Quantitative recovery of solid-fluid interaction and prediction of cause of secondary pores in beach and bar reservoirs in the upper part of Member 4 of Shahejie Formation of Paleogene, Dongying sag
Zhao Wei1, Qiu Longwei1, Jiang Zaixing2
1 School of Geosciences, China University of Petroleum(East China),Qingdao 266580,Shandong; 2 School of Energy Resources, China University of Geosciences(Beijing),Beijing 100038;
Abstract There are large scale of typical lacustrine beach and bar sandbodies of the upper part of the Member 4 of Shahejie Formation of Paleogene in Dongying sag and a great amount of oil and gas has been found in this area. Based on the analysis of cements and secondary pores,which are the products of the solid-fluid interaction,we can quantitatively or semi-quantitatively recover the process of the liquid changing and its effects on the porosity of reservoirs combing with the evolution of the basin and the structure development stages. Finally,in accordance with the fluid sources and time of duration, the whole evolution process can be divided into five stages,which are the reaction stage of initial liquid,the reaction stage of liquid from surrounding rocks,the reaction stage of liquid from outer sources,the reaction stage of liquid with hydrocarbon migration and the reaction stage after hydrocarbon accumulation. According to the formation mechanism of secondary pores and the zoning character of beach and bar sand bodies,we can indentify the secondary pore zones as the zone dominated by the acid fluids in gravelly beach and bar along the shore line,the zone effected commonly by the acid and alkaline fluids in the near shore bar sand bodies,and the zone dominated by the alkaline fluids in the bar far from shore and in the central resonance belt,and the speculation of secondary pores in the plane also been done in this article.
Corresponding Authors:
Zhao Wei,born in 1982,is a post-doctoral fellow in China University of Petroleum(East China). He is mainly engaged in the research of sedimentology,sequence stratigraphy and reservoir geology. E-mail: upc_wee@163.com.
Cite this article:
Zhao Wei,Qiu Longwei,Jiang Zaixing. Quantitative recovery of solid-fluid interaction and prediction of cause of secondary pores in beach and bar reservoirs in the upper part of Member 4 of Shahejie Formation of Paleogene, Dongying sag[J]. JOPC, 2016, 18(5): 769-784.
Zhao Wei,Qiu Longwei,Jiang Zaixing. Quantitative recovery of solid-fluid interaction and prediction of cause of secondary pores in beach and bar reservoirs in the upper part of Member 4 of Shahejie Formation of Paleogene, Dongying sag[J]. JOPC, 2016, 18(5): 769-784.
