Vicissitude of Cenozoic carbonate platforms in the South China Sea:Sedimentation in semi-closed marginal seas
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摘要:
南海发育了广泛的碳酸盐台地，具有分布面积广和时空变化大的特点。南海碳酸盐台地的生命演化史总体上经历了萌生期、扩展期、繁盛期、淹没期和残留期等演化阶段。根据近年来国内外关于南海地质地球物理研究进展，发现南海碳酸盐台地是伴随着华南陆缘张裂、陆海巨变而萌生，台地基底往往发育在两个共轭陆缘伸展地块的伸展断块构造高地。随着大陆岩石圈进一步伸展、减薄和地幔剥露等过程，台地经历了晚渐新世末至早中新世初的萌生，到中中新世的勃发。此外，张裂和扩张期的岩浆构造也成为台地发育的重要控制因素，比如构造沉降提供了台地生长的可容纳空间，构造掀斜作用、断裂作用和前陆盆地前沿挤压褶皱的迁移控制了台地各单元厚度、沉积相和地震反射终止特征在横向上的变化，构造控制的相对海平面控制了不同级序生物礁碳酸盐台地的沉积旋回，而晚中新世构造作用导致半封闭边缘海的形成和大量碳酸盐台地淹没。最后，10.5Ma半封闭边缘海的形成，造成南海海盆古海洋环境的巨大变化，限制了台地的广泛发育，仅残留了数量少、面积小的现代孤立碳酸盐台地。
Abstract:Cenozoic carbonate platforms are widely distributed in the South China Sea. They are characterized by large thickness and strong spatio-temporal variations. This study summarized most of the recently published findings on the geological and geophysical features of the South China Sea. It is found that all these carbonate platforms have experienced a progressive evolution from initiation, extension, flourishing, drowning and relict stages. Most of them are drowned in Late Cenozoic, and often called drowned carbonate platforms by some researchers. The carbonate platforms are unique in the South China Sea and contain rich information on tectonic evolution. The development of carbonate platforms follows the rifting process. They are usually initiated on the high shoulders of a faulted block at the conjugated rifting margin in Eocene and Early Oligocene. By rifting, thinning, and mantle exhumation of the South China Sea margin, the carbonate platforms has kept growing as NE-SW direction ridges, and flourished till Late Early Miocene. Tectonic subsidence provided accommodation space for platform growth. Tectonic tilt, faulting and migration of compressive folds in the front of foreland basins controlled the distribution of thickness and lateral variation in seismic reflection features. Tectonic induced relative sea level change controlled the sedimentary cycles of carbonate platforms in different orders. Furthermore, the rapid subsidence in Late Miocene and the formation of the semi-closed marginal sea caused the drowning of most carbonate platforms. Only a few carbonate platforms might leave behind as isolated platforms with limited distribution and small scale up to present.
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Key words:
- carbonate platform /
- conjugated margin /
- tectonic evolution /
- marginal sea /
- South China Sea
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[1] Zhang Qiaomin. Coral reefs conservation and management in China[C]//In: Ahmed M, Chong C K, Cesar H (eds). Economic Valuation and Policy Priorities for Sustainable Management of Coral Reefs. WorldFish Center Conference Procedings 70. Penang Malaysia: WorldFish Center, 2004: 198-202.
[2] 张乔民, 余克服, 施祺, 等.全球珊瑚礁监测与管理保护[J].热带海洋学报, 2006, 25(2):71-78. doi: 10.3969/j.issn.1009-5470.2006.02.013
ZHANG Qiaomin, YU Kefu, SHI Qi, et al. A review of monitoring conservation and management of global coral reefs[J]. Journal of Tropical Oceanography, 2006, 25(2):71-78. doi: 10.3969/j.issn.1009-5470.2006.02.013
[3] Wu S, Zhang X, Yang Z, et al. Spatial and temporal evolution of Cenozoic carbonate platforms on the continental margins of the South China Sea: Response to opening of the ocean basin[J]. Interpretation-A Journal of Subsurface Characterization, 2016, 4(3): 1-19.
