
   Google Scholar
• Bodorkos, S., Simpson, C. J., Thomas, O. D., Trigg, S. J., Blevin, P. L., Campbell, L. M., … Fitzherbert, J. A. (2010). New SHRIMP U-Pb zircon ages from the eastern Lachlan Orogen, New South Wales, July 2008–June 2009 (pp. 100). Canberra, ACT: Geoscience Australia Record, 2010/31.
   Google Scholar
• Burton, G. R. (2010). New structural model to explain geophysical features in northwestern New South Wales: Implications for the tectonic framework of the Tasmanides. Australian Journal of Earth Sciences, 57, 23–49.
   Web of Science ®Google Scholar
• Calver, C. R., Baillie, P. W., Banks, M. R. & Seymour, D. B. (2014). Ordovician-Lower Devonian successions. In K. D. Corbett, P. G. Quilty, & C. R. Calver (Eds.). Geological evolution of Tasmania (pp. 241–271). Hobart, Tas: Geological Society of Australia Special Publication, 24. Geological Society of Australia ( Tasmania Division).
   Google Scholar
• Cameron, R. G., Meakin, N. S., Vassallo, J. J., & Hendrickx, M. A. (2008). Rankin springs 1:100 000 geological map 8130. Maitland, NSW: Geological Survey of New South Wales.
   Google Scholar
• Cas, R. A. F. (1983). A review of the palaeogeography of the Lachlan Fold Belt, southeastern Australia. Geological Society of Australia Special Publication, 10, 103.
   Google Scholar
• Cas, R. A. F., & Jones, J. G. (1979). Palaeozoic interarc basin in eastern Australia and a modern New Zealand analogue. New Zealand Journal of Geology and Geophysics, 22, 71–81.
   Web of Science ®Google Scholar
• Cas, R. A. F., O'Halloran, G. J., Long, J. A., & VandenBerg, A. H. M. (2003). Middle Devonian to Carboniferous late to post-tectonic sedimentation and magmatism in an arid continental setting. In W. D. Birch (Ed.). Geology of Victoria (pp. 157–193). Melbourne, Vic: Geological Society of Australia Special Publication, 23.
   Google Scholar
• Cayley, R. A. (2011). Exotic crustal block accretion to the eastern Gondwanaland margin in the Late Cambrian — Tasmania, the Selwyn Block, and implications for the Cambrian–Silurian evolution of the Ross, Delamerian, and Lachlan orogens. Gondwana Research, 19, 628–649.
   Web of Science ®Google Scholar
• Cayley, R. A. (2012). Oroclinal folding in the Lachlan Fold Belt: Consequence of southeast-directed Siluro-Devonian subduction rollback superimposed on an accreted Ordovician arc assemblage in eastern Australia. Selwyn Symposium 2012 (pp. 34–43). Sydney NSW: Geological Society of Australia Abstracts, 103.
   Google Scholar
• Cayley, R. A., & Taylor, D. H. (1997). Grampians special area geological report (pp. 150). Melbourne Vic: Geological Survey of Victoria Report, 107.
   Google Scholar
• Cayley, R. A., Korsch, R. J., Moore, D. H., Costelloe, R. D., Nakamura, A., Willman, C. E., … O'Shea P. J. (2011). Crustal architecture of central Victoria: Results from the 2006 deep crustal reflection seismic survey. Australian Journal of Earth Sciences, 58, 113–156.
   Web of Science ®Google Scholar
• Cayley, R. A., Taylor, D. H., VandenBerg, A. H. M., & Moore, D. H. (2002). Proterozoic–Early Palaeozoic rocks and the Tyennan Orogeny in central Victoria: The Selwyn Block and its tectonic implications. Australian Journal of Earth Sciences, 49, 225–254.
   Web of Science ®Google Scholar
• Chappell, B. W., White, A. J. R., Williams, I. S., Wyborn, D., & Wyborn, L. A. I. (2000). Lachlan Fold Belt granites revisited: High‐ and low‐temperature granites and their implications. Australian Journal of Earth Sciences, 47, 123–138.
   Web of Science ®Google Scholar
• Clarke, I., & Sherwin, L. (1990). Geological setting of gold and copper deposits in the Parkes area, New South Wales. Records of the Geological Survey of New South Wales, 23, 196.
   Google Scholar
• Collins, W. J. (2002a). Hot orogens, tectonic switching, and creation of continental crust. Geology, 30, 535–538.
   Web of Science ®Google Scholar
• Collins, W. J. (2002b). Nature of extensional orogens. Tectonics, 21, 6–1 to 6–12. doi:10.1029/2000TC001272.
   Google Scholar
• Collins, W. J., & Vernon, R. H. (1992). Palaeozoic arc growth, deformation and migration across the Lachlan Fold Belt, southeastern Australia. Tectonophysics, 214, 381–400.
   Web of Science ®Google Scholar
• Colquhoun, G. P., Meakin, N. S., & Cameron, R. G. (2005). Cargelligo 1:250 000 Geological Sheet 3rd edition SI/55-6: Explanatory notes (pp. 291). Sydney, NSW: Geological Survey of New South Wales, Sydney.
   Google Scholar
• Colquhoun, G. C., Meakin, N. S., & Cameron, R. G. (2008). Merriwagga 1:100 000 geological map 8030. Maitland, NSW: Geological Survey of New South Wales.
   Google Scholar
• Colquhoun, G. C., Meakin, N. S., Henderson, G. A. M., Krynen, J. P., Jagodzinski, E. A., Watkins, J. J., & Yoo, E. K. (1999). Mudgee 1:100 000 geological map. Canberra, ACT: Australian Geological Survey Organisation. Sydney, NSW: Geological Survey of New South Wales.
   Google Scholar
• Cooney, P. M., & Mantaring, A. M. (2007). The petroleum potential of the Darling Basin. In T. J. Munson & G. J. Ambrose (Eds.). Proceedings of the Central Australian Basins Symposium (CABS) (pp. 216–235). Alice Springs, NT: Northern Territory Geological Survey Special Publication 2. Retrieved from http://conferences.minerals.nt.gov.au/cabsproceedings/4
   Google Scholar
• Cooper, G. T. (1992). Early Carboniferous back‐arc deformation in the Lachlan Fold Belt, Shoalhaven River–Ettrema Creek area, NSW. Australian Journal of Earth Sciences, 39, 529–537.
   Web of Science ®Google Scholar
• Crawford, A. J. (1988). Cambrian. In J. G. Douglas & J. A. Ferguson (Eds.). Geology of Victoria (2nd ed. pp. 37–62). Melbourne, Vic: Victorian Division of the Geological Society of Australia.
   Google Scholar
• Crawford, A. J., Cayley, R. A., Taylor, D. H., Morand, V. J., Gray, C. M., Kemp, A. I. S., … Black, L. P. (2003). Neoproterozoic and Cambrian continental rifting, continent–arc collision and post-collisional magmatism. In W. D. Birch (Ed.). Geology of Victoria (pp. 73–93). Melbourne, Vic: Geological Society of Australia Special Publication, 23.
