南海西南次海盆两侧陆缘新生代构造沉降特征及演化过程

朱荣伟; 刘海龄; 姚永坚; 聂鑫; 徐子英

doi:10.16562/j.cnki.0256-1492.2020052002

南海西南次海盆两侧陆缘新生代构造沉降特征及演化过程

1.
自然资源部海底矿产资源重点实验室，广州海洋地质调查局，广州 510760

2.
中国科学院边缘海与大洋地质重点实验室，中国科学院南海海洋研究所，广州 510301

3.
南方海洋科学与工程广东省实验室(广州)，广州 511458

基金项目: 中国科学院边缘海与大洋地质重点实验室开放基金项目“南海南部中生界构造变形特征及其大地构造意义”（OMG2019-05）；中国地质调查局项目：中国大地构造演化和国际亚洲大地构造图编制（广州海洋地质调查局）（DD20190366），南海文昌和东方海域1∶25万海洋区域地质调查（DD20190627），全国陆域及海区地质图件更新与共享（广州海洋地质调查局）（DD20190378），天然气水合物数据库更新与服务（DD20190216），南部海域1∶100万海洋区域地质调查成果与应用研究（DD20160138）；南方海洋科学与工程广东省实验室（广州）人才团队引进重大专项“大洋钻探科学研究—南海重大基础地质问题与首钻选址”（GML2019ZD0201）；国家自然科学金项目“南海北缘琼南缝合带构造分段性变形机制多尺度研究”（41776072）。

详细信息

作者简介: 朱荣伟（1988—），男，博士，主要从事海洋构造地质与油气地质方面研究，E-mail：zhurongwei1209@126.com

通讯作者: 刘海龄(1958—)，博士，研究员，主要从事南海构造地质研究，E-mail:liuh82@126.com

中图分类号: P736.15

收稿日期: 2020-05-20

修回日期: 2020-07-09

刊出日期: 2020-12-25

Cenozoic tectonic subsidence of the continental margins of southwest sub-basin, South China Sea and its evolution

1.
Key Laboratory of Marine Mineral Resources, Ministry of Natural Resources, Guangzhou Marine Geological Survey, Guangzhou 510760, China

