岩性油气藏 ›› 2015, Vol. 27 ›› Issue (6): 78–86.doi: 10.3969/j.issn.1673-8926.2015.06.011

• 油气地质 • 上一篇    下一篇

准东阜东斜坡区齐古组砂岩成岩作用研究

蒋艳霞 1,文华国 1,张 航 2,刘亚鹏 1,李 云 1,靳 军 3   

  1.  1. 成都理工大学 沉积地质研究院,成都 610059 ; 2. 中国石油西南油气田分公司 川东北气矿,四川 达州 635000 ; 3. 中国石油新疆油田分公司 实验检测研究院,新疆 克拉玛依 834000
  • 出版日期:2015-12-20 发布日期:2015-12-20
  • 第一作者:蒋艳霞( 1990- ),女,成都理工大学在读硕士研究生,研究方向为矿物学、岩石学及矿床学。 地址:( 610059 )四川省成都市成华区二仙桥东三路 1 号成都理工大学。 E-mail : jiangyanxia313@qq.com
  • 基金资助:

    中国石油新疆油田分公司项目“准东阜东斜坡区侏罗系齐古组储层精细研究”(编号: 2013-C4039 )资助

Diagenesis of sandstone reservoirs of Qigu Formation in Fudong slope area, eastern Junggar Basin

Jiang Yanxia 1,Wen Huaguo 1,Zhang Hang2,Liu Yapeng 1,Li Yun 1,Jin Jun 3   

  1.  1. Institute of Sedimentary Geology , Chengdu University of Technology , Chengdu 610059 , China ; 2. Northeastern Sichuan Gas Mine , PetroChina Southwest Oil & Gas Field Company , Dazhou 635000 , Sichuan , China ; 3. Research Institute of Experiment and Detection , PetroChina Xinjiang Oilfield Company , Karamay 834000 , Xinjiang , China
  • Online:2015-12-20 Published:2015-12-20

摘要:

侏罗系岩性油藏是准噶尔盆地阜东斜坡区非常重要的原油产层,探索储层主要成岩作用类型对该区齐古组油气勘探及开发具有重要意义。 利用铸体薄片、扫描电镜、X 射线衍射、阴极发光、镜质体反射率和物性分析等资料,对阜东斜坡区侏罗系齐古组砂岩成岩作用及其对储层物性的影响进行了研究。该区齐古组砂岩储层岩石类型主要为岩屑砂岩,其次为长石岩屑砂岩;成分成熟度较低,结构成熟度较高;主要成岩作用类型包括压实作用、胶结作用以及溶蚀作用,成岩演化阶段已达到中成岩阶段 A 期。 其中,建设性成岩作用主要包括部分绿泥石和伊利石包膜胶结作用和溶蚀作用,破坏性成岩作用主要包括压实作用以及方解石、凝灰质、方沸石和硅质胶结作用。该研究成果为进一步的岩性-地层油藏的储层预测提供了依据。

关键词: 油藏, 油井, 含水率, 见水, 非均质性, 底水, 边水

Abstract:

Jurassic lithologic reservoir is the main exploration layer in Fudong slope area of eastern Junggar Basin, so it is significant to study reservoir diagenesis for oil and gas exploration and development. Based on the analysis of thin sections, scanning electronic microscope, X-diffraction, cathodoluminescence, vitrinite reflectance and physical properties, the diagenesis and its influence on reservoir quality of Qigu Formation in Fudong slope area were detailly studied. The result shows that the sandstone reservoirs are mainly lithic sandstone, followed by feldspar lithic sandstone, which have low compositional maturity and high textural maturity. The main types of diagenetic include compaction, cementation and dissolution, and the diagenetic phase reached the middle diagenetic stage A. Among them, constructive diagenesis includes parts of chlorite envelope and illite envelope cementation and dissolution, while destructive diagenesis mainly includes compaction, multi-phase intense calcite cementation, tuffaceous cementation, siliceous cementation and analcime cementation. This study could provide reference for the reservoir prediction of lithologicstratigraphic reservoirs.

Key words: reservoir, well, water cut, water breakthrough, heterogeneity, bottom water, edge water, water flooding

[1]德勒恰提,王威,李宏,等.准噶尔盆地车排子凸起侏罗系齐古组沉积相分析及储层展布———以车 60 井区齐古组地层-岩性油气藏为例[J].沉积学报,2013,31(3):545-552.

