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Cenozoic tectonic subsidence in the southern continental margin, South China Sea

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Abstract

We analyzed two recently acquired multi-channel seismic profiles across the Dangerous Grounds and the Reed Bank area in the South China Sea. Reconstruction of the tectonic subsidence shows that the southern continental margin can be divided into three stages with variable subsidence rate. A delay of tectonic subsidence existed in both areas after a break-up, which was likely related to the major mantle convection during seafloor spreading, that was triggered by the secondary mantle convection below the continental margin, in addition to the variation in lithospheric thickness. Meanwhile, the stage with delayed subsidence rate differed along strikes. In the Reed Bank area, this stage is between 32–23.8 Ma, while in the Dangerous Grounds, it was much later (between 19–15.5 Ma). We believe the propagated rifting in the South China Sea dominated the changes of this delayed subsidence rate stage.

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References

  • Aurelio M A, Peña R E, Taguibao K J L (2012). Sculpting the Philippine archipelagosince the cretaceous through rifting, oceanic spreading, subduction, obduction, collision and strike-slip faulting: contribution to IGMA5000. J Asian Earth Sci, 72(4): 102–107

    Google Scholar 

  • Barckhausen U, Engels M, Franke D, Ladage S, Pubellierb M (2014). Evolution of the South China Sea: revised ages for breakup and seafloor spreading. Mar Pet Geol, 58: 599–611

    Article  Google Scholar 

  • Barckhausen U, Roeser H A (2004). Seafloor spreading anomalies in the South China Sea revisited. Continent-ocean interactions within East Asian marginal seas, 121–125

    Chapter  Google Scholar 

  • Briais A, Patriat P, Tapponnier P (1993). Updated interpretation of magnetic anomalies and seafloor spreading stages in the South China Sea: implications for the Tertiary tectonics of Southeast Asia. Journal of Geophysical Research: Solid Earth (1978–2012), 98(B4): 6299–6328

    Article  Google Scholar 

  • Buck WR (1986). Small-scale convection induced by passive rifting: the cause for uplift of rift shoulders. Earth Planet Sci Lett, 77(3-4): 362–372

    Article  Google Scholar 

  • Chen L (2014). Stretching factor estimation for the long-duration and multi-stage continental extensional tectonics: application to the Baiyun Sag in the northern margin of the South China Sea. Tectonophysics, 611: 167–180

    Article  Google Scholar 

  • Clavès G, Clift P D, Inam A (2008). Anomalous Subsidence on Rifted Volcanic Margin of Pakistan: No Influence from Deccan Plume. Earth Planet Sci Lett, 272(1–2): 231–239

    Article  Google Scholar 

  • Clift P, Lee G H, Nguyan A D, Barckhausen U, Long H V, Sun Z (2008). Seismic reflection evidence for a dangerous grounds miniplate: no extrusion origin for the South China Sea. Tectonics, 27, TC3008

    Article  Google Scholar 

  • Clift P, Lin J (2001). Preferential mantle lithospheric extension under the South China margin. Mar Pet Geol, 18(8): 929–945

    Article  Google Scholar 

  • Clifton H E (1988). Sedimentologic approaches to paleobathymetry, with applications to the Merced Formation of central California. Palaios, 3(5): 507–522

    Article  Google Scholar 

  • Cullen A B (2010). Transverse segmentation of the Baram-Balabac Basin, NW Borneo: refining the model of Borneo’s tectonic evolution. Petrol Geosci, 16(1): 3–29

    Article  Google Scholar 

  • Ding W W, Franke D, Li J B, Steuer S (2013). Seismic stratigraphy and tectonic structure from a composite multi-channel seismic profile across the entire Dangerous Grounds, South China Sea. Tectonophysics, 582: 162–176

    Article  Google Scholar 

  • Ding W W, Li J B, Dong C Z, Fang Y X (2015). Oligocene-Miocene carbonates in the Reed Bank area, South China Sea, and their tectono-sedimentary evolution. Mar Geophys Res, 36(2-3): 149–165

    Article  Google Scholar 

  • Ding W W, Li J B, Li M B (2011). Seismic stratigraphy, tectonic structure and extension model across the Reed Bank Basin in the South China Sea: evidence from NH973-2 multi-channel seismic profile. Earth Science-Journal of China University of Geosciences, 36(5): 895–904 (in Chinese)

