天然气地球科学

• 天然气地质学 • 上一篇    下一篇

塔里木盆地牙哈_英买力寒武系潜山区优质储层形成模式

张德民1,鲍志东2,郝雁3,杨飞2,陈敏4,仲向云5   

  1. 1.中国石化石油勘探开发研究院,北京 100083;
    2.中国石油大学(北京),北京 102249;
    3.中国石化集团国际石油勘探开发有限公司,北京 100029;
    4.国土资源部油气资源战略研究中心,北京 100034;5.中国石油长庆油田勘探开发研究院,陕西 西安 710018
  • 收稿日期:2016-01-18 修回日期:2016-04-17 出版日期:2016-10-10 发布日期:2016-10-10
  • 通讯作者: 鲍志东(1964-),男,安徽巢湖人,教授,主要从事沉积学及石油地质学研究. E-mail:〖WTBZ〗baozhd@cup.edu.cn.
  • 作者简介:张德民(1983-),男,山东曹县人,博士后,主要从事碳酸盐岩沉积及储层研究. E-mail:〖WTBZ〗zhangdm125@foxmail.com.
  • 基金资助:
    国家科技重大专项“大型油气田及煤层气开发”(编号:2011ZX05004-004-007);中国博士后科学基金(编号:2016M591352)联合资助.

Formation model of high-quality reservoirs within Cambrian buried hillin Yaha-Yingmaili area,Tarim Basin

Zhang De-min1,Bao Zhi-dong2,Hao Yan3,Yang Fei2,Chen Min4,Zhong Xiang-yun5   

  1. 1.Sinopec Research Institute of Petroleum Exploration & Production,Beijing 100083,China;
    2.China University of Petroleum(Beijing),Beijing 102249,China;3.Sinopec Overseas Oil & Gas Ltd.,Beijing 100029,China;
    4.Strategic Research Center of Oil and Gas Resources’ Ministry of Land and Resources,Beijing 100034,China;
    5.Research Institute of Petroleum Exploration and Development Changqing Oilfield,CNPC,Xi’an 710018,China
  • Received:2016-01-18 Revised:2016-04-17 Online:2016-10-10 Published:2016-10-10

摘要: 碳酸盐岩潜山是国内外油气勘探的热点领域,为探讨长期抬升淋滤区多期岩溶的剥离问题,明确潜山优质储层形成演化模式,以塔里木盆地牙哈_英买力寒武系潜山为研究对象,在系统分析储层岩石类型、储集空间类型、储层物性特征的基础上,探讨储层主控因素,建立优质储层形成模式。研究发现:牙哈_英买力地区储层岩性以晶粒云岩,砂屑云岩为主;晶间溶孔、溶蚀孔洞等次生孔隙为主要储集空间;储层非均质性强。台内滩亚相储层物性明显优于潮坪_潟湖亚相,反映了原始沉积相带是储层发育的物质基础;提出前热液表生岩溶和后热液表生岩溶,总结了2类岩溶的识别标志并明确了研究区以前热液表生岩溶作用为主。最终,结合构造演化和成岩作用研究成果,建立了研究区优质储层形成模式,预测了储层平面分布。

关键词: 岩溶期次, 储层形成模式, 寒武系潜山, 牙哈_英买力地区, 塔里木盆地

Abstract: Buried hill reservoir is one of the hottest areas of carbonate exploration in China and abroad.In order to recognize different stages of karstification,confirm formation model of high-quality reservoirs,Yaha-Yingmaili block was chosen as an example and main controlling factors in this block were discussed based on the analysis of reservoir rock types,reservoir space types and reservoir physical property systematically.The results show that main reservoir rocks include crystalline dolostones and sandy dolostones and intercrystalline dissolved pores and vugs are the main reservoir space with high heterogeneity.Reservoir physical property of intraplatform shoal was better than that of tidal flat to lagoon dramatically and this reflects that the original facies was the fundamental factor of reservoir development.Meanwhile,pre-hydrotherm karstification and post-hydrotherm karstification were proposed.Furthermore,identifications of the two kinds of karstification were summarized and pre-hydrotherm karstification had a significance effect on reservoir quality.Finally,combined with the studies of tectonic evolution and diagenesis,formation model of high-quality reservoirs was established and reservoir distribution was predicted.

