Diagenetic Evolution and Mode in the Chaluhe Faulted Depression Reservoir, Yitong Graben
-
摘要: 依据岔路河断陷大量的岩心、薄片、扫描电镜、X衍射等资料, 详细研究了岔路河地区储集层特征及成岩作用类型.按照成岩阶段划分标准, 将成岩阶段分为早成岩A期和B期, 晚成岩A期和B期, 其中晚成岩A期又分为A1和A2两个亚期; 运用BasinMod软件对主要构造部位进行埋藏史和热史的分析, 并结合孔隙演化史的研究, 分析了储层成岩演化过程, 结果显示, 在30Ma以前, 储层以压实和胶结作用为主, 下部的双阳组和奢岭组孔隙度从32%左右下降至15%左右, 上部的永吉组和万昌组孔隙度从32%左右下降至20%左右.在30~10Ma, 各地层都沉降至最大埋深, 较深部的双阳组和奢岭组砂岩中长石大量溶解, 孔隙度增加至18%左右, 为油气储存提供了良好的孔隙空间, 永吉组和万昌组孔隙度变化不大.在充分考虑了岔路河地区的埋藏史、有机质热演化史、成岩作用演化史以及岩石类型与沉积相等影响因素的基础上, 建立了该断陷的3种成岩模式: 冲积扇成岩模式、扇三角洲成岩模式和半深湖-深湖相成岩模式.Abstract: The characteristics and diagenetic types of Chaluhe reservoir were studied in terms of the data of drill cores, slices, scanning electron microscopy, X-ray diffraction.According to the criterion of division, the diagenetic phases are divided into early diagenetic A stage, B stage, and late diagenetic A stage and B stage, and the late diagenetic A stage is divided into A1 stage and A2 stage.By using the software of BasinMode, the burial history and thermal history of the primary structure were analyzed, and combined with the result of porosity evolution history, the reservoir diagenetic evolution was studied.The result is: before 30 Ma, the primary diagenesis was compaction and cementation.The porosity in the formation of Shanyang and Sheling reduced to 15% from 32% approximately, and that of Yongji and Wanchang reduced to 20% from 32% approximately; During the period of 30 Ma and 10 Ma, all the formations had been buried to the deepest depth and the feldspars in the sandstone formations of Shuangyang and Sheling began to dissolve, which caused the porosity to increase to 18%, providing space for the storage of oil and gas; but the porosity unchanged in the formation of Yongji and Wanchang during this period.Three diagenetic modes (alluvial fan, fan-delta, deep and half-deep lacustrine facies) are built in Chaluhe fault depression based on the study of burial history, thermal evolution history of organic, diagenetic evolution history, the rock type and sedimentary facies.
-
Key words:
- Yitong graben /
- Chaluhe fault depression /
- diagenesis /
- porosity evolution /
- diagenetic mode
-
图 1 伊通地堑构造简图
1.靠山凹陷; 2.马鞍山断阶; 3.尖山隆起带; 4.大南凹陷; 5.五星构造带; 6.梁家构造带; 7.新安堡凹陷; 8.万昌构造带; 9.波太凹陷; 10.孤店斜坡带
Fig. 1. Simplified structure map of Yitong graben
图 2 各类成岩作用
a.颗粒凹凸接触及压裂缝, 昌30井, 2 232.4 m (×10);b.石英次生加大, 昌10井, 1 884.0 m (×600);c.书页状高岭石集合体, 昌12井, 3 035.3 m (×600);d.丝缕状伊利石, 昌12井, 3 709.0 m (×5 000);e.针叶片状绿泥石, 昌12井, 3 031.78 m (×2 500);f.长石溶蚀, 昌13井, 2 356.08 m (×1 200)
Fig. 2. The types of diagenesis
图 3 岔路河断陷成岩阶段划分
S为S在I/S中的百分含量; S.蒙皂石; I/S.伊/蒙混层; K.高岭石; I.伊利石; Ch.绿泥石
Fig. 3. Diagenesis stage of Chaluhe fault depression
图 4 梁家-新安堡地区地层埋藏史与孔隙演化史
Fig. 4. History of stratum embedding and porosity evolution in Liangjia and Xin'anbao area
表 1 岔路河断陷储层岩石成分
