天然气地球科学

• 天然气地质学 • 上一篇    下一篇

鄂尔多斯盆地延长组深水砂岩储层岩石学特征及地质意义

龙礼文,李相博,刘广林,廖建波,赵园园,李智勇   

  1. 1.中国石油勘探开发研究院西北分院,甘肃 兰州 730020;
    2.中国石油长庆油田分公司勘探开发研究院,陕西 西安 710018;
    3.中国石油大学(北京)油气资源与探测国家重点实验室,北京 102249
  • 收稿日期:2014-04-14 修回日期:2014-12-02 出版日期:2015-04-10 发布日期:2015-04-10
  • 作者简介:龙礼文(1982-),男,湖北监利人,工程师,主要从事石油地质学研究. E-mail:llw_0401@163.com.
  • 基金资助:

    国家科技重大专项“鄂尔多斯盆地大型岩性地层油气藏勘探开发示范工程”(编号:2008ZX050442-8-2)资助.

Reservoir Petrology and Geological Significance ofDeep Water Sandstone of Chang 6 Formation in Ordos Basin

LONG Li-wen,LI Xiang-bo,LIU Guang-lin,LIAO Jian-bo,ZHAO Yuan-yuan,LI Zhi-yong   

  1. 1.Northwest Branch,PetroChina Research Institute of Exploration and Development,Lanzhou 730020,China;
    2.Institute of Exploration and Development of Changqing Oilfield,PetroChina,Xi′an 710018,China;
    3.State Key Laboratory of Petroleum Resources and Prospecting,China University of Petroleum(Beijing),Beijing 102249,China
  • Received:2014-04-14 Revised:2014-12-02 Online:2015-04-10 Published:2015-04-10

摘要:

以湖盆中心典型露头剖面及成熟井区为研究对象,依据室内分析化验手段,对鄂尔多斯盆地延长组深水砂岩储层岩石学特征进行了综合分析。研究发现延长期湖盆中心不同部位深水砂岩组分、矿物成分、填隙物类型及含量都存在明显的区别,甚至同一类型岩石中矿物含量也存在差异。这种岩石学特征上的差异主要受盆地周缘不同沉积物源体系的控制,反映了不同物源条件下的母岩性质。岩石学特征研究能对深水砂岩类型及储层条件进行评价,为盆地油气勘探开发提供科学依据。

关键词: 储层岩石学, 沉积体系, 深水砂岩, 鄂尔多斯盆地

Abstract:

Based on the analysis of typical outcrops and well areas,combined with indoor test data,the reservoir petrology of deep water sandstone of Chang 6 Formation in Ordos Basin has been investigated.The result shows that it varies greatly in different places,involving sandstone component,mineral composition,interstitial material component and their contents.Moreover,the mineral contents have a wide difference in the same type of sandstone.These differences are controlled by sedimentary source systems in the margin of Ordos Basin.It reflects the different nature of source rocks.The study of reservoir petrology can estimate the type of deep water sandstone and reservoir conditions,also provide the basis for exploration and development of oil and gas in the basin.

Key words: Reservoir petrology, Sedimentary systems, Deep water sandstone, Ordos Basin

中图分类号: 