Key words: Karstification stage, Reservoir formation model, Buried hill, Yaha-Yingmaili block, Tarim Basin

中图分类号: 

  • TE122.2+1

[1]Huang Sijing,Zhang Xuehua,Liu Lihong,et al.Progress of research on carbonate diagenesis[J].Earth Science Frontiers,2009,16(5):219-231.[黄思静,张雪花,刘丽红,等.碳酸盐岩成岩作用研究现状与前瞻[J].地学前缘,2009,16(5):219-231.]
[2]Liu Hongjun,Jia Yani,Li Zhenhong,et al.Existence and significance of microumbones in karst basin:sample from Ordovician karstic paleogeomorphy in Ordos Basin[J].Natural Gas Geoscience,2006,17(4):490-493.[刘洪军,贾亚妮,李振宏,等.岩溶盆地中微隆起带的存在即意义__以鄂尔多斯盆地奥陶纪岩溶古地貌为例[J].天然气地球科学,2007,25(6):858-868.][JP]
[3]Wang Zhaoming,Zhang Lijuan,Sun Chonghao.Classification,period and exploration for carbonate karst in the Ordovician,Tarim Basin[J].Journal of Paleogeography,2015,17(5):635-644.[王招明,张丽娟,孙崇浩.塔里木盆地奥陶系碳酸盐岩岩溶分类、期次及勘探思路[J].古地理学报,2015,17(5):635-644.][JP]
[4]Zhang Baomin,Liu Jingjiang.Classification and characteristics of karst reservoirs in China and related theories[J].Petroleum Exploration and Development,2009,36(1):12-29.[张宝民,刘静江.中国岩溶储集层分类与特征及相关的理论问题[J].石油勘探与开发,2009,36(1):12-29.]
[5]Qian Yixiong,Conxita Taberner,Zou Senlin,et al.Diagenesis comparison between epigenic karstification and burial dissolution in carbonate reservoirs:An instance of ordovician carbonate reservoirs in Tabei and Tazhong regions,Tarim Basin[J].Marine Origin Petroleum Geology,2007,12(2):1-7.[钱一雄,Conxita Taberner,邹森林,等.碳酸盐岩表生岩溶与埋藏溶蚀比较——以塔北和塔中地区为例[J].海相油气地质,2007,12(2):1-7.][JP]
[6]Liu Cunge,Li Guorong,Zhang Yiwei,et al.Application of strontium isotope to the study of paleokarst:An case from Ordovician in the Tahe Oilfield,Tarim Basin[J].Acta Geologica Sinica,2007,81(10):1398-1406.[刘存革,李国蓉,张一伟,等.锶同位素在古岩溶研究中的应用——以塔河油田奥陶系为例[J].地质学报,2007,81(10):1398-1406.]
[7]Shi Shuyuan,Hu Suyun,Liu Wei,et al.Distinguishing paleokarst period by intergrating carbon oxygen isotopes and fluid inclusion characteristics[J].Natural Gas Geoscience,2015,26(2):208-217.[石书缘,胡素云,刘伟,等.综合运用碳氧同位素和包裹体信息判别古岩溶形成期次[J].天然气地球科学,2015,26(2):208-217.]
[8]Zhang Tao,Cai Xiyuan.Caledonian paleo-karstification and its characteristics in Tahe area,Tarim Basin[J].Acta Geologica Sinica,2007,81(8):1125-1134.[张涛,蔡希源.塔河地区加里东中期岩溶作用及分布模式[J].地质学报,2007,81(8):1125-1134.]
[9]Xia Riyuan,Tang Jiansheng,Zou Shengzhang,et al.Palaeo-karst research of the carbonate oil-gas field and its application to oil-gas exploration and development[J].Acta Geoscientica Sinica,2006,27(5):503-509.[夏日元,唐建生,邹胜章,等.碳酸盐岩油气田古岩溶研究及其在油气勘探开发中的应用[J].地球学报,2006,27(5):503-509.]
