LIANG Chao, XIE Xinong, WANG Hua, ZHONG Guangjian, LIU Entao, SUN Ming, YI Hai, QIN Chunyu, CAO Haiyang, HE Jie, ZHAO Yanpu. Effects of igneous bodies on modification of modern slope morphology: Insights from the continental slope offshore Dongsha Islands, South China Sea[J]. Acta Oceanologica Sinica, 2019, 38(5): 109-117. doi: 10.1007/s13131-019-1357-y
Citation: LIANG Chao, XIE Xinong, WANG Hua, ZHONG Guangjian, LIU Entao, SUN Ming, YI Hai, QIN Chunyu, CAO Haiyang, HE Jie, ZHAO Yanpu. Effects of igneous bodies on modification of modern slope morphology: Insights from the continental slope offshore Dongsha Islands, South China Sea[J]. Acta Oceanologica Sinica, 2019, 38(5): 109-117. doi: 10.1007/s13131-019-1357-y

Effects of igneous bodies on modification of modern slope morphology: Insights from the continental slope offshore Dongsha Islands, South China Sea

doi: 10.1007/s13131-019-1357-y
  • Received Date: 2017-11-24
  • A statistical analysis for the morphological parameters extracted from numerous seismic profiles, and a high-resolution seismic study of the southeastern slope of the Dongsha Islands (South China Sea) with water depth between approximately 500 and 3 100 m, has revealed the variation of morphological features due to the intrusion of igneous bodies and associated sedimentary processes. Three types of the continental slope are distinguished:(1) a rough and steep slope with multiple igneous bodies (Type 1), (2) a relatively smooth and gentle slope with the single igneous body (Type 2), and (3) a smooth and gentle slope without igneous bodies (Type 3). These igneous bodies, formed in the post-seafloor spreading of the South China Sea, are often characterized by high positive seismic amplitudes, and chaotic reflections with complex shapes. The igneous bodies in Type 1 separated the slope into two or more upper sub-sags and a lower main-sag, in which the sub-sags and main-sag could be filled with sediments transported by alongslope bottom currents at the same time. Whereas, the igneous body in Type 2 just separated the slope into an upper sub-sag and a lower main-sag, in which the sediments could be transported into the lower main-sag only after the upper sub-sag has been filled up. Type 3 represents a normal slope with common clinoform progradation. The modern slope morphologies in the study area are the results of adjustments of the continental slope due to the intrusion of igneous bodies and associated sedimentary processes. The distinctions among three types of modern slope morphologies indicate different depositional conditions and adjustments of slope morphologies.
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  • Adams E W, Schlager W, Wattel E. 1998. Submarine slopes with an exponential curvature. Sedimentary Geology, 117(3-4):135-141, doi: 10.1016/S0037-0738(98)00044-X
    Brothers D S, Brink U S T, Andrews B D, et al. 2013. Geomorphic characterization of the U. S. Atlantic continental margin. Marine Geology, 338:46-63
    Cacchione D A, Pratson L F, Ogston A S. 2002. The shaping of continental slopes by internal tides. Science, 296(5568):724-727, doi: 10.1126/science.1069803
    Chen Hui, Xie Xinong, Van Rooij D, et al. 2014. Depositional characteristics and processes of alongslope currents related to a seamount on the northwestern margin of the Northwest Sub-Basin, South China Sea. Marine Geology, 355:36-53, doi: 10.1016/j.margeo.2014.05.008
    Cheng Shixiu, Li Sanzhong, Suo Yanhui, et al. 2012. Cenozoic tectonics and dynamics of basin groups of the northern South China Sea. Marine Geology & Quaternary Geology (in Chinese), 32(6):79-93
    Del Bianco F, Gasperini L, Angeletti L, et al. 2015. Stratigraphic architecture of the Montenegro/N. Albania continental margin (Adriatic sea-central Mediterranean). Marine Geology, 359:61-74
    Faugères J C, Stow D A V, Imbert P, et al. 1999. Seismic features diagnostic of contourite drifts. Marine Geology, 162(1):1-38, doi: 10.1016/S0025-3227(99)00068-7
    Faugères J C, Stow D A V. 2008. Contourite drifts:nature, evolution and controls. Developments in Sedimentology, 60:257-288, doi: 10.1016/S0070-4571(08)10014-0
    García M, Hernández-Molina F J, Llave E, et al. 2009. Contourite erosive features caused by the Mediterranean outflow water in the gulf of Cadiz:quaternary tectonic and oceanographic implications. Marine Geology, 257(1-4):24-40, doi: 10.1016/j.margeo.2008.10.009
    Goff J A. 2001. Quantitative classification of canyon systems on continental slopes and a possible relationship to slope curvature. Geophysical Research Letters, 28(23):4359-4362, doi: 10.1029/2001GL013300
    Gong Chenglin, Wang Yingmin, Peng Xuechao, et al. 2012. Sediment waves on the South China Sea slope off southwestern Taiwan:implications for the intrusion of the northern pacific deep water into the South China Sea. Marine and Petroleum Geology, 32(1):95-109, doi: 10.1016/j.marpetgeo.2011.12.005