    Google Scholar 

  • Expedition 349 Scientists (2014). South China Sea tectonics: opening of the South China Sea and its implications for southeast Asian tectonics, climates, and deep mantle processes since the late Mesozoic. International Ocean Discovery Program Preliminary Report, 349

    Google Scholar 

  • Faccenna C, Becker T W (2010). Shaping Mobile Belts by Small-scale Convection. Nature, 465(7298): 602–605

    Article  Google Scholar 

  • Fan K Y, Qian G H (1998). The Cenozoic stratigraphic division and correlation in Nansha Waters. China Offshore Oil And Gas (Geology), 12(6): 370–376 (in Chinese)

    Google Scholar 

  • Fang P G, Ding W W, Fang Y X, Zhao Z X (2015). Development of Carbonate Platform and Its Response to Cenozoic Subsidence in Reed Bank Area, the South China Sea. Earth Science—Journal of China University of Geoscience, 40(12):2052–2066 (in Chinese)

    Article  Google Scholar 

  • Franke D (2013). Rifting, lithosphere breakup and volcanism: Comparison of magma-poor and volcanic rifted margins. Mar Pet Geol, 54(3): 63–87

    Article  Google Scholar 

  • Franke D, Barckhausen U, Baristeas N, Engels M, Ladage S, Lutz R, Montano J, Pellejera N, Ramos E G, Schnabel M (2011). The continent-ocean transition at the southeastern margin of the South China Sea. Mar Pet Geol, 28(6): 1187–1204

    Article  Google Scholar 

  • Franke D, Barckhausen U, Heyde I, Tingay M, Ramli N (2008). Seismic images of a collision zone offshore NWSabah/Borneo. Mar Pet Geol, 25(7): 606–624

    Article  Google Scholar 

  • Franke D, Savva D, Pubellier M, Steuer S, Mouly B, Auxietre J L, Meresse F, Chamot-Rooke N (2014). The final rifting evolution in the South China Sea. Mar Pet Geol, 58: 704–720

    Article  Google Scholar 

  • Hall R (2002). Cenozoic geological and plate tectonic evolution of SE Asia and the SW Pacific: computer-based reconstructions, model and animations. J Asian Earth Sci, 20(4): 353–431

    Article  Google Scholar 

  • Hall R, Clements B, Smyth H R (2009). Sundaland: basement character, structure and plate tectonic development. In: Proceedings, Indonesian Petroleum Association Thirty-Third Annual Convention and Exhibition, May 2009

    Google Scholar 

  • Hall R, van Hattum M W A, Spakman W (2008). Impact of India–Asia collision on SE Asia: the record in Borneo. Tectonophysics, 451(1): 366–389

    Article  Google Scholar 

  • Hayes D E, Nissen S S (2005). The South China Sea margins: implications for rifting contrasts. Earth Planet Sci Lett, 237(3-4): 601–616

    Article  Google Scholar 

  • Hinz K, Schlüter H U (1985). Geology of the dangerous grounds, South China Sea, and the continental margin off southwest Palawan: results of SONNE Cruises SO-23 and SO-27. Energy, 10(3): 297–315

    Article  Google Scholar 

  • Honza E (1995). Spreading mode of backarc basins in the western Pacific. Tectonophysics, 251(1–4): 139–152

    Article  Google Scholar 

  • Honza E, Fujioka K (2004). Formation of arcs and backarc basins inferred from the tectonic evolution of Southeast Asia since the Late Cretaceous. Tectonophysics, 384(1-4): 23–53

    Article  Google Scholar 

  • Huchon P, Nguyen T N H, Chamot-Rooke N (2001). Propagation of continental break-up in the south-western South China Sea. In: Wilson R C L, Whitmarsh R B, Taylor B, Froitzheim N, eds. Nonvolcanic rifting of continental margins: a comparison of evidence from land and sea. London: Special Publication Geological Society, 187: 31–50

    Google Scholar 

  • Hutchison C S (2004). Marginal basin evolution: the southern South China Sea. Mar Pet Geol, 21(9): 1129–1148

    Article  Google Scholar 

  • Hutchison C S, Bergman S C, Swauger D A, Graves J E (2000). A Miocene collisional belt in north Borneo: uplift mechanism and isostatic adjustment quantified by thermochronology. J Geol Soc London, 157(4): 783–793

    Article  Google Scholar 

  • Hutchison C S, Vijayan V (2010). What are the Spratly Islands? J Asian Earth Sci, 39(5): 371–385