Deleqiati,Wang Wei,Li Hong,et al. Facies of the Jurassic Qigu Formation and distribution of reservoir in the Chepaizi Uplift,Junggar Basin:A case study on Qigu Formation stratigraphic-lithologic reservoirs in well Che 60 block[J]. Acta Sedimentologica Sinica,2013,31(3):545-552.

[2]林潼,王东良,王岚,等.准噶尔盆地南缘侏罗系齐古组物源特征及其对储层发育的影响[J].中国地质,2013,40(3):909-918.

Lin Tong,Wang Dongliang,Wang Lan,et al. The provenance feature of Jurassic Qigu Formation and its effect on reservoir development in the southern margin of Junggar basin[J]. Geology in China,2013,40(3):909-918.

[3]文华国,贾斌,蒋宜勤,等.准噶尔盆地阜东斜坡头屯河组二段储层自然产能控制因素分析[J].岩性油气藏,2014,26(2):9-14.

Wen Huaguo,Jia Bin,Jiang Yinqin,et al. Controlling factors for natural productivity of the second member of Toutunhe Formation in eastern Fukang slope,Junggar Basin[J]. Lithologic Reservoirs,2014,26(2):9-14.

[4]靳军,文华国,向宝力,等.准噶尔盆地东部阜东斜坡头屯河组物源分析[J].岩性油气藏,2014,26(2):54-58.

Jin Jun,Wen Huaguo,Xiang Baoli,et al. Provenance analysis of Middle Jurassic Toutunhe Formation in eastern Fukang slope,Junggar Basin[J]. Lithologic Reservoirs,2014,26(2):54-58.

[5]李云,祁利 ,胡作维,等.准噶尔盆地阜东斜坡中侏罗统头屯河组储层敏感性特征[J].岩性油气藏,2014,26(1):52-57.

Li Yun,Qi Liqi,Hu Zuowei,et al. Reservoir sensitivity of Middle Jurassic Toutunhe Formation in eastern Fudong slope,Junggar Basin[J]. Lithologic Reservoirs,2014,26(1):52-57.

[6]牟中海,马力宁,马达德,等.柴达木盆地红柳泉构造下干柴沟组下段岩性油藏主控因素[J].中国石油勘探,2014,19(6):24-32.

Mou Zhonghai,Ma Lining,Ma Dade,et al. Main controlling factors of lithologic reservoirs of Lower Ganchaigou Formation below Hongliuquan structure of Qaidam Basin [J]. China Petroleum Exploration,2014,19(6):24-32.

[7]Pittman E D. Recent advances in sandstone diagenesis[J]. Annual Review of Earth & Planetary Sciences,2003,7(4):39-62.

[8]杨仁超,王秀平,樊爱萍,等.苏里格气田东二区砂岩成岩作用与致密储层成因[J].沉积学报,2012,30(1):111-119.

Yang Renchao,Wang Xiuping,Fan Aiping,et al. Diagenesis of sandstone and genesis of compact reservoirs in the eastⅡPart of Sulige Gas Field,Ordos Basin [J]. Acta Sedimentologica Sinica,2012,30(1):111-119.

[9]郑荣才,耿威,周刚,等.鄂尔多斯盆地白豹地区长 6 砂岩成岩作用与成岩相研究[J].岩性油气藏,2007,19(2):1-8.

Zheng Rongcai,Geng Wei,Zhou Gang,et al. Diagensis and diagenetic facies of Chang 6 sandstone of Yanchang Formation in Baibao area,Ordos Basin[J]. Lithologic Reservoirs,2007,19(2):1-8.

[10]谭先锋,田景春,李祖兵,等.东营凹陷古近系孔店组成岩特征及对储层的控制[J].煤田地质与勘探,2010,38(6):27-32.

Tan Xianfeng,Tian Jingchun,Li Zhubing,et al. Diagenetic character and controlling factor of reservoir of Kongdian Formation of Paleogene in Dongying basin[J]. Coal Geology & Exploration,2010,38(6):27-32.

[11]文华国,郑荣才,陈洪德,等.鄂尔多斯盆地白豹—华池地区长6 砂岩储层特征[J].石油学报,2007,28(4):46-51.

