天然气地球科学
高级检索
作者投稿 专家审稿 编辑办公

天然气地球科学

• 天然气地质学 • 上一篇    下一篇

准噶尔盆地南部霍玛吐构造带古近系紫泥泉子组储层发育特征与控制因素分析

白振华，姜振学，宋岩，赵孟军，方世虎，张健   

  1. 1.中国石油大学( 北京)， 北京 102249； 2.中国石油勘探开发研究院，北京 100083； 3.中国石油天然气集团公司盆地构造与油气成藏重点实验室，北京 100083; 4.中国石油新疆油田分公司勘探开发研究院地物所，新疆 乌鲁木齐 830013
  • 收稿日期:2012-10-16 修回日期:2012-11-20 出版日期:2013-04-10 发布日期:2013-04-10
  • 通讯作者: 白振华baizhh@163.com. E-mail:baizhh@163.com.
  • 作者简介:白振华(1982-)，男，河北保定人，在站博士后，主要从事储层地质学与油气成藏综合研究. E-mail：baizhh@163.com.
  • 基金资助:

    国家科技重大专项(编号：2011ZX05003-001)“中西部前陆盆地大型油气田形成、分布与区带评价”资助.

The Reservoir Characteristics and Its Main Controlling Factor Discussion in Ziniquanzi Formation of Huomatu Tectonic Zone,Southern Junggar Fold-thrust Belt

BAI Zhen-hua, JIANG Zhen-xue, SONG Yan, ZHAO Meng-jun, FANG Shi-hu, ZHANG Jian   

  1. 1.China University of Petroleum, Beijing 102249, China; 2.PetroChina Research Institute of Petroleum Exploration and Development, Beijing 100083, China；3.PetroChina Key Laboratory of Basin Structure and Hydrocarbon Accumulation, Beijing 100083, China; 4.Institute of Geophysics of Research Institute of E and D, Xijiang Oilfield Company, Urumqi 830013, China
  • Received:2012-10-16 Revised:2012-11-20 Online:2013-04-10 Published:2013-04-10

PDF (PC)

559

摘要：

油气勘探与评价结果表明，储层发育的复杂性是除复杂构造变形特征与构造样式之外控制准南前陆盆地霍玛吐构造带油气成藏与油气分布的另一重要因素。从沉积相和岩石学特征入手，结合常规薄片观察、扫描电镜、压汞实验等分析成果，对霍玛吐构造带古近系紫泥泉组储层特征进行分析研究。结果表明,紫泥泉子组三段储层岩性主要为细砂岩和粉砂岩，岩石粒度偏细。由于沉积作用和成岩作用的共同控制，决定了霍玛吐构造带3个构造储层物性的差异性：玛纳斯背斜储层物性最好，孔渗分布模式呈现“后峰型‘’；霍尔果斯背斜储层物性中等，孔渗分布较均匀，呈现“双峰型”；而吐谷鲁背斜储层物性最差，孔隙度分布略呈现“双峰型‘’，渗透率分布则呈现“前峰型”。
 

关键词: 储层特征, 成岩作用, 控制因素, 古近系, 紫泥泉子组, 霍玛吐构造带

Abstract:

Oil and gas exploration and evaluation results show that the complexity of reservoir characteristics is another important factor beside of the complex tectonic deformation and style,which controlled the oil and gas accumulation and distribution of Huomatu tectonic zone in Southern Junggar fold-thrust belt.Based on the depositional facies and petrologic characteristics,combined with the results of conventional thin section,SEM,mercury injection test,reservoir characteristics of the Paleocene Ziniquanzi Formation in Huomatu tectonic zone were analyzed.The results suggest that the E1-2z3   reservoir is mainly composed of fine sandstone and siltstone with small grain size.Because of the controlling factor of both sedimentation and diagenesis,physical property differences exist in the three anticlines of Huomatu tectonic belt.The Manasi anticline reservoir has the best physical property,and the distribution of porosity and permeability appears“after peak type”.The porosity and permeability mainly concentrate in the range of 21% to 26% and 40×10-3μm2 to 640×10-3μm2 respectively,so the E1-2z3 reservoir quality in Manasi anticline is moderate-high porosity and permeability the Huoerguosi anticline reservoir has medium physical property,and the porosity and permeability distribution presents a “double peaks type” with the porosity mainly concentrating in the range of 5% to 9% and 12% to 20% and permeability of 0.16×10-3μm2    to 0.64×10-3μm2   and 1.25×10--3μm2   to 20×10-3μm2 .While the Tugulu anticline reservoir has the worst physical property and the similar porosity distribution with Huoerguosi anticline,whereas,the permeability distribution is characterized by “front peak type” with the peak between 0.16×10-3μm2   and 0.32×10-3μm2 .Consequently,the E1-2z3 reservoir qualities in these two anticlines are moderate porosity and moderate-low permeability generally.

Key words: Reservoir characteristics, Diagenesis, Controlling factor, Paleocene, Ziniquanzi Formation, Huomatu tectonic zone

中图分类号: 

  • TE122.2

［1］Jia Chengzao,He Dengfa,Lei Zhenyu,et al.Exploration of Thrust Belt in Foreland Basin［M］.Beijing:Petroleum Industry Press,2000.［贾承造,何登发,雷振宇,等.前陆冲断带油气勘探［M］.北京:石油工业出版社,2000.］

［2］[ZK（3#]Wei Guoqi,Li Benliang,Chen Hanlin,et al.Tectonics Features Study in Foreland Thrust and Fold Belt in Central and Western of China［M］.Beijing:Petroleum Industry Press,2008:1-164.［魏国齐,李本亮,陈汉林,等.中国中西部前陆盆地构造特征研究［M］.北京:石油工业出版社,2008:1-164.］

［3］Jia Chengzao,Song Yan,Wei Guoqi,et al.Geological features and petroleum accumulation in the foreland basins in central and western China［J］.Earth Science Frontiers,2005,12(3):3-13.［贾承造,宋岩,魏国齐,等.中国中西部前陆盆地的地质特征及油气聚集［J］.地学前缘,2005,12(3):3-13.］

［4］Song Yan,Fang Shihu,Zhao Mengjun,et al.The structural segmentation of foreland thrust belts and its implications for hydrocarbon accumulation in foreland basins in central and western China［J］.Earth Science Frontiers,2005,12(3):31-38.［宋岩,方世虎,赵孟军,等.前陆盆地冲断带构造分段特征及其对油气成藏的控制作用［J］.地学前缘,2005,12(3):31-38.］

［5］Chen Tao,Wei Dongtao,Yang Haibo,et al.The tectonic characteristics on the foreland thrust belt and its influence on reservoiring of oil and natural gas in southern Junggar basin［J］.Natural Gas Geoscience,2006,17(5):711-718.［陈涛,魏东涛,杨海波,等.准南前陆冲断带构造特征及其对油气成藏的影响［J］.天然气地球科学,2006,17(5):711-718.］

［6］Fang Shihu,Jia Chengzao,Song Yan,et al.Late Cenozoic structural deformation and its implication for petroleum accumulation in the southern Junggar thrust belt［J］.Acta Petrolei Sinica,2007,28(6):1-5.［方世虎,贾承造,宋岩,等.准南地区前陆冲断带晚新生代构造变形特征与油气成藏［J］.石油学报,2007,28(6):1-5.］

［7］Ablimit,Wu Xiaozhi,Li Chen,et al.Petroleum distribution and accumulation model in mid-segment of foreland thrust belt in southern Junggar basin［J］.Xinjiang Petroleum  Geology,2004,25(5):489-491.［阿布力米提,吴晓智,李臣,等.准南前陆冲断带中段油气分布规律及成藏模式［J］.新疆石油地质,2004,25(5):489-491.］

