天然气地球科学 ›› 2011, Vol. 22 ›› Issue (2): 260–266.doi: 10.11764/j.issn.1672-1926.2011.02.260

• 天然气地质学 • 上一篇    下一篇

鄯勒地区西山窑组成岩作用及储层评价

崔立伟, 汤达祯, 王炜, 贾自力, 许浩, 李松, 陈晓智   

  1. 1.中国地质大学能源学院,北京 100083;2.吐哈油田分公司鄯善采油厂,新疆 鄯善 838202
  • 收稿日期:2010-06-27 修回日期:2010-08-11 出版日期:2011-04-10 发布日期:2011-04-10
  • 通讯作者: 崔立伟cuiliwei8855@163.com E-mail:cuiliwei8855@163.com
  • 作者简介:崔立伟(1984-),男,吉林松原人,硕士研究生,从事油气成藏机理与机制,煤层气地质与开发研究.
  • 基金资助:

    国家自然科学基金青年基金项目(编号:40802027);国家重点基础研究发展计划(“973”)项目(编号:2009CB219604)联合资助.

Diagenesis and Reservoir Evaluation of  Xishanyao Formation in Shanle Area#br# 

CUI Li-Wei, TANG Da-Zhen, WANG Wei, GU Zi-Li, HU Hao, LI Song, CHEN Xiao-Zhi   

  1. 1.Energy School of China University of Geosciences,Beijing 100083,China;
    2.Shanle Oil Production Company of Turpan Hami Oilfield Branch Company Ltd.,Shanle 838202,China.
  • Received:2010-06-27 Revised:2010-08-11 Online:2011-04-10 Published:2011-04-10

摘要:

通过岩心观察、薄片鉴定、扫描电镜分析、X-射线衍射分析等手段,对鄯勒地区西山窑组碎屑岩储层的成岩作用进行了研究。西山窑组成岩阶段可分为早成岩B期和中成岩A期,中成岩A期又分为中成岩A1亚期和A2亚期,识别出压实作用、胶结作用、交代作用和溶解作用等4种成岩作用;强烈的压实作用和胶结作用是造成储层原生孔隙减少的主要原因,溶解作用形成的次生溶孔则有效地改善了储层的物性。综合储层沉积、成岩作用,可将西山窑组碎屑岩储层划分为3种类型,其中,Ⅰ类储层为低孔特低渗型,Ⅱ类储层和Ⅲ类储层为特低孔特低渗型。

关键词: 鄯勒地区, 碎屑岩储层, 成岩作用, 储层评价

Abstract:

Here we studied the diagenesis characteristics and pore evolution of clastic reservoirs in the Xishanyao Formation of Shanle area by methods of core observation,slices arbitration,scanning electron microscopy and X-diffraction analysis. The diagenetic phases of the Xishanyao Formation included early diagenetic B stage and middle diagenetic A stage which was divided into A1 stage and A2 stage. The diagenesis can be divided into four types,including compaction,cementation,replacement and solution. The intense compaction and cementation were main reasons causing decrease in primary porosity,and the solution improved the reservoir physical properties effectively by developing the secondary porosity. Comprehensively considering the sedimentary and diagenesis on clastic reservoirs,the clastic reservoirs were divided into three categories,of which type Ⅰ was low porosity and the lowest permeability reservoir,and type Ⅱ and Ⅲ were the lowest porosity and permeability reservoir.

Key words: Shanle area, Clastic reservoir, Diagenesis, Reservoir evaluation.