Table 1. Sandstone components in Chaluhe fault depression
-
[1] Alaa, M., Salem, S., Morad, S., et al., 2000. Diagenesis andreservoir-quality evolution of fluvial sandstones duringprogressive burial and uplift: Evidence from the Upper Jurassic Boipeba Member, Reconcavo basin, northeastern Brazil. AAPG Bulletin, 84 (7): 1015-1040. [2] Cowan, G., 1989. Diagenesis of Upper Carboniferous sandstones: Southern North Sea basin. In: Whateley, M. K. G., Picketing, K. T., eds., Deltas: Sites andtraps for fossil fuels. Geological Society of London Special Publication, 41: 57-73. [3] Dixon, S. A., Summers, D. M., Surdam, R. C., 1989. Diagenesis andpreservation of porosity in Norphlet Formation (Upper Jurassic), Southern Alabama. AAPGBulletin, 73: 707-728. [4] Dou, T. J., Wang, W. G., Liu, G. F., et al., 2000. Sandstonediagenesis and porosity genesis of the middle oil-bearing formation in Taikang area, Songliao basin. Journal of Daqing Petroleum Institute, 24 (2): 1-4 (in Chinese with English abstract). [5] He, Y. P., Liu, Z. J., Dong, Q. S., et al., 2006. Diagenesis ofreservoir of the Shuangyang Formation of Paleogene in Moliqing faulted depression of Yitong basin, Jilin Province. Journal of Paleography, 8 (1): 75-82 (in Chinese with English abstract). [6] Jiang, S., Cai, D. S., Zhu, X. M., et al., 2007. Mechanism of the pore evolution in Liaodong Bay area. Earth Science—Journal of China University of Geosciences, 32 (3): 366-372 (in Chinese with English abstract). [7] Kou, F. D., Zhu, Y. J., Li, J. M., 2005. Reservoir diagenesis of LowerJurassic in Lenghu area. Journal of Oil and Gas Technology, 27 (6): 695-698 (in Chinese with English abstract). [8] Li, B., Meng, Z. F., Li, X. B., et al., 2005. Diagenetic characteristics of the Chang6oil-bearinginterval of the Upper Triassic in the Jin'an oilfield, Ordos basin. Acta Sedimentologica Sinica, 23 (4): 574-583 (in Chinese withEnglish abstract). [9] Li, S. H., Chen, X. M., Long, Y. M., et al., 2002. Diagenesis andporosity evolutioninthe reservoir rocks from the Pingbei oil fieldin Shaanxi. Sedimentary Geology and Tethyan Geology, 22 (3): 25-30 (in Chinese with English abstract). [10] Li, X. M., Feng, C. M., Hu, Z. G., 2005. Diagenesis and porosity characteristic of Dujiatai oil layer in Huanxilingoil field. Journal of Oil and Gas Technology, 27 (4): 435-437 (in Chinese with English abstract). [11] Liu, C. L., Zhu, X. M., Zhu, Y. X., et al., 2005. Characteristicsof diagenesis and pore evolution of gas reservoirs formedindifferent tectonic settings. Oil & Gas Geology, 26 (6): 746-752 (in Chinese with English abstract). [12] Liu, Z. J., 2003. Acus subaqueous fan sedi mentary characteristics and influence factor. Acta Sedimentologica Sinica, 21 (1): 148-154 (in Chinese with English abstract). [13] Luo, J. L., Morad, S., Yan, S. K., et al., 2001. The recon-struction of