南海北部深水区白云凹陷地温—地压系统特征及其石油地质意义

郭志峰; 刘震; 王伟; 张功成; 沈怀磊

doi:10.3799/dqkx.2011.086

Volume 36 Issue 5

Sep. 2011

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Article Navigation > Earth Science > 2011 > 36(5): 831-836

GUO Zhi-feng, LIU Zhen, WANG Wei, ZHANG Gong-cheng, SHEN Huai-lei, 2011. Characteristics of Geotemperature-Pressure Systems and Their Implications for Petroleum Geology at Baiyun Depression, Deep-Water Area of Northern South China Sea. Earth Science, 36(5): 831-836. doi: 10.3799/dqkx.2011.086

Citation:

GUO Zhi-feng, LIU Zhen, WANG Wei, ZHANG Gong-cheng, SHEN Huai-lei, 2011. Characteristics of Geotemperature-Pressure Systems and Their Implications for Petroleum Geology at Baiyun Depression, Deep-Water Area of Northern South China Sea. Earth Science, 36(5): 831-836. doi: 10.3799/dqkx.2011.086

Citation:

GUO Zhi-feng, LIU Zhen, WANG Wei, ZHANG Gong-cheng, SHEN Huai-lei, 2011. Characteristics of Geotemperature-Pressure Systems and Their Implications for Petroleum Geology at Baiyun Depression, Deep-Water Area of Northern South China Sea. Earth Science, 36(5): 831-836. doi: 10.3799/dqkx.2011.086

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Characteristics of Geotemperature-Pressure Systems and Their Implications for Petroleum Geology at Baiyun Depression, Deep-Water Area of Northern South China Sea

doi: 10.3799/dqkx.2011.086

1.
State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing 102249, China
2.
Research Institute of China National Offshore Oil Corporation, Beijing 100027, China

Received Date: 2011-05-20
Publish Date: 2011-09-15

Abstract

Abstract

Baiyun depression is characterized by high geotemperature and high pressure formation.By theory of geotemperature-pressure system, the geotemperature, formation pressure and geotemperature-pressure system at Baiyun depression and their relationships with hydrocarbon distribution are analyzed in vertical and lateral sections.Research shows that overpressure composite geotemperature-pressure system develops at Baiyun depression, namely normal geotemperature-pressure system of shallow zone and overpressure system of deep zone.Based on coupling characteristics of geotemperature and pressure, Baiyun depression is divided into six geotemperature-pressure system divisions.The northern slope belt is located in the area with high temperature and normal pressure, as well as high temperature and high pressure.The main sag is mainly located in the area with ultra high temperature and high pressure, and the center belt belongs to ultra high temperature and ultra high pressure region.The southern slope belt is located in the area with high temperature and high pressure.Natural gas pools are mainly distributed in relative low energy area.The special characteristics of geotemperature-pressure system at Baiyun depression provide strong power for hydrocarbon migration, and control the distribution of oil and gas reservoirs.
- deep-water area of northern South China Sea,
- marine geophysics,
- petroleum geology,
- geotemperature-pressure system,
- distribution of hydrocarbon

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References(38)