[1] 蔡春芳. 1996. 沉积盆地流体—岩石相互作用研究的现状. 地球科学进展,11(6): 575-579. [Cai C F. 1996. Advancements of fluid-rock interactions in sedimentary basin. Advance in Earth Sciences,11(6): 575-579] [2] 操应长,王艳忠,徐涛玉,刘惠民,高永进. 2009. 东营凹陷西部沙四上亚段滩坝砂体有效储集层的物性下限及控制因素. 沉积学报,27(2): 230-237. [Cao Y C,Wang Y Z,Xu T Y,Liu H M,Gao Y J. 2009. The petrophysical parameter cutoff and controlling factors of the effective reservoir of beach and bar sandbodies of the Upper Part of the Fourth Member of the Shahejie Formation in west part of Dongying Depression. Aata Sedimentologica Sinica,27(2): 230-237] [3] 邓宏文,钱凯. 1993. 试论湖相泥质岩的地球化学二分性. 石油与天然气地质, 14(2):85-97. Deng H W,Qian K. 1993. Geochemical binary division character of lacustrine argillite. Oil & Gas Geology,14(2): 85-97] [4] 邓宏文,高晓鹏,赵宁,颜晖,邸永香,张培园. 2010. 济阳坳陷北部断陷湖盆陆源碎屑滩坝成因类型、分布规律与成藏特征. 古地理学报,12(6): 737-747. [Deng H W,Gao X P,Zhao N,Yan H,Di Y X,Zhang P Y. 2010. Genetic types,distribution pattern sand hydrocarbon accumulation in terrigenous beach and bar in northern faulted lacustrine basin of Jiyang Depression. Journal of Palaeogeography(Chinese Edition),12(6): 737-747] [5] 黄思静,黄可可,冯文立,佟宏鹏,刘丽红,张雪花. 2009. 成岩过程中长石、高岭石、伊利石之间的物质交换与次生孔隙的形成: 来自鄂尔多斯盆地上古生界和川西凹陷三叠系须家河组的研究. 地球化学,38(5): 498-506. [Huang S J,Huang K K,Feng W L,Tong H P,Liu L H,Zhang X H. 2009. Mass exchanges among feldspar,kaolinite and illite and their influences on secondary porosity formation in clastic diagenesis: A case study on the Upper Paleozoic,Ordos Basin and Xujiahe Formation,Western Sichuan Depression. Geochimica,38(5): 498-506] [6] 李吉君,史颖琳,黄振凯,王伟明,曹群,卢双舫. 2015. 松辽盆地北部陆相泥页岩孔隙特征及其对页岩油赋存的影响. 中国石油大学学报(自然科学版),39(4): 27-34. [Li J J,Shi Y L,Huang Z K,Wang W M,Cao Q,Lu S F. 2015. Pore characteristics of continental shale and its impact on storage of shale oil in northern Songliao Basin. Journal of China University of Petroleum(Edition of Natural Sciences),39(4): 27-34] [7] 李国斌,姜在兴,王升兰,周浩玮,王天奇,张亚军. 2010. 薄互层滩坝砂体的定量预测: 以东营凹陷古近系沙四上亚段(Es4上)为例. 中国地质,37(6): 1659-1671. [Li G B,Jiang Z X,Wang S L,Zhou H W,Wang T Q,Zhang Y J. 2010. The quantitative prognosis of thin interbedded beach-bar sandbodies: A case study of the upper 4th submember of the Paleogene Shahejie Formation in Dongying Sag. Geology in China,37(6): 1659-1671] [8] 刘伟. 1997. 流体—岩石相互作用中氧同位素地球化学及动力学研究现状. 岩石矿物学杂志,16(3): 220-229. [Liu W. 1997. Present state of the study of Oxygen isotope geochemistry and kinetics in fluid-rock interaction. Acta Petrologica et Mineralogica,16(3): 220-229] [9] 庞忠和. 1996. 全体系地球化学模拟与水岩相互作用研究. 地学前缘,3(3): 119-123. [Pang Z H. 1996. Whole-system geochemical modeling and the study of water-rock interaction. Earth Science Frontiers,3(3): 119-123] [10] 邱隆伟,姜在兴,陈文学,李晓红,熊志东. 2002. 一种新的储集层孔隙成因类型—石英溶解型次生孔隙. 沉积学报,20(4): 621-627. [Qiu L W,Jiang Z X,Chen W X,Li X H,Xiong Z D. 2002. A new type of secondary porosity-quartz dissolution porosity. Acta Sedimentologica Sinica,20(4): 621-627] [11] 商晓飞,侯加根,程远忠,安振月,姚瑞香,李燕. 2014. 厚层湖泊滩坝砂体成因机制探讨及地质意义:以黄骅坳陷板桥凹陷沙河街组二段为例. 地质学报,88(9):1705-1718. [Shang X F,Hou J G,Cheng Y Z,An Z Y,Yao R X,Li Y. 2014. Formation mechanism of the thick layer lacustrine beach-bar and its geological implications: An example of the 2nd member of the Shahejie Formation in Banqiao Sag. Acta Geologica Sinica,88(9): 1705-1718] [12] 田继军,姜在兴. 2012. 