吉林大学学报(地球科学版) ›› 2017, Vol. 47 ›› Issue (3): 674-684.doi: 10.13278/j.cnki.jjuese.201703103

• 地质与资源 • 上一篇    下一篇

致密气藏成藏动力及成藏模式——以鄂尔多斯盆地L区块山1储层为例

庞振宇1, 赵习森1, 孙卫2, 党海龙1, 任大忠2, 解伟1   

  1. 1. 陕西延长石油(集团)有限责任公司研究院, 西安 710075;
    2. 西北大学地质学系, 西安 710069
  • 收稿日期:2016-08-31 出版日期:2017-05-26 发布日期:2017-05-26
  • 作者简介:庞振宇(1984-),男,博士,工程师,主要从事油气藏精细描述及开发地质研究,E-mail:pangzhenyu0624@163.com
  • 基金资助:
    陕西省科技统筹创新工程计划项目(2014KTZB03-02);国家科技重大专项(2011ZX05044)

Study on Dynamics and Models of Hydrocarbon Accumulations of Tight Sandstone Gas Reservoir: Taking Shan 1 Formation of Block L in Ordos Basin as an Example

Pang Zhenyu1, Zhao Xisen1, Sun Wei2, Dang Hailong1, Ren Dazhong2, Xie Wei1   

  1. 1. Research Institute of Shaanxi Yanchang Petroleum (Group) Co.,Ltd, Xi'an 710075, China;
    2. Department of Geology, Northwest University, Xi'an 710069, China
  • Received:2016-08-31 Online:2017-05-26 Published:2017-05-26
  • Supported by:
    Supported by Shaanxi Province Science and Technology Entire Innovation Plan Foundation (2014KTZB03-02) and National Science and Technology Major Project (2011ZX05044)

摘要: 研究区主力产气层山1储层属于致密气藏,为了摸清有效储集层的形成机制、寻找勘探开发的有利区域,应用铸体薄片、扫描电镜、核磁共振、恒速压汞等实验手段开展成藏动力及成藏模式研究。结果表明:早白垩世为天然气充注的主要成藏期,水相封存天然气分子的最小孔喉半径和天然气充注的孔喉半径下限分别为0.093 μm和0.25 μm,天然气充注的最大毛细管阻力为1.16 MPa,流体过剩压力是致密砂岩气藏天然气运移的主要动力和阻力;天然气主要聚集在过剩压力高值背景下的低值区,山1段过剩压力小于6 MPa的区域有利于天然气的聚集,隔夹层密度越小、厚度越薄的区域含气饱和度越高;研究区天然气充注模式存在4种模式,煤层连续发育厚度大、储层整体特征优,源储层间压差大、储层顶面的隔夹层和大段较厚泥岩产生的欠压实过剩压力有利于储层段的天然气保存,成为天然气开发的“甜点”。

关键词: 致密气藏, 充注下限, 核磁共振, 充注动力, 过剩压力, 充注模式

Abstract: Shan 1 Formation in the study area belongs to tight gas reservoir. In order to understand the formation mechanism of effective reservoir, and to find the favorable area for exploration and development, the authors carry out a research on the accumulation dynamics and the accumulation model through application of casting thin sections, scanning electron microscopy, nuclear magnetic resonance (NMR), and constant speed mercury injection experiment, etc.. The results show that: The Early Cretaceous is the main period for gas accumulation, the pore-throat radius of water sealed gas molecules is 0.093 μm,the pore-throat radius cutoff of gas filling is 0.25 μm, and the maximum capillary resistance of gas filling is 1.16 MPa; The fluid overpressure in tight sandstone gas reservoir is the main force and resistance of gas migration; Natural gas is mainly gathered in a low overpressune area under high overpressure background; The area whih overpressure less than 6 MPa is advantageous for gas gathering,and the smaller the density and the thickness of isolation layers are, the higher their saturation is; There are four gas filling patterns in the study area. Coal seam with large thickness of continuous development, optimal overall characteristics of reservoir, pressure difference between source bed and reservoir, interlayer and overpressure are beneficial to preserve natural gas, which become "sweet spots" of the development of natural gas.

Key words: tight gas reservoir, filling limit, nuclear magnetic resonance, charging dynamic, overpressure, charging pattern

中图分类号: 

