| 引用本文: |
冯旭亮, 张功成, 王万银, 赵志刚, 邱之云, 谢晓军, 纪晓琳, 鲁宝亮, 宋双. 2018. 基于重磁震资料的南海新生代盆地分布综合研究. 地球物理学报, 61(10): 4242-4254, doi: 10.6038/cjg2018L0567
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| Citation: |
FENG XuLiang, ZHANG GongCheng, WANG WanYin, ZHAO ZhiGang, QIU ZhiYun, XIE XiaoJun, JI XiaoLin, LU BaoLiang, SONG Shuang. 2018. An integrated study on distribution of Cenozoic basins in the South China Sea based on gravity, magnetic and seismic data. Chinese Journal of Geophysics (in Chinese), 61(10): 4242-4254, doi: 10.6038/cjg2018L0567
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An integrated study on distribution of Cenozoic basins in the South China Sea based on gravity, magnetic and seismic data
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摘要:
作为西太平洋最大的边缘海，南海分布有30多个新生代沉积盆地，其蕴含着丰富的油气资源.但由于资料的限制，南海存在不同区域盆地研究程度不同，不同区域盆地面积差别较大，部分盆地只是坳陷而没有达到盆地的级别以及盆地外围可能存在凹陷等问题.南海新生代盆地分布问题制约了其油气分布规律、储量等基础地质问题的研究.本文以地震剖面数据为约束，以重力资料为主、辅以磁力资料，研究了南海新生代盆地分布及构造区划.通过提取新生代盆地及其构造单元引起的重力异常，结合地震剖面等资料反演了新生界底界面深度及新生界厚度.在充分调研已有盆地和构造单元划分方案的基础上，根据南海的地质及地球物理特征，确定了盆地及构造单元划分标准.以新生界厚度为基础并结合重、磁、震、地质等资料，进行地质-重磁震联合解释，将南海原有的36个盆地重新划分为24个盆地，盆地总面积扩大了约15万km2.研究表明，南海新生代盆地沉积层厚度在1.5~16 km之间，有6个北东东/北东向沉积坳陷带、2个近南北向沉积坳陷带以及1个三角沉积坳陷区；盆地展布方向主要为北东和北东东向，其次为北西和近南北向，呈现"南三北三"的分布特征.
Abstract:The South China Sea (SCS), as the largest marginal sea in the western Pacific Ocean, hosts more than 30 Cenozoic sedimentary basins that contain abundant oil and gas. Due to the limit of survey data available, some of these basins lack exhaustive studies or have controversial issues, especially in the central and southern regions. For example, different boundaries of basins in the central and southern SCS have been delineated. The relationship between the basins remain unclear and some basins (e.g. Nanweidong basin and Jiuzhang basin) may not attain the level of a true basin, instead merely a depression. In addition, some sags may exist on the periphery of some basins. To address these problems, we have studied the distribution of the Cenozoic basins in the SCS based on gravity, magnetic seismic data in an integrated way.
We collected the latest satellite altimetry gravity and magnetic ΔT anomalies and analyzed the physical properties of the strata and rocks in the SCS. Then we obtained the Bouguer gravity anomalies by removing the effect caused by seawater and computed the magnetic anomalies reduced to the pole using a varying inclination method. Based on the analysis of the characteristics of the gravity field, we extracted the gravity anomalies of the Cenozoic by using the minimum curvature technique for potential field data separation and inverted the thickness of Cenozoic in the study area under the constraint of seismic profiles.
We established the criteria to divide basins and other tectonic units on the basis of the thickness of Cenozoic and the relative relief of the basement assisted with the characteristics of the gravity and magnetic fields and trend lines of the faults combining other geologic data. Then we re-divided the original 36 Cenozoic basins into 24 sedimentary ones and defined their internal tectonic units. The total area of the newly divided basins has increased by about 150 thousand square kilometers. The thickness of the sedimentary layer of Cenozoic basins in the SCS is between 1.5 km and 16 km, which is rather changeable. These basins are divided into six NE or NEE trending sedimentary depression zones, two nearly NS trending sedimentary depression zones and one triangular sedimentary area. The directions of the basin distribution are mainly NE and NEE, followed by NW and nearly NS. Under the control of the major faults, these structures show a 'south three and north three' pattern.
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图 2
南海及邻区卫星测高重力异常图
Figure 2.