[4] Fournier F, Borgomano J, Montaggioni L F. Development patterns and controlling factor of Tertiary carbonate buildups: Insights from high resolution seismic data and well data in Malampaya gas field (offshore Palawan, Philippines)[J]. Sedimentary Geology, 2005, 175(1-4): 189-215. doi: 10.1016/j.sedgeo.2005.01.009
[5] Steuer S, Frane D, Meresse F, et al. Oligocene-Miocene carbonates and their role for constraining the rifting and collision histroy of the Dangerous Grouds, South China Sea[J]. Marine and Petroleum Geology, 2013, 58: 1-14. https://www.researchgate.net/publication/259512283_Oligocene-Miocene_carbonates_and_their_role_for_constraining_the_rifting_and_collision_history_of_the_Dangerous_Grounds_South_China_Sea
[6] Fyhn M, Nielsen L, Boldreel L, et al. Geological evolution, regional perspectives and hydrocarbon potential of the northwest Phu Khanh Basin, offshore Central Vietnam[J]. Marine and Petroleum Geology, 2009, 26: 1-24. doi: 10.1016/j.marpetgeo.2007.07.014
[7] Shao L, Li Q, Zhu W, et al. Neogene carbonate platform development in the NW South China Sea: Litho-, bio- and chemo-stratigraphic evidence[J]. Marine Geology, 2017, 385: 233-243. doi: 10.1016/j.margeo.2017.01.009
[8] Wu S, Yang Z, Wang D, et al. Architecture, development and geological control of the Xisha carbonate platforms, northwestern South China Sea[J]. Marine Geology, 2014, 350: 71-83. doi: 10.1016/j.margeo.2013.12.016
[9] Zhao Q, Wu S, Xu H, et al. Sedimentary facies and evolution of aeolianites on Shidao Island, Xisha Islands[J]. Chinese Journal of Oceanology and Limnology, 2011, 29(2):398-413. doi: 10.1007/s00343-011-0018-6
[10] 周小康, 汪瑞良, 曾驿, 等.珠江口盆地东沙隆起珠江组碳酸盐岩层序地层及沉积模式[J].石油天然气学报, 2011, 33(9): 1-6. doi: 10.3969/j.issn.1000-9752.2011.09.001
ZHOU Xiaokang, WANG Ruiliang, ZENG Yi, et al. Carbonate sequence stratigraphy and sedimentary modes of Dongsha Massif in Pearl River Mouth Basin[J]. Journal of Oil and Gas Technology, 2011, 33(9): 1-6. doi: 10.3969/j.issn.1000-9752.2011.09.001
[11] Chen D, Wu S, Dong D, et al. Focused fluid flow in the Baiyun Sag, northern South China Sea: implications for the source of gas in hydrate reservoirs[J]. Chinese Journal of Oceanology and Limnology, 2013, 31(1):178-189. doi: 10.1007/s00343-013-2075-5
[12] Swart P, Carling P. Editorial: Citations and other musings[J]. Sedimentology, 2008, 55(5): 1115-1116. doi: 10.1111/j.1365-3091.2008.01000.x
[13] 魏喜, 邓晋福, 谢文彦, 等.南海盆地演化对生物礁的控制及礁油气藏潜力分析[J].地学前缘, 2005, 12(3): 245-252. doi: 10.3321/j.issn:1005-2321.2005.03.026
WEI Xi, DENG Jinfu, XIE Wenyan et al. Constraints on biogenetic reef formation during evolution of the South China Sea and exploration potential nalysis[J]. Earth Science Frontiers, 2005, 12(3): 245-252. doi: 10.3321/j.issn:1005-2321.2005.03.026
[14] 张功成, 赵志刚, 柳永杰.北部湾盆地伸展构造对油气聚集的控制作用[C].中国石油地质年会, 2009.
http://www.wanfangdata.com.cn/details/detail.do?_type=conference&id=7225783 ZHANG Gongcheng, ZHAO Zhigang, LIU Yongjie. Characteristics of fault structure and it control on hydrocarbons in the Beibuwan Basin[C]. CAPG annual meeting, 2009.