Wen Huaguo,Zheng Rongcai,Chen Hongde,et al. Characteristics of Chang 6 sandstone reservoir in Baibao-Huachi region of Ordos Basin[J]. Acta Petrolei Sinica,2007,28(4):46-51.

[12]郑荣才,王海红,侯长冰,等.陇东地区长 9 油层组砂岩储层成岩作用精细研究[J].岩性油气藏,2014,26(1):1-9.

Zheng Rongcai,Wang Haihong,Hou Changbing,et al. Diagenesis of sandstone reservoir of Chang 9 oil reservoir set in Longdong area, Ordos Basin[J]. Lithologic Reservoirs,2014,26(1):1-9.

[13]林良彪,余瑜,高健,等.川南地区须家河组砂岩储层主控因素[J].成都理工大学学报:自然科学版,2015,42(4):400-409.

Lin Liangbiao,Yu Yu,Gao Jian,et al. Main controlling factors of Xujiahe Formation sandstone reservoir in South Sichuan,China[J]. Journal of Chengdu University of Technology:Science and Technology,2015,42(4):400-409.

[14]谭先锋,田景春,林小兵,等.陆相断陷盆地深部碎屑岩成岩演化及控制因素:以东营断陷盆地古近系孔店组为例[J].现代地质,2010,24(5):934-944.

Tan Xianfeng,Tian Jingchun,Lin Xiaobin,et al. Diagenetic evolution and controlling factors of deep-seated clastic rocks in terretrial fault-depressed basin:Taking the Kongdian Formation of Dongying fault-depressed basin for example[J]. Geoscience, 2010, 24(5): 934-944.

[15]张金亮,张鹏辉,谢俊,等.碎屑岩储集层成岩作用研究进展与展望[J].地球科学进展,2013,28(9):957-967.

Zhang Jinliang,Zhang Penghui,Xie Jun,et al. Diagenesis of clastic reservoirs:Advances and prospects[J]. Advances in Earth Science, 2013,28(9):957-967.

[16]郑浚茂,庞明.碎屑储集岩的成岩作用研究[M].武汉:中国地质大学出版社,1989.

Zheng Junmao,Pang Ming. Diagenesis of clastic reservoirs[J]. Wuhan:China University of Geosciences Press,1989.

[17]祝海华,钟大康,姚泾利,等.碱性环境成岩作用及对储集层孔隙的影响———以鄂尔多斯盆地长 7 段致密砂岩为例[J].石油勘探与开发,2015,42(1):51-59.

Zhu Haihua,Zhong Dakang,Yao Jingli,et al. Alkaline diagenesis and its effects on reservoir porosity:A case study of Upper Triassic Chang 7 tight sandstones in Ordos Basin,NW China[J]. Petroleum Exploration and Development,2015,42(1):51-59.

[18]张琴,朱筱敏,张满郎,等.准噶尔盆地阜东斜坡区侏罗系层序地层格架的建立[J].沉积学报,2001,19(4):575-580.

Zhang Qin,Zhu Xiaomin,Zhang Manlang,et al. Sequence stratigraphic frame of Jurassic in east Fukang slope,Junggar Basin[J].Acta Sedimentologica Sinica,2001,19(4):575-580.

[19]张义杰.准噶尔盆地水岩反应产物的地球化学特征[J].新疆石油地质,2002,23(6):482-484.

Zhang Yijie. The geochemical characteristics of water rock interaction products in Junggar Basin[J]. Xinjiang Petroleum Geology, 2002,23(6):482-484.

[20]王宏语,樊太亮,肖莹莹,等.凝灰质成分对砂岩储集性能的影响[J].石油学报,2010,31(3):432-439.

Wang Hongyu,Fan Tailiang,Xiao Yingying,et al. Effect of tuffaceous components on physical property of sandstone reservoir[J].Acta Petrolei Sinica,2010,31(3):432-439.

[21]朱世发,朱筱敏,王一博,等.准噶尔盆地西北缘克百地区三叠系储层溶蚀作用特征及孔隙演化[J].沉积学报,2010,28(3):547-555.