  • P618.13
[1] 贾承造,张永峰,赵霞.中国天然气工业发展前景与挑战[J].天然气工业,2014,34(2):1-11. Jia Chengzao, Zhang Yongfeng, Zhao Xia. Prospects of and Challenges to Natural Gas Industry Development in China[J]. Natural Gas Industry,2014,34(2):1-11.
[2] 戴金星,倪云燕,黄士鹏,等.煤成气研究对中国天然气工业发展的重要意义[J].天然气地球科学,2014,25(1):1-22. Dai Jinxing, Ni Yunyan, Huang Shipeng, et al. Significant Function of Coal-Derived Gas Study for Natural Gas Industry Development in China[J]. Natural Gas Geoscience,2014,25(1):1-22.
[3] 赵文智,王红军,钱凯.中国煤成气理论发展及其在天然气工业发展中的地位[J].石油勘探与开发,2009,36(3):280-289. Zhao Wenzhi, Wang Hongjun, Qian Kai. Progress of Coal-Formed Gas Geological Theory and Its Status in Natural Gas Industry in China [J]. Petroleum Exploration and Development,2009,36(3):280-289.
[4] 刘新社,席胜利,付金华,等.鄂尔多斯盆地上古生界天然气生成[J]. 天然气工业,2000,20(6):19-23. Liu Xinshe, Xi Shengli, Fu Jinhua,et al. Natural Gas Generation in the Upper Paleozoic in Ordos Basin[J]. Natural Gas Industry, 2000,20(6):19-23.
[5] 付金华,段晓文,席胜利.鄂尔多斯盆地上古生界气藏特征[J]. 天然气工业,2000,20(6):16-19. Fu Jinhua, Duan Xiaowen, Xi Shengli. Characteristics of Upper Paleozoic Gas Reservoirs in Ordos Basin[J]. Natural Gas Industry,2000,20(6):16-19.
[6] 周进松,王念喜,赵谦平,等.鄂尔多斯盆地东南部延长探区上古生界天然气成藏特征[J]. 天然气工业,2014,34(2):34-41. Zhou Jinsong, Wang Nianxi, Zhao Qianping, et al. Natural Gas Accumulation Characteristics in the Upper Paleozoic in the Yanchang Exploration Block of Southeastern Ordos Basin [J]. Natural Gas Industry,2014,34(2):34-41.
[7] 朱光有,张水昌,陈玲,等.天然气充注成藏与深部砂岩储集层的形成:以塔里木盆地库车坳陷为例[J]. 石油勘探与开发,2009,36(3):347-357. Zhu Guangyou, Zhang Shuichang, Chen Ling, et al. Coupling Relationship Between Natural Gas Charging and Deep Sandstone Reservoir Formation: A Case from the Kuqa Depression, Tarim Basin [J]. Petroleum Exploration and Development,2009,36(3):347-357.
[8] 陈义才,林杭杰,唐波,等.苏里格地区石炭二叠系天然气充注特点及充注能力[J]. 石油与天然气地质,2011,32(1):91-97. Chen Yicai, Lin Hangjie, Tang Bo, et al. Characteristics and Potential of Gas Charging in the Permo-Carboniferous of Sulige Region [J]. Oil & Gas Geology,2011,32(1):91-97.
[9] 庞振宇,孙卫,李进步,等.低渗透致密气藏微观孔隙结构及渗流特征研究:以苏里格气田苏48和苏120区块储层为例[J].地质科技情报,2013,32(4):133-138. Pang Zhenyu, Sun Wei, Li Jinbu, et al. A Study on Microscopic Pore Structure and Seepage Characteristics Low-Permeability and Tight Sandstone Gas Reservoir: Taking Block Su 48-120 in Sulige Gas Field,as an Example [J]. Geological Science and Technology Information, 2013,32(4):133-138.
[10] 李易霖,张云峰,丛琳,等.X-CT扫描成像技术在致密砂岩微观孔隙结构表征中的应用:以大安油田扶余油层为例 [J].吉林大学学报(地球科学版),2016,46(2):379-387,doi:10.13278/j.cnki.jjuese.201602107. Li Yilin, Zhang Yunfeng, Cong Lin, et al. Application of X-CT Scanning Technique in the Characterization of Micro Pore Structure of Tight Sandstone Reservoir: Taking the Fuyu Oil Layer in Daan Oilfield as an Example[J]. Journal of Jilin University (Earth Science Edition),2016,46(2):379-387. doi:10.13278/j.cnki.jjuese.201602107.
[11] Mousavi M A,Bryant S L.Connectivity of Pore Space as a Control on Two-Phase Flow Properties of Tight-Gas Sandstones[J].Transport in Porous Media,2012,94(2):537-554.
[12] 薛会,王毅,毛小平,等.鄂尔多斯盆地北部上古生界天然气成藏期次:以杭锦旗探区为例[J]. 天然气工业,2009,29(12):9-12. Xue Hui, Wang Yi, Mao Xiaoping, et al. The Timing of Gas Pooling in the Upper Paleozoic in the Northern Ordos Basin: A Case Study of the Hangjinqi Block [J]. Natural Gas Industry,2009,29(12):9-12.