［8］Wei Dongtao,Zhao Yingcheng,Abulimiti,et al.Difference of hydrocarbon accumulation in the foreland thrust-fold belt of the southern Junggar basin［J］.Geological Journal of China Universities,2010,16(3):339-350.［魏东涛,赵应成,阿布力米提,等.准噶尔盆地南缘前陆冲断带油气成藏差异性分析［J］.高校地质学报,2010,16(3):339-350.］

［9］Hong Feng,Song Yan,Liu Shaobo,et al.A study on the source-reservoir-seal associations and matching of hydrocarbon accumulation factors in the foreland basins in central-western China［J］.Natural Gas Geoscience,2007,18(1):27-36.［洪峰,宋岩,柳少波,等.中国中西部前陆盆地生储盖组合及成藏基本要素匹配分析［J］.天然气地球科学,2007,18(1):27-36.］

［10］Wei Guoqi,Jia Chengzao,Li Benliang,et al.Particularity and diversity of the foreland basins in the central and western China and the natural gas exploration in the foreland basins［J］.Geological Journal of China Universities,2005,11(4):552-557.［魏国齐,贾承造,李本亮.我国中西部前陆盆地的特殊性和多样性及其天然气勘探［J］.高校地质学报,2005,11(4):552-557.］

［11］Li Shixiang,Hu Mingyi,Li Fuping.Diagenesis and porosity evolution of upper Triassic Xujiahe Formation sandstone in western Sichuan foreland basin［J］.Natural Gas Geoscience,2007,18(4):535-539.［李士祥,胡明毅,李浮萍.川西前陆盆地上三叠统须家河组砂岩成岩作用及孔隙演化［J］.天然气地球科学,2007,18(4):535-539.］

［12］Xiao Yan,Peng Jun,Zhang Jizhi,et al.Reservoir spaces of the second section of Xujiahe Formation and evolution in middle part of west Sichuan Foreland basin［J］.Natural Gas Geoscience,2012,23(1):501-507.［肖艳,彭军,张纪智,等.川西前陆盆地中段须家河组二段储层储集空间特征及演化［J］.天然气地球科学,2012,23(1):501-507.］

［13］Yu Xinghe.Basis of Hydrocarbon Reservoir Geology［M］.Beijing:Petroleum Industry Press,2009.［于兴河.油气储层地质学基础［M］.北京:石油工业出版社,2009.］

［14］Yang Jinglin,Shen Yixin.The temporal and spatial distribution of the Ziniquanzi Formation on the southern margin of the Junggar basin and the explanation of contributing factors［J］.Journal of Stratigraphy,2004,28(3):215-222.［杨景林,沈一新.准噶尔盆地南缘紫泥泉子组的时空展布及成因解释［J］.地层学杂志,2004,28(3):215-222.］

［15］Fang Shihu,Guo Zhaojie,Yan Song,et al.Sedimentary facies evolution and basin pattern of the Jurassic in southern margin area of Junggar basin［J］.Journal of Palaeogeography,2005,7(3):347-356.［方世虎,郭召杰,宋岩,等.准噶尔盆地南缘侏罗纪沉积相演化与盆地格局［J］.古地理学报,2005,7(3):347-356.］

［16］Shen Yulin,Guo Yinghai,Li Zhuangfu,et al.Sedimentary facies of Zinquanzi Formation of Paleogene in piedmont fault-fold zone of southern margin of Junggar basin［J］.Xinjiang Petroleum Geology,2008,29(6):716-718.［沈玉林,郭英海,李壮福,等.准噶尔盆地南缘山前断褶带紫泥泉子组沉积相［J］.新疆石油地质,2008,29(6):716-718.］

［17］Xiao Lixin,Chen Nenggui,Zhang Jian,et al.Sedimentary systems of Paleogene Ziniquanzi Formation,south edge of Junggar basin［J］.Natural Gas Geoscience,2011,22(3):426-431.［肖立新,陈能贵,张健,等.准噶尔盆地南缘古近系紫泥泉子组沉积体系分析［J］.天然气地球科学,2011,22(3):426-431.］