References

[1]	Barker, C., 1972. Aquathermal pressuring: role of temperature in development of abnormal pressure zones. AAPG Bulletin, 56(10): 2068-2071. http://aapgbull.geoscienceworld.org/content/56/10/2068
[2]	Hao, F., 2005. Kinetics of hydrocarbon generation and mechanisms of petroleum accumulation in overpressure basins. Science Press, Beijing (in Chinese).
[3]	Hao, F., Zou, H. Y., Fang, Y., et al., 2006. Kinetics of organic matter maturation and hydrocarbon generation inoverpressure environment. Acta Petrolei Sinica, 27(5): 9-18 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYXB200605001.htm
[4]	Hunt, J. M., 1990. Generation and migration of petroleum from abnormally pressured fluid compartment. AAPG Bulletin, 74: 1-12. http://archives.datapages.com/data/meta/bulletns/1990-91/images/pg/00750002/0000/03280_firstpage.pdf
[5]	Jin, B., Liu, Z., Li, X. S., et al., 2008. Relationship between accumulation of natural gas and geotemperature-geopressure system in Yinggehai basin. Natural Gas Geoscince, 19(1): 49-55 (in Chinese with English abstract). http://www.nggs.ac.cn/CN/article/downloadArticleFile.do?attachType=PDF&id=1246
[6]	Liu, F. N., Yang, J. H., Wen, W. M., 1994. The geopressure field and its relation to petroleum migration in Qiongdongnan basin. China Offshore Oil and Gas (Geology), 8(6): 363-376 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZHSD199406000.htm
[7]	Liu, J. R., Qin, J. S., Wu, X. D., 2001. Experimental study on relation between temperature and rocky permeability. Journal of the University of Petroleum, China, 25(4): 51-53 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYDX200104015.htm
[8]	Liu, Z., Dai, L. C., Zhao, Y., et al., 2005. Characteristics of geotemperature-pressure systems and their controlling functions on pools' distribution in the Jiyang depression. Chinese Journal of Geology, 40(1): 1-15 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKX200501000.htm
[9]	Liu, Z., He, W. Y., Han, J., et al., 2000. Relation of geotemperature-formation pressure systems with migration and accumulation of petroleum in the east of Junggar basin. Journal of the University of Petroleum, China, 24(4): 15-20 (in Chinese with English abstract). http://www.researchgate.net/publication/293268900_Relation_of_geotemperature-formation_pressure_systems_with_migration_and_accumulation_of_petroleum_in_the_east_of_Junggar_basin
[10]	Liu, Z., Zeng, X. B., Zhang, W. X., et al., 1997. Relation between subsurface temperatures and formation pressures in sedimentary basins. Acta Geologica Sinica, 71(2): 180-185 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/ http://search.cnki.net/down/default.aspx?filename=DZXE199702009&dbcode=CJFD&year=1997&dflag=pdfdown
[11]	Liu, Z., Zhao, Y., Liang, Q. S., et al., 2007. Formation and enrichment of subtle reservoir. Geological Publishing, Beijing, 3-14 (in Chinese).
[12]	Ma, Q. F., Chen, S. Z., Zhang, Q. M., et al., 2000. Overpressure basin and hydrocarbon distribution. Geological Publishing, Beijing, 3-4 (in Chinese).
[13]	Mi, L. J., Yuan, Y. S., Zhang, G. C., et al., 2009. Characteritics and genesis of geothermal field in deep water area of the northern South China Sea. Acta Petrolei Sinica, 30(1): 27-32 (in Chinese with English abstract). http://www.researchgate.net/profile/Shengbiao_Hu/publication/279599733_Characteristics_and_genesis_of_geothermal_field_in_deep-water_area_of_the_northern_South_China_Sea/links/56a1ad2c08ae27f7de267873.pdf
[14]	Pusey, W. C., 1973. How to evaluate potential gas and oilsource rocks? World Oil, 176(5): 71-75. http://gateway.proquest.com/openurl?res_dat=xri:pqm&ctx_ver=Z39.88-2004&rfr_id=info:xri/sid:baidu&rft_val_fmt=info:ofi/fmt:kev:mtx:article&genre=article&jtitle=World%20Oil&atitle=How%20to%20evaluate%20potential%20gas%20and%20oil%20source%20rocks.