   Google Scholar
• Dadd, K. A. (1998). Incipient backarc magmatism in the Silurian Tumut Trough, New South Wales: An ancient analogue of the early Lau Basin. Australian Journal of Earth Sciences, 45, 109–121.
   Web of Science ®Google Scholar
• Davis, D. Suppe, J., & Dahlen, F. A. (1983). Mechanics of fold-and-thrust belts and accretionary wedges. Journal of Geophysical Research, 88, B2, 1153–1172.
   Web of Science ®Google Scholar
• Domeier, M., & Torsvik, T. H. (2014). Plate tectonics in the late Paleozoic. Geoscience Frontiers, 5, 303–350.
   Web of Science ®Google Scholar
• Donchak, P., Purdy, D. J., Withnall, I. W., Blake, P. R., & Jell, P. A. (2013). New England Orogen. In P. Jell (Ed.). Geology of Queensland (pp. 305–472). Brisbane, Qld: Geological Survey of Queensland.
   Google Scholar
• Downes, P. M., Blevin, P. L., Armstrong, R., Simpson, C. J., Sherwin, L., Tilley, D. B., & Burton, G. R. (2016). Outcomes of the Nymagee mineral system study — an improved understanding of the timing of events and prospectivity of the central Lachlan Orogen. Quarterly Notes Geological Survey of New South Wales, 147, 38.
   Google Scholar
• Drummond, B., Goleby, B., Wake-Dyster, K., Glen, R. A., & Palmer, D. (1992). New tectonic model for the Cobar Basin, NSW, points to new exploration targets in Lachlan Fold Belt. BMR Research Newsletter, 16, 16–17.
   Google Scholar
• Durney, D. W., & Hood, D. I. A. (2003). Reply Sequence and kinematics of multiple deformation around Taemas Bridge, Eastern Lachlan Fold Belt, New South Wales, Australian Journal of Earth Sciences, 50, 829–833.
   Web of Science ®Google Scholar
• Elburg, M. A. (1996). U–Pb ages and morphologies of zircon in microgranitoid enclaves and peraluminous host granite: Evidence for magma mingling. Contributions to Mineralogy and Petrology, 123, 177–189.
   Web of Science ®Google Scholar
• Felton, E. A., & Huleatt, M. B. (1977). Geology of the Braidwood 1: 100 000 sheet (pp. 97). Sydney, NSW: Geological Survey of New South Wales.
   Google Scholar
• Fergusson, C.L. (1979). Pre-cleavage folds in the Mid-Palaeozoic sequence near Capertee, New South Wales. Journal and Proceedings of the Royal Society of New South Wales, 112, 125–132.
   Google Scholar
• Fergusson, C. L. (2003). Ordovician–Silurian accretion tectonics of the Lachlan Fold Belt, southeastern Australia. Australian Journal of Earth Sciences, 50, 475–490.
   Web of Science ®Google Scholar
• Fergusson, C. L. (2010). Plate-driven extension and convergence along the East Gondwana active margin: Late Silurian–Middle Devonian tectonics of the Lachlan Fold Belt, southeastern Australia. Australian Journal of Earth Sciences, 57, 627–649.
   Web of Science ®Google Scholar
• Fergusson, C. L. (2014). Late Ordovician to mid-Silurian Benambran subduction zones in the Lachlan Orogen, southeastern Australia. Australian Journal of Earth Sciences, 61, 587‒606.
   Google Scholar
• Fergusson, C. L., & Coney, P. J. (1992). Convergence and intraplate deformation in the Lachlan Fold Belt of southeastern Australia. Tectonophysics, 214, 417–439.
   Web of Science ®Google Scholar
• Fergusson, C. L., & Gray, D. R. (1989). Folding of angular unconformable sequences and effects on early folds, Tabberabbera district, eastern Victoria, Australia. Tectonophysics, 158, 93–111.
   Web of Science ®Google Scholar
• Fergusson, C. L., & VandenBerg, A. H. M. (1990). Middle Palaeozoic thrusting in the eastern Lachlan Fold Belt, southeastern Australia. Journal of Structural Geology, 12, 577–589.
   Web of Science ®Google Scholar
• Fitzherbert, J. F., Thomas, O. D., Deyssing, L., Bewert-Vassallo, K. E., Simpson, C. J., & Sherwin, L. (2011). Braidwood 1:100 000 geological sheet 8827, preliminary second edition. Orange, NSW: Geological Survey of New South Wales.
   Google Scholar
• Forster, M. A., Lister, G. S., & Lennox, P. G. (2014). Dating deformation using crushed alkali feldspar: 40Ar/39Ar geochronology of shear zones in the Wyangala Batholith, NSW, Australia. Australian Journal of Earth Sciences, 61, 619–629.
   Web of Science ®Google Scholar
• Foster, D. A., & Gray, D. R. (2000). Evolution and structure of the Lachlan Fold Belt (Orogen) of eastern Australia. Annual Review of Earth and Planetary Sciences, 28, 47–80.
   Web of Science ®Google Scholar
• Foster, D. A., & Gray, D. R. (2007). Strain rate in Paleozoic thrust sheets, the western Lachlan Orogen, Australia: Strain analysis and fabric geochronology. In J. W. Sears, T. A. Harms, & C. A. Evenchick (Eds.). Whence the mountains? Inquiries into the evolution of orogenic systems: A volume in honor of Raymond A. Price (pp. 349–368). Boulder, USA: Geological Society of America Special Paper, 433.
   Google Scholar
• Foster, D. A., Gray, D. R., & Bucher, M. (1999). Chronology of deformation within the turbidite-dominated Lachlan orogen: Implications for the tectonic evolution of eastern Australia and Gondwana. Tectonics, 18, 452–485.
   Web of Science ®Google Scholar
• Glen, R. A. (1982). Nature of late‐Early to Middle Devonian tectonism in the Buckambool area, Cobar, New South Wales. Journal of the Geological Society of Australia, 29, 127–138
   Web of Science ®Google Scholar
• Glen, R. A. (1985). Basement control on the deformation of cover basins: An example from the Cobar district in the Lachlan Fold Belt, Australia. Journal of Structural Geology, 7, 301–315.
   Web of Science ®Google Scholar
• Glen, R. A. (1990). Formation and inversion of transtensional basins in the western part of the Lachlan Fold Belt, Australia, with emphasis on the Cobar Basin. Journal of Structural Geology, 12, 601–620.
   Web of Science ®Google Scholar
• Glen, R. A. (1991). Inverted transtensional basin setting for gold and copper and base metal deposits at Cobar, New South Wales. Bureau of Mineral Resources Journal of Geology and Geophysics 12, 13–24.
   Google Scholar
• Glen, R. A. (1992). Thrust, extensional and strike-slip tectonics in an evolving Palaeozoic orogen—a structural synthesis of the Lachlan Orogen of southeastern Australia. Tectonophysics, 214, 341–380.