[15] 朱伟林, 张功成, 钟锴, 等.中国南海油气资源前景[J].中国工程科学, 2013, 12(5): 46-50. http://d.old.wanfangdata.com.cn/Periodical/zggckx201005007
ZHU Werlin, ZHANG Gongcheng, ZHONG Kai, et al. South China Sea: Oil and gas outlook[J]. Engineering Sciences, 2013, 12(5): 46-50. http://d.old.wanfangdata.com.cn/Periodical/zggckx201005007
[16] 范嘉松.中国生物礁与油气[M].北京:科学出版社, 1996: 329.
FAN Jiasong. China Reefs, Oil and Gas[M]. Beijing: Science Press, 1996: 329.
[17] Story C, Peng P, Heubeck C, et al. An integrated geoscience and reservoir simulation study of the Liuhua 11-1 Field: South China Sea[C]//In 32nd Annual Offshore Technology Conference Transactions, Houston, 2000: 1-11.
https://www.researchgate.net/publication/249856885_An_integrated_study_of_the_Liuhua_11-1_Field_using_an_ultra_high_resolution_3D_seismic_dataset_South_China_Sea [18] Wilson M E J. Cenozoic carbonates in Southeat Asia: Implications for equatorial carbonate development[J]. Sedimentary Geology, 2002, 147: 295-428. doi: 10.1016/S0037-0738(01)00228-7
[19] Betzler C, Lindhorst S, Eberli G P, et al. Periplatform drift: The combined result of contour current and off-bank transport along carbonate platforms[J]. Geology, 2014, 42: 871-874. doi: 10.1130/G35900.1
[20] Willams T D, Kroon S, Spezzaferri. Middle-upper-Miocene cyclostratigraphy of downhole logs and short to long term astronomical cycles in carbonate production of Great Bahama Bank[J]. Marine Geology, 2002, 185:75-93 doi: 10.1016/S0025-3227(01)00291-2
[21] Harris P M, Purkis S J, Ellis J, et al. Mapping bathymetry and depositional facies on Great Bahama Bank[J]. Sedimentology, 2015, 62(2): 566-589. doi: 10.1111/sed.12159
[22] Jorry S J, Camoin G F, Jouet G, et al. Modern sediments and Pleistocene reefs from isolated carbonate platforms (Iles Eparses, SW Indian Ocean): A preliminary study[J]. Acta Oecol, 2016, 72: 129-143. doi: 10.1016/j.actao.2015.10.014
[23] Saqab M M, Bourget J. Seismic geomorphology and evolution of early-mid Miocene isolated carbonate build-ups in the Timor Sea, North West Shelf of Australia[J]. Marine Geology, 2016, 379: 224-245. doi: 10.1016/j.margeo.2016.06.007
[24] 何起祥, 张明书, 业治铮, 等.西沙群岛石岛晚更新世碳酸盐沉积物的稳定同位素地层学[J].海洋地质与第四纪地质, 1986, 3(3): 3-10. http://d.old.wanfangdata.com.cn/Conference/108093
HE Qixiang, ZHANG Mingshu, YE Zhizheng, et al. Carbonand oxygen stable isotope stratigraphy of late Pleistocene carbonate deposits at Shidao island, Xisha island, Chna[J]. Marine Geology & Quaternary Geology, 1986, 3(3): 3-10. http://d.old.wanfangdata.com.cn/Conference/108093
[25] Yi L, Jian Z, Liu X, et al. Astronical tuning and magnetostratigraphy of Neogene biogenic reefs in the Xisha Islands, South China Sea[J]. Science Bulletin, 2018, 63: 564-573. doi: 10.1016/j.scib.2018.04.001
[26] Zhu W L, Xie X N, Wang Z F, et al. New insights on the origin of the basement of the Xisha Uplift, South China Sea[J]. Science China Earth Science, 2017, 60: 2214-2222. doi: 10.1007/s11430-017-9089-9
[27] 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
[28] Cullen A, Reemst P, Henstra G, et al. Rifting of the South China Sea: new perspectives[J]. Petroleum Geoscience, 2010, 16(3): 273-282. doi: 10.1144/1354-079309-908
[29] Franke D, Savva D, Pubellier M, et al. The final rifting evolution in the South China Sea[J]. Marine and Petroleum Geology, 2014, 43: 63-87. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=84cf03738e5f31266e5d95ad8bc9642d
[30] Hayes D E, Nissen S S. The South China sea margins: Implications for rifting contrasts[J]. Earth & Planetary Science Letters, 2005, 237(3): 601-616. https://www.researchgate.net/publication/222827346_The_South_China_Sea_margins_Implications_for_rifting_contrasts
[31] Li C, 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, 2015, 15(12): 4958-4983. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=10.1002/2014GC005567
[32] Taylor B, Hayes D E. Origin and history of the South China Sea[C]//In Hayes D E (Ed.).The tectonics and geological evolution of Southeast Asia Seas and islands, Part 2. American Geophysical Union Monograph, 1983, 27: 23-56.