The satellite altimetry gravity anomaly in SCS and its adjacent region
图 4
南海盆地分布研究技术路线图
Figure 4.
The technique processes for basin distribution research in SCS
图 6
南海及邻区化极磁力异常图
Figure 6.
The magnetic anomaly reduced to the pole in SCS and its adjacent region
图 7
南海及邻区剩余重力异常图
Figure 7.
The residual gravity anomaly in SCS and its adjacent region
图 8
利用最小曲率位场分离方法提取的新生界重力异常(a)与地震剖面对比图(b)
Figure 8.
Comparison between the residual gravity anomaly (a) in Fig. 7 and the seismic profiles (b)
图 10
南海及邻区新生界厚度相对变化图
Figure 10.
The relative thickness of Cenozoic in SCS and its adjacent region
图 11
南海及邻区新生代沉积盆地分布图
Figure 11.
The distribution of deduced Cenozoic sedimentary basins in SCS and its adjacent area
图 12
南海及邻区新生代沉积盆地分布及新生界厚度图
Figure 12.
The distribution of deduced Cenozoic sedimentary basins and the thickness of Cenozoic
图 13
南海及邻区新生代沉积盆地分布及内部构造单元划分图
Figure 13.
The distribution of deduced Cenozoic sedimentary basins and their internal tectonic units in SCS and its adjacent area
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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, 98(B4):6299-6328. doi: 10.1029/92JB02280
Chen J, Wen N, Li X J. 2007. The status of the resource potential and petroleum exploration of the South China Sea.Progress in Geophysics (in Chinese), 22(4):1285-1294, doi:10.3969/j.issn.1004-2903.2007.04.039.
Chen Q, Jin Q H. 2017. Activity features of Wan'an fault and its constraints on Wan'an basin, western South China Sea.Marine Geology Frontiers (in Chinese), 33(10), 1-8. http://en.cnki.com.cn/Article_en/CJFDTotal-HYDT201710001.htm
Chen X, Su D Q, Lin J F. 1997. The separation of low frequency and middle frequency gravity fields in Nansha islands and its environs.Tropic Oceanology (in Chinese), 16(1):30-38. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199700441997
Deng Y H. 2016. Difference analyses on petroleum geology between the two basin belts in South China Sea.China Offshore Oil and Gas (in Chinese), 28(6):1-8. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zghsyq-gc201606001
Fan K Y, Qian G H. 1998. Division and correlation of Cenozoic in Nansha offshore area of South China Sea.China Offshore Oil and Gas (Geology) (in Chinese), 12(6):370-376. http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZHSD199806001.htm
Feng C M, Wang H J, Xie X N, et al, 2015. Thermal evolution of source rocks and contributing factors of the northern and southern continental marginal basins in the South China Sea.Geoscience (in chinese), 29(1):97-108, doi:10.3969/j.issn.1000-8527.2015.01.012.
Gao H F, Zeng X H, Liu Z H, et al. 2005. Simulating of subsidence history and analysis of tectonic evolutionary characteristics of Liyue basin in South China Sea.Geotectonica et Metallogenia (in Chinese), 29(3):385-390, doi:10.3969/j.issn.1001-1552.2005.03.014.
Hao T Y, Liu J H, Huang Z X, et al. 2004. Research on the lithosphere structure of Chinese Marginal Seas.Progress in Geophys. (in Chinese), 19(3):583-589, doi:10.3969/j.issn.1004-2903.2004.03.015.
Hu W J, Jiang W W, Hao T Y, et al. 2011. Integrated geophysical research on the distribution of Pre-Cenozoic residual basins in the South China Sea.Chinese J. Geophys. (in Chinese), 54(12):3315-3324, doi:10.3969/j.issn.0001-5733.2011.12.029.
Ji X L, Wang W Y, Qiu Z Y. 2015. The research to the minimum curvature technique for potential field data separation.Chinese J. Geophys. (in Chinese), 58(3):1042-1058, doi:10.6038/cjg20150329.