2.
CAS Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Science, Guangzhou 510301, China

3.
Guangdong Laboratory of Marine Science and Engineering, Guangzhou 511458, China

More Information

Corresponding author: LIU hailing, liuh82@126.com

Received Date: 20 May 2020

Revised Date: 09 July 2020

Publish Date: 25 December 2020

摘要

摘要:
构造沉降史分析有助于认识盆地的形成演化过程，是盆地分析的重要基础。为对比分析南海西南次海盆两侧陆缘新生代构造演化特征，本文选取了横穿南海西南次海盆两侧陆缘的多道地震剖面测线，其中NH973-3测线横跨西南次海盆北侧陆缘中-西沙地块，NH973-1+SO27-04联合剖面跨越西南次海盆南侧陆缘南沙地块，在地震地层解释的基础上，采用回剥法和平衡剖面技术分析了西南次海盆两侧陆缘构造沉降特征及伸展过程。分析结果表明：（1）西南次海盆两侧陆缘的构造沉降曲线特征表现为裂陷初始期曲线斜率平缓，裂陷强烈期和末期曲线斜率较陡，断-拗转换期和拗陷期曲线斜率又回归相对平缓的反“S”形多段式特征；（2）两侧陆缘的构造沉降具有一定的延迟滞后性，造成此现象的原因可能与西南次海盆两侧陆缘岩石圈的分层差异伸展及南海西缘断裂的右旋走滑活动有关，且南海西缘断裂的右旋走滑活动造成两侧陆缘的构造沉降中心向南迁移；（3）两侧陆缘盆地主要形成于晚渐新世，北侧陆缘因受晚渐新世南海西缘断裂右旋走滑活动的改造影响而形成伸展-走滑相关的沉积盆地，南侧陆缘在早中新世因受到挤压碰撞的改造影响而形成伸展-挠曲复合型沉积盆地。这些研究成果可为南海西南次海盆两侧陆缘沉积盆地的油气和天然气水合物的勘探开发提供重要的科学背景支持。
- 构造演化 /
- 伸展过程 /
- 构造沉降 /
- 共轭陆缘 /
- 南海西南次海盆
Abstract:
Tectonic subsidence analysis is helpful for understanding the origin and evolution of a basin, which are critical for basin analysis. In order to reveal the characteristics of Cenozoic tectonic evolution of the continental margins of the southwest sub-sea basin, South China Sea, the multi-channel seismic profile lines, NH973-3 and NH973-1+SO27-04 across the continental margins, were selected as research targets. The structures of the continental margins are studied using the methods of back stripping and balanced profile. It is observed that: (1) the structural subsidence curves of the above-mentioned continental margins are characterized by a multiple segment pattern in a reversed “s” shape, with a gentle slope in the initial rifting stage, a steep slope in the strong rifting stage and the end stage. The slope of the curve return to the relatively gentle during the transitional period from fault-depression to subsidence; (2) the tectonic subsidence along the continental margins have certain time delay, probably due to the layered differentiation and the extension of lithosphere and the dextral strike slip movement of the faults on the western margin of the South China Sea. The dextral strike slip movement of the faults on the western margin of the South China Sea might have resulted in the southward migration of the tectonic subsidence centers; (3) The basins on the continental margins were mainly formed in Late Oligocene, as the basins related to extensional strike slip on the northern margin of the South China Sea were formed due to the modification of the dextral strike slip movement of the west margin fault in Late Oligocene, whereas the flexure-extensional complex basins formed on the southern margin of the South China Sea due to the compression and collision in Early Miocene. The research results have provided important scientific background for the exploration and development of hydrocarbon and gas hydrate in the sedimentary basins on both sides of the southwest sub basin of the South China Sea.
- tectonic evolution /
- extension process /
- tectonic subsidence /
- conjugated continental margins /
- Southwest sub-basin of South China Sea

HTML全文

图 1 研究区区域位置及测线分布图

Figure 1.

下载: 全尺寸图片幻灯片

图 2 南海西南次海盆两侧陆缘盆地地层柱状图与构造演化简图（岩性组合及沉积环境参考文献[15-16]，地质年代参考2018年地层年代表^[36]，全球海平面变化曲线引自文献[37]）

Figure 2.

下载: 全尺寸图片幻灯片

图 3 NH973-3测线的伪井位置分布（测线位置见图1，剖面据文献[47]修改）

Figure 3.

下载: 全尺寸图片幻灯片

图 4 NH973-1+SO27-04测线伪井位置分布（测线位置见图1，剖面据文献[48]修改）

Figure 4.

下载: 全尺寸图片幻灯片

图 5 NH973-3测线（a）和NH973-1+ SO27-04测线（b）伪井构造沉降曲线

Figure 5.

下载: 全尺寸图片幻灯片

图 6 NH973-3测线（a）和NH973-1+SO27-04测线（b）各伪井不同地质时期构造沉降速率

Figure 6.

下载: 全尺寸图片幻灯片

图 7 南海西南次海盆南北两侧陆缘伸展系数、拉张量和拉张速率变化

Figure 7.

