南海的形成与演变

doi:10.3969/j.issn.0253-9608.2022.01.003

Abstract

Abstract: South China Sea is the largest marginal sea of the eastern Asia. It has developed complex structures and rich hydrocarbon potential. For a long time, scientists are arguing about how South China Sea evolved into its present situation, as well as the deep driving mechanism and controlling factors. In order to resolve the above-mentioned questions, large amounts of geophysical investigations and 3 turns with 5 International Ocean Discovery Program (IODP) expeditions were carried out in South China Sea, which in turn led to significant progress. This paper summarized the dynamic attribute and the evolution history of the South China Sea based on the past decades of research progress. Three existing scientific questions were raised the following summary, including the mechanism of margin transition from active to passive, the breaking up pattern of the South China Sea continental margin and the dynamics of extraordinary large amount of magmatism during the South China Sea evolution. Hopefully these questions can be resolved through more cutting-edge investigation and IODP drilling expeditions, serving for the natural resources exploration and submarine hazards monitoring.

SUN Zhen. Evolution of the South China Sea[J]. Chinese Journal of Nature, 2022, 44(1): 31-38.

References

[1] SUN Z, LIN J, QIU N, et al. The role of magmatism in the thinning and breakup process of the South China Sea continental margin [J]. National Science Review, 2019, 6(5): 871-876. https://doi. org/10.1093/nsr/nwz116.

[2] LI F, SUN Z, YANG H, et al. Continental interior and edge breakup at convergent margins induced by subduction direction reversal: A numerical modeling study applied to the South China Sea margin [J]. Tectonics, 2020, 39: e2020TC006409. https://doi. org/10.1029/2020TC006409

[3] SUN L H, SUN Z, ZHANG Y Y, et al. Multi-stage carbonate veins at IODP site U1504 document Early Cretaceous to Early Cenozoic extensional events on the South China Sea margin [J]. Marine Geology, 2021, 442: 106656. https://doi.org/10.1016/ j.margeo.2021.106656.

[4] TAYLOR B, HAYES D E. Origin and history of the South China Sea basin [M]//HAYES D E. The tectonic and geologic evolution of Southeast Asian Seas and islands: part 2. Washington D C: American Geophysical Union, 1983: 23-56.

[5] BRIAIS A, PATRIAT P, TAPPONNIER P. 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, 1993, 98: 6299-6328.

[6] 李家彪, 丁巍伟, 吴自银, 等. 南海西南海盆的渐进式扩张[J]. 科学通报, 57(20): 1896-1905.

[7] LI C-F, XU X, LIN J, et al. Ages and magnetic structures of the South China Sea constrained by deep tow magnetic surveys and IODP Expedition 349 [J]. Geochemistry Geophysical Geosystems, 2014, 15: 4958-4983. DOI:10.1002/2014GC005567.

[8] 汪品先. 亚洲形变与全球变冷—探索气候与构造的关系[J]. 第四纪研究, 1998(3): 213-221.

[9] WU J, SUPPE J, LU R, et al. Philippine Sea and East Asian plate tectonics since 52 Ma constrained by new subducted slab reconstruction methods [J]. J Geophys Res Solid Earth, 2016, 121: 4670-4741. DOI:10.1002/2016JB012923.

[10] WU J, SUPPE J. Proto-South China Sea plate tectonics using subducted slab constraints from tomography [J]. Journal of Earth Science, 2018, 29(6): 1304-1318. https://doi.org/10.1007/s12583- 017-0813-x.

[11] LI F C, SUN Z, YANG H F. Possible spatial distribution of the Mesozoic volcanic arc in the present-day South China Sea continental margin and its tectonic implications [J]. Journal of Geophysical Research: Solid Earth, 2018, 123: 6215-6235. https:// doi.org/10.1029/2017JB014861.

[12] TAPPONNIER P, PELTZER G, LEDAIN A Y, et al. Propagation extrusion tectonics in Asia: New insights from simple experiments with plasticine [J]. Geology, 1982, 22(4): 611-616.

[13] KARIG D E. Origin and development of marginal basins in the western Pacific [J]. J Geophy Res, 1971, 76(11): 2542-2561.

[14] 郭令智, 施央申, 马瑞士. 西太平洋中、新生代活动大陆边缘和岛弧构造的形成及演化[J]. 地质学报, 1983, 57(1): 11-21.

[15] HALL R. Reconstructing Cenozoic SE Asia [M]//HALL R, BLUNDELL D J. Tectonic Evolution of Southeast Asia. Geological Society Special Publication. No.106. London: Geological Society Pub House, 1996: 203-224.

[16] SUN Z, ZHONG Z H, KEEP M, et al. 3D analogue modeling of the South China Sea: A discussion on breakup pattern [J] Journal of Asian Earth Sciences, 2009, 34: 544-556. DOI:10.1016/ j.jseaes.2008.09.002.

[17] HUANG C-Y, WANG P X, YU M M, et al. Potential role of strikeslip faults in opening up the South China Sea [J]. National Science Review, 2019, 6: 891-901. DOI: 10.1093/nsr/nwz119.

[18] SUN Z, JIAN Z, STOCK J M, et al. South China Sea rifted margin. Proceedings of the International Ocean Discovery Program, 367/368: College Station, TX (International Ocean Discovery Program)[EB/OL].(2011-10-11) https://doi.org/10.14379/iodp. proc.367368.2018.

[19] 孙珍, 李付成, 林间, 等. 被动大陆边缘张-破裂过程与岩浆活动：南海的归属[J]. 地球科学, 2021, 46(3): 770-789.

[20] YANG F, HUANG X L, XU Y G, et al. Plume-ridge interaction in the South China Sea: Thermometric evidence from Hole U1431E of IODP Expedition 349 [J]. Lithos, 2019, 324/325: 466-478.

[21] ZHANG G L, CHEN L H, JACKSON M G, et al. Evolution of carbonated melt to alkali basalt in the South China Sea [J]. Nature Geoscience, 2017, 10: 229-236. DOI: 10.1038/NGEO2877.

[22] MARUYAMA S, SANTOSH S, ZHAO D. Superplume, supercontinent, and post-perovskite: Mantle dynamics and anti-plate tectonics on the Core-Mantle Boundary [J]. Gondwana Research, 2007, 11: 7-37. DOI: 10.1016/j.gr.2006.06.003.

[23] LIN J, XU Y G, SUN Z, et al. Mantle upwelling beneath the South China Sea and links to surrounding subduction systems [J]. National Science Review, 2019, 6(5): 877-881. https://doi.org/10.1093/nsr/ nwz123.

Evolution of the South China Sea

PDF

Knowledge

Abstract

Cite this article

share this article

References

Related Articles 0

Recommended Articles

Metrics

Comments