Jiang W W, Song H B, Xu Y. 2003. Characters of geophysical field and deep crustal structures of Northwestern South China Sea and Honghe region.Journal of Tropical Oceanography. (in Chinese), 22(2):40-48. http://en.cnki.com.cn/Article_en/CJFDTotal-RDHY200302004.htm
Jin Q H, Li T G. 2000. Regional geologic tectonics of the Nansha sea area.Marine Geology & Quaternary Geology (in Chinese), 20(1):1-8. http://en.cnki.com.cn/Article_en/CJFDTOTAL-HYDZ200001000.htm
Lang Y Q, Hu D Q, Liu C, et al. 2011. Mineralogy study of magnetic susceptibility of rocks along the coast of the northern South China Sea.Chinese J. Geophys. (in Chinese), 54(2):573-587, doi:10.3969/j.issn.0001-5733.2011.02.037.
Li C F, Xu X, Lin J, et al. 2014. Ages and magnetic structures of the South China Sea constrained by deep tow magnetic surveys and IODP Expedition 349. Geochemistry, Geophysics, Geosystems, 15(12):4958-4983. doi: 10.1002/2014GC005567
Li S Z, Suo Y H, Liu X, et al. 2012. Basin dynamics and basin groups of the South China Sea.Marine Geology & Quaternary Geology (in Chinese), 32(6):55-78, doi:10.3724/SP.J.1140.2012. 06055.
Li W Y, Li D X. 2006. Tectonic characteristics on the sedimentary basins with different plate margins in the South China Sea.Geoscience (in Chinese), 20(1):19-29. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xddz200601002
Li Y J, Yang H J, Zhang G Y, et al. 2012. Redivision of the tectonic units of Tabei Rise in Tarim Basin, NW China.Acta Petrologica Sinica (in Chinese), 28(8):2466-2478. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201208014
Lin Z. 2003. Characteristics and interpretation of gravity and magnetic anomalies in the Beikang Zengmu basin of central Nansha islands.Geophysical & Geochemical Exploration (in Chinese), 27(4):263-268. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=wtyht200304005
Liu G D. 1992. The Characteristic of Geological and Geophysical in China Seas and Adjacent Regions (in Chinese). Beijing:Science Press.
Liu Z H. 2005. Distribution of sedimentary basins and petroleum potential in southern South China Sea.Geotectonica et Metallogenia (in Chinese), 29(3):410-417. http://en.cnki.com.cn/Article_en/CJFDTotal-DGYK200503018.htm
Liu Z S. 2000. Geotectonics and hydrocarbon resources in the South China Sea.Quaternary Sciences (in Chinese), 20(1):69-77. http://en.cnki.com.cn/article_en/cjfdtotal-dsjj200001012.htm
Lu B L, Sun X M, Zhang G C, et al. 2011. Seismic-potential field response characteristics and identification of basement lithology of the northern South China Sea basin.Chinese J. Geophys. (in Chinese), 54(2):563-572:563-572, doi:10.3969/j.issn.0001-5733.2011.02.036.
Maus S, Barckhausen U, Berkenbosch H, et al. 2009. EMAG2:A 2-arc min resolution earth magnetic anomaly grid compiled from satellite, airborne, and marine magnetic measurements.Geochemistry, Geophysics, Geosystems, 10(8):1-12. http://d.old.wanfangdata.com.cn/Periodical/dqwlxjz201204063
Peng X C, Chen L. 1995. Geologic tectonic features of Wan'an basin in Nansha sea area.Marine Geology & Quaternary Geology (in Chinese), 15(2):35-48. http://en.cnki.com.cn/Article_en/CJFDTOTAL-HYDZ502.004.htm
Qin J X, Hao T Y, Xu Y, et al. 2011. The distribution characteristics and the relationship between the tectonic units of the Moho Depth in South China Sea and Adjacent Areas.Chinese J. Geophys. (in Chinese), 54(12):3171-3183, doi:10.3969/j.issn.0001-5733.2011.12.017.
Qiu X L, Ye S Y, Wu S M, et al. 2001. Crustal structure across the Xisha Trough, northwestern South China Sea.Tectonophysics, 341(1-4):179-193, doi:10.1016/S0040-1951(01)00222-0.
Qiu Y, Chen G N, Xie X N, et al. 2005. Sedimentary filling evolution of Cenozoic strata in Zengmu basin, southwestern South China Sea.Journal of Tropical Oceanography (in Chinese), 24(5):43-52, doi:10.3969/j.issn.1009-5470.2005.05.005.
Sandwell D T, Garcia E, Soofi K, et al. 2013. Towards 1-mGal accuracy in global marine gravity from CryoSat-2, Envisat, and Jason-1.The Leading Edge, 32(8):892-899, doi:10.1190/tle32080892.1.
