伊-陕斜坡山2段包裹体古流体势恢复及天然气聚集条件

刘建章; 陈红汉; 李剑; 胡国艺; 单秀琴; 罗霞

伊-陕斜坡山2段包裹体古流体势恢复及天然气聚集条件

1.
中国地质大学资源学院石油系, 湖北武汉 430074
2.
中国石油勘探开发研究院廊坊分院, 河北廊坊 065007

基金项目:

国家自然科学基金项目 40372068

详细信息

作者简介:
刘建章(1976-), 男, 博士研究生, 主要从事石油地质方面的研究.E-mail: liujzh@126.com

中图分类号: P618.13
计量
- 文章访问数: 3570
- HTML全文浏览量: 90
- PDF下载量: 4
- 被引次数: 0
出版历程
- 收稿日期: 2006-03-11
- 刊出日期: 2007-01-25

Using Fluid Inclusion Thermodynamic Modeling to Study Paleo-Fluid Potential and Natural Gas Migration and Accumulation of the No.2 Member of Shanxi Formation of the Upper Paleozoic in Yi-Shaan Slope, Ordos Basin

1.
Department of Petroleum Geology, Faculty of Earth Resources , China University of Geosciences, Wuhan 430074, China
2.
Langfang Branch of RIPED of Petro China, Langfang 065007, China

摘要

摘要: 恢复自烃类生成以来的各个地史时期的古流体势, 有助于正确认识油气藏的分布规律.通过对鄂尔多斯盆地伊-陕斜坡太原组—山西组砂岩储层流体包裹体样品的系统分析, 将其油气充注划分为6个期次; 结合埋藏史分析, 确定出6期油气充注发生的时间.在此基础上, 运用流体包裹体pVT热动力学模拟的方法, 获得了6期油气充注的古压力数据, 并计算出伊-陕斜坡山2段6期次天然气充注的古气势, 分析了古气势分布及时空演化规律, 认为区域构造和热史演化是其主要控制因素.结合区域地质资料, 探讨了天然气运移与聚集规律: 晚三叠世中期至中侏罗世末期, 山2段储层气势西南高而北部、东北部低, 天然气主要从西南向北、东北向运移; 中侏罗世末期至早白垩世末期, 气势西高东低, 天然气主要由西向东就近运移, 再向北和东北向运移; 早白垩世末至现今, 天然气藏进入聚集与散失的动平衡状态, 形成现今分布特征.榆林及其南部地区是天然气聚集的最有利地带, 其次为神木-米脂地区.
- 鄂尔多斯盆地 /
- 流体包裹体 /
- 古流体势 /
- 油气运移
Abstract: Reconstruction of paleo-fluid potential during each geological period after hydrocarbon generation may be helpful to clearly recognize the hydrocarbon reservoir distribution. In this research, the samples including reservoir fluid from Taiyuan and Shanxi formations of the Upper Paleozoic in Yi-Shaan slope, Ordos basin were obtained, and the systematic analysis of the sample was used to measure the homogenization temperature for all orders of fluid inclusions mainly in trails, salinity for aqueous inclusions and the fluorescence colors for hydrocarbon inclusions. The result indicates that there are six period times of hydrocarbon charging in the sandstone reservoirs, and the gas charging is statistically dominating. By integrating the average homogenization temperatures with burial historical curves, the six charging times are determined. By employing the fluid inclusion pVT thermodynamic modeling, the paleo-formation pressure of these six times of hydrocarbon charging is obtained, and the six periods of paleo-gas potential of No.2 member of Shanxi Formation of the Upper Paleozoic in Yi-Shaan slope are calculated, and the paleo-gas potential distribution and evolution are depicted, and the evolution of regional tectonics and geothermal history are found out to be the main controlling factors. According to the regional geological conditions, the law of the nature gas migration and accumulation of No.2 member of Shanxi Formation of the Upper Paleozoic in Yi-Shaan slope is discussed. From the middle Late Triassic to the late Middle Jurassic, the natural gas mainly migrated from southwest to north, northeast, because the paleo-gas potential in the southwest zone was higher than that in the north and northeast zones; from the late Middle Jurassic to the late Early Cretaceous, the paleo-gas potential in the west zone was higher than that in the east zone and the natural gas migrated eastward and then northeastward; after that, the natural gas accumulation is in equilibrium with dissipation, which results in today's distribution features. The Yulin zone and the southern zone of Yulin have the most important significance to the exploration of the No.2 member of Shanxi Formation of the Upper Paleozoic in Yi-Shaan slope, and secondly to the Shenmu-Mizhi zone.
- the Ordos basin /
- fluid inclusions /
- paleo-fluid potential /
- hydrocarbon migration