Zhu Shifa,Zhu Xiaomin,Wang Yibo,et al. Dissolution characteristics and pore evolution of Triassic reservoir in Ke-Bai area,northwestern margin of Junggar Basin[J]. Acta Sedimentologica Sinica, 2010,28(3):547-555.

[22]Morad S,Khalid A R,Ketzer J M,et al. The impact of diagenesis on the heterogeneity of sandstone reservoirs:A review of the role of depositional facies and sequence stratigraphy[J]. AAPG Bulletin,2010,94(8):1267-1309.

[23]Surdam R C,Crossey L J,Sven Hagen E,et al. Organic-inorganic interactions and sandstone diagenesis[J]. AAPG Bulletin,1989, 73(1):1-23.

[24]Saigal G C,Bjorlykke K,Larter S. The effect of oil emplacement on diagenetic processes:Examples from the Fulmar reservoir sandstones,Central North Sea[J]. AAPG Bulletin,1992,76(7):1024-1033.

[25]Giles M R,de Boer R B. Origin and significance of redistributional secondary porosity[J]. Marine and Petroleum Geology,1990,7(3): 378-397.

[26]赖兴运,于炳松,陈军元,等.碎屑岩骨架颗粒溶解的热力学条件及其在克拉 2 气田的应用[J].中国科学:地球科学,2004,34(1):45-53.

Lai Xingyun,Yu Bingsong,Chen Junyuan,et al. The thermodynamic condition of rock fragment dissolution and its application in Kela 2 gas field[J]. Science in China (Series D):Earth Sciences, 2004,34(1):45-53.

[27]黄思静,黄可可,冯文立,等.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[J].地球化学,2009,38(5):498-506.

Huang Sijing,Huang Keke,Feng Wenli,et al. Mass exchanges among feldspar,kaolinite and their influences on secondary porosity formation in clastic diagenesis—A case study on the Upper Paleozoic,Ordos Basin and Xujiahe Formation,Wesern Sichuan Depression[J]. Geochimica,2009,38(5):498-506.

[28]应凤祥,何东博,龙玉梅,等. SY/T 5477—2003 碎屑岩成岩阶段划分[S].北京:石油工业出版社,2003:1-14.

Ying Fengxiang,He Dongbo,Long Yumei,et al. SY/T 5477-2003 Division of clastic diagenetic stage[S]. Beijing:Petroleum Industry Press,2003:1-14.

[29] 杜红权,朱如凯,何幼斌,等.合川地区须二段砂岩储层成岩作用及其对储层的影响[J].岩石矿物学杂志,2012,31(3):403-411.

Du Hongquan,Zhu Rukai,He Youbin,et al. The diagenesis of the 2nd member reservoirs of Xujiahe Formation and its influence on reservoirs of Hechuan area[J]. Acta Petrologica et Mineralogica, 2012,31(3):403-411.