https://www.researchgate.net/publication/258928283_Origin_and_History_of_the_South_China_Sea_Basin [33] Morley R. Correlation across the South China Sea Using VIM Transgressive-Regressive Cycles[C]// American Association of Petroleum Geologists Workshop on Southchina Sea Kota Kinabalu May, 2015.
[34] Clift P, Lin J. Preferential mantle lithospheric extension under the South China margin[J]. Marine & Petroleum Geology, 2001, 18(8): 929-945. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=224f4679ff8f8be29b5644a4ab57502d
[35] Franke D, Savva D, Pubellier M, et al. The final rifting evolution in the South China Sea[J]. Marine & Petroleum Geology, 2014, 58: 704-720.
[36] 李家彪.南海大陆边缘动力学:科学实验与研究进展[J].地球物理学报, 2011, 54(12): 2993-3003. doi: 10.3969/j.issn.0001-5733.2011.12.002
LI Jiabiao. Dynamics of the continental margins of South China Sea: scientific experiments and research progress[J]. Chinese J. Geophysics, 2011, 54(12): 2993-3003. doi: 10.3969/j.issn.0001-5733.2011.12.002
[37] Ding W, Li J, Clift P D. 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
[38] Gao J, Wu S, Mcintosh K, et al. Crustal structure and extension mode in the northwestern margin of the South China Sea[J]. Geochemistry Geophysics Geosystems, 2016, 17(6): 2143-2167. doi: 10.1002/2016GC006247
[39] Reston. The extension discrepance at North Atlantic non-volcanic rifted margins: depth dependent stretching or unrecognized fault?[J]. Geology, 2007, 35: 367-370. doi: 10.1130/G23213A.1
[40] Sun Z, Zhong Z, 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(4): 544-556. doi: 10.1016/j.jseaes.2008.09.002
[41] Hutchison C S. Marginal basin evolution: the south Southern China Sea[J]. Marine & Petroleum Geology, 2004, 21: 1129-1148. http://d.old.wanfangdata.com.cn/Periodical/zgsykt200702005
[42] Savva D, Pubellier M, Franke D, et al. Different expressions of rifting on the South China Sea margins[J]. Marine & Petroleum Geology, 2014, 58: 579-598. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=e4907d54982ff67ebaba3b3aba3c59d2
[43] Steuer S, Franke D, Meresse F, et al. Using Oligocene to Pliocene limestone formations to constrain the collision history of Palawan Island and the Dangerous Grounds at the southeastern margin of the South China Sea[C]// Petroleum Geology and Exploration of Palawan and Surrounding areas. 2014.