    Article  Google Scholar 

  • King S D, Anderson D L (1998). Edge-driven convection. Earth Planet Sci Lett, 160(3-4): 289–296

    Article  Google Scholar 

  • Kudrass H R, Wiedicke M, Cepek P, Kreuzer H, Müller P (1986). Mesozoic and Cainozoic rocks dredged from the South China Sea (Reed Bank area) and Sulu Sea and their significance for platetectonic reconstructions. Mar Pet Geol, 3(1): 19–30

    Article  Google Scholar 

  • Lee T Y, Lawver L A (1995). Cenozoic plate reconstruction of Southeast Asia. Tectonophysics, 251(1-4): 85–138

    Article  Google Scholar 

  • Li C, Song T (2012). Magnetic recording of the Cenozoic oceanic crustal accretion and evolution of the South China Sea basin. Chin Sci Bull, 57(24): 3165–3181

    Article  Google Scholar 

  • Li C F, Xu X, Lin J, Sun Z, Zhu J, Yao Y J, Zhao X X, Liu Q S, Kulhanek D K, Wang J, Song T R, Zhao J F, Qiu N, Guan Y, Zhou Z, Williams T, Bao R, Briais A, Brown E A, Chen Y, Clift P D, Colwell F S, Dadd K A, Ding W, Almeida I H, Huang X L, Hyun S, Jiang T, Koppers A A P, Li Q, Liu C, Liu Z, Nagai R H, Peleo-Alampay A, Su X, Tejada M L G, Trinh H S, Yeh Y C, Zhang C, Zhang F, Zhang G L (2014b). Ages and magnetic structures of the South China Sea constrained by deep tow magnetic surveys and IODP Expedition 349. Geochem Geophys Geosyst, 15(12): 4958–4983

    Article  Google Scholar 

  • Li J B (2011). Dynamics of the Continental Margins in South China Sea: Scientific Experiments and Research Progresses. Chin J Geophys, 54(6): 883–893 (in Chinese)

    Article  Google Scholar 

  • Li S Z, Suo Y H, Liu X, Liming Dai S Y, Zhao S J (2012). Basic structural pattern and tectonic models of the South China Sea: problems, advances and controversies. Marine Geology & Quaternary Geology, 32(6): 35–53 (in Chinese)

    Article  Google Scholar 

  • Li S, Zhao S, Liu X, Suo Y, Cao H, Dai L, Guo L, Liu B, Yu S, Zhang G (2014a). Processes of Ocean Continent Transition and Coupling. Periodical of Ocean University of China, 44(10): 113–133 (in Chinese)

    Google Scholar 

  • Li X H, Li Z X, Li W X, Liu Y, Yuan C, Wei G J, Qi C S (2007). U–Pb zircon, geochemical and Sr–Nd–Hf isotopic constraints on age and origin of Jurassic I- and A-type granites from central Guangdong, SE China: A major igneous event in response to foundering of a subducted flat-slab? Lithos, 96(1-2): 186–204

    Article  Google Scholar 

  • McKenzie D (1978). Some remarks on the development of sedimentary basins. Earth Planet Sci Lett, 40(1): 25–32

    Article  Google Scholar 

  • Pang X, Chen C M, Peng D J, Zhu M, Shu Y, He M, Shen J, Liu B J (2007). Sequence stratigraphy of Pearl River Deep-water Fan System in the South China Sea. Earth Sci Front, 14(1): 220–229 (in Chinese)

    Article  Google Scholar 

  • Pichot T, Delescluse M, Chamot-Rooke N, Pubellier M, Qiu Y, Meresse F, Sun G, Savva D, Wong K P, Watremez L, Auxiètre J L (2014). Deep crustal structure of the conjugate margins of the SW South China Sea from wide-angle refraction seismic data. Mar Pet Geol, 58: 627–643

    Article  Google Scholar 

  • Qin J X, Hao T Y, Xu Y, Song H, Lu C C, Hu W J (2011). The distribution characteristics and the relationship between the tectonic units of the Moho Depth in South China Sea and Adjacent Areas. Chin J Geophys, 54(12): 3171–3183 (in Chinese)

    Google Scholar 

  • Reston T J (2009). The Extension Discrepancy and Syn-Rift Subsidence Deficit at Rifted Margins. Petrol Geosci, 15(3): 217–237

    Article  Google Scholar 

  • Ru K, Pigott J D (1986). Episodic rifting and subsidence in the South China Sea. AAPG Bulletin, September, 70: 1136–1155