中图分类号: 

  • TE122

[1] Zhang Huquan,Yu Junmin,Li Zaiguang,et al.Application of gas pool integrated description technique in Tertiary shallow gas pool in Shanle area,Turpan basin[J].Natural Gas Geoscience,2004,15(1):62-67.[张虎权,于均民,李在光,等.气藏综合描述在吐哈盆地鄯勒地区第三系浅层气藏描述中的应用[J].天然气地球科学,2004,15(1):62-67.]
[2]Zheng Leiqing.Identification methods for shallow gas formation in Shanle region,Tuha basin[J].Tuha Oil & Gas,2004,9(1):17-19.[郑雷清.吐哈盆地鄯勒地区浅层气层识别方法研究[J].吐哈油气,2004,9(1):17-19.]
[3]Li Zhuangfu,Guo Yinghai,Li Xizhe,et al.Diagenesis and its influence on property of reservoirs in Wangfu depression[J].Journal of China University of Mining & Technology,2001,31(1):94-98.[李壮福,郭英海,李熙哲,等.王府凹陷储集层成岩作用及对储集性能的影响[J].中国矿业大学学报,2001,31(1):94-98.]
[4]Qi Binwen, Lin Chunming,Qiu Guiqiang,et al.Reservoir diagenesis of the intermediate section in Member 3 of Shahejie Formation(Paleogene) in Niuzhuang sub-sag, Shandong province[J].Acta Sedimentologica Sinica,2007,25(1):98-109.[漆滨汶,林春明,邱桂强,等.山东省牛庄洼陷古近系沙河街组沙三中亚段储集层成岩作用研究[J].沉积学报,2007,25(1):98-109.]
[5]Chen Xin,Yuan Jing,Zhong Jianhua,et al.Clay minerals in clastic rock reservoir of deep formation in paleogene of Dongying sag[J].Journal of China University of Petroleum:Edition of Natural Science,2009,33(2):29-48.[陈鑫,袁静,钟建华,等.东营凹陷古近系深部碎屑岩储层中的黏土矿物[J].中国石油大学学报:自然科学版,2009,33(2):29-48.]
[6]Liu Baojun,Li Wei,Fu Jiankui,et al.Genesis of abnormal evolution of clay minerals at different diagenetic dtages in Taibei depression of Tuha basin[J].Earth Science:Journal of China University of Geosciences,2002,27(5):504-508.[刘宝珺,李伟,付建奎,等.吐哈盆地台北凹陷粘土矿物纵向异常演化与成因分析[J].地球科学:中国地质大学学报,2002,27(5):504-508.]
[7]Chen Guojun,Du Guichao,Zhang Gongcheng,et al.Diagenesis and main factors controlling the Tertiary reservoir properties of the Panyu low-uplift reservoirs,Pearl River Mouth basin[J].Natural Gas Geoscience,2009,20(6):854-861.[陈国俊,杜贵超,张功成,等.珠江口盆地番禺低隆起第三系储层成岩作用及物性影响因素分析[J].天然气地球科学,2009, 20(6):854-861.]
[8]Lian Chengbo,Zhong Jianhua,Yang Yufang,et al.Influence of Quan 4 Formation sandstone diagenesis on reservoir properties in Longxi region,Songliao basin[J].Natural Gas Geoscience,2009,20(5):692-694.[连承波,钟建华,杨玉芳,等.松辽盆地龙西地区泉四段砂岩成岩作用对储层物性的影响[J].天然气地球科学,2009, 20(5):692-694.]
[9]Zhou Haiyan, Hu Jianyi,Zheng Junzhang,et al.Diagenesis and pore evolution of reservoirs in south Turgai basin[J].Acta Petrologica et Mineralogica,2008,27(6):548-558.[周海燕,胡见义,郑俊章,等.南图尔盖盆地储层成岩作用及孔隙演化[J].岩石矿物学,2008, 27(6):548-558.]
[10]Feng Zengzhao. Sedimentary Petrology:The Second Edition,Book One[M].Beijing:Petroleum Industry Press,1993.[冯增昭.沉积岩石学:第二版,上册[M].北京:石油工业出版社,1993.]
[11]Ying Fengxiang,Wang Yangqi,Wang Keyu,et al.Reservoir Catalog in Petroleum of China,Volume One: Clastic Rock[M].Beijing:Petroleum Industry Press,1994.[应凤祥,王衍奇,王克玉,等.中国油气储层研究图集,卷一:碎屑岩[M].北京:石油工业出版社,1994.]
[12]Han Huijun,Lui Hua,Liu Changjiang,et al.Reservoir characteristics and their depositional control of the Permo-Carboniferous in Jiyang depression[J].Journal of China University of Mining & Technology,2007,36(4):522-526.[韩会军,刘华,刘长江,等.济阳坳陷石炭二叠系储层特征及其沉积控制[J].中国矿业大学学报,2007,36(4):522-526.]