Sandwell D T, Müller R D, Smith W H F, et al. 2014. New global marine gravity model from CryoSat-2 and Jason-1 reveals buried tectonic structure.Science, 346(6205):65-67. doi: 10.1126/science.1258213
Sandwell D T, Smith W H F. 2009. Global marine gravity from retracked Geosat and ERS-1 altimetry:Ridge Segmentation versus spreading rate.J. Geophys. Res., 114:B01411:1-B01411:18, doi:10.1029/2008JB006008.
Sun Z, Zhong Z H, Zhou D, et al. 2006. Research on the dynamics of the South China Sea opening:evidence from analogue modeling.Science in China (Series D:Earth Science) (in Chinese), 36(9):797-810. https://link.springer.com/article/10.1007%2Fs11430-006-1053-6
Talor B, Hayes D E. 1983. Origin and history of the South China Sea basin.Washington DC American Geophysical Union Geophysical Monograph, 27:23-56. http://adsabs.harvard.edu/abs/1983gms....27...23t
Trung N N, Lee S M, Que B C. 2004. Satellite gravity anomalies and their correlation with the major tectonic features in the South China Sea. Gondwana Research, 7(2):407-424. doi: 10.1016/S1342-937X(05)70793-0
Wang B Q, Huang Z B, Ma P L, et al. 2009. Establishment of division standard, evidence and principle of structure units in Tarim basin.Geotectonica et Metallogenia (in Chinese), 33(1):86-93, doi:10.3969/j.issn.1001-1552.2009.01.011.
Wang H B, Yao B C, Liang J Q, et al. 2001. Tectonic characteristics and division of the Beikang basin.Marine Geology & Quaternary Geology (in Chinese), 21(2):49-54. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hydzydsjdz200102009
Wang W Y, Pan Z S. 1993. Fast solution of forward and inverse problem for gravity field in a dual interface model.Geophysical Prospecting for Petroleum (in Chinese), 32(2):81-87. http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYWT199302008.htm
Wang W Y, Zhang J A, Liu Y, et al. 2013. Research on the tectonic boundary of Ying-Qiong basin and adjacent faults' features based on gravity and magnetic data.Progress in Geophysics (in Chinese), 28(3):1575-1583, doi:10.6038/pg20130355.
Wu B W. 2007. Analysis on the resource potential in the main depositional basins of Nansha area. South China Sea. Offshore Oil (in Chinese), 27(1):30-35. http://en.cnki.com.cn/Article_en/CJFDTOTAL-HYSY200701005.htm
Xia S H, Guo X W, Huang H B, et al. 2014. Geophysical features of lithosphere and tectonic boundaries in the South China Sea.Chinese J. Geophys. (in Chinese), 57(12):3957-3967, doi:10.6038/cjg20141209.
Xie J L, Yu H Z, Tang L M, et al. 2010. The basement features and basin types of Cenozoic sediments in South China Sea.Marine Origin Petroleum Geology (in Chinese), 15(4):35-47, doi:10.3969/j.issn.1672-9854.2010.04.006.
Xiong L J, Li S Z, Suo Y H, et al. 2012. Cenozoic basin-controlling faults and their bearing on basin groups formation in the southern South China Sea.Marine Geology & Quaternary Geology (in Chinese), 32(6):113-127, doi:10.3724/SP.J.1140.2012.06113.
Yan P, Zhou D, Liu Z S. 2001. A crustal structure profile across the northern continental margin of the South China Sea.Tectonophysics, 338(1):1-21, doi:10.1016/S0040-1951(01)00062-2.
Yang M H, Zhang H H, Liao Z B, et al. 2015. Petroleum systems of the major sedimentary basins in Nansha sea waters (South China Sea).Earth Science Frontiers (in Chinese), 22(3):48-58. http://d.old.wanfangdata.com.cn/Periodical/dxqy201503004
Yang M H, Zhang H H, Liao Z B, et al. 2017. Tectonic evolution and hydrocarbon accumulation of the sedimentary basins in Nansha Sea Waters (South China Sea).Geotectonica et Metallogenia, 41(4):710-720, doi:10.16539/j.ddgzyckx.2017.04.007.