    Google Scholar 

  • Ruan A G, Niu X W, Qiu X L, Li J B, Wu Z L, Zhao MH (2011). A wide angle ocean bottom seismometer profile across Liyue Bank, the southern margin of South China Sea. Chin J Geophys, 54(12): 3139–3149 (in Chinses)

    Google Scholar 

  • Sandiford M, Hand M, Mclaren S (1998). High geothermal gradient metamorphism during thermal subsidence. Earth Planet Sci Lett, 163(1-4): 149–165

    Article  Google Scholar 

  • Savva D, Pubellier M, Franke D, Chamot-Rooke N, Meresse F, Steuer S, Auxietre J L (2014). Different expressions of rifting on the South China Sea margins. Mar Pet Geol, 58: 579–598

    Article  Google Scholar 

  • Schlüter H U, Hinz K, Block M (1996). Tectono-stratigraphic terranes and detachment faulting of the South China Sea and Sulu Sea. Mar Geol, 130(1-2): 39–78

    Article  Google Scholar 

  • Shipboard Scientific Party (2000) Leg 184 summary: exploring the Asian Monsoon through drilling in the South China Sea. In: Wang P, Prell W, Blum P, eds. Proc. ODP, Initial results. IODP, College Station, TX, 1–77

    Google Scholar 

  • Song T, Li C F (2015). Rifting to drifting transition of the Southwest Subbasin of the South China Sea. Mar Geophys Res, 36(2–3): 167–185.

    Article  Google Scholar 

  • Steckler M S, Watts A B (1978). Subsidence of the Atlantic-type continental margin off New York. Earth Planet Sci Lett, 41(1): 1–13

    Article  Google Scholar 

  • Steuer S, Franke D, Meresse F, Savvab D, Pubellierb M, Auxietrec J L (2013). Oligocene–Miocene carbonates and their role for constraining the rifting and collision history of the Dangerous Gounds, South China Sea. Mar Pet Geol, 76: 412–427

    Google Scholar 

  • Sun Z, Zhao Z X, Zhou D, Yang S K, Lin H M (2011). The stratigraphy and the sequence achitecture of the basins in Nansha Region. Earth Science-Journal of China University of Geosciences, 36(5): 798–806 (in Chinese)

    Google Scholar 

  • Sun Z, Zhong Z, Keep M, Zhou D, Cai D S, Li X H, Wu S M, Jiang J Q (2009). 3D analogue modeling of the South China Sea: a discussion on breakup pattern. J Asian Earth Sci, 34(4): 544–556

    Article  Google Scholar 

  • Taylor B, Hayes D E (1980). The tectonic evolution of the South China Basin. The tectonic and geologic evolution of Southeast Asian seas and islands, 89–104

    Chapter  Google Scholar 

  • Taylor B, Hayes D E (1983). Origin and history of the South China Sea basin. The Tectonic and Geologic Evolution of Southeast Asian Seas and Islands: Part 2, 23–56

    Chapter  Google Scholar 

  • Tong D J, Ren J Y, Lei C, Yang H Z, Yin X Y (2009). Lithosphere stretching model of deep water in Qiongdongnan Basin, northern continental margin of South China Sea and controlling of the post-rift subsidence. Earth Sci, 34(6): 963–974 (in Chinese)

    Google Scholar 

  • Ungerer P, Bessis F, Chenet P Y, Durand B, Nogaret E, Chiarelli A, Oudin J L, Perrin J F (1984). Geological and geochemical models in oil exploration; principles and practical examples. In Demaison G, Murris R J, eds. Petroleum Geochemistry and Basin Evaluation: AAPG Memoir, 35: 53–77

    Google Scholar 

  • Van Wijk J W, Baldridge W S, van Hunen J, Goes S, Aster R C, Coblentz D (2010). Small-scale Convection at the Edge of the Colorado Plateau: Implications for Topography, Magmatism, and Evolution of Proterozic Lithosphere. Geology, 38(7): 611–614

    Article  Google Scholar 

  • Van Wijk J W, Van Hunen J, Goes S (2008). Small-scale Convection during Continental Rifting: Evidence from the Rio Grande Rift. Geology, 36(7): 575–578

    Article  Google Scholar 

  • Wu N Y, Zeng W J, Song H B, Zhou Z Y, Du D L, Wan L (2003). Tectonic subsidence of the South China Sea. Marine Geology & Quaternary Geology, 23(1): 55–65 (in Chinese)

