Petroleum Potential Prediction of the Lile Basin in Nansha
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摘要: 礼乐盆地是南沙海域热点研究区域.为揭示该盆地油气资源潜力，依据礼乐盆地地震剖面、钻井及拖网资料，对礼乐盆地的油气成藏控制因素进行综合分析，进而探讨该盆地的油气成藏潜力.中生代和古新世－早渐新世沉积是主要烃源岩；晚渐新世礁体以及中生代风化碎屑岩是主要储层；识别出晚渐新世-早中新世礁体和中生代晚期风化剥蚀而形成的断块构造是最主要的圈闭类型.长期活动断层沟通底部中生代地层和浅层礁体，是主要的油气垂向运移输导体，控制了礼乐盆地油气的空间分布.晚中新世的菲律宾弧碰撞运动类似南海北部东沙运动，有利于排烃和油气运移，之后构造活动减弱，有利于稳定成藏.礼乐盆地具备油气成藏的6大要素条件，盆地中、东部断裂发育区是盆地油气运聚成藏的优势前景区域.Abstract: Lile basin is a hot research spot in Nansha area. We probe into the petroleum potential of Lile basin based on geological and geophysical analysis of seismic profiles, wells and dredging data. All necessary elements for a hydrocarbon accumulation are analyzed in the basin. We suggest that the Mesozoic to early Cenozoic sediments are the major source rock. Potential reservoirs include the late Oligocene reefs and Mesozoic aerated layer. The principal play-types recognized in the basin are the Late Oligocene to Early Miocene reefs and erosional Mesozoic faulted blocks. Long term active faults connect the Mesozoic source rock and shallow layer play, so the faults are major transport channel and control the spatial distribution of hydrocarbon reservoir. Similar to the Dongsha movement in the northern of South China Sea, Late Miocene tectonic event was good for hydrocarbon migration. The attenuated tectonic movement thereafter benefited the hydrocarbon accumulation.
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Key words:
- Lile basin /
- fault /
- Mesozoic /
- hydrocarbon accumulation /
- petroleum potential /
- petroleum geology
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图 4 礼乐盆地地层柱状图(Sales et al., 1997)
Fig. 4. Stratigraphic column of the Lile basin
图 5 Sampaguita-1井和Aboabo-1井柱状图(Taylor and Hayes, 1980)
Fig. 5. Histogram of Sampaguita-1 and Aboabo-1 well
图 6 SO23-31拖网位置剖面及其解释剖面(Hinz and Schluter, 1985)(位置见图 1)
Fig. 6. Seismic and its interpreted profiles for dredge at SO23-31
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[1] 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, 98(B4): 6299-6328. doi: 10.1029/92JB02280 [2] Fontaine, H., Davis, P., Parded, R., et al., 1983. Marine Jurassic in Southeast Asia. CCOP Technical Bulletin, 16: 3-30. [3] Guo, Z.Q., Xiao, D.M., Tang, J.S., 1996. Function of discordogenic faults during forming of hydrocarbon pools. Acta Petrolei Sinica, 17(3): 27-32 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-SYXB603.003.htm [4] Hall, R., 2002. Cenozoic geological and plate tectonic evolution of SE Asia and the SW Pacific: computer-based reconstructions, model and animations. Journal of Asian Earth Sciences, 20(4): 353-431. doi: 10.1016/S1367-9120(01)00069-4 [5] Hinz, K., Schluter, 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(3-4): 297-315. doi: 10.1016/0360-5442(85)90048-9 [6] Holloway, N.H., 1982. North Palawan block Philippines—its relation to Asian mainland and role in evolution of South China Sea. AAPG Bulletin, 66(9): 1355-1383. [7] Hutchison, C.S., 2004. Marginal basin evolution: the southern South China Sea. Marine and Petroleum Geology, 21(9): 1129-1148. doi: 10.1016/j.marpetgeo.2004.07.002 [8] Jin, Q.H., Li, T.G., 2000. Regional