Yang M Z, Wu J M. 1996. Tectonic stress field and tectonic evolution in the south of South China Sea.Tropic Oceanology (in Chinese), 15(2):45-52. http://d.old.wanfangdata.com.cn/Periodical/OA000002605
Yao B C, Liu Z H. 2006. Sedimentary basins and petroleum resources in Nansha offshore area, South China Sea.China Offshore Oil and Gas (in Chinese), 18(3):150-160. http://d.old.wanfangdata.com.cn/Periodical/zghsyq-gc200603002
Yao B C, Wan L, et al. 2006. The Three-dimensional Structure of Lithosphere and Its Evolution in the South China Sea (in Chinese). Beijing:Geological Publishing House.
Yao B C, Wan L, Liu Z H, et al. 2004a. Tectonic significance and its petroleum effect of the Wan'an tectonic movement in the south of the South China Sea.Marine Geology & Quaternary Geology (in Chinese), 24(1):69-77.
Yao B C, Wan L, Liu Z H. 2004b. Tectonic dynamics of Cenozoic sedimentary basins and hydrocarbon resources in the South China Sea.Earth Science-Journal of China University of Geosciences (in Chinese), 29(5):543-549, doi:10.3321/j.issn:1000-2383.2004.05.007.
Yao B C. 1998. The tectonic evolution and sedimentary basins of South China Sea in Cenozoic. Geological Research of South China Sea (in Chinese), 10:1-17. http://d.old.wanfangdata.com.cn/Periodical/dizhixb201804013
Yao Y J, Jiang Y K, Zeng X H. 2002. Cenozoic tectonic movements in Nansha area. South China Sea. China Offshore Oil and Gas (Geology) (in Chinese), 16(2):113-124. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zghsyq-dz200202008
Yao Y J, Xia B, Xu X. 2005. Tectonic evolution of the main sedimentary basins in southern area of the South China Sea.Geological Research of South China Sea (in Chinese), 1:1-11. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK200501913663
Yu C H, Zhao J F, Shi X B, et al. 2017. Sediment density correction of gravity anomaly in the South China Sea and its significance to analyze regional tectonic characteristics.Chinese J. Geophys. (in Chinese), 60(8):3151-3166, doi:10.6038/cjg20170822.
Zhang G C, Li Y C, Xie X J, et al. 2016. Tectonic cycle of marginal sea controls the ordered distribution of source rocks of deep water areas in South China Sea.China Offshore Oil and Gas (in Chinese), 28(2):23-36, doi:10.11935/j.issn.1673-1506.2016.02.003.
Zhang G C, Wang P J, Wu J F, et al. 2015. Tectonic cycle of marginal oceanic basin:A new evolution model of the South China Sea.Earth Science Frontiers (in Chinese), 22(3):027-037, doi:10.13745/j.esf.2015.03.002.
Zhang G C, Xie X J, Wang W Y, et al. 2013. Tectonic types of petroliferous basins and its exploration potential in the South China Sea.Acta Petrolei Sinica (in Chinese), 34(4):611-627, doi:10.7623/syxb2013040.
Zhang P Q, Zhao Q Y. 1996. Methods of the magnetic direction transform of aeromagnetic anomalies with differential inclinations in low magnetic latitudes.Computing Techniques for Geophysical and Geochemical Explaration (in Chinese), 18(3):206-214. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199600551159
Zhang Z W, Wu S M, Fan K Y, et al. 2005. Evaluation of hydrocarbon resources and key exploration areas in Nansha block, southern South China Sea.Geotectonica et Metallogenia (in Chinese), 29(3):418-424, doi:10.3969/j.issn.1001-1552.2005.03.018.
Zhao C Y, Song H B, Yang Z W, et al. 2014. Tectonic and thermal evolution modeling for the marginal basins of the southern South China Sea.Chinese Journal of Geophysics (in chinese), 57(5):1543-1553, doi:10.6038/cjg20140518.
Zhou D, Wang W Y, Pang X, et al. 2006. Mesozoic subduction-accretion zone in northeastern South China Sea inferred from geophysical interpretations.Science in China Series D (Earth Science) (in Chinese), 36(3):209-218, doi:10.3969/j.issn.1674-7240.2006.03.001.
Zhou X H, Yu Y X, Tang L J, et al. 2010. Cenozoic offshore basin architecture and division of structural elements in Bohai sea.China Offshore Oil and Gas (in Chinese), 22(5):285-289, doi:10.3969/j.issn.1673-1506.2010.05.001.