    Google Scholar 

  • Xie H, Zhou D, Li Y, Pang X, Li P C, Chen G H, Li F C, Cao J H (2014). Cenozoic tectonic subsidence in deepwater sags in the Pearl River Mouth Basin, northern South China Sea. Tectonophysics, 615: 182–198

    Article  Google Scholar 

  • Yan P, Liu H (2004). Tectonic-stratigraphic division and blind fold structures in Nansha Waters, South China Sea. J Asian Earth Sci, 24(3): 337–348

    Article  Google Scholar 

  • Yang M Z, Wu J M, Yang R, Duan W W (1996). Stratigraphic division and nomenclature of the southwestern Nansha sea area. Geol. Res. South China Sea, 8: 37–46 (in Chinese)

    Google Scholar 

  • Yao B C (1996). Tectonic evolution of the south china sea in Cenozoic. Marine Geology & Quaternary Geology, 16(2): 1–12 (in Chinese)

    Google Scholar 

  • Yao Y J, Liu H L, Yang C P, Han B, Tian J J, Yin Z X, Gong J L, Xu Q Y (2012). Characteristics and evolution of Cenozoic sediments in the Liyue Basin, SE South China Sea. J Asian Earth Sci, 60: 114–129

    Article  Google Scholar 

  • Yeh Y, Sibuet J, Hsu S, Liu C (2010). Tectonic evolution of the Northeastern South China Sea from seismic interpretation. J Geophys Res Solid Earth, 115, B060103

    Article  Google Scholar 

  • Yumul G P Jr, Dimalanta C B, Maglambayan V B, Marquez E J (2008). Tectonic setting of a composite terrane: a review of the Philippine island arc system. Geosci J, 12(1): 7–17

    Article  Google Scholar 

  • Yumul G P Jr, Dimalanta C B, Tamayo R A Jr, Maury R C (2003). Collision, subduction and accretion events in the Philippines: a synthesis. Isl Arc, 12(2): 77–91

    Article  Google Scholar 

  • Zhao Z X, Sun Z, Chen G H (2011). Cenozoic structural characteristics and subsidence evolution in Nansha. Earth Science-Journal of China University of Geosciences, 36(5): 815–822 (in Chinese)

    Google Scholar 

  • Zhao Z X, Sun Z, Wang Z, Sun Z P, Liu J B, Wang Z W, Sun L T (2013). The dynamic mechanism of post-rift accelerated subsidence in Qiongdongnan Basin, northern South China Sea. Mar Geophys Res, 34(3-4): 295–308

    Article  Google Scholar 

  • Zhao Z X, Zhou D, Liao J, He M, Guo X Y, Zhang Y F, Xu Z Y (2010). Lithospheric Stretching Modeling of the Continental Shelf in the Pearl River Mouth Basin and Analysis of Post-Breakup Subsidence. Acta Geol Sin, 84(8): 1135–1145 (in Chinese)

    Google Scholar 

  • Zhou D, Ru K, Chen H (1995). Kinematics of Cenozoic extension on the South China Sea continental margin and its implications for the tectonic evolution of the region. Tectonophysics, 251(1): 161–177

    Article  Google Scholar 

  • Zhou D, Sun Z, Chen H, Xu H H, Wang W Y, Pang X, Cai D S, Hu D K (2008). Mesozoic paleogeography and tectonic evolution of South China Sea and adjacent areas in the context of Tethyan and Paleo-Pacific interconnections. Isl Arc, 17(2): 186–207

    Article  Google Scholar 

  • Zhu D, Larin K V, Luo Q, Tuchin V V (2013). Recent progress in tissue optical clearing. Laser Photonics Rev, 7(5): 732–757

    Article  Google Scholar 

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Acknowledgements

We want to thank the anonymous reviewers for their helpful comments. This paper benefits from early discussions with Peter D Clift from State Louisiana Univeristy. This work was financially supported by the National Natural Science Foundation of China (No. 41376066), the National Program on Global Change and Air-Sea Interaction, SOA (No. GASI-GEOGE-01), MOST of China (No. 2016YFC0600402), and Continental Shelf Drilling Project (No. GZH201100202).

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Fang, P., Ding, W., Fang, Y. et al. Cenozoic tectonic subsidence in the southern continental margin, South China Sea. Front. Earth Sci. 11, 427–441 (2017). https://doi.org/10.1007/s11707-016-0594-z

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