[10]Qiao Zhanfeng,Shen Anjiang,Zou Weihong,et al.A fault-controlled non-exposed meteoric karstification:A case study of Ordovician carbonate reservoir at structure YM2 in northern Tarim Basin,northwest China[J].Acta Geologica Sinica,2011,85(12):2070-2083.[乔占峰,沈安江,邹伟宏,等.断裂控制的非暴露型大气水岩溶作用模式——以塔北英买2构造奥陶系碳酸盐岩储层为例[J].地质学报,2011,85(12):2070-2083.][JP]
[11]He Jinyou,Jia Chengzao,Wu Guanghui,et al.Characteristics and model of Sinian weathering paleo-karst in Aksu area,Xinjiang.[J].Acta Petrologica Sinica,2010,26(8):2513-2518.[何金有,贾承造,邬光辉,等.新疆阿克苏地区震旦系风化壳古岩溶特征及其发育模式[J].岩石学报,2010,26(8):2513-2518.]
[12]Shen Anjiang,Pan Wenqing,Zheng Xingping,et al.Types and characteristics of Lower Paleozoic karst reservoir in Tarim Basin[J].Marine Origin Petroleum Geology,2010,15(2):20-29.[沈安江,潘文庆,郑兴平,等.塔里木盆地下古生界岩溶型储层类型及特征[J].海相油气地质,2010,15(2):20-29.]
[13]Ouyang Yonglin,Ma Xiaoming,Guo Xiaolong,et al.Prediction of ancient weathering crust karst reservoirs using separate frequency seismic attributes[J].Natural Gas Geoscience,2008,19(3):381-384.[欧阳永林,马小明,郭晓龙,等.利用分频地震属性进行古风化壳岩溶储层预测__以千米桥潜山凝析气田为例[J].天然气地球科学,2008,19(3):381-384.]
[14]Wang Buqing,Huang Zhibin,Ma Peiling,et al.Establishment of division standard,evidence and principle of structural units in Tarim Basin[J].Geotectonica et Metallogenia,2009,33(1):86-93.[王步清,黄志斌,马培领,等.塔里木盆地构造单元划分标准、依据和原则的建立[J].大地构造与成矿学,2009,33(1):86-93.][JP]
[15]Xu Guoqiang,Liu Shugen,Li Guorong,et al.Comparison of tectonic evolutions and petroleum geological conditions in Tazhong and Tabei paloehighs in Tarim Basin[J].Oil & Gas Geology,2005,26(1):114-129.[徐国强,刘树根,李国蓉,等.塔中、塔北古隆起形成演化及油气地质条件对比[J].石油与天然气地质,2005,26(1):114-129.]
[16]An Haiting,Li Haiyin,Wang Jianzhong,et al.Tectonic evolution and its controlling on oil and gas accumulation in the northern Tarim Basin[J].Geotectonica et Metallogenia,2009,33(1):142-147.[安海亭,李海银,王建忠,等.塔里木盆地北部地区构造和演化特征及其对油气成藏的控制[J].大地构造与成矿学,2009,33(1):142-147.]
[17]Zhang Demin,Bao Zhidong,Pan Wenqing,et al.Type and origin of the Lower Paleozoic dolostones in Tarim Basin[J].Journal of Paleogeography,2013,15(5):693-706.[张德民,鲍志东,潘文庆,等.塔里木盆地下古生界白云岩类型及成因[J].古地理学报,2013,15(5):693-706.]
[18]Su Zhongtang,Chen Hongde,Xu Fenyan,et al.Geochemistry and dolomitization mechanism of Majiagou dolomites in Ordovician[J].Acta Petrogica Sinica,2011,27(8):2230-2238.[苏中堂,陈洪德,徐粉燕,等.鄂尔多斯盆地马家沟组白云岩地球化学特征及白云岩化机制分析[J].岩石学报,2011,27(8):2230-2238.]
[19]Shao Longyi,He Hong,Peng Suping,et al.Types and origin of dolostones of the Cambrian and Ordovician of Bachu Uplift area in Tarim Basin[J].Journal of Paleogeography,2002,4(2):19-28.[邵龙义,何宏,彭苏萍,等.塔里木盆地巴楚隆起寒武系及奥陶系白云岩类型及形成机理[J].古地理学报,2002,4(2):19-28.]
[20]Davies G R,Smith L B.Structurally controlled hydrothermal dolomite reservoir facies:An overview[J].AAPG Bulletin,2006,90(11):5-109.