https://www.sciencedirect.com/science/article/pii/S136791201300031X [44] Bai Y, Wu S, Liu Z, et al. Full-fit reconstruction of the South China Sea conjugate margins[J]. Tectonophysics, 2015, 661: 121-135. doi: 10.1016/j.tecto.2015.08.028
[45] Fan J K, Wu S G. P-wave seismic tomography of the Manila subduction zone[J]. Chinese Journal of Geophysics, 2014, 57(7): 2127-2137. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ad92b788851e03301c42b39ad2a450ab
[46] Wu J, Suppe J. Proto-South China Sea plate tectonics using subducted slab constraints from tomography[J]. Journal of Earth Science, 2017(B4):1-15. http://d.old.wanfangdata.com.cn/Periodical/dqkx-e201806002
[47] Rudolph K W, Lehmann P J. Platform evolution and sequence stratigraphy of the Natuna Platform, South China Sea[M]// Controls on Carbonate Platforms and Basin Development. 1987: 353-361.
[48] Williams, Harold H. Play concepts-northwest Palawan, Philippines[J]. Journal of Southeast Asian Earth Sciences, 1997, 15(2-3): 251-273. doi: 10.1016/S0743-9547(97)00011-1
[49] 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, 2002, 16(2): 113-117. http://d.old.wanfangdata.com.cn/Periodical/zghsyq-dz200202008
YAO Yongjian, JIANG Yukun, ZENG Xianghui. Cenozoic tectonic movements in Nansha area, South China Sea[J], China Offshore Oll and Gas(Geology), 2002, 16(2): 113-117. http://d.old.wanfangdata.com.cn/Periodical/zghsyq-dz200202008
[50] Zampetti V, Schlager W. Architecture and growth history of a Miocene carbonate platform from 3D seismic reflection data, Luconia province, off shore Sarawak, Malaysia[J]. Marine and Petroleum Geology, 2004, 21: 517-534. doi: 10.1016/j.marpetgeo.2004.01.006
[51] Sattler U, Zampetti V, Schlager W, et al. Late Leaching under deep burial conditions: a case study from the Miocene Zhujiang Carbonate Reservoir, South China Sea[J]. Marine and Petroleum Geology, 2004, 21(8): 977-992. doi: 10.1016/j.marpetgeo.2004.05.005
[52] 朱伟林, 张功成, 杨少坤, 等.南海北部大陆边缘盆地天然气地质[M].北京:石油工业出版社, 2007: 391.
ZHU Weilin, ZHANG Gongcheng, YANG Shaokun, et al. Gas geology of continental margin basins in Northern South China Sea[M]. Beijing: Petroleum Industry Press, 2007:391.
[53] 杜学斌, 陆永潮, 裴建祥, 等.南海南部礼乐盆地上渐新统-下中新统生物礁生长模式及分布规律[J].海洋地质与第四纪地质, 2018, 38(6):85-94.
DU Xuebin, LU Yongchao, PEI Jianxiang, et al. The characteristics and distribution of Upper Oligocene to Lower Miocene reefs in Liyue Basin, South China Sea[J]. Marine Geology & Quaternary Geology, 2018, 38(6):85-94
[54] 鄢伟, 张光学, 张莉, 等.南海北康盆地碳酸盐台地的地震响应及分布特征[J].海洋地质与第四纪地质, 2018, 38(6):105-113.
YAN Wei, ZHANG Guangxue, ZHANG Li, et al. The seismic response and distribution characteristics of the Middle Miocene carbonate platform in Beikang Basin of the southern South China Sea[J]. Marine Geology & Quaternary Geology, 2018, 38(6):105-113.
[55] 王彬, 吴时国, 吕福亮, 等.南海中建岛礁的地震反射特征及其沉积演化研究[J].海洋地质与第四纪地质, 2018, 38(6):18-24.
WANG Bin, WU Shiguo, LV Fuliang, et al. Seismic Reflect Characteristics and Evolution of Sedimentary at Zhongjian Ree, South China Sea[J], Marine Geology & Quaternary Geology, 2018, 38(6):18-24.
