An Experiment Study on Influence of Fault on Petroleum Migration and Accumulation in Guantao Formation, Zhanhua Depression
-
摘要: 在沾化凹陷馆陶组油气成藏地质研究基础上, 利用二维模型模拟了断层开启条件下, 断层对馆陶组石油运移和聚集的影响. 研究结果表明: (1) 断层带的流体运动方式和运动相态对馆陶组石油的运移路径和方式构成重要的影响.连续(稳态) 充注条件下, 油首先充注断层带, 然后在馆陶组上段顶部侧向运移, 最后一部分油沿馆陶组下段砂层的顶部侧向运移. 但幕式(非稳态) 充注条件下, 油首先充注断层下部和馆陶组下段→充注断层上部, 并在馆陶组下段侧向运移→充注馆陶组上段, 并在其中侧向运移. 另外油/水两相充注时, 由于水动力的作用, 导致油和水的运移出现分异现象; (2) 连续(稳态) 充注条件下, 油的侧向运移发生在隔层上部(馆陶组上段) 砂层, 而幕式(非稳态) 充注条件下, 馆陶组上、下段均发生了侧向运移, 其中单一油相充注时, 下部砂层油的侧向运移量大于上部砂层, 而油/水两相充注时, 上部砂层侧向运移量稍大于下部砂层; (3) 连续(稳态) 充注时有利于馆陶组上段砂层油的聚集, 而幕式(非稳态) 充注时则有利于馆陶组下段砂层油的聚集. 另外由于水动力作用的影响, 油水两相充注时, 有利于馆陶组上段油的聚集.Abstract: On the basis of the geological study of hydrocarbon migrating and accumulating into reservoir in Guantao Fm., Zhanhua depression, this experiment models the influence of opening fault on petroleum migration and accumulation in the formation with a 2-D model. The results are as follows: (1) The moving pattern and phase of fluids in fault zone have great influence on moving path and pattern of petroleum in Guantao Fm.. When continuously injected, petroleum could have occupied the fault zone firstly, then moved laterally down the top of its upper formation, and finally down the top of its lower formation. However, in impulsive (unsteady) injection, petroleum occupied lower part of fault and the lower Guantao Fm., firstly, then upper part of fault, and migrates laterally in the lower Guantao Fm.. Finally, the upper Guantao Fm. moved laterally. In addition, when petroleum and water injected together, they would separate because of hydrodynamics. (2) When injected continuously (steadily), petroleum migrated laterally in sand bed above the barrier, while in impulsive (unsteady) injection, it migrated in both upper and lower Guantao Fm., in which quantity of lateral migration in lower sand bed is bigger than that in the upper sand bed when petroleum is injected only, and the quantity of lateral migration in upper sand bed is slightly bigger than that in lower sand bed when petroleum and water are injected together. (3) Continuous (steady) injection is favorable for petroleum accumulation in upper Guantao Fm., sand bed, while impulsive (unsteady) injection is favorable for petroleum accumulation in lower Guantao Fm., sand bed. In addition, petroleum is apt to accumulate in upper of Guantao Fm., when it is injected together with water because of hydrodynamics.
-
Key words:
- fault /
- petroleum migration and accumulation /
- simulation experiment /
- Zhanhua depression
-
图 2 单一油相连续(稳态) 充注条件下(实验1) 油的运移过程示意图
a.注油量10.66 mL, 注油时间213 min; b.注油量52.63 mL, 注油时间1 052 min; c.注油量76.98 mL, 注油时间1 539 min; d.注油量122.80 mL, 注油时间2 455 min; e.注油量622.75 mL, 注油时间12 448 min; 1~3.不同含油饱和度的油层(其中从1→2→3含油饱和度逐渐变大); 4.水层; 5.盖层
Fig. 2. Diagrammatic sketch of oil migration with oil continuously (steadily) injected (experiment 1)
图 3 单一油相幕式(非稳态) 充注条件下(实验3) 油的运移过程示意图
a.第1次脉冲; b.第3次脉冲; c.第6次脉冲; d.第10次脉冲; e.第16次脉冲; 图例同图 2]
Fig. 3. Diagrammatic sketch of oil migration with oil impulsively (unsteadily) injected (experiment 3)
表 1 实验模型参数
Table 1. Parameters for experimental model
表 2 模拟实验条件
Table 2. Parameters for experiments
表 3 隔层上部(A+C砂层) (馆陶组上段) 和下部(B+D砂层) (馆陶组下段) 石油运移和聚集结果
Table 3. Result of petroleum migration and accumulation above barrier (A+C sand beds) (upper Guantao Fm.) and beneath barrier (B+D sand beds) (lower Guantao Fm.)