下载: 全尺寸图片幻灯片

表 1 不同类型沉积相古水深参考值

Table 1. Paleo-depth reference values for different types of sedimentary facies

沉积相类型	古水深参考值
冲积—河流相	0 m
滨湖相	＜5 m
浅湖相	5～20 m
深湖相	20～30 m或更深
扇三角洲相	≤30 m
海陆交互相	＜15 m
滨浅海相	＜30 m
浅海相	30～200 m
半深海相	200～500 m
深海相	＞500 m

下载: 导出CSV

参考文献(62)

[1]	Taylor B, Hayes D E. Origin and history of the South China Sea Basin[C]//Hayes D E. The Tectonic and Geologic Evolution of Southeast Asian Seas and Islands, Geophysical Monograph Series 27. Washington, DC: American Geophysical Union, 1983: 23-56.
[2]	Taylor B, Hayes D E. The tectonic evolution of the South China Basin[C]//Hayes D E. The Tectonic and Geologic Evolution of Southeast Asian Seas and Islands, Geophysical Monograph Series 23. Washington, DC: American Geophysical Union, 1980: 89-104.
[3]	李家彪, 丁巍伟, 高金耀, 等. 南海新生代海底扩张的构造演化模式: 来自高分辨率地球物理数据的新认识[J]. 地球物理学报, 2011, 54(12):3004-3015 doi: 10.3969/j.issn.0001-5733.2011.12.003 LI JiaBiao, DING Weiwei, GAO Jinyao, et al. Cenozoic evolution model of the sea-floor spreading in South China Sea: New constraints from high resolution geophysical data [J]. Chinese Journal of Geophysics, 2011, 54(12): 3004-3015. doi: 10.3969/j.issn.0001-5733.2011.12.003
[4]	Shi X B, Burov E, Leroy S, et al. Intrusion and its implication for subsidence: A case from the Baiyun Sag, on the northern margin of the South China Sea [J]. Tectonophysics, 2005, 407(1-2): 117-134. doi: 10.1016/j.tecto.2005.07.004
[5]	Northrup C J, Royden L H, Burchfiel B C. Motion of the Pacific plate relative to Eurasia and its potential relation to Cenozoic extension along the eastern margin of Eurasia [J]. Geology, 1995, 23(8): 719-722. doi: 10.1130/0091-7613(1995)023<0719:MOTPPR>2.3.CO;2
[6]	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 GUO Lingzhi, SHI Yangshen, MA Ruishi. On the formation and evolution of the Mesozoic-Cenozoic active continental margin and island arc tectonics of the Western Pacific Ocean [J]. Acta Geologica Sinica, 1983, 57(1): 11-21.
[7]	Schlüter H U, Hinz K, Block M. Tectono-stratigraphic terranes and detachment faulting of the South China Sea and Sulu Sea [J]. Marine Geology, 1996, 130(1-2): 39-78. doi: 10.1016/0025-3227(95)00137-9
[8]	朱伟林, 吴景富, 张功成, 等. 中国近海新生代盆地构造差异性演化及油气勘探方向[J]. 地学前缘, 2015, 22(1):88-101 ZHU Weilin, WU Jingfu, ZHANG Gongcheng, et al. Discrepancy tectonic evolution and petroleum exploration in China offshore Cenozoic basins [J]. Earth Science Frontiers, 2015, 22(1): 88-101.
[9]	包汉勇, 郭战峰, 张罗磊, 等. 太平洋板块形成以来的中国东部构造动力学背景[J]. 地球科学进展, 2013, 28(3):337-346 doi: 10.11867/j.issn.1001-8166.2013.03.0337 BAO Hanyong, GUO Zhanfeng, ZHANG Luolei, et al. Tectonic dynamics of eastern China since the formation of the Pacific plate [J]. Advances in Earth Science, 2013, 28(3): 337-346. doi: 10.11867/j.issn.1001-8166.2013.03.0337
