WANG Zhangshi, ZHONG Guangfa, SHI Hesheng, WANG Liaoliang. SEISMIC SEQUENCE FRAMEWORK AND DEPOSITIONAL EVOLUTION OF THE SEDIMENT DRIFT AT ODP SITE 1144, DONGSHA SLOPE, NORTHERN SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2011, 31(6): 55-63. DOI: 10.3724/SP.J.1140.2011.06055
Citation: WANG Zhangshi, ZHONG Guangfa, SHI Hesheng, WANG Liaoliang. SEISMIC SEQUENCE FRAMEWORK AND DEPOSITIONAL EVOLUTION OF THE SEDIMENT DRIFT AT ODP SITE 1144, DONGSHA SLOPE, NORTHERN SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2011, 31(6): 55-63. DOI: 10.3724/SP.J.1140.2011.06055
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SEISMIC SEQUENCE FRAMEWORK AND DEPOSITIONAL EVOLUTION OF THE SEDIMENT DRIFT AT ODP SITE 1144, DONGSHA SLOPE, NORTHERN SOUTH CHINA SEA

  • 1 State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China;

  • 2 Shenzhen Branch of CNOOC Limited, Guangzhou 510240, China;

  • 3 Guangzhou Marine Geological Survey, Guangzhou 510760, China

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  • Received Date: July 19, 2011
  • Revised Date: November 22, 2011
    Graphical Abstract
    • Abstract
  • Seismic stratigraphic framework and depositional evolution of the sediment drift at ODP Site 1144, Leg 184 Dongsha Slope, Northern South China Sea, are studied using high-resolution 2-D seismic data, combined with the drilling data and geophysical well logs. Seven seismic discontinuities with reflection terminations (onlap, downlap, toplap and erosional truncation), named SB1 to SB7 upwards, are identified within the drift. As a result, seven seismic sequences S1 to S7, from bottom to top are defined. The bottommost sequence is characterized with chaotic, weak amplitude reflections and interpreted as pre-drift slumping or debris deposits. The other sequences (S2-S7),which consist mainly of reflections with sub-parallel to wavy, continuous, medium to strong amplitude, are interpreted as the main components of the drift. Well-to-seismic correlation with the synthetic seismogram of Site 1144 suggests that the sequence boundaries of SB2 to SB7 were approximately developed at 1.09, 0.88, 0.65, 0.30, 0.13 and 0.02 Ma, respectively. Time thickness maps of the sequences suggest that depositional centers shifted frequently, mostly in a direction parallel to the slope strike. The drift extends in NE-SW along the slope. According to the thickness distribution, the drift is estimated at least 1 100 km2 in area, with a maximum thickness of about 520 m.
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    • References (20)
  • [1]
    Wong H K, Lüdmann T, Wollschläger M. Seismic reflection profiling at the northern continental margin of the South China Sea (SONNE-95 cruise)[R]. Reports, Geol.-Palont. Ins. Univ. Kiel, 1994, 68:41-53.
    [2]
    Wang L, Sarenthein M, Erlenkeuser H, et al. East Asian monsoon climate during the late Pleistocene:high-resolution sediment records from the South China Sea[J]. Marine Geology, 1999, 156:245-284.
    [3]
    王律江, Sarmhein M. 南海北部陆坡近四万年的高分辨率古海洋学纪录[J].第四纪研究,1999,1:27-31.[WANG Lü

    ;jinag, Sarmhein M. High-resolution Paleoceanographic Records during the last 40000 Years from the Northern Slope of South China Sea[J]. Quaternary Sciences, 1999, 1:27-31.]
    [4]
    Wang P X, Prell W L, Blum P, et al. Leg 184 summary:exploring the Asian monsoon through the South China Sea. In:Proceedings of the Ocean Drilling Program, Initial Reports, Volume 184[R]. Texas A&M University, College Station TX, 2000:18-29.
    [5]
    Shao L, Li X H, Wei G J, et al. Provenance of a prominent sediment drift on the northern slope of the South China Sea[J]. Science China Series D:Earth Sciences, 2001, 44(10):919-925.
    [6]
    Lüdmann T, Wong H K, Berglar K. Upward flow of North Pacific Deep Water in the northern South China Sea as deduced from the occurrence of drift sediments[J]. Geophysical Research Letters, 2005, 32:L05614.
    [7]
    Shao L, Li X J, Geng J H, et al. Deep water bottom current deposition in the northern South China Sea[J]. Science China Series D:Earth Sciences, 2007, 50(7):1060-1066.
    [8]
    钟广法,李前裕,郝沪军,等.深水沉积物波及其在南海研究之现状[J].地球科学进展, 2007, 22(9):907-913.