   Web of Science ®Google Scholar
• Glen, R. A. (1994). Geology of the Cobar 1:100 000 Sheet 8035 (pp. 132). Sydney, NSW: Geological Survey of New South Wales.
   Google Scholar
• Glen, R. A. (2005). The Tasmanides of eastern Australia. In A. P. M. Vaughan, P. T. Leat, & R. J. Pankhurst (Eds.). Terrane processes at the margins of Gondwana (pp. 23–96). London, UK: Geological Society of London Special Publication, 246.
   Google Scholar
• Glen, R. A. (2013). Refining accretionary orogen models for the Tasmanides of eastern Australia. Australian Journal of Earth Sciences, 60, 315–370.
   Web of Science ®Google Scholar
• Glen, R. A., & Lewis, P. C. (1990). The Budawang Synclinorium: A mineralised thrust system with implications for the Carboniferous and younger tectonics of New South Wales. Quarterly Notes Geological Survey of New South Wales, 81, 17.
   Google Scholar
• Glen, R. A., & VandenBerg, A. H. M. (1987). Thin-skinned tectonics in part of the Lachlan Fold Belt near Delegate, southeastern Australia. Geology, 15, 1070–1073.
   Web of Science ®Google Scholar
• Glen, R. A., & Watkins, J. J. (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, 35–52.
   Web of Science ®Google Scholar
• Glen, R. A., Clare, A., & Spencer, R. (1996). Extrapolating the Cobar Basin model to the regional scale: Devonian basin-formation and inversion in western New South Wales. In W. G. Cook, A. J. H. Ford, J. J. McDermott, P. N. Standish, C. L. Stegman, & T. M. Stegman (Eds.). The Cobar mineral field—a 1996 perspective (pp. 43–83). Melbourne, Vic: Australasian Institute of Mining and Metallurgy Spectrum Series, 3/96.
   Google Scholar
• Glen, R. A., Dallmeyer, R. D., & Black, L. P. (1992). Isotopic dating of basin inversion—the Palaeozoic Cobar Basin, Lachlan Orogen, Australia. Tectonophysics, 214, 249–268.
   Web of Science ®Google Scholar
• Glen, R. A., Drummond, B. J., Goleby, B. R., Palmer, D., & Wake-Dyster, K. D. (1994). Structure of the Cobar Basin, New South Wales, based on seismic reflection profiling. Australian Journal of Earth Sciences, 41, 341–352.
   Web of Science ®Google Scholar
• Glen, R. A., Felton, E. A., & Brown, R. E. (1985). Wrightville 1:100 000 geological map 8134. Sydney, NSW: Geological Survey of New South Wales.
   Google Scholar
• Glen, R. A., Korsch, R. J., Direen, N. G., Jones, L. E. A., Johnstone, D. W., Lawrie, K. C., … Shaw, R. D. (2002). Crustal structure of the Ordovician Macquarie Arc, eastern Lachlan Orogen, based on seismic reflection profiling. Australian Journal of Earth Sciences, 49, 323–348.
   Web of Science ®Google Scholar
• Glen, R. A., Korsch, R. J., Hegarty, R., Saeed, A., Poudjom Djomani, Y., Costello, R. D., & Griffin, W. L. (2013). Geodynamic significance of the boundary between the Thomson Orogen and the Lachlan Orogen, northwestern New South Wales and implications for Tasmanide tectonics. Australian Journal of Earth Sciences, 60, 371–412.
   Web of Science ®Google Scholar
• Glen, R. A., Meffre, S., & Scott, R. J. (2007). Benambran Orogeny in the Eastern Lachlan Orogen, Australia. Australian Journal of Earth Sciences, 54, 385–415.
   Web of Science ®Google Scholar
• Glen, R. A., Powell, C. McA., & Khaiami, R. (1987). Devonian to ?Carboniferous sedimentary rocks. In R. A. Glen. (ed.). Geology of the Wrightville 1:100,000 Sheet 8034 (pp. 149–203). Sydney, NSW: Geological Survey of New South Wales.
   Google Scholar
• Goscombe, B. D., Finlay, R. H., McClenaghan, M. P., & Everard, J. (1994). Multi-scale kinking in northeast Tasmania: Crustal shortening at shallow crustal levels. Journal of Structural Geology, 16, 1077–1092.
   Web of Science ®Google Scholar
• Graham, I. T., Franklin, B. J., Marshall, B., Leitch, E. C., & Fanning, C. M. (1996). Tectonic significance of 400 Ma zircon ages for ophiolitic rocks from the Lachlan Fold Belt, eastern Australia. Geology, 24, 1111–1114.
   Web of Science ®Google Scholar
• Gray, D. R. (1995). Thrust kinematics and transposition fabrics from a basal detachment zone, eastern Australia. Journal of Structural Geology, 17, 1637–1654.
   Web of Science ®Google Scholar
• Gray, D. R., & Foster, D. A. (1997). Orogenic concepts – application and definition: Lachlan fold belt, eastern Australia. American Journal of Science, 297, 859–891.
   Web of Science ®Google Scholar
• Gray, D. R., & Foster, D. A. (2004). Tectonic evolution of the Lachlan Orogen, southeast Australia: Historical review, data synthesis and modern perspectives. Australian Journal of Earth Sciences, 51, 773–817.
   Web of Science ®Google Scholar
• Gray, D. R., & Gregory, R. T. (2003). Fault geometry as evidence for inversion of a former rift basin in the Eastern Lachlan Orogen. Australian Journal of Earth Sciences, 50, 513–523.
   Web of Science ®Google Scholar
• Gray, D. R., & Mortimer, L. (1996). Implications of overprinting deformations and fold interference patterns in the Melbourne Zone, Lachlan Fold Belt. Australian Journal of Earth Sciences, 43, 103–114.
   Web of Science ®Google Scholar
• Gray, D. R., Foster, D. A., & Bucher, M. (1997). Recognition and definition of orogenic events in the Lachlan Fold Belt. Australian Journal of Earth Sciences, 44, 489–581.
   Web of Science ®Google Scholar
• Gray, D. R., Willman, C. E., & Foster, D. A. (2006). Crust restoration for the western Lachlan Orogen using the strain-reversal, area balancing technique: Implications for crustal components and original thicknesses. Australian Journal of Earth Sciences, 53, 329–341.
   Web of Science ®Google Scholar
• Greenfield, J. E., Gilmore, P. J., & Mills, K.J. (2010). Explanatory notes for the Koonenberry Belt geological maps. Geological Survey of New South Wales, Bulletin, 35, 528.
   Google Scholar
• Hallet, M., Vassallo, J., Glen, R., & Webster, S. (2005). Murray–Riverina region: An interpretation of bedrock Palaeozoic geology based on geophysical data. Quarterly Notes of the Geological Survey of New South Wales, 118, 1–16.