[10]	谢文彦, 王涛, 张一伟. 南沙群岛海域断裂体系构造特征及其形成机制[J]. 热带海洋学报, 2007, 26(6):26-33 doi: 10.3969/j.issn.1009-5470.2007.06.005 XIE Wenyan, WANG Tao, ZHANG Yiwei. Structural features and formation mechanism of fault systems in Nansha sea area [J]. Journal of Tropical Oceanography, 2007, 26(6): 26-33. doi: 10.3969/j.issn.1009-5470.2007.06.005
[11]	Liu H L, Zheng H B, Wang Y L, et al. Basement of the South China Sea area: tracing the Tethyan Realm [J]. Acta Geologica Sinica-English Edition, 2011, 85(3): 637-655. doi: 10.1111/j.1755-6724.2011.00457.x
[12]	姚伯初. 南海南部地区的新生代构造演化[J]. 南海地质研究, 1994(6):1-15 YAO Bochu. Tectonical evolution on the southern margin of South China Sea [J]. Geological Research of South China Sea, 1994(6): 1-15.
[13]	姚伯初, 万玲, 吴能友. 大南海地区新生代板块构造活动[J]. 中国地质, 2004, 31(2):113-122 doi: 10.3969/j.issn.1000-3657.2004.02.001 YAO Bochu, WAN Ling, WU Nengyou. Cenozoic plate tectonic activities in the Great South China Sea area [J]. Geology in China, 2004, 31(2): 113-122. doi: 10.3969/j.issn.1000-3657.2004.02.001
[14]	姚永坚, 姜玉坤, 曾祥辉. 南沙海域新生代构造运动特征[J]. 中国海上油气(地质), 2002, 16(2):113-117, 124 YAO Yongjian, JIANG Yukun, ZENG Xianghui. Cenozoic tectonic movements in Nansha area, South China Sea [J]. China Offshore Oil and Gas (Geology), 2002, 16(2): 113-117, 124.
[15]	解习农, 任建业, 王振峰, 等. 南海大陆边缘盆地构造演化差异性及其与南海扩张耦合关系[J]. 地学前缘, 2015, 22(1):77-87 XIE Xinong, REN Jianye, WANG Zhenfeng, et al. Difference of tectonic evolution of continental marginal basins of South China Sea and relationship with SCS spreading [J]. Earth Science Frontiers, 2015, 22(1): 77-87.
[16]	解习农, 张成, 任建业, 等. 南海南北大陆边缘盆地构造演化差异性对油气成藏条件控制[J]. 地球物理学报, 2011, 54(12):3280-3291 doi: 10.3969/j.issn.0001-5733.2011.12.026 XIE Xinong, ZHANG Cheng, REN Jianye, et al. Effects of distinct tectonic evolutions on hydrocarbon accumulation in northern and southern continental marginal basins of South China Sea [J]. Chinese Journal of Geophysics, 2011, 54(12): 3280-3291. doi: 10.3969/j.issn.0001-5733.2011.12.026
[17]	Li J B, Ding W W, Wu Z Y, et al. The propagation of seafloor spreading in the southwestern subbasin, South China Sea [J]. Chinese Science Bulletin, 2012, 57(24): 3182-3191. doi: 10.1007/s11434-012-5329-2
[18]	Ding W W, Li J B. Propagated rifting in the Southwest Sub-basin, South China Sea: Insights from analogue modelling [J]. Journal of Geodynamics, 2016, 100: 71-86. doi: 10.1016/j.jog.2016.02.004
[19]	赵长煜, 宋海斌, 李家彪, 等. 南海西南次海盆NH973-1测线地震解释[J]. 地球物理学报, 2011, 54(12):3258-3268 doi: 10.3969/j.issn.0001-5733.2011.12.024 ZHAO Changyu, SONG Haibin, LI Jiabiao, et al. Tectonic and seismic interpretation of line NH973-1 along southwest sub-basin in South China Sea [J]. Chinese Journal of Geophysics, 2011, 54(12): 3258-3268. doi: 10.3969/j.issn.0001-5733.2011.12.024