    [ZHONG Guangfa, LI Qianyu, HAO Hujun, et al. Current Status of Deep-water Sediment Wave Studies and the South China Sea Perspectives[J]. Advances in Earth Science, 2007, 22(9):907-913.]
    [9]
    栾锡武,彭学超,邱燕. 南海北部陆坡高速堆积体的构造成因[J].现代地质, 2009, 23(2):183-199.

    [LUAN Xiwu, PENG Xuechao, QIU Yan. Tectonic Control on the Formation of High-deposition-rate Sediment Drift in the Northern Slope of the South China Sea[J]. Geoscience, 2009, 23(2):183-199.]
    [10]
    Liu Z, Huang W, Li J, et al. Sedimentology. In:Wang P, Li Q, ed.The South China Sea:Paleoceanography and Sedimentology[M]. Berlin/Heidelberg:Springer-Verlag, 2009:178-180.
    [11]
    Vail P R, Mitchum R M Jr, et al. Seismic stratigraphy and global changes of sea level. In:Seismic Stratigraphy-Applications to Hydrocarbon Exploration[C]. AAPG Memoir, 1977, 26:49-212.
    [12]
    Buehring C, Sarnthein M, Erlenkeuser H. Toward a high-resolution stable isotope stratigraphy of the last 1.1 million years:Site 1144, South China Sea[C]//Proceedings of the Ocean Drilling Program, Scientific Results Volume 184. Texas:Texas A & M University, 2004:1-29.
    [13]
    Wang P X, Prell W L, Blum P, et al. Seismic reflection stratigraphy of Leg 184, South China Sea. In:Proceedings of the Ocean Drilling Program, Initial Reports, Volume 184[R]. Texas A & M University, College Station TX, 2000:1-37.
    [14]
    Faugères J C, Stow D A V, Imbert P, et al. Seismic features diagnostic of contourite drifts[J]. Marine Geology, 1999, 162:1-38.
    [15]
    Rebesco M, Stow D. Seismic expression of contourites and related deposits:a preface[J]. Marine Geophysical Researches, 2001, 22:303-308.
    [16]
    Faugères J C, Stow D A V. Contourite Drifts:Nature, Evolution and Controls. In:Rebesco M and Camerlenghi A, ed. Contourite[M]. Elsevier Science, Oxford, 2008:259-288.
    [17]
    Chen M T, Beaufort L and the Shipboard scientific Party of the IMAGESⅢ(MD106)-IPHIS Cruise. Exploring Quaternary variability of the East Asia monsoon, Kuroshio current, and Western Pacific Warm Pool systems:high-resolution investigations of paleoceanography from the IMAGESⅢ(MD106)-IPHIS cruise[J]. Tao, 1998,9(1):129-142.
    [18]
    Wang P, Zhao Q, Jian Z, et al. Thirty million year deep-sea records in the South China Sea[J]. Chinese Science Bulletin, 2003, 48(23):2524-2535.
    [19]
    Lin D C, Liu C H, Fang T H, et al. Millennial-scale changes in terrestrial sediment input and Holocene surface hydrography in the northern South China Sea (IMAGES MD972146)[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2006, 236:56-73.
    [20]
    杨文光,郑洪波,谢昕,等. 南海北部陆坡沉积记录的全新世早期夏季风极强事件[J].第四纪研究, 2008, 28(3):425-430.

    [YANG Wenguang, ZHENG Hongbo, XIE Xin, et al. East Asian Summer Monsoon Maximum Records in Northern South China Sea During the Early Holocene[J]. Quaternary Sciences, 2008, 28(3):425-430.]
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