［18］Luo Chao,Yang Ju,Chen Wei,et al.Characteristics and types of sedimentary facies of Paleogene-Neogene in the middle segment of the southern margin of Junggar basin［J］.Journal of Chongqing University of Science and Technology:Natural Sciences Edition,2010,19(1):23-26.［罗超,杨菊,陈伟,等.准噶尔盆地南缘中段古近系—新近系沉积特征及沉积相类型［J］.重庆科技学院学报:自然科学版,2010,19(1):23-26.］

［19］Zhang Chuanlin,Zhao Xingmin,Wen Zhigang.Sedimentary chracteristics and reservoir quality of braided deltas in southern margin of Junggar basin［J］.Xinjiang Petroleum Geology,2003,24(3):202-204.［张传林,赵省民,文志刚.准噶尔盆地南缘辫状河三角洲沉积特征及储集性［J］.新疆石油地质,2003,24(3):202-204.］

［20］Editorial Committee of Petroleum Geology of China.Petroleum Geology of China:（Vo1.15）,Xinjiang Oil-Gas Field［M］.Beijing:Petroleum Industry Press,1993.［石油地质志编辑委员会.中国石油地质志:卷十五,新疆油气区(上册)准噶尔盆地［M］.北京:石油工业出版社,1993.］

［21］Ying Fengxiang,He Dongbo,Long Yumei,et al.SY/T 5477-2003:The Industry Standard of China and Division of Diagenetic Stages in Clastic Rocks［S］.Beijing:Petroleum Industry Press,2003.［应凤祥,何东博,龙玉梅,等.SY/T 5477-2003:中华人民共和国石油天然气行业标准并碎屑岩成岩阶段划分［S］.北京:石油工业出版社,2003.］

［22］Wu Xiaozhi,Song Zhigang.Tertiary reservoir characteristics and influence factor in western part of margin of Junggar basin［J］.Acta Petrolei Sinica,1994,15(4):23-30.［吴晓智,宋志刚.准噶尔盆地南缘西部第三系储集层特征及影响因素［J］.石油学报,1994,15(4):23-30.］

［23］Evans  B,Bernabe Y,Hirth G.Relations among porosity,permeability,and deformation in rocks at high temperatures［J］.Theoretical and Experimental Earth Science Series,2004:311-339.

［24］Qiu Nansheng,Wang Xulong,Yang Haibo,et al.The characteristics of temperature distribution in the Junggar basin［J］.Chinese Journal of Geology,2001,36(3):350-358.［邱楠生,王绪龙,杨海波,等.准噶尔盆地地温分布特征［J］.地质科学,2001,36(3):350-358.］

［25］Wang Shejiao,Hu Shengbiao,Wang Jiyang.The characteristics of heat flow and geothermal fields in Junggar basin［J］.Chinese Journal of Geophysics,2000,43(6):771-779.［王社教,胡圣标,汪集旸.准噶尔盆地热流及地温场特征［J］.地球物理学报,2000,43(6):771-779.］

［26］Gao Zhiyong,Hu Yongjun,Zhang Lihua,et al.The interpretation of the controlling action of Cretaceous to Tertiary tectonic compression on the reservoir in the southern margin of Junggar vitrinite reflectance and grain packing density［J］.Geology in China,2010,37(5):1336-1352.［高志勇,胡永军,张莉华,等.准噶尔南缘前陆盆地白垩纪—新近纪构造挤压作用与储层关系的新表征:镜质体反射率与颗粒填集密度［J］.中国地质,2010,37(5):1336-1352.］