[20]	姚伯初. 南海西南海盆的岩石圈张裂模式探讨[J]. 海洋地质与第四纪地质, 1999, 19(2):37-48 YAO Bochu. On the lithospheric rifting model in the southwest subbasin of South China Sea [J]. Marine Geology and Quaternary Geology, 1999, 19(2): 37-48.
[21]	丘学林, 赵明辉, 敖威, 等. 南海西南次海盆与南沙地块的OBS探测和地壳结构[J]. 地球物理学报, 2011, 54(12):3117-3128 doi: 10.3969/j.issn.0001-5733.2011.12.012 QIU Xuelin, ZHAO Minghui, AO Wei, et al. OBS survey and crustal structure of the Southwest Sub-basin and Nansha Block, South China Sea [J]. Chinese Journal of Geophysics, 2011, 54(12): 3117-3128. doi: 10.3969/j.issn.0001-5733.2011.12.012
[22]	Hall R. Cenozoic geological and plate tectonic evolution of SE Asia and the SW Pacific: computer-based reconstructions, model and animations [J]. Journal of Asian Earth Sciences, 2002, 20(4): 353-431. doi: 10.1016/S1367-9120(01)00069-4
[23]	刘海龄, 阎贫, 张伯友, 等. 南海前新生代基底与东特提斯构造域[J]. 海洋地质与第四纪地质, 2004, 24(1):15-28 LIU Hailing, YAN Pin, ZHANG Boyou, et al. Pre-Cenozoic basements of the South China Sea and eastern Tethyan realm [J]. Marine Geology and Quaternary Geology, 2004, 24(1): 15-28.
[24]	刘海龄, 阎贫, 孙岩. 南沙微板块的层块构造[J]. 中国地质, 2002, 29(4):374-381 doi: 10.3969/j.issn.1000-3657.2002.04.008 LIU Hailing, YAN Pin, SUN Yan. Layer-block tectonics of the Nansha microplate [J]. Geology in China, 2002, 29(4): 374-381. doi: 10.3969/j.issn.1000-3657.2002.04.008
[25]	赵美松, 刘海龄, 吴朝华. 南海南北陆缘中生代地层—构造特征及碰撞造山[J]. 地球物理学进展, 2012, 27(4):1454-1464 doi: 10.6038/j.issn.1004-2903.2012.04.020 ZHAO Meisong, LIU Hailing, WU Chaohua. Mesozoic stratigraphic and structural features and collisional orogeny between the northern and southern continental margins of South China Sea [J]. Progress in Geophysics, 2012, 27(4): 1454-1464. doi: 10.6038/j.issn.1004-2903.2012.04.020
[26]	Zhu R W, Liu H L, Yao Y J, et al. Mesozoic deformation and its geological significance in the southern margin of the South China Sea [J]. Journal of Ocean University of China, 2018, 17(4): 835-845. doi: 10.1007/s11802-018-3581-z
[27]	朱荣伟, 刘海龄, 姚永坚, 等. 南海中-西沙地块前新生代构造变形特征[J]. 海洋地质与第四纪地质, 2017, 37(2):67-74 ZHU Rongwei, LIU Hailing, YAO Yongjian, et al. A preliminary analysis of pre-cenozoic tectonic deformation of Zhongsha-Xisha block in South China Sea [J]. Marine Geology and Quaternary Geology, 2017, 37(2): 67-74.
[28]	朱荣伟, 刘海龄, 姚永坚, 等. 南沙海域中生代构造挤压及其成因[J]. 海洋地质与第四纪地质, 2017, 37(6):57-64 ZHU Rongwei, LIU Hailing, YAO Yongjian, et al. Mesozoic tectonic compression and its genesis in the sea area of Nansha [J]. Marine Geology and Quaternary Geology, 2017, 37(6): 57-64.
[29]	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 [J]. Journal of Geophysical Research: Solid Earth, 1993, 98(B4): 6299-6328. doi: 10.1029/92JB02280
[30]	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, Geophysics, Geosystems, 2014, 15(12): 4958-4983. doi: 10.1002/2014GC005567
[31]	Franke D, Savva D, Pubellier M, et al. The final rifting evolution in the South China Sea [J]. Marine and Petroleum Geology, 2014, 58: 704-720. doi: 10.1016/j.marpetgeo.2013.11.020