[21]Amel H,Jafarian A,Husinec A,et al.Microfacies,depositional environment and diagenetic evolution controls on the reservoir quality of the Permian upper Dalan Formation,Kish Gasfield,Zagros basin[J].Marine and Petroleum Geology,2015,67:57-71.
[22]Ma Yongsheng,Cai Xunyu,Zhao Peirong,et al.Formation mechanism of deep-buried carbonate reservoir and its model of Three-Element controlling reservoir:A case study from the Puguang Oilfield in Sichuan[J].Acta Geologica Sinica,2010,84(8):1087-1094.[马永生,蔡勋育,赵培荣,等.深层—超深层碳酸盐岩优质储层发育机理和“三元控储”模式[J].地质学报,2010,84(8):1087-1094.]
[23]Liu Shugen,Ma Yongsheng,Wang Guozhi,et al.Formation and conservation mechanism of the high-quality reservoirs in Sinian-Lower Paleozoic Sichuan Basin[J].Petroleum Geology and Recovery Efficiency,2008,15(1):1-5.[刘树根,马永生,王国芝,等.四川盆地震旦系—下古生界优质储层形成与保存机理.油气地质与采收率[J],2008,15(1):1-5.]
[24]Chen Hanlin,Yang Shufeng,Jia Chengzao,et al.Confirmation of Permian intermediate-acid igneous rock zone and a new understanding of tectonic evolution in the northern part of the Tarim Basin[J].Acta Mineralogica Sinica,1998,18(2):370-376.[陈汉林,杨树锋,贾承造,等.塔里木盆地北部二叠纪中酸性火成岩带的厘定及其对塔北构造演化的新认识[J].矿物学报,1998,18(2):370-376.]
[25]Li Yong,Su Wen,Kong Ping,et al.Zircon U-Pb ages of the early Permian magmatic rocks in the Tazhong-Bachu region,Tarim Basin by LA-ICP-MS[J].Acta Petrologica Sinica,2007,23(5):1097-1107.[李勇,苏文,孔屏,等.塔里木盆地塔中—巴楚地区早二叠世岩浆岩的LA-ICP-MS锆石U-Pb年龄[J].岩石学报,2007,23(5):1097-1107.]
[26]Sun Bonian.Disscussion on the northern Tarim Basin Permian phytogeographical department[M]//Jia Runxu.China North Tarim Basin Oil and Gas Geological Research.Beijing:China University of Geosciences Press,1991:115-124.[孙柏年.塔里木盆地北缘二叠纪植物地理区系探讨[M]//贾润胥主编.中国塔里木盆地北部油气地质研究.北京:中国地质大学出版社,1991:115-124.]
[27]Yang Shufeng,Chen Hanlin,Li Zilong,et al.Early Permian Tarim Large Igneous Province in northwest China[J].Science China:Earth Sciences,2014,44(2):187-199.[杨树锋,陈汉林,厉子龙,等.塔里木早二叠世大火成岩省[J].中国科学:地球科学 2014,44(2):187-199.]
[28]Zhu Dongya,Hu Wenxuan,Zhang Xuefeng,et al.Characteristics of burial dissolution in the Ordovician limestone of Tahe Oilfield[J].Acta Petrolei Sinica,2007,28(5):57-62.[朱东亚,胡文瑄,张学丰,等.塔河油田奥陶系灰岩埋藏溶蚀作用特征[J].石油学报,2007,28(5):57-62.]
[29]Hu Mingyi,Cai Xiyao,Hu Zhonggui,et al.Deep buried dissolution of Ordovician carbonates in Tazhong area of Tarim Basin[J].Journal of Oil and Gas Technology,2009,31(6):49-54.[胡明毅,蔡习尧,胡忠贵,等.塔中地区奥陶系碳酸盐岩深部埋藏溶蚀作用研究[J].石油天然气学报:江汉石油学院学报,2009,31(6):49-54.]
[30]Jin Zhijun,Zhu Dongya,Hu Wenxuan,et al.Geological and geochemical Signatures of hydrothermal activity and their influence on carbonate reservoir beds in the Tarim Basin[J].Acta Geologica Sinica,2006,80(2):245-253.[金之钧,朱东亚,胡文瑄,等.塔里木盆地热液活动地质地球化学特征及其对储层影响[J].地质学报,2006,80(2):245-253.]