  • TE122.2

[1]Shanmugam G.New Perspectives on Deep-water Sandstones:Origin,Recognition and Reservoir Quality[M].Amsterdam:Elsevier,2012.
[2]Li Xiangbo,Chen Qilin,Liu Huaqing,et al.Three types of sediment gravity flows and their petroliferous features of Yanchang Formation in Ordos Basin[J].Lithologic Reservoirs,2010,22(3):16-20.[李相博,陈启林,刘化清,等.鄂尔多斯盆地延长组3种沉积物重力流及其含油气性[J].岩性油气藏,2010,22(3):16-20.]
[3]Zou Caineng,Zhao Zhengzhang,Yang Hua,et al.Genetic mechanism and distribution of sandy debris flows in terrestrial lacustrine basin[J].Acta Sedimentologica Sinica,2009,27(6):1066-1071.[邹才能,赵政璋,杨华,等.陆相湖盆深水砂质碎屑流成因机制与分布特征[J].沉积学报,2009,27(6):1066-1071.]
[4]Shanmugam G.Ten turbidite myths[J].Earth Science Reviews,2002,58:311-341.
[5]Li Xiangbo,Liu Huaqing,Wan Yanrong,et al.First discovery of the sandy debris flow from the Triassic Yanchang Formation in Ordos Basin[J].Lithologic Reservoirs,2009,21(4):20-21.[李相博,刘化清,完颜容,等.鄂尔多斯盆地三叠系延长组砂质碎屑流储集体的首次发现[J].岩性油气藏,2009,21(4):20-21.]
[6]Fu Jinhua,Li Shixiang,Liu Xianyang.Geological theory and practice of petroleum exploration in the Ordos Basin[J].Natural Gas Geoscience,2013,24(6):1092-1096.[付金华,李士祥,刘显阳.鄂尔多斯盆地石油勘探地质理论与实践[J].天然气地球科学,2013,24(6):1092-1096.]
[7]Wang Feng,Tian Jingchun,Fan Liyong,et al.Evolution of sedimentary fillings in Triassic Yanchang Formation and its response to Indosinian Movement in Ordos Basin[J].Natural Gas Geoscience,2010,21(6):883-887.[王峰,田景春,范立勇,等.鄂尔多斯盆地三叠系延长组沉积充填演化及其对印支构造运动的响应[J].天然气地球科学,2010,21(6):883-887.]
[8]Liu Huaqing,Yuan Jianying,Li Xiangbo,et al.Lake basin evolution of Ordos Basin during Middle-Late Triassic and its origin analysis[J].Lithologic Reservoirs,2007,19(1):52-62.[刘化清,袁剑英,李相博,等.鄂尔多斯盆地延长期湖盆演化及其成因分析[J].岩性油气藏,2007,19(1):52-62.]
[9]Deng Xiuqin,Lin Fangxiao,Liu Xianyang,et al.Discussion on relationship between sedimentary evolution of the Triassic Yanchang Formation and the Early Indosinian Movement in Ordos Basin[J].Journal of Palaeogeography,2008,10(2):156-166.[邓秀芹,蔺昉晓,刘显阳,等.鄂尔多斯盆地三叠系延长组沉积演化及其与早印支运动关系的探讨[J].古地理学报,2008,10(2):156-166.]
[10]Zhao Wenzhi,Wang Xinmin,Guo Yanru,et al.Restoration and tectonic reworking of the Late Triassic basin in western Ordos Basin[J].Petroleum Exploration and Development,2006,33(1):6-13.[赵文智,王新民,郭彦如,等.鄂尔多斯盆地西部晚三叠世原型盆地恢复及其改造演化[J].石油勘探与开发,2006,33(1):6-13.]
[11]He Jing,Feng Shengbin,Yuan Xiaoqi,et al.Sandstone component of outcrops of Yanchang Formation in the margin of Ordos Basin and its geological significance[J].Lithologic Reservoirs,2011,23(6):31-37.[贺静,冯胜斌,袁效奇,等.鄂尔多斯盆地周缘延长组露头剖面砂岩组分及地质意义分析[J].岩性油气藏,2011,23(6):31-37.]
[12]Liao Jiangbo,Li Zhiyong,Long Liwen,et al.The effect of provenance intersection on the petroleum enrichment[J].Xingjiang Petroleum Geology,2014,34(1):21-23.[廖建波,李智勇,龙礼文,等.物源交汇作用对油气富集的影响[J].新疆石油地质,2014,34(1):21-23.]
[13]Zhao Chenglin,Zhu Xiaomin.Sedimentary Petrology[M].Beijing:Petroleum Industry Press,2001:41-55.[赵澄林,朱筱敏.沉积岩石学[M].北京:石油工业出版社,2001:41-55.]
[14]Li Xiangbo,Wei Pingsheng,Liu Huaqing,et al.Discussion on the classification of sediment gravity flow and the deep-water sedimentary model[J].Geological Review,2013,59(4):609-612.[李相博,卫平生,刘化清,等.浅谈沉积物重力流分类及深水沉积模式[J].地质论评,2013,59(4):609-612.]
[15]Fu Jinhua,Deng Xiuqin,Zhang Xiaolei,et al.Relationship between deep water sand-stone and tight oil of the Triassic Yanchang Formation in Ordos Basin[J].Journal of Palaeogeography,2013,15(5):625-633.[付金华,邓秀芹,张晓磊,等.鄂尔多斯盆地三叠系延长组深水砂岩与致密油的关系[J].古地理学报,2013,15(5):625-633.]
[16]Zhang Shaonan,Ding Xiaoqi.Characters and causes of tight sandstones of Yanchang Formation in southern Ordos Basin[J].Journal of Chengdu University of Technology:Science and Technology Edition,2010,37(4):386-393.[张哨楠,丁晓琪.鄂尔多斯盆地南部延长组致密砂岩储层特征及其成因[J].成都理工大学学报:自然科学版,2010,37(4):386-393.]

