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Rossiter, A. G., Gray, C. M. (2011) 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, 58 (1) 109-110 doi:10.1080/08120099.2010.535851

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Reference TypeJournal (article/letter/editorial)
TitlePlate-driven extension and convergence along the East Gondwana active margin: Late Silurian–Middle Devonian tectonics of the Lachlan Fold Belt, southeastern Australia
JournalAustralian Journal of Earth Sciences
AuthorsRossiter, A. G.Author
Gray, C. M.Author
Year2011 (February)Volume58
Issue1
PublisherInforma UK Limited
DOIdoi:10.1080/08120099.2010.535851Search in ResearchGate
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Mindat Ref. ID500098Long-form Identifiermindat:1:5:500098:6
GUID0
Full ReferenceRossiter, A. G., Gray, C. M. (2011) 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, 58 (1) 109-110 doi:10.1080/08120099.2010.535851
Plain TextRossiter, A. G., Gray, C. M. (2011) 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, 58 (1) 109-110 doi:10.1080/08120099.2010.535851
In(2011, February) Australian Journal of Earth Sciences Vol. 58 (1) Informa UK Limited

See Also

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Fergusson, C. L. (2011) 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, 58 (1) 111-112 doi:10.1080/08120099.2010.535852
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 (5) 627-649 doi:10.1080/08120099.2010.494767
Fergusson, C. L. (2003) Ordovician‐Silurian accretion tectonics of the Lachlan Fold Belt, southeastern Australia. Australian Journal of Earth Sciences, 50 (4) 475-490 doi:10.1046/j.1440-0952.2003.01013.x
Fergusson, C. L., Fanning, C. M. (2002) Late Ordovician stratigraphy, zircon provenance and tectonics, Lachlan Fold Belt, southeastern Australia. Australian Journal of Earth Sciences, 49 (3) 423-436 doi:10.1046/j.1440-0952.2002.00929.x
Rossiter, A. G., Gray, C. M. (2008) Barium contents of granites: key to understanding crustal architecture in the southern Lachlan Fold Belt?. Australian Journal of Earth Sciences, 55 (4) 433-448 doi:10.1080/08120090801888586
Dadd, K. A. (2011) Extension-related volcanism in the Middle to Late Devonian of the Lachlan Orogen: geochemistry of mafic rocks in the Comerong Volcanics. Australian Journal of Earth Sciences, 58 (2) 209-222 doi:10.1080/08120099.2011.535563
Murphy, N. C., Gray, D. R. (1992) East‐directed overthrusting in the Melbourne Zone, Lachlan Fold Belt. Australian Journal of Earth Sciences, 39 (1) 37-53 doi:10.1080/08120099208727999
Flood, P. G., Aitchison, J. C. (1992) Late devonian accretion of the Gamilaroi Terrane to eastern Gondwana: Provenance linkage suggested by the first appearance of Lachlan Fold Belt‐derived quartzarenite. Australian Journal of Earth Sciences, 39 (4) 539-544 doi:10.1080/08120099208728045
Fergusson, C. L. (2014) Late Ordovician to mid-Silurian Benambran subduction zones in the Lachlan Orogen, southeastern Australia. Australian Journal of Earth Sciences, 61 (4) 587-606 doi:10.1080/08120099.2014.903858
Glen, R. A., Percival, I. G., Quinn, C. D. (2009) Ordovician continental margin terranes in the Lachlan Orogen, Australia: Implications for tectonics in an accretionary orogen along the east Gondwana margin. Tectonics, 28 (6). doi:10.1029/2009tc002446
Chappell, B. W., White, A. J. R., Hine, R. (1988) Granite provinces and basement terranes in the Lachlan Fold Belt, southeastern Australia. Australian Journal of Earth Sciences, 35 (4) 505-521 doi:10.1080/08120098808729466
 
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