[15]	Shi, W. Z., Chen, H. H., Chen, C. M., et al., 2006. Modelling of pressure evolution and hydrocarbon migration in Baiyun depression, Pearl River Mouth basin, China. Earth Science—Journal of China University of Geosciences, 31(2): 229-236 (in Chinese with English abstract). http://www.cqvip.com/QK/94035X/2006002/21402864.html
[16]	Somerton, W. H., Mehta, M. M., Dean, G. W., 1965. Thermal alteration of sandstones. Journal of Petroleum Technology, 17(5): 589-593. doi: 10.2118/907-PA.
[17]	Xiao, H. Q., Liu, Z., Zhao, Y., et al., 2003. Characteristics of geotemperature and geopressure fields in the Jiyang depression and their significance petroleum geology. Petroleum Exploration and Development, 30(3): 68-70 (in Chinese with English abstract). http://www.researchgate.net/publication/288927556_Characteristics_of_geotemperature_and_geopressure_fields_in_the_Jiyang_Depression_and_their_significance_of_petroleum_geology
[18]	Yang, J. H., 1999. Influence of geothermal-geopressure field on the migration and accumulation of nature gas in Ying-Qiong basin. Nature Gas Industry, 19(1): 39-43 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-TRQG901.010.htm
[19]	Ye, J. R., Yang, X. H., 2001. Thermal fluid flow in sedimentary basins and its significance to pool-forming dynamics. Acta Sedimentologica Sinica, 19(2): 214-218 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CJXB200102008.htm
[20]	Zhang, G. C., Mi, L. J., Wu, S. G., et al., 2007. Deepwater area: the prospecting targets of northern continental margin of South China Sea. Acta Petrolei Sinica, 28(2): 15-21 (in Chinese with English abstract). http://www.researchgate.net/publication/279551230_Deepwater_area_-_The_new_prospecting_targets_of_northern_continental_margin_of_South_China_Sea
[21]	Zhu, G. H., Chen, G., Diao, Y. H., 2000, Characteristics of geotherm-pressure field and its relationship with hydrocarbon migration and accumulation in Qiongdongnan basin, South China Sea. China Offshore Oil and Gas (Geology), 14(1): 29-36 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZHSD200001005.htm
[22]	郝芳, 2005. 超压盆地生烃作用动力学与油气成藏机理. 北京: 科学出版社.
[23]	郝芳, 邹华耀, 方勇, 等, 2006. 超压环境有机质热演化和生烃作用机理. 石油学报, 27(5): 9-18. doi: 10.3321/j.issn:0253-2697.2006.05.002
[24]	金博, 刘震, 李绪深, 等, 2008. 莺歌海盆地地温—地压系统特征及其对天然气成藏的意义. 天然气地球科学, 19(1): 49-55. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX200801013.htm
[25]	刘福宁, 杨计海, 温伟明, 1994. 琼东南盆地地压场与油气运移. 中国海上油气(地质), 8(6): 363-376. https://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD199406000.htm
[26]	刘均荣, 秦积舜, 吴晓东, 2001. 温度对岩石渗透率影响的实验研究. 石油大学学报, 25(4): 51-53. https://www.cnki.com.cn/Article/CJFDTOTAL-SYDX200104015.htm
[27]	刘震, 戴立昌, 赵阳, 等, 2005. 济阳坳陷地温—地压系统特征及其对油气藏分布的控制作用. 地质科学, 40(1): 1-15. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX200501000.htm
[28]	刘震, 贺维英, 韩军, 等, 2000. 准噶尔盆地东部地温—地压系统与油气运聚成藏的关系. 石油大学学报, 24(4): 15-20. https://www.cnki.com.cn/Article/CJFDTOTAL-SYDX200004003.htm
[29]	刘震, 曾宪斌, 张万选, 等, 1997. 沉积盆地地温与地层压力关系研究. 地质学报, 71(2): 180-185. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE199702009.htm
[30]	刘震, 赵阳, 梁全胜, 等, 2007. 隐蔽油气藏形成与富集. 北京: 地质出版社, 3-14.
[31]	马启富, 陈斯忠, 张启明, 等, 2000. 超压盆地与油气分布. 北京: 地质出版社, 3-4.
[32]	米立军, 袁玉松, 张功成, 等, 2009. 南海北部深水区地热特征及其成因. 石油学报, 30(1): 27-32. doi: 10.3321/j.issn:0253-2697.2009.01.005
[33]	石万忠, 陈红汉, 陈长民, 等, 2006. 珠江口盆地白云凹陷地层压力演化与油气运移模拟. 地球科学——中国地质大学学报, 31(2): 229-236. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200602012.htm
[34]	肖焕钦, 刘震, 赵阳, 等, 2003. 济阳坳陷地温—地压特征及其石油地质意义. 石油勘探与开发, 30(3): 68-70. doi: 10.3321/j.issn:1000-0747.2003.03.019
[35]	杨计海., 1999. 莺—琼盆地温压场与天然气运聚关系. 天然气工业, 19(1): 39-43. doi: 10.3321/j.issn:1000-0976.1999.01.011
[36]	叶加仁, 杨香华, 2001. 沉积盆地热流体活动及其成藏动力学意义. 沉积学报, 19(2): 214-218. doi: 10.3969/j.issn.1000-0550.2001.02.009
[37]	张功成, 米立军, 吴时国, 等, 2007. 深水区——南海北部大陆边缘盆地油气勘探新领域. 石油学报, 28(2): 15-21. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB200702002.htm
[38]	朱光辉, 陈刚, 刁应护, 2000. 琼东南盆地温压场特征及其与油气运聚的关系. 中国海上油气(地质), 14(1): 29-36. doi: 10.3969/j.issn.1673-1506.2000.01.008