[32]	Ding W W, Li J B, Clift P D, et al. Spreading dynamics and sedimentary process of the Southwest Sub-basin, South China Sea: Constraints from multi-channel seismic data and IODP Expedition 349 [J]. Journal of Asian Earth Sciences, 2016, 115: 97-113. doi: 10.1016/j.jseaes.2015.09.013
[33]	吴朝华, 赵美松, 刘海龄. 南沙中部海域沉积地层特征及其构造成因[J]. 地球科学-中国地质大学学报, 2011, 36(5):853-860 WU Chaohua, ZHAO Meisong, LIU Hailing. Characteristics of sedimentary strata in Central Nansha Sea area and its tectonic origin [J]. Earth Science-Journal of China University of Geosciences, 2011, 36(5): 853-860.
[34]	Wang Y L, Qiu Y, Yan P, et al. Seismic evidence for Mesozoic strata in the northern Nansha waters, South China Sea [J]. Tectonophysics, 2016, 677-678: 190-198. doi: 10.1016/j.tecto.2016.04.003
[35]	Yan P, Liu H L. Tectonic-stratigraphic division and blind fold structures in Nansha Waters, South China Sea [J]. Journal of Asian Earth Sciences, 2004, 24(3): 337-348. doi: 10.1016/j.jseaes.2003.12.005
[36]	Cohen K M, Finney S C, Gibbard P L, et al. The ICS international chronostratigraphic chart [J]. Episodes, 2013, 36(3): 199-204. doi: 10.18814/epiiugs/2013/v36i3/002
[37]	Haq B U, Hardenbol J, Vail P R. Chronology of fluctuating sea levels since the Triassic [J]. Science, 1987, 235(4793): 1156-1167. doi: 10.1126/science.235.4793.1156
[38]	Dong D D, Wu S G, Zhang G C, et al. Rifting process and formation mechanisms of syn-rift stage prolongation in the deepwater basin, northern South China Sea [J]. Chinese Science Bulletin, 2008, 53(23): 3715-3725. doi: 10.1007/s11434-008-0326-1
[39]	Watts A B, Ryan W B F. Flexure of the lithosphere and continental margin basins [J]. Tectonophysics, 1976, 36(1-3): 25-44. doi: 10.1016/0040-1951(76)90004-4
[40]	Bond G C, Kominz M A. Construction of tectonic subsidence curves for the early Paleozoic miogeocline, southern Canadian Rocky Mountains: implications for subsidence mechanisms, age of breakup, and crustal thinning [J]. GSA Bulletin, 1984, 95(2): 155-173. doi: 10.1130/0016-7606(1984)95<155:COTSCF>2.0.CO;2
[41]	Sclater J G, Christie P A F. Continental stretching: an explanation of the Post-Mid-Cretaceous subsidence of the central North Sea basin [J]. Journal of Geophysical Research: Solid Earth, 1980, 85(B7): 3711-3739. doi: 10.1029/JB085iB07p03711
[42]	杨军, 施小斌, 王振峰, 等. 琼东南盆地张裂期沉降亏损与裂后期快速沉降成因[J]. 海洋地质与第四纪地质, 2015, 35(1):81-90 YANG Jun, SHI Xiaobin, WANG Zhenfeng, et al. Origin of syn-rift subsidence deficit and rapid post-rift subsidence in Qiongdongnan Basin [J]. Marine Geology and Quaternary Geology, 2015, 35(1): 81-90.
[43]	张云帆, 廖杰, 孙珍, 等. 南海海域构造沉降特征[J]. 地球科学-中国地质大学学报, 2011, 36(5):949-955 ZHANG Yunfan, LIAO Jie, SUN Zhen, et al. Characteristics of tectonic subsidence Nansha Area [J]. Earth Science-Journal of China University of Geosciences, 2011, 36(5): 949-955.