[56] 周小康, 卫哲, 傅恒, 等.南海北部珠江口盆地深水区碳酸盐岩发育特征及地震识别[J].海洋地质与第四纪地质, 2018, 38(6):123-135. http://www.cnki.com.cn/Article/CJFDTotal-HYDZ201806014.htm
ZHOU Xiaokang, WEI Zhe, FU heng, et al. Development characteristics and seismic identification of carbonate rocks in the deep-water area of the Pearl River Mouth Basin in the northern South China Sea[J]. Marine Geology & Quaternary Geology, 2018, 38(6):123-135. http://www.cnki.com.cn/Article/CJFDTotal-HYDZ201806014.htm
[57] 杨朝云, 韩孝辉, 冯亚坤, 等.西沙海区宣德环礁的地震层序发育特征[J].海洋地质与第四纪地质, 2018, 38(6):25-36. http://www.cnki.com.cn/Article/CJFDTotal-HYDZ201806003.htm
YANG Chaoyun, HAN Xiaohui, FENG Yakun, et al. Seismic Sequence Development Characteristics of Xuande Atoll, Xisha Area[J]. Marine Geology & Quaternary Geology, 2018, 38(6):25-36. http://www.cnki.com.cn/Article/CJFDTotal-HYDZ201806003.htm
[58] Betzler C, Fürstenau J, Lüdmann T, et al. Sea-level and ocean-current control on carbonate-platform growth, Maldives, Indian Ocean[J]. Basin Research, 2013, 25(2):172-196. doi: 10.1111/j.1365-2117.2012.00554.x
[59] Christian B, Eberli G P, Dick K, et al. The abrupt onset of the modern South Asian Monsoon winds[J]. Scientific Reports, 2016, 6:29838. doi: 10.1038/srep29838
[60] Wan S, Li A, Clift P D, et al. Development of the East Asian monsoon: Mineralogical and sedimentologic records in the northern South China Sea since 20Ma[J]. Palaeogeography Palaeoclimatology Palaeoecology, 2007, 254(3):561-582.
[61] Zhao Quanhong, Jian Zhimin, Wang Jiliang, et al. Neogene oxygen isotopic stratigraphy, ODP Site 1148, northern South China Sea[J]. Science China Earth Sciences, 2001, 44(10):934-942. doi: 10.1007/BF02907086
[62] Bosence D. A genetic classification of carbonate platforms based on their basinal and tectonic settings in the Cenozoic[J]. Sedimentary Geology, 2005, 175: 49-72. doi: 10.1016/j.sedgeo.2004.12.030
[63] Purser B H. Syn-rift diagenesis of Middle Miocene carbonate platforms on the north-western Red Sea coast, Egypt[J]. 1998.
https://link.springer.com/chapter/10.1007%2F978-94-011-4930-3_20 [64] Lü C L, Wu S G, Yao Y, et al. Development and controlling factors of Miocene carbonate platform in the Nam Con Son Basin, Southwestern South China Sea[J]. Marine and Petroleum Geology, 2013, 45: 55-68. doi: 10.1016/j.marpetgeo.2013.04.014
[65] 吕炳全, 徐国强, 王红罡, 等.南海新生代碳酸盐台地淹没事件纪录的海底扩张[J].地质科学, 2002, 37(4): 405-414. doi: 10.3321/j.issn:0563-5020.2002.04.003
LV Binquan, XU Guoqiang, WANG Hongzheng, et al. Sea floor spreading recorded by drowning events of Cenozoic carbonate platforms in the South China Sea[J]. Chinese journal of geology, 2002, 37(4): 405-414. doi: 10.3321/j.issn:0563-5020.2002.04.003
[66] 徐国强, 吕炳全, 王红罡.新生代南海北部碳酸盐台地的淹没事件研究[J], 同济大学学报, 2002, 30(1): 35-40. doi: 10.3321/j.issn:0253-374X.2002.01.007
XU Guoqiang, LV Bingquan, WANG Hongzheng. Drowning events research: insights from Cenozoic carbonate platforms in Northern South China Sea[J]. Journal of Tongji University, 2002, 30(1): 35-40. doi: 10.3321/j.issn:0253-374X.2002.01.007
[67] Wu S, Gao J, Zhao S, et al. Post-rift uplift and focused fluid flow in the passive margin of northern South China Sea[J]. Tectonophysics, 2014, 615: 27-39. https://www.researchgate.net/publication/261013664_Post-rift_uplift_and_focused_fluid_flow_in_the_passive_margin_of_northern_South_China_Sea
[68] Ma Y, Wu S, Lv F, et al. Seismic characteristics and development of the xisha carbonate platforms, northern margin of the South China Sea[J]. Journal of Asian Earth Sciences, 2011, 40(3), 770-783. doi: 10.1016/j.jseaes.2010.11.003
[69] Moldovanyi E P, Wall F M, Zhang J Y. Regional exposure events and platform evolution of Zhujiang Formation carbonates, Pearl River Mouth Basin: Evidence from primary and diagenetic seismic facies[J]. AAPG Memoir, 1995, 63: 125-140.