-
[1] 张善文. 沾化凹陷浅层勘探的思考[J]. 复式油气田, 1999, 3: 6-7.ZHANG S W. Some think for oil-gas exploration of shallow zone in Zhanhua sag[J]. Multiple Oil-Gas Field, 1999, 3: 6-7. [2] 帅德福, 刘兴材, 王秉海, 等. 中国石油地质志(卷六)胜利油田[M]. 北京: 石油工业出版社, 1993.SHUAI D F, LIU X C, WANG B H, et al. Petroleum geology of China(Vol. 6) Shengli oilfield[M]. Beijing: Petroleum Industry Press, 1993. [3] 毕研鹏, 陈云井, 田波, 等. 孤岛油田[A]. 见: 张文昭. 中国陆相大油田[C]. 北京: 石油工业出版社, 1997. 646-654.BI Y P, CHEN Y J, TIAN B, et al. Gudao oilfield[A]. In: ZHANG W Z, ed. Major nonmarine oilfields of China [C]. Beijing: Petroleum Industry Press, 1997. 646-654. [4] 吴静, 陈广军. 埕岛地区馆陶组河流相储层油藏描述技术[A]. 见: 杜贤樾, 孙焕泉, 郑和荣. 胜利油区勘探开发论文集(第一辑)[C]. 北京: 地质出版社, 1997. 67-76.WU J, CHEN G J. Reservoir discription technology for fluvial facies of Guantao Formation in Chengdao eara[A]. In: DU X Y, SUN H Q, ZHENG H R, eds. Collected works for petroleum exploration and development in Shengli oilfield(No. 1)[C]. Beijing: Geological Publishing House, 1997. 67-76. [5] 庞雄奇, 李素梅, 黎茂稳, 等. 八面河油田油气运聚、成藏模式探讨[J]. 地球科学——中国地质大学学报, 2002, 27(6): 666-670. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200206002.htmPANG X Q, LI S M, LI M W, et al. Discussion on petroleum migration in Bamianhe oilfield of dongying depression, eastern China[J]. Earth Science—Journal of China University of Geosciences, 2002, 27(6): 666-670. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200206002.htm [6] 王尚旭, 狄帮让, 魏建新. 断层物理模型实验及其地震响应特征分析[J]. 地球科学——中国地质大学学报, 2002, 27(6): 736-740. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200206013.htmWANG S X, DI B R, WEI J X. Seismic physical modeling of fault and its analysis[J]. Earth Science—Journal of China University of Geosciences, 2002, 27(6): 736-740. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200206013.htm [7] 贾献斌, 李开勐, 王元安. 孤东油田[A]. 见: 张文昭. 中国陆相大油田[C]. 北京: 石油工业出版社, 1997. 655-665.JIA X B, LI K Q, WANG Y A. Gudong oilfield[A]. In: ZHANG W Z, ed. Major nonmarine oilfields of China [C]. Beijing: Petroleum Industry Press, 1997. 655-665. [8] Hooper E C D. Fluid migration along growth faultsin compacting sedimentary basins[J]. Jour Petrol Geol, 1991, 4 (2): 161-180. [9] 龚再升, 杨甲明, 郝芳, 等. 莺歌海盆地与琼东南盆地成藏条件的比较及天然气勘探方向[J]. 地球科学——中国地质大学学报, 2001, 26(3): 286-290. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200103010.htmGONG Z S, YANG J M, HAO F, et al. Difference in nature gas accumulation conditions between Yinggehai and Qiongdongnan basins and its implications for natural gas exploration[J]. Earth Science—Journal of China University of Geosciences, 2001, 26(3): 286-290. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200103010.htm [10] 张启明, 胡忠良. 莺-琼盆地高温高压环境及油气运移机制[J]. 中国海上油气, 1992, 6(1): 1-9. https://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD199201003.htmZHANG Q M, HU Z L. Hot, geopressured Yinggehai-Qiongdongnan basin and its hydrocarbon migration[J]. Offshore Oil & Gas, 1992, 6(1): 1-9. https://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD199201003.htm [11] 华保钦. 构造应力场、地震泵和油气运移[J]. 沉积学报, 1995, 13(2): 234-236. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB502.009.htmHUA B Q. Stress field, seismic pumping and oil-gas migration[J]. Acta Sedimentologica Sinica, 1995, 13(2): 234-236. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB502.009.htm [12] 杨巍然, 张文淮. 断裂性质与流体包裹体组合性质[J]. 地球科学——中国地质大学学报, 1996, 21(3): 285-290. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX603.009.htmYANG W R, ZHANG W H. Character of fault property and combination of fluid inclusions[J]. Earth Science—Journal of China University of Geosciences, 1996, 21 (3): 285-290. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX603.009.htm [13] 杨明慧, 金之钧, 吕修祥, 等. 库车褶皱冲断带克拉苏三角带及其油气潜力[J]. 地球科学——中国地质大学学报, 2002, 27(6): 745-750. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200206016.htmYANG M H, JIN Z J, L X X, et al. Kelasu triangle zone and its hydrocarbon potential in Kuqa thrust-and-fold belts, Tarim Basin[J]. Earth Science—Journal of China University of Geosciences, 2002, 27(6): 745-750. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200206016.htm[14] 曾溅辉, 王洪玉. 输导层和岩性圈闭中石油运移和聚集模拟实验研究[J]. 地球科学——中国地质大学学报, 1999, 24(2): 193-196. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX902.018.htmZENG J H, WANG H Y. An experimental study of petroleum migration and accumulation in carrier bed and lithological trap[J]. Earth Science—Journal of China University of Geosciences, 1999, 24(2): 193-196. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX902.018.htm [15] 曾溅辉, 王洪玉. 层间非均质砂层石油运移和聚集的模拟实验研究[J]. 石油大学学报(自然科学版), 2000, 24 (4): 108-111. https://www.cnki.com.cn/Article/CJFDTOTAL-SYDX200004027.htmZENG J H, WANG H Y. Experimental study on oil migration and accumulation in the heterogeneous sand beds of different porosity and permeability[J]. Journal of the University of Petroleum(edition of Natural Science), 2000, 24(4): 108-111. https://www.cnki.com.cn/Article/CJFDTOTAL-SYDX200004027.htm