［27］Zhang Liqiang,Luo Xiaorong,Liu Loujun,et al.Controls on clay mineral distribution in the cenozoic sediments of the southern Junggar basin,NW China［J］.Chinese Journal of Geology,2005,40(3):353-365.［张立强,罗晓容,刘楼军,等.准噶尔盆地南缘新生界黏土矿物分布及影响因素［J］.地质科学,2005,40(3):353-365.］
[1] 李梦茹,唐友军,刘岩,胡辉,贺其川. 江陵凹陷不同地区原油地球化学特征及油源对比[J]. 天然气地球科学, 2018, 29(9): 1240-1251.
[2] 朱立文，王震亮，张洪辉. 鄂尔多斯盆地乌审召地区山2亚段致密气“甜点”控因分析[J]. 天然气地球科学, 2018, 29(8): 1085-1093.
[3] 李红哲,马峰,谢梅,杨巍,张成娟,王朴,赵健. 柴达木盆地阿尔金东段基岩气藏盖层特征及控藏机制#br# [J]. 天然气地球科学, 2018, 29(8): 1102-1110.
[4] 吕正祥，王先东，吴家洋，卿元华. 渤海海域中部古近系湖相碳酸盐岩储层成岩演化特征[J]. 天然气地球科学, 2018, 29(7): 921-931.
[5] 王珊，曹颖辉，杜德道，王石，李洪辉，董洪奎，严威，白莹. 塔里木盆地柯坪—巴楚地区肖尔布拉克组储层特征与主控因素[J]. 天然气地球科学, 2018, 29(6): 784-795.
[6] 倪新锋，沈安江，韦东晓，乔宇婷，王莹. 碳酸盐岩沉积学研究热点与进展：AAPG百年纪念暨2017年会及展览综述[J]. 天然气地球科学, 2018, 29(5): 729-742.
[7] 王国龙，杜社宽. 准噶尔盆地北三台凸起二叠系梧桐沟组一段碎屑岩储层特征及控制因素[J]. 天然气地球科学, 2018, 29(5): 675-681.
[8] 钟 佳，尤丽，张迎朝，曲希玉，代龙，吴仕玖. 琼东南盆地乐东—陵水凹陷黄流组峡谷水道储层成岩作用与孔隙演化[J]. 天然气地球科学, 2018, 29(5): 708-718.
[9] 胡向阳，李宏涛，史云清，肖开华，郭艳东，李浩，高君. 川西坳陷斜坡带蓬莱镇组三段沉积特征与储层分布——以什邡地区JP32砂组为例[J]. 天然气地球科学, 2018, 29(4): 468-480.
[10] 杨丽杰，侯读杰，陈晓东，刁慧. 东海盆地西湖凹陷中部古近系地层水化学特征及地质意义[J]. 天然气地球科学, 2018, 29(4): 559-571,596.
[11] 李国欣, 易士威, 林世国, 高阳, 李明鹏, 李德江, 王昌勇. 塔里木盆地库车坳陷东部地区下侏罗统储层特征及其主控因素[J]. 天然气地球科学, 2018, 29(10): 1506-1517.
[12] 肖敦清, 姜文亚, 蒲秀刚, 王娜, 岳云福, 孙超囡, 代昆, 滑双君. 渤海湾盆地歧口凹陷中深层天然气成藏条件与资源潜力[J]. 天然气地球科学, 2018, 29(10): 1409-1421.
[13] 王媛,林畅松,李浩,孙彦达,何海全,王清龙,姬牧野,张曼莉. 高频层序地层格架中碳酸盐岩成岩作用研究——以哈萨克斯坦Marsel探区下石炭统谢尔普霍夫阶为例[J]. 天然气地球科学, 2018, 29(1): 28-41.
[14] 贾成业,贾爱林,韩品龙,王建君,袁贺,乔辉. 四川盆地志留系龙马溪组优质页岩储层特征与开发评价[J]. 天然气地球科学, 2017, 28(9): 1406-1415.
[15] 任丽华，代俊杰，林承焰，曹铮. 松辽盆地扶新隆起带南部青山口组超压特征及油气地质意义[J]. 天然气地球科学, 2017, 28(7): 1020-1030.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
No Suggested Reading articles found!