diagenesis and it's affection on reservoir'sphysical evolution of sandstone of fluvial-delta facies. Science in China (Ser. D), 31 (12): 1006-1016. [14] Qiu, L. W., Jiang, Z. X., Chen, W. X., et al., 2002. A new type of secondary porosity-quartz dissolution porosity. Acta Sedimentologica Sinica, 20 (4): 621-627 (in Chinese with English abstract). [15] Ronald, C., Surdam, L. J., Crossey, E. S. H., et al., 1989. Organic-in-organic interactions and sandstone diagenesis. AAPG Bulletin, 73 (1): 1-23. [16] Shao, H. M., Liu, Z. J., Wang, C., et al., 2005. Diagenesis and poreevolution of deepsandstonein North of Songliao basin. Global Geology, 24 (1): 58-62 (in Chinese with English abstract). [17] Sylvia, M. C., dos Anjos, L. F., de Ros, R. S., et al., 2000. Depositional and diagenetic controls on the reservoirquality of Lower Cretaceous Pendência sandstones, Pot-iguar rift basin, Brazil. AAPG Bulletin, 84 (11): 1719-1742. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ202101006.htm [18] Wang, B. Q., Zhang, D. N., Liu, S. Q., et al., 2000. Diagenesis of reservoir rocks of Gaotaizi oil bed (Cretaceous) and its influence on porosity modificationin Longhupaofield area. Acta Sedimentologica Sinica, 18 (3): 414-418 (in Chinese with English abstract). [19] Wang, J., Zhao, Y. C., Liu, K., et al., 2006. Super imposing controls of acidic and alkaline dissolutions on sandstonereservoir quality of the Paleozoic Xiashihezi and Shanxiformations in Tabamiao area, Ordos basin. Earth Science—Journal of China University of Geosciences, 31 (2): 221-228 (in Chinese with English abstract). [20] Worden, R. H., Oxtoby, N. H., Smalley, P. C., 1998. Can oilemplacement prevent quartz cementationin sandstones? Petroleum Geoscience, 4: 129-137. doi: 10.1144/petgeo.4.2.129 [21] Xiao, L. H., Meng, Y. L., Hou, C. Y., et al., 2003. Diagenetic modeling and prediction of secondary pore zone in the deepof the Shengping areainthe Songliao basin. Geological Review, 49 (5): 544-550 (in Chinese with English abstract). [22] Yu, S. Y., He, J. Y., 1989. Sedimentary petrology. Geological Publishing House, Beijing (in Chinese). [23] Zhang, L., Zhu, X. M., Zhong, D. K., et al., 2007. Vertical distribution of secondary pores in Paleogene sandstonesin Hui min depression and its genesis analysis. Earth Science—Journal of China University of Geosciences, 32 (2): 253-259 (in Chinese with English abstract). [24] Zhong, D. K., Zhu, X. M., Wen, Y. C., et al., 2003. Diagenesis, porosity evolution and secondary porosity predictionof Jurassic sandstone reservoir in Fudong slope, Junggarbasin. China Offshore Oil and Gas (Geology), 17 (4): 249-251 (in Chinese with English abstract). [25] Zhao, G. Q., Li, Y. T., Tian, C., 2004. Astudy on petrological features and genesis of Chaluhe fault depression inYitong grabenin Jilin. Henan Petroleum, 18 (4): 4-7 (in Chinese with English abstract). [26] Zhou, Y. S., Wang, D. P., Kuang, L. C., et al., 1995. Proper-ties of Eogene sedi mentary systemin Yishu graben andits hydrocarbon significance. Oil & Gas Geology, 16 (1): 55-61 (in Chinese with English abstract). [27] 窦同君, 王文广, 刘国范, 等, 2000. 