Zhou X Z, Jiang S R, Ye X K. 1993. Geology and oil-gas potential of Nansha Islands in South China Sea.China Offshore Oil and Gas (in Chinese), 7(5):1-7. http://en.cnki.com.cn/Article_en/CJFDTotal-ZHSD199305004.htm
陈洁, 温宁, 李学杰. 2007.南海油气资源潜力及勘探现状.地球物理学进展, 22(4):1285-1294, doi:10.3969/j.issn.1004-2903.2007.04.039.
陈强, 金庆焕. 2017.南海西部万安断裂活动特征及其对万安盆地的控制作用.海洋地质前沿, 33(10):1-8. http://d.old.wanfangdata.com.cn/Periodical/hydzdt201710001
陈雪, 苏达权, 林进峰. 1997.南沙群岛及其邻区低频和中频重力场的分离.热带海洋, 16(1):30-38. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199700441997
邓运华. 2016.试论中国南海两个盆地带油气地质差异性.中国海上油气, 28(6):1-8, doi:10.11935/j.issn.1673-1506.2016.06.001.
樊开意, 钱光华. 1998.南沙海域新生代地层划分与对比.中国海上油气, 12(6):370-376. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ZHSD199806001&dbname=CJFD&dbcode=CJFQ
冯常茂, 王后金, 解习农等. 2015.南海南、北大陆边缘盆地烃源岩热演化差异及成因分析.现代地质, 29(1):97-108, doi:10.3969/j.issn.1000-8527.2015.01.012.
高红芳, 曾祥辉, 刘振湖等. 2005.南海礼乐盆地沉降史模拟及构造演化特征分析.大地构造与成矿学, 29(3):385-390, doi:10.3969/j.issn.1001-1552.2005.03.014.
郝天珧, 刘建华, 黄忠贤等. 2004.中国边缘海岩石层结构研究.地球物理学进展, 19(3):583-589, doi:10.3969/j.issn.1004-2903.2004.03.015.
胡卫剑, 江为为, 郝天珧等. 2011.南海前新生代残留盆地分布综合地球物理研究.地球物理学报, 54(12):3315-3324, doi:10.3969/j.issn.0001-5733.2011.12.029. http://www.geophy.cn//CN/abstract/abstract8317.shtml
纪晓琳, 王万银, 邱之云. 2015.最小曲率位场分离方法研究.地球物理学报, 58(3):1042-1058, doi:10.6038/cjg20150329. http://www.geophy.cn//CN/abstract/abstract11372.shtml
江为为, 宋海斌, 胥颐. 2003.南海西北部与红河地区地球物理场及其地壳深部结构特征.热带海洋学报, 22(2):40-48. doi: 10.3969/j.issn.1009-5470.2003.02.005
金庆焕, 李唐根. 2000.南沙海域区域地质构造.海洋地质与第四纪地质, 20(1):1-8. http://d.old.wanfangdata.com.cn/Periodical/hydzydsjdz200001001
郎元强, 胡大千, 刘畅等. 2011.南海北部陆区岩石磁化率的矿物学研究.地球物理学报, 54(2):573-587, doi:10.3969/j.issn.0001-5733.2011.02.037. http://www.geophy.cn//CN/abstract/abstract7777.shtml
李三忠, 索艳慧, 刘鑫等. 2012.南海的盆地群与盆地动力学.海洋地质与第四纪地质, 32(6):55-78, doi:10.3724/SP.J.1140.2012. 06055.
李文勇, 李东旭. 2006.中国南海不同板块边缘沉积盆地构造特征.现代地质, 20(1):19-29. doi: 10.3969/j.issn.1000-8527.2006.01.002
李曰俊, 杨海军, 张光亚等. 2012.重新划分塔里木盆地塔北隆起的次级构造单元.岩石学报, 28(8):2466-2478. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201208014
林珍. 2003.南沙中部海域北康、曾母盆地重磁异常特征及解释.物探与化探, 27(4):263-268. doi: 10.3969/j.issn.1000-8918.2003.04.005
刘光鼎. 1992.中国海区及邻域地质地球物理特征.北京:科学出版社.
刘昭蜀. 2000.南海地质构造与油气资源.第四纪研究, 20(1):69-77. doi: 10.3321/j.issn:1001-7410.2000.01.012
刘振湖. 2005.南海南沙海域沉积盆地与油气分布.大地构造与成矿学, 29(3):410-417, doi:10.3969/j.issn.1001-1552.2005.03.017.