[70] 施小斌, 丘学林, 夏戡原, 等.南海热流特征及其构造意义[J].热带海洋学报, 2003, 22(2):63-73. doi: 10.3969/j.issn.1009-5470.2003.02.007
SHI Xiaobin, QIU Xuelin, XIA Kanyuan, et al. Heat flow characteristics and its tectonic significance of South China Sea[J]. Journal of Tropical Oceanography, 2003, 22(2):63-73. doi: 10.3969/j.issn.1009-5470.2003.02.007
[71] 徐行, 罗贤虎, 许鹤华, 等.南海地热流探测、研究与展望[J].南海地质研究, 2015:1-18. http://www.cnki.com.cn/Article/CJFDTotal-NHDZ201500001.htm
XU Dai, LUO Xianhu, XU Hehua, et al, Heat flow's detection, research and prospects in South China Sea[J]. Research of Eological South China Sea, 2015:1-18 http://www.cnki.com.cn/Article/CJFDTotal-NHDZ201500001.htm
[72] Lin M, Zhang J. Thermal structure about southwest sub-basin of South China Sea[J]. Earthquake Science, 2011, 24(5):427-436 doi: 10.1007/s11589-011-0805-3
[73] 施小斌, 于传海, 陈梅, 等.南海北部陆缘热流变化特征及其影响因素分析[J].地学前缘, 2017, 24(3):56-64. http://d.old.wanfangdata.com.cn/Periodical/dxqy201703005
SHI Xiaobin, YU Chuanhai, CHEN Mei, et al. Analyses of variation features and influential factors of heat flow in the northern margin of the South China Sea[J]. Earth Science Frontiers, 2017, 24(3): 56-64. http://d.old.wanfangdata.com.cn/Periodical/dxqy201703005
[74] 陈爱华, 徐行, 罗贤虎, 等.南海北康盆地热流分布特征及其构造控制因素探讨[J].地质学报, 2017, 91(8):1720-1728. doi: 10.3969/j.issn.0001-5717.2017.08.005
CHEN Aihua, XU Xing, LUO Xianhu, et al. Heat flow characteristics and controlling factors of Beikang Basin in South China Sea[J], Acta Geological Sinica, 2017, 91(8): 1720-1728. doi: 10.3969/j.issn.0001-5717.2017.08.005
[75] 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(7):2915-2925. http://d.old.wanfangdata.com.cn/Periodical/dqwlxb201807021
XU Hang, YAO Yongjian, PEN Deng, et al. The Characteristics and analysis of heat flow in the Southwest sub-basin of South China Sea[J]. Chinese Journal of Geophysic, 2018(7): 2915-2925. http://d.old.wanfangdata.com.cn/Periodical/dqwlxb201807021
[76] Li Q, Wang P, Zhao Q, et al. A 33 Ma lithostratigraphic record of tectonic and paleoceanographic evolution of the South China Sea[J]. Marine Geology, 2006, 230 (3): 217-235. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=23faff45b02eed9c5929cdc3eab7d69b
[77] Ma B, Wu S, Betzler C, et al. Geometry, internal architecture, and evolution of buried volcanic mounds in the northern South China Sea[J]. Marine and Petroleum Geology, 2018, 97: 540-555. doi: 10.1016/j.marpetgeo.2018.07.029
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