HTML全文

图 1 伊-陕斜坡上古生界山2段储层古气势分布与演化

a.第1期: T₃中期—J₁中期; b.第2期: J₁中期—J₂中期; c.第3期: J₂中期—J₂末期; d.第4期: J₂末期—K₁中早期; e.第5期: K₁中早期—K₁中晚期; f.第6期: K₁中晚期—K₁末期

Fig. 1. Map showing the paleo-gas potential distribution and evolution of No.2 member reservoir of Shanxi Formation of the Upper Paleozoic in Yi-Shaan slope, Ordos basin

下载: 全尺寸图片幻灯片

参考文献(32)

[1]	Aplin, A. C., Larter, S. R., Bigge, M. A., et al., 2000. PVTX history of the North Sea' Judy oil field. Journal of Geochemical Exploration, 60-70: 641-644.
[2]	Aplin, A. C., Macleod, G., Larter, S. R., et al., 1999. Combined use of confocal laser microscopy and pVT simulation for esti mating the composition and physical properties of petroleumin fluid inclusions. Marine Petrolum Geo, 16: 97-110. doi: 10.1016/S0264-8172(98)00079-8
[3]	Chen, H. H., Dong, W. L., Zhang, S. L., et al., 2002. Application of fluid inclusion in palaeopressure modeling research. Oil & Gas Geology, 9: 207-211 (in Chinese with English abstract).
[4]	Chen, H. H., Wang, J. H., Xie, Y. H., et al., 2003. Geothermometry and geobarometry of overpressured environments in Qiongdongnan basin, South China Sea. Geofluids, 3: 177-187. doi: 10.1046/j.1468-8123.2003.00061.x
[5]	Chen, H. H., Yao, S. Z., Wang, J. H., et al., 2002. Thermodynamic modeling of fluid-bearing natural gas inclusions for geothermometer and geobarometer of overpressured environments in Qiongdongnan basin, South China Sea. Journal of China University of Geosciences, 13 (3): 240-247.
[6]	Dai, J. X., Chen, J. F., Zhong, N. N., 2003. Large-sized gas fields and their gas source in China. Science Press, Beijing (in Chinese).
[7]	England, W. A., Mackenzie, A. S., Mann, D. M., et al., 1987. The movement and entrapment of petroleum fluids in the subsurface. Journal of the Geological Society, 144: 327-347. doi: 10.1144/gsjgs.144.2.0327
[8]	Hubbert, M. K., 1953. Entrapment of petroleumunder hydrodynamic conditions. AAPG Bulletin, 37 (8): 1954-2026.
[9]	Jin, A. M., Lou, Z. H., Zhu, R., et al., 2003. Formation and evolution of the hydrodynamic field andits fluid property in the Up-Palaeozoic reservoir of the Ordos basin. Journal of Zhejiang University (Science Edition), 30 (3): 337-343 (in Chinese with English abstract).
[10]	Liu, B., Shen, K., 1998. Application of fluid potential map obtained from fluid inclusion data to the research of oil-gas migration. Geological Science and Technology Information, 17 (Suppl.): 81-86 (in Chinese with English abstract).
[11]	Liu, J. Z., Chen, H. H., Li, J., et al., 2005. Using fluid inclusion of reservoir to determine hydrocarbon charging orders and times in the Upper Paleozoic of Ordos basin. Geological Science and Technology Information, 24 (4): 60-66 (in Chinese with English abstract).
[12]	Mi, J. K., Xiao, X. M., Liu, D. H., et al., 2003. Using fluid inclusion of reservoir pVT characteristic to model the forming paleo-pressure of natural gas reservoir-A case study of the Upper Paleozoic deep basin gas in Ordos basin. Science in China (Series D), 7: 679-685 (in Chinese).
