Deepwater Canyons Reworked by Bottom Currents: Sedimentary Evolution and Genetic Model

Based on multi-beam bathymetric data and 2D high-resolution, multi-channel seismic prof'des, combing ODPl148 drilling data, the morphology, internal sedimentary architecture, and evo-lution pattern of 17 deepwater canyons from the Middle Miocene to present are documented in the northern Baiyun (白云)...

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Published inJournal of earth science (Wuhan, China) Vol. 23; no. 5; pp. 731 - 743
Main Author 吕彩丽 姚永坚 龚月华 吴时国 李学杰
Format Journal Article
LanguageEnglish
Published China University of Geosciences China University of Geosciences 01.10.2012
Springer Nature B.V
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Summary:Based on multi-beam bathymetric data and 2D high-resolution, multi-channel seismic prof'des, combing ODPl148 drilling data, the morphology, internal sedimentary architecture, and evo-lution pattern of 17 deepwater canyons from the Middle Miocene to present are documented in the northern Baiyun (白云) sag (BS), Pearl River Mouth basin (PRMB), and northern South China Sea (SCS). There exist six seismic architectural elements in these canyons, including basal erosive surfaces (BES), thalweg deposits (TD), lateral migration packages (LMP), mass transport deposits (MTD), can- yon margin deposits (CMD), and drape deposits (DD). According to the stratigraphical ages and geo-metrical features of these canyons, their formation and evolution processes are divided into three stages: (1) Middle Miocene scouring-filling, (2) Late Miocene lateral migration, and (3) Pliocene-Quaternary vertical overlay. An auto-cyclic progressive process of eroding and filling by turbidity currents results in the scouring-filling and vertical overlay; bottom currents are responsible for the remarkable asym-metry between the two flanks of canyons; and faults are inherent dynamic forces triggering these can yons. It is inferred that these canyons are caused by the double effects of turbidity and bottom currents under the control of faults as inherent dynamic forces.
Bibliography:Caili Lü,Yongjian Yao, Yuehua Gong ,Shiguo Wu ,Xuejie Li(1Key Laboratory of Marine Geology & Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China; Graduate University of Chinese Academy of Sciences, Beijing 100049, China;2Guangzhou Marine Geological Survey, Guangzhou 510075, China;3Key Laboratory of Marine Geology & Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingda
deepwater canyon-channel, bot-tom current, turbidity current, lateral migration,South China Sea.
42-1788/P
Based on multi-beam bathymetric data and 2D high-resolution, multi-channel seismic prof'des, combing ODPl148 drilling data, the morphology, internal sedimentary architecture, and evo-lution pattern of 17 deepwater canyons from the Middle Miocene to present are documented in the northern Baiyun (白云) sag (BS), Pearl River Mouth basin (PRMB), and northern South China Sea (SCS). There exist six seismic architectural elements in these canyons, including basal erosive surfaces (BES), thalweg deposits (TD), lateral migration packages (LMP), mass transport deposits (MTD), can- yon margin deposits (CMD), and drape deposits (DD). According to the stratigraphical ages and geo-metrical features of these canyons, their formation and evolution processes are divided into three stages: (1) Middle Miocene scouring-filling, (2) Late Miocene lateral migration, and (3) Pliocene-Quaternary vertical overlay. An auto-cyclic progressive process of eroding and filling by turbidity currents results in the scouring-filling and vertical overlay; bottom currents are responsible for the remarkable asym-metry between the two flanks of canyons; and faults are inherent dynamic forces triggering these can yons. It is inferred that these canyons are caused by the double effects of turbidity and bottom currents under the control of faults as inherent dynamic forces.
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ISSN:1674-487X
1867-111X
DOI:10.1007/s12583-012-0280-3