    Hernández-Molina F J, Larter R D, Rebesco M, et al. 2006. Miocene reversal of bottom water flow along the Pacific Margin of the Antarctic Peninsula:stratigraphic evidence from a contourite sedimentary tail. Marine Geology, 228(1-4):93-116, doi: 10.1016/j.margeo.2005.12.010
    Kenyon P M, Turcotte D L. 1985. Morphology of a delta prograding by bulk sediment transport. GSA Bulletin, 96(11):1457-1465, doi: 10.1130/0016-7606(1985)96<1457:MOADPB>2.0.CO;2
    Li Wei, Alves T M, Wu Shiguo, et al. 2016. A giant, submarine creep zone as a precursor of large-scale slope instability offshore the Dongsha Islands (South China Sea). Earth and Planetary Science Letters, 451:272-284, doi: 10.1016/j.epsl.2016.07.007
    Li Pinglu, Rao Chuntao. 1994. Tectonic characteristics and evolution history of the Pearl river mouth basin. Tectonophysics, 235(1-2):13-25, doi: 10.1016/0040-1951(94)90014-0
    Li Hua, Wang Yingmin, Zhu Weilin, et al. 2013. Seismic characteristics and processes of the Plio-Quaternary unidirectionally migrating channels and contourites in the northern slope of the South China Sea. Marine and Petroleum Geology, 43:370-380, doi: 10.1016/j.marpetgeo.2012.12.010
    Lüdmann T, Wong H K. 1999. Neotectonic regime on the passive continental margin of the northern South China Sea. Tectonophysics, 311(1-4):113-138, doi: 10.1016/S0040-1951(99)00155-9
    O'Grady D B, Syvitski J P M, Pratson L F, et al. 2000. Categorizing the morphologic variability of siliciclastic passive continental margins. Geology, 28(3):207-210, doi: 10.1130/0091-7613(2000)28<207:CTMVOS>2.0.CO;2
    Pratson L F, Haxby W F. 1996. What is the slope of the U. S. continental slope?. Geology, 24(1):3-6, doi: 10.1130/0091-7613(1996)024<0003:WITSOT>2.3.CO;2
    Rebesco M, Hernández-Molina F J, Van Rooij D, et al. 2014. Contourites and associated sediments controlled by deep-water circulation processes:state-of-the-art and future considerations. Marine Geology, 352:111-154, doi: 10.1016/j.margeo.2014.03.011
    Sayago-Gil M, Long D, Hitchen K, et al. 2010. Evidence for current-controlled morphology along the western slope of Hatton Bank (Rockall Plateau, NE Atlantic Ocean). Geo-Marine Letters, 30(2):99-111, doi: 10.1007/s00367-009-0163-5
    Schlager W, Camber O. 1986. Submarine slope angles, drowning unconformities, and self-erosion of limestone escarpments. Geology, 14(9):762-765, doi: 10.1130/0091-7613(1986)14<762:SSADUA>2.0.CO;2
    Song Xiaoxiao, Li Chunfeng, Yao Yongjian, et al. 2017. Magmatism in the evolution of the South China Sea:geophysical characterization. Marine Geology, 394:4-15, doi: 10.1016/j.margeo.2017.07.021
    Steckler M S, Mountain G S, Miller K G, et al. 1999. Reconstruction of Tertiary progradation and clinoform development on the New Jersey passive margin by 2-D backstripping. Marine Geology, 154(1-4):399-420, doi: 10.1016/S0025-3227(98)00126-1
    Taylor B, Hayes D E. 1983. Origin and history of the South China Sea basin. In:Hayes D E, ed. The Tectonic and Geologic Evolution of Southeast Asian Seas and Islands:Part 2. Washington, DC:AGU Geophysical Monograph, 23-56
    Wang Pinxian, Li Qianyu. 2009. Oceanographical and geological background. In:Wang Pinxia, Li Qianyu, eds. The South China Sea:Paleoceanography and Sedimentology. Dordrecht:Springer
    Wu Shiguo, Gao Jinwei, Zhao Shujuan, et al. 2014a. Post-rift uplift and focused fluid flow in the passive margin of northern South China Sea. Tectonophysics, 615-616:27-39, doi: 10.1016/j.tecto.2013.12.013
    Wu Ziyin, Li Jiabiao, Li Shoujun, et al. 2017. A new method to identify the foot of continental slope based on an integrated profile analysis. Marine Geophysical Research, 38(1-2):199-207, doi: 10.1007/s11001-016-9273-4
    Wu Ziyin, Li Jiabiao, Jin Xianglong, et al. 2014b. Distribution, features, and influence factors of the submarine topographic boundaries of the Okinawa trough. Science China Earth Sciences, 57(8):1885-1896, doi: 10.1007/s11430-013-4810-3
    Wynn R B, Stow D A V. 2002. Classification and characterisation of deep-water sediment waves. Marine Geology, 192(1-3):7-22, doi: 10.1016/S0025-3227(02)00547-9
    Xie Qiang, Xiao Jingen, Wang Dongxiao, et al. 2013. Analysis of deep-layer and bottom circulations in the South China Sea based on eight quasi-global ocean model outputs. Chinese Science Bulletin, 58(32):4000-4011, doi: 10.1007/s11434-013-5791-5
    Xu Weihai, Yan Wen, Chen Zhong, et al. 2014. Organic matters and lipid biomarkers in surface sediments from the northern South China Sea:origins and transport. Journal of Earth Science, 25(1):189-196, doi: 10.1007/s12583-014-0412-z
    Yao Bochu, Wan Ling, Wu Nengyou. 2004. Cenozoic plate tectonic activities in the Great South China Sea area. Geology in China (in Chinese), 31(2):113-122
    Zhang Liansheng, Zhong Dalai. 1996. The red river strike-slip shear zone and Cenozoic tectonics of east Asia continent. Scientia Geologica Sinica (in Chinese), 31(4):327-341
    Zhao Quanhong, Li Qianyu, Jian Zhimin. 2009. Deep waters and oceanic connection. In:Wang Pinxian, Li Qianyu, eds. The South China Sea. Dordrecht:Springer, 395-437
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