[13]	Middleton, D., Parnell, J., Carey, P., et al., 2000. Recon-struction of fluid migration history Northwest Ireland using fluid inclusion studies. Journal of Geochemical Exploration, 69-70: 633-677.
[14]	Min, Q., Yang, H., Fu, J. H., 2000. Deep basin gas in Ordosbasin. Natural Gas Industry, 20 (6): 11-15 (in Chinese with English abstract).
[15]	Munz, I. A., 2001. Petroleum inclusions in sedimentary basins: Systematics, analytical methods and application. Lithos, 55: 195-212. doi: 10.1016/S0024-4937(00)00045-1
[16]	Parnell, J., Middleton, D., Honghan, C., et al., 2001. The use of integrated fluid inclusion studies in constraining oil charge history and reservoir compartmentation: Examples from the Jeanne'd Arc basin, offshore Newfoundland. Marine and Petroleum Geology, 18: 535-549. doi: 10.1016/S0264-8172(01)00018-6
[17]	Wang, Z. L., Chen, H. L., 1998. A palaeohydrodynamic analysis of Upper Palaeozoic in middle Ordos basin. Acta Sedimentologica Sinica, 12 (4): 105-108 (in Chinese with English abstract).
[18]	Wang, Z. L., Zhang, L. K., Sun, M. L., et al., 2004. Natural gas accumulation mechanism in Upper Shihezi and Shiqianfeng formations of Shenmu-Yulin district in northeastern Ordos basin. Acta Petrolei Sinica, 25 (3): 37-43 (in Chinese with English abstract).
[19]	Yang, J. J., 2002. Tectonic evolution and oil-gas reservoirs distribution in Ordos basin. Petroleum Industry Press, Beijing (in Chinese).
[20]	Zhang, J. L., Chang, X. C., 2002. Geological theory of deep basin gas and its application. Geological Publishing House, Beijing (in Chinese).
[21]	陈红汉, 董伟良, 张树林, 等, 2002. 流体包裹体在古压力模拟研究中的应用. 石油与天然气地质, 9: 207-211. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT200203001.htm
[22]	戴金星, 陈践发, 钟宁宁, 2003. 中国大气田及其气源. 北京: 科学出版社.
[23]	金爱民, 楼章华, 朱蓉, 等, 2003. 地下水动力场的形成、演化及其流体特征分析——以鄂尔多斯盆地上古生界为例. 浙江大学学报(理学版), 30 (3): 337-343. doi: 10.3321/j.issn:1008-9497.2003.03.025
[24]	刘斌, 沈昆, 1998. 包裹体流体势图在油气运聚研究方面的应用. 地质科技情报, 17 (增刊): 81-86. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ8S1.016.htm
[25]	刘建章, 陈红汉, 李剑, 等, 2005. 运用流体包裹体确定鄂尔多斯盆地上古生界油气成藏期次和时期. 地质科技情报, 24 (4): 60-66. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ200504011.htm
[26]	米敬奎, 肖贤明, 刘德汉, 等, 2003. 利用储层流体包裹体的pVT特征模拟计算天然气藏形成古压力——以鄂尔多斯盆地上古生界深盆气藏为例. 中国科学(D辑), 7: 679-685. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200307009.htm
[27]	闵琪, 杨华, 付金华, 2000. 鄂尔多斯盆地的深盆气. 天然气工业, 20 (6): 11-15. doi: 10.3321/j.issn:1000-0976.2000.06.003
[28]	汪正江, 陈红德, 张锦全, 2002. 鄂尔多斯盆地二叠纪煤成气藏特征. 矿物岩石, 22 (3): 47-52. doi: 10.3969/j.issn.1001-6872.2002.03.011
[29]	王震亮, 陈荷立, 1998. 鄂尔多斯盆地中部上古生界古流体动力分析. 沉积学报, 12 (4): 105-108. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB804.016.htm
[30]	王震亮, 张立宽, 孙明亮, 等, 2004. 鄂尔多斯盆地神木-榆林地区上石盒子组-石千峰组天然气成藏机理. 石油学报, 25 (3): 37-43. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB200403007.htm
[31]	杨俊杰, 2002. 鄂尔多斯盆地构造演化与油气分布规律. 北京: 石油工业出版社.
[32]	张金亮, 常象春, 2002. 深盆气地质理论及应用. 北京: 地质出版社.