[44]	蔡佳, 王华, 崔敏. 琼东南盆地古近系沉降特征[J]. 海洋地质前沿, 2014, 30(4):14-19, 27 CAI Jia, WANG Hua, CUI Min. Subsidence character of the Paleogene Qiongdongnan Basin [J]. Marine Geology Frontiers, 2014, 30(4): 14-19, 27.
[45]	Walsh J, Watterson J, Yielding G. The importance of small-scale faulting in regional extension [J]. Nature, 1991, 351(6325): 391-393. doi: 10.1038/351391a0
[46]	Lü C C, Hao T Y, Lin J, et al. The role of rifting in the development of the continental margins of the southwest subbasin, South China Sea: Insights from an OBS experiment [J]. Marine Geophysical Research, 2017, 38(1-2): 105-123. doi: 10.1007/s11001-016-9295-y
[47]	Ding W W, Franke D, Li J B, et al. Seismic stratigraphy and tectonic structure from a composite multi-channel seismic profile across the entire Dangerous Grounds, South China Sea [J]. Tectonophysics, 2013, 582: 162-176. doi: 10.1016/j.tecto.2012.09.026
[48]	Clift P D, Sun Z. The sedimentary and tectonic evolution of the Yinggehai-Song Hong basin and the southern Hainan margin, South China Sea: Implications for Tibetan uplift and monsoon intensification [J]. Journal of Geophysical Research: Solid Earth, 2006, 111(B6): B06405.
[49]	赵中贤, 孙珍, 陈广浩, 等. 南沙海域新生代构造特征和沉降演化[J]. 地球科学-中国地质大学学报, 2011, 36(5):815-822 ZHAO Zhongxian, SUN Zhen, CHEN Guanghao, et al. Cenozoic structural characteristics and subsidence evolution in Nansha [J]. Earth Science-Journal of China University of Geosciences, 2011, 36(5): 815-822.
[50]	Shi X B, Jiang H Y, Yang J, et al. Models of the rapid post-rift subsidence in the eastern Qiongdongnan Basin, South China Sea: implications for the development of the deep thermal anomaly [J]. Basin Research, 2017, 29(3): 340-362. doi: 10.1111/bre.12179
[51]	陈梅, 施小斌, 刘凯, 等. 南海北缘珠三坳陷新生代构造沉降特征[J]. 海洋地质与第四纪地质, 2017, 37(6):47-56 CHEN Mei, SHI Xiaobin, LIU Kai, et al. Cenozoic tectonic subsidence of the Zhu Ⅲ depression in the Pearl River Mouth basin, Northern South China Sea [J]. Marine Geology and Quaternary Geology, 2017, 37(6): 47-56.
[52]	Zhao Z X, Sun Z, Wang Z F, et al. The dynamic mechanism of post-rift accelerated subsidence in Qiongdongnan Basin, northern South China Sea [J]. Marine Geophysical Research, 2013, 34(3-4): 295-308. doi: 10.1007/s11001-013-9188-2
[53]	徐行, 姚永坚, 彭登, 等. 南海西南次海盆的地热流特征与分析[J]. 地球物理学报, 2018, 61(7):2915-2925 doi: 10.6038/cjg2018L0223 XU Xing, YAO Yongjian, PENG Deng, et al. The characteristics and analysis of heat flow in the Southwest sub-basin of South China Sea [J]. Chinese Journal of Geophysics, 2018, 61(7): 2915-2925. doi: 10.6038/cjg2018L0223
[54]	Savva D, Meresse F, Pubellier M, et al. Seismic evidence of hyper-stretched crust and mantle exhumation offshore Vietnam [J]. Tectonophysics, 2013, 608: 72-83. doi: 10.1016/j.tecto.2013.07.010