[1] 刘琴琴,陈桂华,陈晓智,祝彦贺,杨小峰. 鄂尔多斯盆地L地区上古生界上石盒子组物源特征及其对储层的控制作用[J]. 天然气地球科学, 2018, 29(8): 1094-1101.
[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] 高崇龙,纪友亮,靳军,王剑,任影,曾力,王道伟,张昊,李谨杰. 古隆起埋藏期沟谷残丘地貌下沉积体系及油气藏发育模式——以准噶尔盆地腹部石南地区清水河组一段为例[J]. 天然气地球科学, 2018, 29(8): 1120-1137.
[4] 杨智峰,曾溅辉,韩菲. 鄂尔多斯盆地西南部延长组7段致密油充注影响因素分析[J]. 天然气地球科学, 2018, 29(7): 961-972.
[5] 王香增,张丽霞,姜呈馥,尹锦涛,高潮,孙建博,尹娜,薛莲花. 鄂尔多斯盆地差异抬升对长7页岩孔隙的影响——以东南部甘泉地区和南部渭北隆起地区为例[J]. 天然气地球科学, 2018, 29(5): 597-605.
[6] 杨超,贺永红,马芳侠,雷裕红,陈义国. 鄂尔多斯盆地南部三叠系延长组有机流体活动期次划分[J]. 天然气地球科学, 2018, 29(5): 655-664.
[7] 葛岩,朱光辉,万欢,潘新志,黄志龙. 鄂尔多斯盆地东缘紫金山侵入构造对上古生界致密砂岩气藏形成和分布的影响[J]. 天然气地球科学, 2018, 29(4): 491-499.
[8] 杨占龙,黄云峰,沙雪梅,吴青鹏,黄小鹏,郝彬. 吐哈盆地鄯善弧形带东翼中—下侏罗统沉积体系发育模式[J]. 天然气地球科学, 2018, 29(3): 349-357.
[9] 屈雪峰,周晓峰,刘丽丽,丁黎. 鄂尔多斯盆地古峰庄—麻黄山地区长82低渗透砂岩致密化过程分析[J]. 天然气地球科学, 2018, 29(3): 337-348.
[10] 魏新善,魏柳斌,任军峰,蔡郑红,周黎霞. 鄂尔多斯盆地下古生界风化壳气藏差异性[J]. 天然气地球科学, 2018, 29(2): 178-188.
[11] 陈跃,马东民,吴圣,李新虎,方世跃,郭晨. 鄂尔多斯盆地东缘煤系伴生泥页岩孔隙特征及主控因素[J]. 天然气地球科学, 2018, 29(2): 189-198.
[12] 姚泾利, 胡新友, 范立勇, 刘新社, 季海锟, . 鄂尔多斯盆地天然气地质条件、资源潜力及勘探方向[J]. 天然气地球科学, 2018, 29(10): 1465-1474.
[13] 张建勇,倪新峰,吴兴宁,李文正,郝毅,陈娅娜,吕学菊,谷明峰,田瀚,朱茂. 中国主要克拉通盆地深层白云岩优质储层发育主控因素及分布[J]. 天然气地球科学, 2017, 28(8): 1165-1175.
[14] 王晖,张磊,石军太,张丽霞,高潮,张亮,郭超. 鄂尔多斯盆地东南部山西组泥页岩生烃热模拟实验[J]. 天然气地球科学, 2017, 28(7): 1078-1084.
[15] 杨智峰,曾溅辉,韩菲,冯枭,冯森,张译丹,乔俊程. 鄂尔多斯盆地西南部长6—长8段致密砂岩储层微观孔隙特征[J]. 天然气地球科学, 2017, 28(6): 909-919.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!