   Google Scholar
• Hand, M., & Sandiford, M. (1999). Intraplate deformation in central Australia, the link between subsidence and fault reactivation. Tectonophysics, 305, 121–140.
   Web of Science ®Google Scholar
• Hood, D. I. A., & Durney, D. W. (2002). Sequence and kinematics of multiple deformation around Taemas Bridge, eastern Lachlan Fold Belt, New South Wales. Australian Journal of Earth Sciences, 49, 291–309.
   Web of Science ®Google Scholar
• Kemežys, K. J. (1978). Ordovician and Silurian lithofacies and base metal deposits of the Lachlan Fold Belt. Journal of the Geological Society of Australia, 25, 97–107.
   Google Scholar
• Kemp, A. I. S., Hawkesworth, C. J., Collins, W. J., Gray, C. M., Blevin, P. L., & EIMF (2009). Isotopic evidence for rapid continental growth in an extensional accretionary orogen: The Tasmanides, eastern Australia. Earth and Planetary Science Letters, 284, 455–466.
   Web of Science ®Google Scholar
• Khalifa, M. Kh. (2009). Tectonostratigraphic evolution of the Blantyre Sub-basin and adjacent regions, New South Wales, based on integration of seismic, gravity and well data. Journal and Proceedings of the Royal Society of New South Wales, 142, 29–56.
   Google Scholar
• Khalifa, M. Kh., & Ward, C. R. (2009). Stratigraphic correlation of the Devonian sequence in the Blantyre Sub-basin, Darling Basin, western New South Wales. Australian Journal of Earth Sciences, 56, 111–133.
   Web of Science ®Google Scholar
• Konstantinovskaia, E., & Malavieille, J. (2005). Erosion and exhumation in accretionary orogens: Experimental and geological approaches. Geochemistry Geophysics Geosystems 6, Q02006, 25. doi:10.1029/2004GC000794. Retrieved from http://www.agu.org/pubs/crossref/2005/2004GC000794.shtml
   Web of Science ®Google Scholar
• Krynen, J. P., Morgan, E. J., Scott, M. M., Raymond, O. L., & Warren, A. Y. E. (1997). Molong 1:100 000 geological map. Canberra, ACT: Australian Geological Survey Organisation. Sydney, NSW: Geological Survey of New South Wales.
   Google Scholar
• Krynen, J. P., Sherwin, L., & Clarke, I. (1990). Parkes special 1:100 000 geological sheet. Sydney, NSW: Geological Survey of New South Wales.
   Google Scholar
• Lennox, P. G., Forster, M. A., & Williams, I. S. (2014). Emplacement and deformation ages of the Wyangala Granite, Cowra, NSW. Australian Journal of Earth Sciences, 61, 607–618.
   Web of Science ®Google Scholar
• Lewis, P. C., Glen, R. A., Pratt, G. W., & Clarke, I. (1994). Explanatory Notes: Bega – Mallacoota 1:250,000 Geological Sheet, SJ/55-4, SJ/55-8 (pp. 148). Sydney, NSW: Geological Survey of New South Wales.
   Google Scholar
• Li, C., Zhang, C., Cope, T. D., & Lin, Y. (2016). Out-of-sequence thrusting in polycyclic thrust belts: An example from the Mesozoic Yanshan belt, North China Craton: Out-of-sequence thrusting in the Yanshan. Tectonics, 35, 2082–2116.
   Web of Science ®Google Scholar
• Lu, J., Seccombe, P. K., Foster, D., & Andrew, A. S. (1996). Timing of mineralization and source fluids in a slate-belt auriferous vein system, Hill End goldfield, NSW, Australia: Evidence from 40Ar/39Ar dating and O- and H-isotopes. Lithos, 38, 147–165.
   Web of Science ®Google Scholar
• Lyons, P., Raymond, O. L., & Duggan, M. B. (2000). Forbes 1:250,000 geological sheet SI55-7, explanatory notes (2nd ed. pp. 230). Canberra, ACT: Australian Geological Survey Organisation Record, 2000/20.
   Google Scholar
• Mackay, R. M. (1961). The Lambie Group at Mount Lambie: Part 1, stratigraphy and structure. Journal and Proceedings of the Royal Society of New South Wales, 95, 17–21.
   Google Scholar
• MacRae, G. P. (1989). Lachlan Downs 1:100 000 geological map 8033. Sydney, NSW: Geological Survey of New South Wales.
   Google Scholar
• MacRae, G. P., & Pogson, D. J. (1985). Gindoono 1:100 000 Geological Sheet 8232, provisional edition 1985. Sydney, NSW: Geological Survey of New South Wales ( unpubl.).
   Google Scholar
• McClay, K. R. (1995). The geometries and kinematics of inverted fault systems: A review of analogue model studies. In J. G. Buchanan, & P. G. Buchanan (Eds.). Basin inversion (pp. 97–118). London, UK: Geological Society Special Publication, 88.
   Google Scholar
• McLean, M. A., Morand, V. J., & Cayley, R. A. (2010). Gravity and magnetic modelling of crustal structure in central Victoria: What lies under the Melbourne Zone? Australian Journal of Earth Sciences, 57, 153–173.
   Web of Science ®Google Scholar
• Meakin, N. S., & Morgan, E. J. (1999). Dubbo 1:250 000 Geological Sheet 2nd edition SI/55-4: Explanatory notes (pp. 504). Sydney, NSW: Geological Survey of New South Wales.
   Google Scholar
• Meffre, S., Scott, R. J., Glen, R., & Squire, R. (2007). Re-evaluation of contact relationships between Ordovician volcanic belts & the quartz-rich turbidites of the Lachlan Orogen. Australian Journal of Earth Sciences, 54, 363–383.
   Web of Science ®Google Scholar
• Meschede, M., Zweigel, P., & Keifer, E. (1999). Subsidence and extension at a convergent plate margin: Evidence for subduction erosion off Costa Rica. Terra Nova, 11, 112–117.
   Web of Science ®Google Scholar
• Miller, J. McL., Wilson, C. J. L., & Dugdale, L. J. (2006). Stawell gold deposit: A key to unravelling the Cambrian to Early Devonian structural evolution of the western Victorian goldfields. Australian Journal of Earth Sciences, 53, 677–695.
   Web of Science ®Google Scholar
• Mills, K. J. (2002). Explanatory notes to accompany Kayrunnera 1:100 000 Geological Sheet 7436, Koonenberry Region, far western New South Wales (pp. 145). Sydney, NSW: Geological Survey of New South Wales, Report GS2002/752.
   Google Scholar
• Monaldi, C. R., Salfity, J. A., & Kley, J. (2008). Preserved extensional structures in an inverted Cretaceous rift basin, northwestern Argentina: Outcrop examples and implications for fault reactivation. Tectonics, 27, TC1011, 21. doi: 10.1029/2006TC001993.
   Web of Science ®Google Scholar
• Moore, D. H., Betts, P. G., & Hall, M. (2013). Towards understanding the early Gondwanan margin in southeastern Australia. Gondwana Research, 23, 1581–1598.