geologic tectonics of the Nansha sea area. Marine Geology and Quaternary Geology, 20(1): 1-8 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HYDZ200001000.htm [9] Klemme, H.D., Ulmishek, G.F., 1991. Effective petroleum source rocks of the world: stratigraphic distribution and controlling depositional factors. AAPG Bulletin, 75(12): 1809-1851. doi: 10.1306/0C9B2A47-1710-11D7-8645000102C1865D [10] Kudrass, H.R., Wiedicke, M., Cepeck, P., et al., 1986. Mesozoic and Cenozoic rocks dredged from the South China Sea (Reed Bank area) and Sulu sea and their significance for plate-tectonic reconstructions. Marine and Petroleum Geology, 3(1): 19-30. doi: 10.1016/0264-8172(86)90053-X [11] Sales, A.O., Jacobsen, E.C., Morado, A.A., et al., 1997. The petroleum potential of deep-water Northwest Palawan block GSEC 66. Journal of Asian Earth Science, 15(2-3): 217-240. doi: 10.1016/S0743-9547(97)00009-3 [12] Schlueter, H.U., Hinz, K., Block, M., 1996. Tectono-stratigraphic terranes and detachment faulting of the South China Sea and Sulu sea. Marine Geology, 130(1-2): 39-78. doi: 10.1016/0025-3227(95)00137-9 [13] Shao, L., You, H.Q., Hao, H.J., et al., 2007. Petrology and depositional environments of Mesozoic strata in the northeastern South China Sea. Geological Review, 53(2): 164-169 (in Chinese with English abstract). http://www.researchgate.net/publication/284609950_Petrology_and_depositional_environments_of_Mesozoic_strata_in_the_northeastern_South_China_Sea [14] Sun, L.T., Sun, Z., Zhou, D., et al., 2008. Stratigraphy and structure of Lile basin in Nansha area. Geotectonica et Metallogenia, 32(2): 151-158 (in Chinese with English abstract). http://www.researchgate.net/publication/301346686_Stratigraphic_and_structural_characteristics_of_Lile_basin_in_Nansha_area [15] Sun, Z., Zhou, D., Zhong, Z.H., et al., 2006. Research on the dynamics of the South China Sea opening: evidence from analogue modeling. Science in China (Ser. D), 49(10): 1053-1069. doi: 10.1007/s11430-006-1053-6 [16] Sun, Z., Sun, L.T., Zhou, D., et al., 2009. Discussion on the South China Sea evolution and lithospheric breakup through 3D analogue modeling. Earth Science—Journal of China University of Geosciences, 34(3): 435-447 (in Chinese with English abstract). doi: 10.3799/dqkx.2009.049 [17] Taylor, B., Hayes, D.E., 1980. The tectonic evolution of the South China Sea basin. In: Hayes, D.E., ed., The tectonic and geologic evolution of southeast Asian seas and islands. Geophys Monogr Set. 23, AGU, Washington, D.C. . [18] Taylor, B., Hayes, D.E., 1983. Origin and history of the South China Sea Basin. In: Hayes, D.E., ed., The tectonic and geologic evolution of Southeast Asian seas and islands, Part 2. Geophys Monogr Set., 27, AGU, Washington, D.C. . [19] Xia, K.Y., Huang, C.L., 2000. The discovery of Meso-Tethys sedimentay basins in the South China Sea and their oil and gas perspective. Earth Science Frontiers, 7(3): 227-238 (in Chinese with English abstract). http://www.researchgate.net/publication/285504858_The_discovery_of_Meso-Tethys_sedimentary_basins_in_the_South_China_Sea_and_their_oil_and_gas_perspective [20] Yan, P., Liu, H.L., 2004. Tectonic-stratigraphic division and