[1] 洪智宾, 吴嘉, 方朋, 余进洋, 伍正宇, 于佳琦. 纳米限域下页岩中可溶有机质的非均质性及页岩油赋存状态[J]. 岩性油气藏, 2024, 36(6): 160-168.
[2] 程焱, 王波, 张铜耀, 齐玉民, 杨纪磊, 郝鹏, 李阔, 王晓东. 渤中凹陷渤中A-2区新近系明化镇组岩性油气藏油气运移特征[J]. 岩性油气藏, 2024, 36(5): 46-55.
[3] 卢科良, 吴康军, 李志军, 孙永河, 徐少华, 梁锋, 刘露, 李爽. 川中古隆起北斜坡寒武系龙王庙组油气成藏特征及演化模式[J]. 岩性油气藏, 2024, 36(4): 159-168.
[4] 唐述凯, 郭天魁, 王海洋, 陈铭. 致密储层缝内暂堵转向压裂裂缝扩展规律数值模拟[J]. 岩性油气藏, 2024, 36(4): 169-177.
[5] 秦正山, 何勇明, 丁洋洋, 李柏宏, 孙双双. 边水气藏水侵动态分析方法及水侵主控因素[J]. 岩性油气藏, 2024, 36(4): 178-188.
[6] 杨为华. 松辽盆地双城断陷白垩系营城组四段致密油成藏主控因素及模式[J]. 岩性油气藏, 2024, 36(4): 25-34.
[7] 钟会影, 余承挚, 沈文霞, 毕永斌, 伊然, 倪浩铭. 考虑启动压力梯度的致密油藏水平井裂缝干扰渗流特征[J]. 岩性油气藏, 2024, 36(3): 172-179.
[8] 刘仁静, 陆文明. 断块油藏注采耦合提高采收率机理及矿场实践[J]. 岩性油气藏, 2024, 36(3): 180-188.
[9] 李启晖, 任大忠, 甯波, 孙振, 李天, 万慈眩, 杨甫, 张世铭. 鄂尔多斯盆地神木地区侏罗系延安组煤层微观孔隙结构特征[J]. 岩性油气藏, 2024, 36(2): 76-88.
[10] 尹路, 许多年, 乐幸福, 齐雯, 张继娟. 准噶尔盆地玛湖凹陷三叠系百口泉组储层特征及油气成藏规律[J]. 岩性油气藏, 2024, 36(1): 59-68.
[11] 周浩, 梁利侠. 水平井探测半径计算方法[J]. 岩性油气藏, 2024, 36(1): 157-168.
[12] 白佳佳, 司双虎, 陶磊, 王国庆, 王龙龙, 史文洋, 张娜, 朱庆杰. DES+CTAB复配驱油剂体系提高低渗致密砂岩油藏采收率机理[J]. 岩性油气藏, 2024, 36(1): 169-177.
[13] 马文杰, 王景春, 田作基, 马中振, 万学鹏, 林金逞, 许翔麟, 周玉冰. 南美洲Oriente盆地斜坡带W区块构造-岩性复合油藏成藏模式及有利区预测[J]. 岩性油气藏, 2023, 35(6): 29-36.
[14] 马峰, 庞文珠, 赵文光, 张斌, 赵艳军, 薛罗, 郑茜, 陈彬滔. 南苏丹境内裂谷盆地源上构造-岩性油藏成藏主控因素与成藏模式[J]. 岩性油气藏, 2023, 35(6): 92-105.
[15] 胡望水, 高飞跃, 李明, 郭志杰, 王世超, 李相明, 李圣明, 揭琼. 渤海湾盆地廊固凹陷古近系沙河街组油藏单元精细表征[J]. 岩性油气藏, 2023, 35(5): 92-99.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] . 2022年 34卷 2 期 封面[J]. 岩性油气藏, 2022, 34(2): 0 .
[2] 李在光, 李琳. 以井数据为基础的AutoCAD 自动编绘图方法[J]. 岩性油气藏, 2007, 19(2): 84 -89 .
[3] 程玉红, 郭彦如, 郑希民, 房乃珍, 马玉虎. 井震多因素综合确定的解释方法与应用效果[J]. 岩性油气藏, 2007, 19(2): 97 -101 .
[4] 刘俊田,靳振家,李在光,覃新平,郭 林,王 波,刘玉香. 小草湖地区岩性油气藏主控因素分析及油气勘探方向[J]. 岩性油气藏, 2007, 19(3): 44 -47 .
[5] 商昌亮,付守献. 黄土塬山地三维地震勘探应用实例[J]. 岩性油气藏, 2007, 19(3): 106 -110 .
[6] 王昌勇, 郑荣才, 王建国, 曹少芳, 肖明国. 准噶尔盆地西北缘八区下侏罗统八道湾组沉积特征及演化[J]. 岩性油气藏, 2008, 20(2): 37 -42 .
[7] 王克, 刘显阳, 赵卫卫, 宋江海, 时振峰, 向惠. 济阳坳陷阳信洼陷古近纪震积岩特征及其地质意义[J]. 岩性油气藏, 2008, 20(2): 54 -59 .
[8] 孙洪斌, 张凤莲. 辽河坳陷古近系构造-沉积演化特征[J]. 岩性油气藏, 2008, 20(2): 60 -65 .
[9] 李传亮. 地层抬升会导致异常高压吗?[J]. 岩性油气藏, 2008, 20(2): 124 -126 .
[10] 魏钦廉,郑荣才,肖玲,马国富,窦世杰,田宝忠. 阿尔及利亚438b 区块三叠系Serie Inferiere 段储层平面非均质性研究[J]. 岩性油气藏, 2009, 21(2): 24 -28 .