   Web of Science ®Google Scholar
• Morand, V. J. (1990). Low-pressure regional metamorphism in the Omeo Metamorphic Complex, Victoria, Australia. Journal of Metamorphic Geology, 8, 1–12.
   Web of Science ®Google Scholar
• Morand, V. J., & Fanning, C. M. (2006). SHRIMP zircon dating results for various rocks from Victoria, 2006. Geological Survey of Victoria Technical Record, 2006/2, 70.
   Google Scholar
• Morand, V. J., & Fanning, C. M. (2009). SHRIMP zircon dating results for various rocks from Victoria, 2009. Geological Survey of Victoria Technical Record, 2009/2, 38.
   Google Scholar
• Morand, V. J., & Gray, D. R. (1991). Major fault zones related to the Omeo metamorphic complex, northeastern Victoria. Australian Journal of Earth Sciences, 38, 203–221.
   Web of Science ®Google Scholar
• Morand, V. J., Hughes, M. J., & Jones, G. N. (1997). Discussion Implications of overprinting deformations and fold interference patterns in the Melbourne Zone, Lachlan Fold Belt. Australian Journal of Earth Sciences, 44, 145–147.
   Web of Science ®Google Scholar
• Morand, V. J., Simons, B. A., Taylor, D. H., Cayley, R. A., Maher, S., Wohlt, K. E., & Radojkovic, A. M. (2005). Bogong 100 000 map area geological report (pp. 208). Melbourne Vic: Geological Survey of Victoria Report, 12.
   Google Scholar
• Moresi, L., Betts, P. G., Miller, M. S., & Cayley, R. A. (2014). Dynamics of continental accretion. Nature, 495, 245–248.
   Web of Science ®Google Scholar
• Murphy, N. C., & Gray, D. R. (1992). East–directed overthrusting in the Melbourne Zone, Lachlan Fold Belt. Australian Journal of Earth Sciences, 39, 37–53.
   Web of Science ®Google Scholar
• Murray, C. G., Fergusson, C. L., Flood, P. G., Whitaker, W. G., & Korsch, R. J. (1987). Plate tectonic model for the Carboniferous evolution of the New England Fold Belt. Australian Journal of Earth Sciences, 34, 213–236.
   Web of Science ®Google Scholar
• Musgrave, R. J. (2015). Oroclines in the Tasmanides. Journal of Structural Geology, 80, 72–98.
   Web of Science ®Google Scholar
• Neef, G. (2004). Stratigraphy, sedimentology, structure and tectonics of Lower Ordovician and Devonian strata of South Mootwingee, Darling Basin, western New South Wales. Australian Journal of Earth Sciences, 51, 15–29.
   Web of Science ®Google Scholar
• Neef, G. (2005). Devonian–Carboniferous structure and tectonics at Maccullochs Range and the recognition of the Darling Basin Conjugate Fault System showing switching of the directions of principal horizontal stress. Australian Journal of Earth Sciences, 52, 315–326.
   Web of Science ®Google Scholar
• Neef, G. (2012). Mid Silurian–Carboniferous tectonic and depositional history of the Darling Basin Conjugate Fault System, western New South Wales: Overview. Australian Journal of Earth Sciences, 59, 91–117.
   Web of Science ®Google Scholar
• Neef, G., & Bottrill, R. S. (1996). Devonian geology of Copper Mine Range, far west New South Wales. Journal and Proceedings of the Royal Society of New South Wales, 129, 105–122.
   Google Scholar
• Neef, G., & Larsen, D. F. (2003). Devonian fluvial strata in and adjacent to the Emsian–Eifelian Moona Vale Trough, western New South Wales. Australian Journal of Earth Sciences, 50, 81–96.
   Web of Science ®Google Scholar
• Neef, G., Bottrill, R. S., & Ritchie, A. (1995) Phanerozoic stratigraphy and structure of the northern Barrier Ranges, western New South Wales. Australian Journal of Earth Sciences, 42, 557–570.
   Web of Science ®Google Scholar
• Neef, G., Edwards, A. C., Bottrill, R. S., Hatty, J., Holzberger, I., Kelly, R., & Vaughan, J. (1989). The Mt Daubeny Formation: Arenite-rich ?Late Silurian–Early Devonian (Gedinnian) strata in far western New South Wales. Journal and Proceedings of the Royal Society of New South Wales, 122, 97–106.
   Google Scholar
• O'Halloran, G. J., & Cas, R. A. F. (1995). Evidence for syndepositional deformation from the Late Devonian of the Mansfield Basin, east‐central Victoria. Australian Journal of Earth Sciences, 42, 581–596.
   Web of Science ®Google Scholar
• Offler, R., & Murray, C. S. (2011). Devonian volcanics in the New England Orogen: Tectonic setting and polarity. Gondwana Research, 19, 706–715.
   Web of Science ®Google Scholar
• Offler, R., McKnight, S., & Morand, V. J. (1998b). Tectonothermal history of the western Lachlan Fold Belt: Insights from white mica studies. Journal of Metamorphic Geology 16, 531–540.
   Web of Science ®Google Scholar
• Offler, R., Miller, J. McL., Gray, D. R., Foster, D. A., & Bale, R. (1998a). Crystallinity and b0 spacing of K-white micas in a Paleozoic accretionary complex, eastern Australia: Metamorphism, paleogeotherms, and structural style of an underplated sequence. Journal of Geology, 106, 495–509.
   Web of Science ®Google Scholar
• Orth, K., VandenBerg, A. H. M., King, R. L., Nott, R. J., & Tickell, S. J. (1993). Murrindal 1: 100 000 Geological Map. Melbourne, Vic: Geological Survey of Victoria.
   Google Scholar
• Orth, K., VandenBerg, A. H. M., Nott, R. J., & Simons, B. A. (1995). Murrindal 1:100 000 map geological report (pp. 237). Melbourne, Vic: Geological Survey of Victoria Report, 100.
   Google Scholar
• Owen, M., & Wyborn, D. (1979). Geology and geochemistry of the Tantangara and Brindabella 1:100 000 Sheet areas, New South Wales and Australian Capital Territory. Canberra, ACT: Bureau of Mineral Resources Bulletin, 204.
   Google Scholar
• Packham, G. H. (1999). Radiometric evidence for Middle Devonian inversion of the Hill End Trough, northeast Lachlan Fold Belt. Australian Journal of Earth Sciences, 46, 23–33.
   Web of Science ®Google Scholar
• Packham, G. H. (2003). Discussion Sequence and kinematics of multiple deformation around Taemas Bridge, Eastern Lachlan Fold Belt, New South Wales. Australian Journal of Earth Sciences, 50, 827–829.
   Web of Science ®Google Scholar
• Packham, G. H. & Hubble, T. C. T. (2016). The Narooma Terrane offshore: A new model for the southeastern Lachlan Orogen using data from rocks dredged from the New South Wales continental slope. Australian Journal of Earth Sciences, 63, 23–61.