鲁宝亮, 孙晓猛, 张功成等. 2011.南海北部盆地基底岩性地震-重磁响应特征与识别.地球物理学报, 54(2):563-572, doi:10.3969/j.issn.0001-5733.2011.02.036. http://www.geophy.cn//CN/abstract/abstract7776.shtml
彭学超, 陈玲. 1995.南沙海域万安盆地地质构造特征.海洋地质与第四纪地质, 15(2):35-48. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK201204815630
秦静欣, 郝天珧, 徐亚等等. 2011.南海及邻区莫霍面深度分布特征及其与各构造单元的关系.地球物理学报, 54(12):3171-3183, doi:10.3969/j.issn.0001-5733.2011.12.017. http://www.geophy.cn//CN/abstract/abstract8305.shtml
邱燕, 陈国能, 谢习农等. 2005.南海西南海域曾母盆地新生界沉积充填演化研究.热带海洋学报, 24(5):43-52, doi:10.3969/j.issn.1009-5470.2005.05.005.
孙珍, 钟志洪, 周蒂等. 2006.南海的发育机制研究:相似模拟证据.中国科学D辑:地球科学, 36(9):797-810. http://d.old.wanfangdata.com.cn/Periodical/zgkx-cd200609002
王步清, 黄智斌, 马培领等. 2009.塔里木盆地构造单元划分标准、依据和原则的建立.大地构造与成矿学, 33(1):86-93, doi:10.3969/j.issn.1001-1552.2009.01.011.
王宏斌, 姚伯初, 梁金强等. 2001.北康盆地构造特征及其构造区划.海洋地质与第四纪地质, 21(2):49-54. http://d.old.wanfangdata.com.cn/Periodical/hydzydsjdz200102009
王万银, 潘作枢. 1993.双界面模型重力场快速正反演问题.石油物探, 32(2):81-87. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000003044210
王万银, 张瑾爱, 刘莹等. 2013.利用重磁资料研究莺琼盆地构造分界及其两侧断裂特征.地球物理学进展, 28(3):1575-1583, doi:10.6038/pg20130355.
吴炳伟. 2007.南沙海域主要沉积盆地资源潜力分析.海洋石油, 27(1):30-35. doi: 10.3969/j.issn.1008-2336.2007.01.006
夏少红, 郭兴伟, 黄海波等. 2014.南海岩石层及边界构造的地球物理特征, 57(12): 3957-3967, doi: 10.6038/cjg20141209.
谢锦龙, 余和中, 唐良民等. 2010.南海新生代沉积基底性质和盆地类型.海相油气地质, 15(4):35-47, doi:10.3969/j.issn.1672-9854.2010.04.006.
熊莉娟, 李三忠, 索艳慧等. 2012.南海南部新生代控盆断裂特征及盆地群成因.海洋地质与第四纪地质, 32(6):113-127, doi:10.3724/SP.J.1140.2012.06113.
杨明慧, 张厚和, 廖宗宝等. 2015.南海南沙海域主要盆地含油气系统特征.地学前缘, 22(3):048-058, doi:10.13745/j.esf.2015.03.004.
杨明慧, 张厚和, 廖宗宝等. 2017.南海南沙海域沉积盆地构造演化与油气成藏规律.大地构造与成矿学, 41(4):710-720, doi:10.16539/j.ddgzyckx.2017.04.007.
杨木壮, 吴进民. 1996.南海南部新生代构造应力场特征与构造演化.热带海洋, 15(2):45-52. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199600785019
姚伯初, 刘振湖. 2006.南沙海域沉积盆地及油气资源分布.中国海上油气, 18(3):150-160. doi: 10.3969/j.issn.1673-1506.2006.03.002
姚伯初, 万玲, 刘振湖等. 2004a.南海南部海域新生代万安运动的构造意义及其油气资源效应.海洋地质与第四纪地质, 24(1):69-77. http://d.old.wanfangdata.com.cn/Periodical/hydzydsjdz200401010
姚伯初, 万玲, 刘振湖. 2004b.南海海域新生代沉积盆地构造演化的动力学特征及其油气资源.地球科学-中国地质大学学报, 29(5):543-549, doi:10.3321/j.issn:1000-2383.2004.05.007.