[13] 张文忠,郭彦如,汤达祯,等.苏里格气田上古生界储层流体包裹体特征及成藏期次划分[J]. 石油学报,2009,30(5):685-691. Zhang Wenzhong, Guo Yanru, Tang Dazhen, et al. Characteristics of Fluid Inclusions and Determination of Gas Accumulation Period in the Upper Paleozoic Reservoirs of Sulige Gas Field[J]. Acta Petrolei Sinica,2009,30(5):685-691.
[14] 刘小洪,冯明友,罗静兰,等.鄂尔多斯盆地乌审召地区盒8、山1段储层流体包裹体特征及其意义[J]. 石油与天然气地质,2010,31(3):360-374. Liu Xiaohong, Feng Mingyou, Luo Jinglan, et al. Characteristics of Fluid Inclusions in Reservoirs in the Eighth Member of the Shihezi Formation and the First Member of the Shaanxi Formation in Uxin Ju Area, the Ordos Basin and Their Signincance [J]. Oil & Gas Geology,2010,31(3):360-374.
[15] 樊爱萍,杨仁超,冯乔,等.鄂尔多斯盆地上古生界流体包裹体特征及研究[J]. 山东科技大学学报(自然科学版),2006,25(2):20-26. Fan Aiping, Yang Renchao, Feng Qiao, et al. Research on Characteristics of Fluid Inclusions in the Upper Paleozoic in Ordos Basin and Its Application [J]. Journal of Shandong University of Science and Technology (Natural Science),2006,25(2):20-26.
[16] 王康东,李贤庆,冯松宝,等.苏里格大气田上古生界储层流体包裹体特征及天然气成藏意义[J]. 天然气地球科学,2011,22(6):961-968. Wang Kangdong, Li Xianqing, Feng Songbao, et al. Characteristic of Fluid Inclusions and Natural Gas Pool-Forming Significance of the Upper Paleozoic Reservoirs in Sulige Gas Field [J]. Natural Gas Geoscience,2011,22(6):961-968.
[17] 刘新社,周立发,侯云东.运用流体包裹体研究鄂尔多斯盆地上古生界天然气成藏[J]. 石油学报,2007,28(6):37-42. Liu Xinshe, Zhou Lifa, Hou Yundong. Study of Gas Charging in the Upper Paleozoic of Ordos Basin Using Fluid Inclusion [J]. Acta Petrolei Sinica,2007,28(6):37-42.
[18] 李艳霞,赵靖舟,李净红.鄂尔多斯盆地东部上古生界气藏成藏史[J]. 兰州大学学报(自然科学版),2011,47(3):29-39. Li Yanxia, Zhao Jingzhou, Li Jinghong. Gas Accumulation History in Upper Palaeozoic, East of Ordos Basin [J]. Journal of Lanzhou University(Natural Sciences),2011,47(3):29-39.
[19] 宁方兴.济阳坳陷地层油气藏成藏动力与含油高度预测[J]. 新疆石油天然气,2010,6(3):17-22. Ning Fangxing. Research on Reservoir-Forming Dynamics and Oil-Bearing Prediction of the Stratigraphic Hydrocarbon Reservoir in Jiyang Depressin[J]. Xinjiang Oil & Gas,2010,6(3):17-22.
[20] 孙明亮,管红.鄂尔多斯盆地榆林气田上古生界成藏动力与油气分布[J]. 科技导报,2013,31(35):39-43. Sun Mingliang,Guan Hong. Characteristic of Hydrodynamic and Its Relation to Distribution of Hydrocarbon in Palaeizoic Yulin Gas Pool [J]. Science & Technology Review,2013,31(35):39-43.
[21] 过敏,李仲东,惠宽洋,等.储层压力与天然气分布关系:以鄂北塔巴庙地区上古生界储层为例[J]. 天然气工业,2007,27(4):15-18. Guo Min, Li Zhongdong, Hui Kuanyang, et al. Relationship Between Characteristics of Reservoir Pressure and Distribution of Natural Gas: An Example of Tabamiao Area, the Northern Ordos Basin[J]. Natural Gas Industry,2007,27(4):15-18.
[22] 李兴文,李仲东,过敏,等.鄂尔多斯麻黄山西区中生界过剩压力与油气关系[J]. 石油勘探与开发,2011,38(3):294-298. Li Xingwen, Li Zhongdong, Guo Min, et al. Relations of Overpressure and Hydrocarbons in the Mesozoic of Western Mahuangshan, Ordos Basin[J]. Petroleum Exploration and Development,2011,38(3):294-298.
[23] 王志欣,张金川.鄂尔多斯盆地上古生界深盆气成藏模式[J]. 天然气工业,2006,26(2):52-54. Wang Zhixin, Zhang Jinchuan. Mechanism of Deep Basin Gas Accumulation in the Upper Paleozoic in Ordos Basin [J]. Natural Gas Industry,2006,26(2):52-54.
[24] 杨华,刘新社,闫小雄,等.鄂尔多斯盆地神木气田的发现与天然气成藏地质特征[J]. 天然气工业,2015,35(6):1-13. Yang Hua, Liu Xinshe, Yan Xiaoxiong, et al. The Senmu Gas Field in the Ordos Basin: Its Discovery and Reservoir-Forming Geological Characteristics [J]. Natural Gas Industry,2015,35(6):1-13.
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