blind fold structures in Nansha waters, South China Sea. Journal of Asian Earth Sciences, 24(3): 337-348. doi: 10.1016/S0040-1951(01)00062-2 [21] Yan, P., Liu. H.L., Deng, H., 2005. Characteristics of the Paleogene deposits in Nansha waters and their relations to the petroleum potertial. Geotectonica et Metallogenia, 29 (3): 391-402 (in Chinese with English abstract). http://epub.cnki.net/grid2008/docdown/docdownload.aspx?filename=DGYK200503016&dbcode=CJFD&year=2005&dflag=pdfdown [22] Yao, B.C., Wan, L., Liu, Z.H., 2004. Tectonic dynamics of Cenozoic sedimentary basins and hydrocarbon resources in the South China Sea. Earth Science—Journal of China University of Geosciences, 29(5): 543-549 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200405006.htm [23] 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), 16(2): 113-118 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZHSD200202009.htm [24] Zhang, L., Li, W.C., Zeng, X.H., 2003. Stratigraphic sequence and hydrocarbon potential in Lile basin. Petroleum Geology and Experiment, 25(5): 469-573 (in Chinese with English abstract). http://www.researchgate.net/publication/313526366_Stratigraphic_sequence_and_hydrocarixn_potential_in_Lilt_basinJ [25] Zhou, D., Ru, K., Chen, H.Z., 1995. Kinematics of Cenozoic extension on the South China Sea continental margin and its implications for the tectonic evolution of the region. Tectonophysics, 251(1-4): 161-177. doi: 10.1016/0040-1951(95)00018-6 [26] Zhou, D., 2002. Mesozoic strata and sedimentary environment in SW Taiwan basin of NE South China Sea and Peikang high of western Taiwan. Journal of Tropical Oceanography, 21(2): 50-57 (in Chinese with English abstract). http://www.zhangqiaokeyan.com/academic-journal-cn_journal-tropical-oceanography_thesis/0201252198648.html [27] 郭占谦, 萧德铭, 唐金生, 1996. 深大断裂在油气藏形成中的作用. 石油学报, 17(3): 27-32. doi: 10.3321/j.issn:0253-2697.1996.03.004 [28] 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. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200001000.htm [29] 邵磊, 尤洪庆, 郝沪军, 等, 2007. 南海东北部中生界岩石学特征及沉积环境. 地质论评, 53(2): 164-169. doi: 10.3321/j.issn:0371-5736.2007.02.003 [30] 孙龙涛, 孙珍, 周蒂, 等, 2008. 南沙海区礼乐盆地沉积地层与构造特征分析. 大地构造与成矿学, 32(2): 151-158. doi: 10.3969/j.issn.1001-1552.2008.02.003 [31] 孙珍, 孙龙涛, 周蒂, 等, 2009. 南海岩石圈破裂方式与扩张过程的三维物理模拟. 地球科学——中国地质大学学报, 34(3): 435-447. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200903008.htm [32] 夏戡原, 黄慈流, 2000. 南海中生代特提斯期沉积盆地的发现与找寻中生代含油气盆地的前景. 地学前缘, 7(3): 227-238. doi: 10.3321/j.issn:1005-2321.2000.03.021 [33] 阎贫, 刘海龄, 邓辉, 2005. 南沙地区下第三系沉积特征及其与含油气性的关系. 大地构造与成矿学, 29(3): 391-402. doi: 10.3969/j.issn.1001-1552.2005.03.015 [34] 姚伯初, 万玲, 刘振湖, 2004. 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. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200405006.htm [35] 姚永坚, 姜玉坤, 曾祥辉, 2002. 南沙海域新生代构造运动特征. 中国海上油气(地质), 16(2): 113-118. https://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD200202009.htm [36] 张莉, 李文成, 曾祥辉, 2003. 礼乐盆地地层发育特征及其与油气的关系. 石油实验地质, 25(5): 469-573. doi: 10.3969/j.issn.1001-6112.2003.05.009 [37] 周蒂, 2002. 台西南盆地和北港隆起的中生界及其沉积环境. 热带海洋学报, 21(2): 50-57. doi: 10.3969/j.issn.1009-5470.2002.02.006 -
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