松辽盆地泰康地区中部含油组合砂岩成岩作用及孔隙成因. 大庆石油学院学报, 24 (2): 1-4. https://www.cnki.com.cn/Article/CJFDTOTAL-DQSY200002000.htm [28] 何玉平, 刘招君, 董清水, 等, 2006. 吉林伊通盆地莫里青断陷古近系双阳组储层成岩作用研究. 古地理学报, 8 (1): 75-82. doi: 10.3969/j.issn.1671-1505.2006.01.008 [29] 蒋恕, 蔡东升, 朱筱敏, 等, 2007. 辽东湾地区孔隙演化的机理. 地球科学——中国地质大学学报, 32 (3): 366-372. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200703008.htm [30] 寇福德, 朱玉洁, 李建明, 2005. 冷湖地区下侏罗统储层成岩作用研究. 石油天然气学报, 27 (6): 695-698. doi: 10.3969/j.issn.1000-9752.2005.06.006 [31] 李斌, 孟自芳, 李相博, 等, 2005. 靖安油田上三叠统长6储层成岩作用研究. 沉积学报, 23 (4): 574-583. doi: 10.3969/j.issn.1000-0550.2005.04.003 [32] 李少华, 陈新民, 龙玉梅, 等, 2002. 坪北油田储层成岩作用与孔隙演化. 沉积与特提斯地质, 22 (3): 25-30. doi: 10.3969/j.issn.1009-3850.2002.03.005 [33] 李相明, 冯常茂, 胡忠贵, 2005. 欢喜岭油田杜家台油层成岩作用及孔隙特征. 石油天然气学报, 27 (4): 435-437. doi: 10.3969/j.issn.1000-9752.2005.04.009 [34] 刘成林, 朱筱敏, 朱玉新, 等, 2005. 不同构造背景天然气储层成岩作用及孔隙演化特点. 石油与天然气地质, 26 (6): 746-752. doi: 10.3321/j.issn:0253-9985.2005.06.008 [35] 刘招君, 2003. 湖泊水下扇沉积特征及影响因素. 沉积学报, 21 (1): 148-154. doi: 10.3969/j.issn.1000-0550.2003.01.024 [36] 罗静兰, Morad, S., 阎世可, 等, 2001. 河流-湖泊三角洲相砂岩成岩作用的重建及其对储层物性演化的影响. 中国科学(D辑), 31 (12): 1006-1016. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200112005.htm [37] 邱隆伟, 姜在兴, 陈文学, 等, 2002. 一种新的储层孔隙成因类型——石英溶解型次生孔隙. 沉积学报, 20 (4): 621-627. doi: 10.3969/j.issn.1000-0550.2002.04.014 [38] 邵红梅, 刘招君, 王成, 等, 2005. 松辽盆地北部深层砂岩成岩作用与孔隙演化. 世界地质, 24 (1): 58-62. doi: 10.3969/j.issn.1004-5589.2005.01.010 [39] 王宝清, 张荻楠, 刘淑芹, 等, 2000. 龙虎泡地区高台子油层成岩作用及其对储集岩孔隙演化的影响. 沉积学报, 18 (3): 414-418. doi: 10.3969/j.issn.1000-0550.2000.03.015 [40] 王京, 赵彦超, 刘琨, 等, 2006. 鄂尔多斯盆地塔巴庙地区上古生界砂岩储层"酸性+碱性"叠加溶蚀作用与储层质量主控因素. 地球科学——中国地质大学学报, 31 (2): 221-228. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200602011.htm [41] 肖丽华, 孟元林, 侯创业, 等, 2003. 松辽盆地升平地区深层成岩作用数值模拟与次生孔隙带预测. 地质论评, 49 (5): 544-550. doi: 10.3321/j.issn:0371-5736.2003.05.013 [42] 余素玉, 何镜宇, 1989. 沉积岩石学. 北京: 地质出版社. [43] 张莉, 朱筱敏, 钟大康, 等, 2007. 惠民凹陷古近系碎屑岩次生孔隙纵向分布规律. 地球科学——中国地质大学学报, 32 (2): 253-259. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200702014.htm [44] 钟大康, 朱筱敏, 文应初, 等, 2003. 准噶尔盆地阜东斜坡侏罗系砂岩成岩作用、孔隙演化及次生孔隙预测. 中国海上油气(地质), 17 (4): 249-251. https://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD200304005.htm [45] 赵国泉, 李永涛, 田成, 2004. 吉林省伊通地堑岔路河断陷岩石学特征及成岩作用研究. 河南石油, 18 (4): 4-7. doi: 10.3969/j.issn.1673-8217.2004.04.002 [46] 周永胜, 王东坡, 匡立春, 等, 1995. 伊舒地堑下第三系沉积体系特征及其油气勘探意义. 石油与天然气地质, 16 (1): 55-61. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT501.006.htm -
下载:
点击查看大图
图(5) / 表(1)
计量
- 文章访问数: 3712
- HTML全文浏览量: 134
- PDF下载量: 68
- 被引次数: 0