   Web of Science ®Google Scholar
• Percival, I. G., & Glen, R. A. (2007). Ordovician to earliest Silurian history of the Macquarie Arc Lachlan Orogen. Australian Journal of Earth Sciences, 54, 137–165.
   Web of Science ®Google Scholar
• Phillips, D., Fu, B., Wilson, C. J. L., Kendrick, M. A., Fairmaid, A. M. & Miller, J. MCL. 2012. Timing of gold mineralisation in the western Lachlan Orogen, SE Australia: A critical overview. Australian Journal of Earth Sciences, 59, 495–525.
   Web of Science ®Google Scholar
• Pogson, D. J. (1991a). Geology of the Bobadah 1:100 000 sheet 8233 (pp. 130). Sydney, NSW: Geological Survey of New South Wales.
   Google Scholar
• Pogson, D. J. (1991b). Bobadah 1:100 000 geological sheet 8233 (1st ed.). Sydney, NSW: Geological Survey of New South Wales.
   Google Scholar
• Pogson, D. J., & Watkins, J. J. (1998). Bathurst 1:250 000 Geological Sheet SI/55-8: Explanatory notes (pp. 430). Sydney, NSW: Geological Survey of New South Wales.
   Google Scholar
• Powell, C. McA. (1983). Geology of the New South Wales South Coast and adjacent Victoria with emphasis on the pre-Permian structural history. Specialist group in tectonics and structural geology field guide, 1 (pp. 118). Sydney, NSW: Geological Society of Australia.
   Google Scholar
• Powell, C. McA. (1984a). Ordovician to earliest Silurian: Marginal sea and island arc. Silurian to mid-Devonian—dextral transtensional margin. Late Devonian and Early Carboniferous: Continental magmatic arc along the eastern edge of the Lachlan Fold Belt. In J. J. Veevers (Ed.). Phanerozoic earth history of Australia (pp. 290–340). Clarendon Press, Oxford, UK: Geological Sciences Series, 2.
   Google Scholar
• Powell, C. McA. (1984b). Terminal fold-belt deformation: Relationship of mid-Carboniferous megakinks in the Tasman fold belt to coeval thrusts in cratonic Australia. Geology, 12, 546–549.
   Web of Science ®Google Scholar
• Powell, C. McA., & Baillie, P. W. (1992). Tectonic affinity of the Mathinna Group in the Lachlan Fold Belt. Tectonophysics, 214, 193–209.
   Web of Science ®Google Scholar
• Powell, C. McA., & Edgecombe, D. R. (1978). Mid-Devonian movements in the northeastern Lachlan Fold Belt. Journal of the Geological Society of Australia, 25, 165–184.
   Google Scholar
• Powell, C. McA., & Fergusson, C. L. (1979). The relationship of structures across the Lambian unconformity near Taralga, New South Wales. Journal of the Geological Society of Australia, 26, 209–219.
   Google Scholar
• Powell, C. McA., Baillie, P. W., Conaghan, P. J., & Turner, N. J. (1993). The mid-Palaeozoic turbiditic Mathinna Group, northeast Tasmania. Australian Journal of Earth Sciences, 40, 169–196.
   Web of Science ®Google Scholar
• Powell, C. McA., Baillie, P. W., & VandenBerg, A. H. M. (2003). Silurian to mid-Devonian basin development of the Melbourne Zone, Lachlan Fold Belt, southeastern Australia. Tectonophysics, 375, 9–36.
   Web of Science ®Google Scholar
• Powell, C. McA., Cole, J. P., & Cudahy, T. J. (1985). Megakinking in the Lachlan Fold Belt, Australia. Journal of Structural Geology, 7, 281–300.
   Web of Science ®Google Scholar
• Powell, C. McA., Edgecombe, D. R., Henry, N. M., & Jones, J. G. (1977). Timing of regional deformation in the Hill Trough: A reassessment. Journal of the Geological Society of Australia, 23, 407–422.
   Google Scholar
• Powell, C. McA., Fergusson, C. L., & Williams, A. J. (1980). Structural relationships across the Lambian Unconformity in the Hervey Ranges Parkes area, N.S.W. Proceedings of the Linnean Society of New South Wales, 104, 195–210.
   Google Scholar
• Powell, C. McA., Gilfillan, M. A., & Henry, N. M. (1978). Early east–southeast trending folds in the Sofala Volcanics, New South Wales. Journal and Proceedings of the Royal Society of New South Wales, 111, 121–128.
   Google Scholar
• Powell, C. McA., Khaiami, R., & Scheibner, E. (1987). Mulga Downs Group. In E. Scheibner (ed.). Geology of the Mount Allen 1:100,000 Sheet 8032 (pp. 107–140). Sydney, NSW: Geological Survey of New South Wales.
   Google Scholar
• Prendergast, E., Offler, R., & Zwingman, H. (2012). Adaminaby Group west of Batemans Bay: Deformation and metamorphism of the Narooma accretionary complex, NSW. Australian Journal of Earth Sciences, 59, 1049–1066.
   Web of Science ®Google Scholar
• Quinn, C. D., Percival, I. G., Glen, R. A., & Xiao, W.-J. (2014). Ordovician marginal basin evolution near the palaeo-Pacific east Gondwana margin, Australia. Journal of the Geological Society, London, 171, 723–736.
   Web of Science ®Google Scholar
• Raimando, T., Hand, M., & Collins, W. J. (2014). Compressional intracontinental orogens: Ancient and modern perspectives. Earth-Science Reviews, 130, 128–153.
   Web of Science ®Google Scholar
• Ramsay, J. G. (1967). Folding and fracturing of rocks (pp. 568). New York, USA: McGraw-Hill.
   Google Scholar
• Raymond, O. L., & Wallace, D. A. (2000). Marsden 1:100 000 geological map. Canberra, ACT: Australian Geological Survey Organisation. Sydney, NSW: Geological Survey of New South Wales.
   Google Scholar
• Raymond, O. L., Sherwin, L., Wallace, D. A., Wyborn, D., Young, G. C., Percival, I. G., & Glen, R. A. (2000a). Parkes 1:100 000 geological map. Canberra, ACT: Australian Geological Survey Organisation. Sydney, NSW: Geological Survey of New South Wales.
   Google Scholar
• Raymond, O. L., Wallace, D. A., Krynen, J. P., & Young, G. C. (2000b). Grenfell 1:100 000 geological map. Canberra, ACT: Australian Geological Survey Organisation. Sydney, NSW: Geological Survey of New South Wales.
   Google Scholar
• Reed, A. R. (2001). Pre-Tabberabberan deformation in eastern Tasmania: A southern extension of the Benambran Orogeny. Australian Journal of Earth Sciences, 48, 785–796.
   Web of Science ®Google Scholar
• Rixon, L. K., Bucknell, W. R., & Rickard, M. J. (1983). Mega kink folds and related structures in the Upper Devonian Merrimbula Group, south coast of New South Wales. Journal of the Geological Society of Australia, 30, 277–293.
