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King, R. C., Backé, G. (2010) A balanced 2D structural model of the Hammerhead Delta–Deepwater Fold-Thrust Belt, Bight Basin, Australia. Australian Journal of Earth Sciences, 57 (7) 1005-1012 doi:10.1080/08120099.2010.509409

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Reference TypeJournal (article/letter/editorial)
TitleA balanced 2D structural model of the Hammerhead Delta–Deepwater Fold-Thrust Belt, Bight Basin, Australia
JournalAustralian Journal of Earth Sciences
AuthorsKing, R. C.Author
Backé, G.Author
Year2010 (October)Volume57
Issue7
PublisherInforma UK Limited
DOIdoi:10.1080/08120099.2010.509409Search in ResearchGate
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Mindat Ref. ID500048Long-form Identifiermindat:1:5:500048:1
GUID0
Full ReferenceKing, R. C., Backé, G. (2010) A balanced 2D structural model of the Hammerhead Delta–Deepwater Fold-Thrust Belt, Bight Basin, Australia. Australian Journal of Earth Sciences, 57 (7) 1005-1012 doi:10.1080/08120099.2010.509409
Plain TextKing, R. C., Backé, G. (2010) A balanced 2D structural model of the Hammerhead Delta–Deepwater Fold-Thrust Belt, Bight Basin, Australia. Australian Journal of Earth Sciences, 57 (7) 1005-1012 doi:10.1080/08120099.2010.509409
In(2010, October) Australian Journal of Earth Sciences Vol. 57 (7) Informa UK Limited

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King, Rosalind C., Backé, Guillaume, Morley, Christopher K., Hillis, Richard R., Tingay, Mark R.P. (2010) Balancing deformation in NW Borneo: Quantifying plate-scale vs. gravitational tectonics in a delta and deepwater fold-thrust belt system. Marine and Petroleum Geology, 27 (1) 238-246 doi:10.1016/j.marpetgeo.2009.07.008
Paul, E., Sandiford, M., Flöttmann, T. (2000) Structural geometry of a thick‐skinned fold‐thrust belt termination: The Olary Block in the Adelaide Fold Belt, South Australia. Australian Journal of Earth Sciences, 47 (2) 281-289 doi:10.1046/j.1440-0952.2000.00779.x
Bray, A., Hatherly, P., Fergusson, C. L. (2010) Seismic reflection evidence for the evolution of the Camden Syncline and Lapstone Structural Complex, central Sydney Basin, Australia. Australian Journal of Earth Sciences, 57 (7) 993-1004 doi:10.1080/08120099.2010.509406
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
Morley, C.K., King, R., Hillis, R., Tingay, M., Backe, G. (2011) Deepwater fold and thrust belt classification, tectonics, structure and hydrocarbon prospectivity: A review. Earth-Science Reviews, 104 (1) 41-91 doi:10.1016/j.earscirev.2010.09.010
Lennox, PG, Trzebski, R, Armstrong, R, Siebel, W (2005) Structural evolution and granite chronology of the central Molong Zone, Eastern Lachlan Fold Belt, Australia. Australian Journal of Earth Sciences, 52 (1) 79-99 doi:10.1080/08120090500109102
Flo¨ttmann, Thomas, James, Patrick (1997) Influence of basin architecture on the style of inversion and fold-thrust belt tectonics—the southern Adelaide Fold-Thrust Belt, South Australia. Journal of Structural Geology, 19 (8). 1093-1110 doi:10.1016/s0191-8141(97)00033-3
Burton, G. R. (2023) Analogue modelling of a Tabberabberan fold-thrust belt in the Cobar region and implications for the origin of Cobar-type mineral deposits. Australian Journal of Earth Sciences, 70 (4) 548-566 doi:10.1080/08120099.2023.2180092
Robson, A. G., Holford, S. P., King, R. C. (2017) Structural evolution of a normal fault array in the Gambier Embayment, offshore Otway Basin, South Australia: insights from 3D seismic data. Australian Journal of Earth Sciences, 64 (5) 611-624 doi:10.1080/08120099.2017.1324822
Mukhopadhyay, Dilip K., Mishra, Premanand (2005) A balanced cross section across the Himalayan frontal fold-thrust belt, Subathu area, Himachal Pradesh, India: thrust sequence, structural evolution and shortening. Journal of Asian Earth Sciences, 25 (5) 735-746 doi:10.1016/j.jseaes.2004.07.007
Cruciani, Francesco, Barchi, Massimiliano R. (2016) The Lamu Basin deepwater fold-and-thrust belt: An example of a margin-scale, gravity-driven thrust belt along the continental passive margin of East Africa. Tectonics, 35 (3). 491-510 doi:10.1002/2015tc003856
 
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