[1] 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.
[2] 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.
[3] 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.
[4] 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.
[5] 刘小岑,林承焰,任丽华,马鹏杰,陈雁雁. 渤海湾盆地渤南洼陷北部沙四上亚段储层有利成岩相研究[J]. 天然气地球科学, 2017, 28(11): 1657-1667.
[6] 马明,陈国俊,李超,张功成,晏英凯,赵钊,沈怀磊. 珠江口盆地白云凹陷恩平组储层成岩作用与孔隙演化定量表征[J]. 天然气地球科学, 2017, 28(10): 1515-1526.
[7] 王淑芳,张子亚,董大忠,王玉满,李新景,胡俊文,黄金亮,管全中. 四川盆地下寒武统筇竹寺组页岩孔隙特征及物性变差机制探讨[J]. 天然气地球科学, 2016, 27(9): 1619-1628.
[8] 耳闯,赵靖舟,王芮,张杰,袁野,沈武显. 鄂尔多斯盆地三叠系延长组富有机质页岩孔隙特征及发育机制[J]. 天然气地球科学, 2016, 27(7): 1202-1214.
[9] 李军,胡东风,邹华耀,李平平. 四川盆地元坝_通南巴地区须家河组致密砂岩储层成岩—成藏耦合关系[J]. 天然气地球科学, 2016, 27(7): 1164-1178.
[10] 万青青,刘洛夫,肖飞,常敏,吴雅君,胡青. 准噶尔盆地车排子地区下白垩统清水河组储层成岩作用及物性影响因素[J]. 天然气地球科学, 2016, 27(7): 1264-1276.
[11] 杨宪彰,毛亚昆,钟大康,李勇,能源,孙海涛,刘云龙. 构造挤压对砂岩储层垂向分布差异的控制——以库车前陆冲断带白垩系巴什基奇克组为例[J]. 天然气地球科学, 2016, 27(4): 591-599.
[12] 李彦举,赵龙,史基安,张银,邹妞妞. 准噶尔盆地阜东斜坡区侏罗系三工河组碎屑岩成岩作用及孔隙演化[J]. 天然气地球科学, 2015, 26(S2): 44-51.
[13] 邹妞妞,庞雷,史基安,陈鑫,欧阳敏,张大权. 准噶尔盆地西北缘玛北地区百口泉组砂砾岩储层评价[J]. 天然气地球科学, 2015, 26(S2): 63-72.
[14] 孔令明,万茂霞,严玉霞,邹春艳,刘文平,田冲,易力. 四川盆地志留系龙马溪组页岩储层成岩作用[J]. 天然气地球科学, 2015, 26(8): 1547-1555.
[15] 朱华银,安来志,焦春艳. 恒速与恒压压汞差异及其在储层评价中的应用[J]. 天然气地球科学, 2015, 26(7): 1316-1322.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 李新虎, 王婷茹, 郭媛. HSS油田H1储层测井沉积微相研究[J]. 天然气地球科学, 2011, 22(2): 254 -259 .
[2] L.Sag, 朱岳年, . 匈亚利油气地质特征、开发历史及油气生产的经济作用[J]. 天然气地球科学, 1990, 1(1): 34 -36 .
[3] 郑民, 李建忠, 吴晓智, 王社教, 郭秋麟, 于京都, 郑曼, 陈宁生, 易庆. 我国常规与非常规天然气资源潜力、重点领域与勘探方向[J]. 天然气地球科学, 2018, 29(10): 1383 -1397 .
[4] 白雪峰, 梁江平, 张文婧, 付丽, 彭建亮, 薛涛, 杨立伟, 刘继莹. 松辽盆地北部深层天然气地质条件、资源潜力及勘探方向[J]. 天然气地球科学, 2018, 29(10): 1443 -1454 .