惠民凹陷与东营凹陷沙四上亚段滩坝沉积特征对比与分析. 吉林大学学报(地球科学版),42(3): 612-623. [Tian J J,Jiang Z X. 2012. Comparison and analysis of beach bars sedimentary characteristics of Upper E s 4 in Huimin and Dongying Depression. Journal of Jilin Unviersity(Earth Science Edition),42(3): 612-623] [13] 徐宁宁,邱隆伟,杨生超,解超,刘魁元,单宝杰,刘连启. 2015. 渤南断阶带沙四上亚段储集层成岩演化研究. 中国矿业大学学报,44(1): 104-115. [Xu N N,Qiu L W,Yang S C,Xie C,Liu K Y,Shan B J,Liu L Q. 2015. Research on the diagenetic evolution of the upper fourth member of Shahejie formation reservoir in Bonan step-fault zone. Journal of China University of Mining & Technology,44(1): 104-115] [14] 杨勇强,邱隆伟,姜在兴,银熙炉. 2011. 陆相断陷湖盆滩坝沉积模式: 以东营凹陷古近系沙四上亚段为例. 石油学报,32(3):417-423. [Yang Y Q,Qiu L W,Jiang Z X,Yin X L. 2011. A depositional pattern of beach bar in continental rift lake basins: A case study on the upper part of the fourth member of the Shahejie Formation in the Dongying Sag. Acta Petrolei Sinica,32(3): 417-423] [15] 张军华,刘培金,朱博华,刘显太,杨勇,王军. 2014. 滩坝砂储集层地震解释存在的问题及对策. 石油地球物理勘探,49(1):167-175. [Zhang J H,Liu P J,Zhu B H,Liu X T,Yang Y,Wang J. 2014. Problems and countermeasures in seismic interpretation of beach bar sandstone reservoirs. Oil Geophysical Prospecting,49(1): 167-175] [16] 张林晔,宋一涛,王广利,黄第藩. 2005. 济阳坳陷湖相烃源岩有机质化学组成特征及其石油地质意义. 科学通报,50(21):2392-2402. [Zhang L Y,Song Y T,Wang G L,Huang D F. 2005. Organic compositions of lacustrine source rocks in Jiyang super-depression and its implication to petroleum geology. Chinese Science Bulletin,50(21): 2392-2402] [17] 张善文,袁静,隋风贵,陈鑫. 2008. 东营凹陷北部沙河街组四段深部储集层多重成岩环境及演化模式. 地质科学,43(3): 576-587. [Zhang S W,Yuan J,Sui F G,Chen X. 2008. Multiple diagenetic environments and evolvement model in deep formation of the 4th Member,Shahejie Formation in the northern Dongying Sag. China Journal of Geology,43(3): 576-587] [18] 张枝焕,胡文瑄,曾溅辉,于炳松,陆现彩,贾红育. 2000. 东营凹陷下第三系流体—岩石相互作用研究. 沉积学报,18(4): 560-566. [Zhang Z H,Hu W X,Zeng J H,Yu B S,Lu X C,Jia H Y. 2000. Study of fluid-rock interactions in Eogene Formation in Dongying Depression,Bohai Gulf Basin,Acta Sedimentologica Sinica,18(4): 560-566] [19] Gaupp R,Matter A,Platt J. Ramseyer K, Walzebuck J. 1993. Diagenesis and fluid evolution of deeply buried Permian(Rotliegende)gas reservoirs,northwest Germany. American Association of Petroleum Geologists Bulletin,77(7): 1111-1128. [20] Hayes J B. 1979. Sandstone diagenesis: The hole trouth. In: Scholle P A,Schiuger P R(eds). Aspects of diagenesis: SEPM Special Publication,26: 127-139. [21] Lundegard P D,Land L S,Galloway W E. 1984. Problem of secondary porosity: Frio Formation(Oligocene),Texas Gulf Coast. Geology,12(7): 399-402. [22] Pettijohn F J,Potter P E,Siever R. 1972. Sand and Sandstone. New York: Springer-Verlag. [23] Schmidt V,McDonald D A. 1979. The role of secondary porosity in the course of sandstong diagenesis. In: Scholle P A,Schiuger P R(eds). Aspects of diagenesis. SEPM Special Publication,26: 175-207.