   Web of Science ®Google Scholar
• Sandiford, M., Martin, S. F., & Lohe, E. M. (1988). Shear-zone deformation in the Yackandandah Granite, northeast Victoria. Australian Journal of Earth Sciences, 35, 223–230.
   Web of Science ®Google Scholar
• Scheibner, E. (1985). Mount Allen 1:100 000 geological map 8032. Sydney, NSW: Geological Survey of New South Wales.
   Google Scholar
• Scheibner, E., & Basden, H. (1998). Geology of New South Wales–Synthesis. Volume 2. Geological evolution. Geological Survey of New South Wales Memoir Geology, 13(2), 666.
   Google Scholar
• Scheibner, E., & Veevers, J. J. (2000). Tasman Fold Belt System. In J. J. Veevers (Ed.). Billion-year earth history of Australia and neighbours in Gondwanaland (pp. 154–234). Sydney, NSW: GEMOC Press.
   Google Scholar
• Schellart, W. P. (2008). Overriding plate shortening and extension above subduction zones: A parametric study to explain formation of the Andes Mountains. Geological Society of America Bulletin, 120, 1441–1454.
   Web of Science ®Google Scholar
• Schellart, W. P., Stegman, D. R., Farrington, R. J., Freeman, J., & Moresi, L. (2010). Cenozoic tectonics of Western North America controlled by evolving width of Farallon slab. Science, 329, 316–319.
   PubMed Web of Science ®Google Scholar
• Scott, M. M., Raymond, O., Henderson, G. A. M., Morgan, E., Warren, A. Y. E., & Wyborn, D. (1999). Wellington 1:100 000 geological map. Canberra, ACT: Australian Geological Survey Organisation. Sydney, NSW: Geological Survey of New South Wales.
   Google Scholar
• Seymour, D. B., McClenaghan, M. P., Green, G. R., Everard, J. L., Berry, R. F., Callaghan, T., … Hills, P. B. (2014). Mid-Palaeozoic orogenesis, magmatim and mineralisation. In K. D. Corbett, P. G. Quilty, & C. R. Calver (Eds.). Geological evolution of Tasmania (pp. 273–362). Hobart, Tas: Geological Society of Australia Special Publication, 24. Geological Society of Australia ( Tasmania Division).
   Google Scholar
• Shaw, S. E., & Flood, R. H. (1993). Carboniferous magmatic activity in the Lachlan and New England fold belts. In P. G. Flood & J. C. Aitchison (Eds.). New England Orogen, eastern Australia (pp. 113–121). Armidale, NSW: NEO ’93 Conference Proceedings, Department of Geology and Geophysics, University of New England Armidale.
   Google Scholar
• Sherwin, L. (1996). Narromine 1:250 000 Geological Sheet SI/55-3: Explanatory notes (pp. 104). Sydney, NSW: Geological Survey of New South Wales.
   Google Scholar
• Sherwin, L. (1997). Narromine 1:250 000 geological sheet, SI/55-3 (2nd ed.). Sydney, NSW: Geological Survey of New South Wales.
   Google Scholar
• Sherwin, L., Raymond, O. L., & Wallace, D. A. (2000). Bogan Gate 1:100 000 geological map. Canberra, ACT: Australian Geological Survey Organisation. Sydney, NSW: Geological Survey of New South Wales.
   Google Scholar
• Simpson, C. J., & Fergusson, C. L., (1997a). Combienbar and part Craigie 1:50 000 geological map. Melbourne, Vic: Geological Survey of Victoria.
   Google Scholar
• Simpson, C. J., & Fergusson, C. L., (1997b). Wangarabell and part Nungatta 1:50 000 geological map. Melbourne, Vic: Geological Survey of Victoria.
   Google Scholar
• Simpson, C. J., & Woodfull, C. J. (1994). Geological Note. New field evidence resolving the relationship between the Grampians Group and the Rocklands Rhyolite, western Victoria. Australian Journal of Earth Sciences, 41, 621–624.
   Web of Science ®Google Scholar
• Simpson, C. J., Cas, R. A. F., & Arundell, M. C. (2005). Volcanic evolution of a long-lived Ordovician island-arc province in the Parkes region of the Lachlan Fold Belt, southeastern Australia. Australian Journal of Earth Sciences, 52, 863–886.
   Web of Science ®Google Scholar
• Simpson, C. J., Fergusson, C. L., & Oranskaia, A. (1997). Craigie 1: 100 000 map area geological report (pp. 160). Melbourne, Vic: Geological Survey of Victoria Report, 111.
   Google Scholar
• Smith, J. V, & Marshall, B. (1992). Patterns of folding and fold interference in oblique contraction of layered rocks of the inverted Cobar Basin, Australia. Tectonophysics, 215, 319–334.
   Web of Science ®Google Scholar
• Spaggiari, C. V., Gray, D. R., & Foster, D. A. (2002a). Blueschist metamorphism during accretion in the Lachlan Orogen, south-eastern Australia. Journal of Metamorphic Geology, 20, 711–726.
   Web of Science ®Google Scholar
• Spaggiari, C. V., Gray, D. R., & Foster, D. A. (2004). Ophiolite accretion in the Lachlan Orogen, Southeastern Australia. Journal of Structural Geology, 26, 87–112.
   Web of Science ®Google Scholar
• Spaggiari, C. V., Gray, D. R., Foster, D. A., & Fanning, C. M. (2002b). Occurrence and significance of blueschist in the southern Lachlan Orogen. Australian Journal of Earth Sciences, 49, 255–269.
   Web of Science ®Google Scholar
• Stern, C. R. (2011). Subduction erosion: Rates, mechanisms, and its role in arc magmatism and the evolution of the continental crust and mantle. Gondwana Research, 20, 284–308.
   Web of Science ®Google Scholar
• Stokes, N., Fergusson, C. L., & Offler, R. (2015). Back-arc basin and ocean island basalts in the Narooma Accretionary Complex, Australia: Setting and tectonics. Australian Journal of Earth Sciences, 62, 37–53.
   Web of Science ®Google Scholar
• Stuart-Smith, P. G., Hill, R. I., Rickard, M. J., & Etheridge, M. A. (1992). The stratigraphy and deformation history of the Tumut region: Implications for the development of the Lachlan Fold Belt. Tectonophysics, 214, 211–237.
   Web of Science ®Google Scholar
• Suppe, J. (1985). Principles of structural geology (pp. 537). Englewood Cliffs, USA: Prentice-Hall.
   Google Scholar
• Taylor, D. H. (2006). Tabberabberan Orogeny occurs at 400 Ma, not 385 Ma: Evidence and implications in Victoria. In D. Denham (Ed.). Australian Earth Sciences Convention, Melbourne, Australia, extended abstracts (pp. 3). Sydney NSW: Geological Society of Australia.