姚伯初, 万玲等著. 2006.中国南海海域岩石圈三维结构及演化.北京:地质出版社.
姚伯初. 1998.南海新生代的构造演化与沉积盆地.南海地质研究, 10:1-17. http://d.old.wanfangdata.com.cn/Periodical/dqkx200405007
姚永坚, 姜玉坤, 曾祥辉. 2002.南沙海域新生代构造特征.中国海上油气(地质), 16(2):113-124. http://d.old.wanfangdata.com.cn/Periodical/dqkx201105005
姚永坚, 夏斌, 徐行. 2005.南海南部海域主要沉积盆地构造演化特征.南海地质研究, 1:1-11. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK200501913663
于传海, 赵俊峰, 施小斌等. 2017.南海重力异常的沉积层密度改正及其对区域构造特征分析的意义.地球物理学报, 60(8):3151-3166, doi:10.6038/cjg20170822. http://www.geophy.cn//CN/abstract/abstract13926.shtml
张功成, 李友川, 谢晓军等. 2016.南海边缘海构造旋回控制深水区烃源岩有序分布.中国海上油气, 28(2):23-36, doi:10.11935/j.issn.1673-1506.2016.02.003.
张功成, 王璞珺, 吴景富等. 2015.边缘海构造旋回:南海演化的新模式.地学前缘, 22(3):027-037, doi:10.13745/j.esf.2015.03.002.
张功成, 谢晓军, 王万银等. 2013.中国南海含油气盆地构造类型及勘探潜力.石油学报, 34(4):611-627, doi:10.7623/syxb2013040.
张培琴, 赵群友. 1996.低磁纬度区航磁异常变倾角磁方向转换方法.物探化探计算技术, 18(3):206-214. http://d.old.wanfangdata.com.cn/NSTLQK/10.1071-AH09663/
张智武, 吴世敏, 樊开意等. 2005.南沙海区沉积盆地油气资源评价及重点勘探地区.大地构造与成矿学, 29(3):418-424, doi:10.3969/j.issn.1001-1552.2005.03.018.
赵长煜, 宋海斌, 杨振武等. 2014.南海南部边缘沉积盆地构造-热演化历史.地球物理学报, 57(5):1543-1553, doi:10.6038/cjg20140518. http://www.geophy.cn//CN/abstract/abstract10323.shtml
周蒂, 王万银, 庞雄等. 2006.地球物理资料所揭示的南海东北部中生代俯冲增生带.中国科学D辑(地球科学), 36(3):209-218, doi:10.3969/j.issn.1674-7240.2006.03.001.
周效中, 姜绍仁, 叶秀开. 1993.南沙群岛海域地质与油气远景.中国海上油气, 7(5):1-7. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ZHSD199305004&dbname=CJFD&dbcode=CJFQ
周心怀, 余一欣, 汤良杰等. 2010.渤海海域新生代盆地结构与构造单元划分.中国海上油气, 22(5):285-289, doi:10.3969/j.issn.1673-1506.2010.05.001.
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Figure 1.
Topography in SCS and its adjacent region
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Figure 2.
The satellite altimetry gravity anomaly in SCS and its adjacent region
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Figure 3.
The magnetic ΔT anomaly in SCS and its adjacent region
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Figure 4.
The technique processes for basin distribution research in SCS
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Figure 5.
The Bouguer gravity anomaly in SCS and its adjacent region
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Figure 6.
The magnetic anomaly reduced to the pole in SCS and its adjacent region
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Figure 7.
The residual gravity anomaly in SCS and its adjacent region
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Figure 8.
Comparison between the residual gravity anomaly (a) in Fig. 7 and the seismic profiles (b)
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Figure 9.
Thickness of Cenozoic in SCS and its adjacent region
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Figure 10.
The relative thickness of Cenozoic in SCS and its adjacent region
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Figure 11.
The distribution of deduced Cenozoic sedimentary basins in SCS and its adjacent area
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Figure 12.
The distribution of deduced Cenozoic sedimentary basins and the thickness of Cenozoic
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Figure 13.
The distribution of deduced Cenozoic sedimentary basins and their internal tectonic units in SCS and its adjacent area
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Figure 14.
The distribution of deduced Cenozoic sedimentary basins and their internal tectonic units and the relative thickness of Cenozoic in SCS and its adjacent area