[55]	汪俊, 邱燕, 阎贫, 等. 跨南海西南次海盆OBS、多道地震与重力联合调查[J]. 热带海洋学报, 2019, 38(4):81-90 WANG Jun, QIU Yan, YAN Pin, et al. A joint investigation using OBS, multi-channel seismic and gravity data across the Southwestern Sub-basin of the South China Sea [J]. Journal of Tropical Oceanography, 2019, 38(4): 81-90.
[56]	张云帆, 孙珍, 周蒂, 等. 南海北部陆缘新生代地壳减薄特征及其动力学意义[J]. 中国科学(D辑: 地球科学), 2008, 51(3):422-430 doi: 10.1007/s11430-008-0019-2 ZHANG Yunfan, SUN Zhen, ZHOU Di, et al. Stretching characteristics and its dynamic significance of the northern continental margin of South China Sea [J]. Science in China Series D: Earth Sciences, 2008, 51(3): 422-430. doi: 10.1007/s11430-008-0019-2
[57]	雷超, 任建业, 佟殿君. 南海北部洋陆转换带盆地发育动力学机制[J]. 地球物理学报, 2013, 56(4):1287-1299 doi: 10.6038/cjg20130423 LEI Chao, REN Jianye, TONG Dianjun. Geodynamics of the ocean-continent transition zone, northern margin of the South China Sea: Implications for the opening of the South China Sea [J]. Chinese Journal of Geophysics, 2013, 56(4): 1287-1299. doi: 10.6038/cjg20130423
[58]	佟殿君, 任建业, 雷超, 等. 琼东南盆地深水区岩石圈伸展模式及其对裂后期沉降的控制[J]. 地球科学-中国地质大学学报, 2009, 34(6):963-974 doi: 10.3321/j.issn:1000-2383.2009.06.011 TONG Dianjun, REN Jianye, LEI Chao, et al. Lithosphere stretching model of deep water in Qiongdongnan Basin, northern continental margin of South China Sea, and controlling of the post-rift subsidence [J]. Earth Science-Journal of China University of Geosciences, 2009, 34(6): 963-974. doi: 10.3321/j.issn:1000-2383.2009.06.011
[59]	安慧婷, 李三忠, 索艳慧, 等. 南海西部新生代控盆断裂及盆地群成因[J]. 海洋地质与第四纪地质, 2012, 32(6):95-111 AN Huiting, LI Sanzhong, SUO Yanhui, et al. Basin-controlling faults and formation mechanism of the Cenozoic basin groups in the western South China Sea [J]. Marine Geology and Quaternary Geology, 2012, 32(6): 95-111.
[60]	高红芳. 南海西缘断裂带走滑特征及其形成机理初步研究[J]. 中国地质, 2011, 38(3):537-543 doi: 10.3969/j.issn.1000-3657.2011.03.003 GAO Hongfang. A tentative discussion on strike-slipping character and formation mechanism of western-edge fault belt in South China Sea [J]. Geology in China, 2011, 38(3): 537-543. doi: 10.3969/j.issn.1000-3657.2011.03.003
[61]	刘海龄, 姚永坚, 沈宝云, 等. 南海西缘结合带的贯通性[J]. 地球科学-中国地质大学学报, 2015, 40(4):615-632 doi: 10.3799/dqkx.2015.049 LIU Hailing, YAO Yongjian, SHEN Baoyun, et al. On linkage of western boundary faults of the South China Sea [J]. Earth Science-Journal of China University of Geosciences, 2015, 40(4): 615-632. doi: 10.3799/dqkx.2015.049
[62]	袁玉松, 杨树春, 胡圣标, 等. 琼东南盆地构造沉降史及其主控因素[J]. 地球物理学报, 2008, 51(2):376-383 doi: 10.3321/j.issn:0001-5733.2008.02.010 YUAN Yusong, YANG Shuchun, HU Shengbiao, et al. Tectonic subsidence of Qiongdongnan Basin and its main control factors [J]. Chinese Journal of Geophysics, 2008, 51(2): 376-383. doi: 10.3321/j.issn:0001-5733.2008.02.010