   Google Scholar
• Teyssier, C., Tikoff, B., & Markley, M. (1995). Oblique plate motion and continental tectonics. Geology, 23, 447–450.
   Web of Science ®Google Scholar
• Thomas, O. D., & Pogson, D. J. (2012). Goulburn 1:250 000 geological sheet SI/55-12, 2^nd edition, explanatory notes (pp. 1931). Maitland, NSW: Geological Survey of New South Wales.
   Google Scholar
• Thomas, O. D., Johnston, A. J., Scott, M. M., Pogson, D. J., Sherwin, L., Simpson, C. J., … Vassallo, J. J. (2013a). Goulburn 1:250 000 geological sheet SI/55-12 (2nd ed.). ( 2 sheets). Maitland, NSW: Geological Survey of New South Wales.
   Google Scholar
• Thomas, O. D., Pogson, D. J., Johnston, A. J., Scott, M. M., Warren, A. Y. E., Sherwin, L., … Vassallo, J. J. (2013b). Goulburn 1:100 000 geological sheet. Maitland, NSW: Geological Survey of New South Wales.
   Google Scholar
• van der Pluijm, B. A., & Marshak, S. (1997). Earth structure an introduction to structural geology and tectonics (pp. 495). New York, USA: WCB/McGraw Hill.
   Google Scholar
• VandenBerg, A. H. M. (1977). Warburton 1:250 000 geological map. Melbourne, Vic: Geological Survey of Victoria.
   Google Scholar
• VandenBerg, A. H. M. (2003). Silurian to Early Devonian the Lachlan Fold Belt at its most diverse. In W. D. Birch (Ed.). Geology of Victoria (pp. 117–155). Melbourne, Vic: Geological Society of Australia Special Publication, 23.
   Google Scholar
• VandenBerg, A. H. M., Cayley, R. A., Willman, C. E., Morand, V. J., Seymon, A. R., Osborne, C. R., … Sandford, A. C. (2006). Walhalla–Woods Point–Tallangallook special map area geological report (pp. 448). Melbourne, Vic: Geological Survey of Victoria Report, 127.
   Google Scholar
• VandenBerg, A. H. M., Hendrickx, M. A., Willman, C. E., Magart, A. P. M., & Simons, B. A. (1998a). Dart 1:50 000 geological map. Melbourne, Vic: Geological Survey of Victoria.
   Google Scholar
• VandenBerg, A. H. M., Magart, A. P. M., Simons, B. A., Willman, C. E., & Hendrickx, M. A. (1998b). Benambra 1:50 000 geological map. Melbourne, Vic: Geological Survey of Victoria.
   Google Scholar
• VandenBerg, A. H. M., Nott, R. J., & Glen, R. A. (1992). Bendoc 1:100 000 geological map report. Melbourne, Vic: Geological Survey of Victoria Report, 90.
   Google Scholar
• VandenBerg, A. H. M., Nott, R. J., Roberts, P. S., King, R. L., & Orth, K. (1990). Bendoc 1:100 000 geological map. Melbourne, Vic: Geological Survey of Victoria.
   Google Scholar
• VandenBerg, A. H. M., Willman, C. E., Hendrickx, M. A., Bush, M. D., & Sands, B. (1995). The geology and prospectivity of the 1993 Mount Wellington Airborne Survey area (pp. 165). Melbourne, Vic: Victorian Initiative for Minerals & Petroleum Report, 2.
   Google Scholar
• VandenBerg, A. H. M., Willman, C. E., Maher, S., Simons, B. A., Cayley, R. A., Taylor, D. H., … Radojkovic, A. (2000). The Tasman Fold Belt System in Victoria (pp. 462). Melbourne, Vic: Special Publication, Geological Survey of Victoria.
   Google Scholar
• VandenBerg, A. H. M., Willman, C. E., Morand, V. J., McHaffie, I. W., Simons, B. A., Quinn, C., & Westcott, A. L. (2004). Buffalo 100 000 map area geological report (pp. 205). Melbourne Vic: Geological Survey of Victoria Report, 124.
   Google Scholar
• Watkins, J. J., Moffitt, R. S., Pogson, D. J., Hawley, D. J., & Henderson, G. A. M. (1997). Bathurst 1:100 000 geological map. Canberra, ACT: Australian Geological Survey Organisation. Sydney, NSW: Geological Survey of New South Wales.
   Google Scholar
• Wilde, S. A. (2002). SHRIMP U–Pb dating of four samples from the Goulburn 1:250 000 map sheet NSW. Sydney, NSW: Geological Survey of New South Wales Report, GS2009/0158.
   Google Scholar
• Willcox, J. B., Yeates, A. N., Meixner, A. J., & Shaw, R. D. (2003). Structural evolution and potential petroleum plays in the Darling Basin (Pondie Range–Mt Jack area). Geoscience Australia Record, 2003/5, 36.
   Google Scholar
• Willman, C. E., Cayley, R. A., Vandenberg, A. H. M., Haydon, S. J., Osborne, C. R., Seymon, A. R., & Thom, J. L. (2005). Dargo 100 000 map area geological report (pp. 189). Melbourne Vic: Geological Survey of Victoria Report, 126.
   Google Scholar
• Willman, C. E., Morand, V. J., Haydon, S. J., & Carney, C. (1999a). Brookville 1:50 000 geological map. Melbourne, Vic: Geological Survey of Victoria.
   Google Scholar
• Willman, C. E., Morand, V. J., Hendrickx, M. A., VandenBerg, A. H. M., Haydon, S. J., & Carney, C. (1999b). Omeo 1:100 000 map geological report (pp. 339). Melbourne, Vic: Geological Survey of Victoria Report, 118.
   Google Scholar
• Willman, C. E., VandenBerg, A. H. M., & Morand, V. J. (2002). Evolution of the southeastern Lachlan Fold Belt in Victoria. Australian Journal of Earth Sciences, 49, 271–289.
   Web of Science ®Google Scholar
• Wyborn, D., & Owen, M. (1983). Araluen 1:100 000 geological map. Canberra, ACT: Bureau of Mineral Resources, Geology & Geophysics.
   Google Scholar
• Wyborn, D., & Owen, M. (1986). 1:100 000 Geological Map Commentary: Araluen, New South Wales (pp. 44). Canberra, ACT: Bureau of Mineral Resources.
   Google Scholar
• Yin, A. (2010). Cenozoic tectonic evolution of Asia: A preliminary synthesis. Tectonophysics, 488, 293–325.
   Web of Science ®Google Scholar
• Young, G. C. (2006). Devonian fish remains, biostratigraphy and unconformities, Narromine 1:250 000 map sheet area, central New South Wales (Lachlan Fold Belt). Australian Journal of Earth Sciences, 53, 605–615.
   Web of Science ®Google Scholar
• Young, G. C. (2007). Devonian formations, vertebrate faunas and age control on the far south coast of New South Wales and adjacent Victoria. Australian Journal of Earth Sciences, 54, 991–1008.
   Web of Science ®Google Scholar