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Page, Michael C., Dickens, Gerald R., Dunbar, Gavin B. (2003) Tropical view of Quaternary sequence stratigraphy: Siliciclastic accumulation on slopes east of the Great Barrier Reef since the Last Glacial Maximum. Geology, 31 (11) 1013 doi:10.1130/g19622.1

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Reference TypeJournal (article/letter/editorial)
TitleTropical view of Quaternary sequence stratigraphy: Siliciclastic accumulation on slopes east of the Great Barrier Reef since the Last Glacial Maximum
JournalGeology
AuthorsPage, Michael C.Author
Dickens, Gerald R.Author
Dunbar, Gavin B.Author
Year2003Volume31
Issue11
PublisherGeological Society of America
DOIdoi:10.1130/g19622.1Search in ResearchGate
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Mindat Ref. ID138723Long-form Identifiermindat:1:5:138723:4
GUID0
Full ReferencePage, Michael C., Dickens, Gerald R., Dunbar, Gavin B. (2003) Tropical view of Quaternary sequence stratigraphy: Siliciclastic accumulation on slopes east of the Great Barrier Reef since the Last Glacial Maximum. Geology, 31 (11) 1013 doi:10.1130/g19622.1
Plain TextPage, Michael C., Dickens, Gerald R., Dunbar, Gavin B. (2003) Tropical view of Quaternary sequence stratigraphy: Siliciclastic accumulation on slopes east of the Great Barrier Reef since the Last Glacial Maximum. Geology, 31 (11) 1013 doi:10.1130/g19622.1
In(2003) Geology Vol. 31 (11) Geological Society of America

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Dunbar, Gavin B., Dickens, Gerald R. (2003) Late Quaternary shedding of shallow-marine carbonate along a tropical mixed siliciclastic-carbonate shelf: Great Barrier Reef, Australia. Sedimentology, 50 (6). 1061-1077 doi:10.1046/j.1365-3091.2003.00593.x
Dunbar, Gavin B, Dickens, Gerald R (2003) Massive siliciclastic discharge to slopes of the Great Barrier Reef Platform during sea-level transgression: constraints from sediment cores between 15°S and 16°S latitude and possible explanations. Sedimentary Geology, 162 (1) 141-158 doi:10.1016/s0037-0738(03)00216-1
Page, Michael C., Dickens, Gerald R. (2005) Sediment fluxes to Marion Plateau (southern Great Barrier Reef province) over the last 130 ky: New constraints on ‘transgressive-shedding’ off northeastern Australia. Marine Geology, 219 (1) 27-45 doi:10.1016/j.margeo.2005.05.002
Yokoyama, Yusuke (2012) Climate and Sea-level changes since the last glacial maximum: Preliminary results from IODP Expedition 325 the Great Barrier Reef Environmental Change. Quaternary International, 279. 550pp. doi:10.1016/j.quaint.2012.08.1938
Fielding, C.R., Trueman, J.D., Dickens, G.R., Page, M. (2003) Anatomy of the buried Burdekin River channel across the Great Barrier Reef shelf: how does a major river operate on a tropical mixed siliciclastic/carbonate margin during sea level lowstand?. Sedimentary Geology, 157 (3) 291-301 doi:10.1016/s0037-0738(02)00238-5
Dunbar, G.B., Dickens, G.R., Carter, R.M. (2000) Sediment flux across the Great Barrier Reef Shelf to the Queensland Trough over the last 300ky. Sedimentary Geology, 133 (1) 49-92 doi:10.1016/s0037-0738(00)00027-0
Fujita, Kazuhiko, Yagioka, Noriko, Nakada, Choko, Kan, Hironobu, Miyairi, Yosuke, Yokoyama, Yusuke, Webster, Jody M. (2020) Reef-flat and back-reef development in the Great Barrier Reef caused by rapid sea-level fall during the Last Glacial Maximum (30–17 ka) Geology, 48 (1) 39-43 doi:10.1130/g46792.1
Eden, D (2003) Dust accumulation in the New Zealand region since the last glacial maximum. Quaternary Science Reviews, 22 (18). 2037-2052 doi:10.1016/s0277-3791(03)00168-9
Heap, A. D., Dickens, G. R., Stewart, L. K., Woolfe, K. J. (2002) Holocene storage of siliciclastic sediment around islands on the middle shelf of the Great Barrier Reef Platform, north-east Australia. Sedimentology, 49 (3). 603-621 doi:10.1046/j.1365-3091.2002.00464.x
Lee, Bo-Ram, Yoo, Dong-Geun, Lee, Gwang-Soo (2022) High-resolution sequence stratigraphy and evolution of the Jeju Strait shelf, Korea, since the Last Glacial Maximum. Marine and Petroleum Geology, 135. 105389pp. doi:10.1016/j.marpetgeo.2021.105389
Jiwarungrueangkul, Thanakorn, Liu, Zhifei (2021) East Asian monsoon and sea-level controls on clay mineral variations in the southern South China Sea since the Last Glacial Maximum. Quaternary International, 592. 1-11 doi:10.1016/j.quaint.2021.04.033
 
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