[1] 戴金星, 洪峰, 倪云燕, 廖凤蓉. 塔里木盆地英吉苏凹陷煤成气前景良好[J]. 天然气地球科学, 2019, 30(6): 771-782.
[2] 贾爱林, 唐海发, 韩永新, 吕志凯, 刘群明, 张永忠, 孙贺东, 黄伟岗, 王泽龙. 塔里木盆地库车坳陷深层大气田气水分布与开发对策[J]. 天然气地球科学, 2019, 30(6): 908-918.
[3] 陈永权, 严威, 韩长伟, 闫磊, 冉启贵, 亢茜, 何皓, 马源. 塔里木盆地寒武纪/前寒武纪构造—沉积转换及其勘探意义[J]. 天然气地球科学, 2019, 30(1): 39-50.
[4] 张荣虎, 王珂, 王俊鹏, 孙雄伟, 李君, 杨学君, 周露. 塔里木盆地库车坳陷克深构造带克深8区块裂缝性低孔砂岩储层地质模型[J]. 天然气地球科学, 2018, 29(9): 1264-1273.
[5] 王清龙, 林畅松, 李浩, 韩剑发, 孙彦达, 何海全. 塔里木盆地西北缘中下奥陶统碳酸盐岩沉积微相特征及演化[J]. 天然气地球科学, 2018, 29(9): 1274-1288.
[6] 朱光有, 曹颖辉, 闫磊, 杨海军, 孙崇浩, 张志遥, 李婷婷, 陈永权. 塔里木盆地8 000m以深超深层海相油气勘探潜力与方向[J]. 天然气地球科学, 2018, 29(6): 755-772.
[7] 周波, 曹颖辉, 齐井顺, 黄世伟, 刘策, 贾进华, 陈秀艳. 塔里木盆地古城地区下奥陶统储层发育机制[J]. 天然气地球科学, 2018, 29(6): 773-783.
[8] 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.
[9] 曹颖辉, 李洪辉, 闫磊, 王洪江, 张君龙, 杨敏, 赵一民. 塔里木盆地满西地区寒武系台缘带分段演化特征及其对生储盖组合的影响[J]. 天然气地球科学, 2018, 29(6): 796-806.
[10] 闫磊, 李洪辉, 曹颖辉, 杨敏, 赵一民. 塔里木盆地满西地区寒武系台缘带演化及其分段特征[J]. 天然气地球科学, 2018, 29(6): 807-816.
[11] 杨敏, 赵一民, 闫磊, 李洪辉, 张欣欣, 徐振平, 罗浩渝. 塔里木盆地东秋里塔格构造带构造特征及其油气地质意义[J]. 天然气地球科学, 2018, 29(6): 826-833.
[12] 陈斐然, 张义杰, 朱光有, 张宝收, 卢玉红, 张志遥. 塔里木盆地台盆区深层天然气地球化学特征及成藏演化[J]. 天然气地球科学, 2018, 29(6): 880-891.
[13] 黄少英, 杨文静, 卢玉红, 张科, 赵青, 凡闪. 塔里木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): 1497-1505.
[14] 陈燕燕,胡素云,李建忠,王铜山, 陶小晚. 原油裂解过程中组分演化模型及金刚烷类化合物的地球化学特征[J]. 天然气地球科学, 2018, 29(1): 114-121.
[15] 任宇泽,林畅松,高志勇,刘景彦,宋宁宁. 塔里木盆地西南坳陷白垩系层序地层与沉积充填演化[J]. 天然气地球科学, 2017, 28(9): 1298-1311.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 倪金龙;夏斌;. 济阳坳陷坡折带组合类型及石油地质意义[J]. 天然气地球科学, 2006, 17(1): 64 -68 .
[2] USGS,郑军卫(译). 美国地质调查局油气资源研究计划[J]. 天然气地球科学, 2002, 13(3-4): 15 .
[3] 周兴熙;. 库车油气系统油气藏相态分布及其控制因素[J]. 天然气地球科学, 2004, 15(3): 205 -213 .
[4] 杨宁,吕修祥,陈梅涛,赵风云,张亚光,郑多明 . 英买力地区碳酸盐岩古风化壳油气聚集模式探讨[J]. 天然气地球科学, 2005, 16(1): 35 -39 .
[5] 刘春慧;金振奎;朱桂芳;王庆东;张建良. . 准噶尔盆地东部吉木萨尔凹陷二叠系梧桐沟组储层物性特征及控制因素[J]. 天然气地球科学, 2007, 18(3): 375 -379 .
[6] 曹刚;李其荣;安辉;. 川南地区下二叠统茅口组“岩溶型气藏”地震、地质特征探讨[J]. 天然气地球科学, 1999, 10(3-4): 76 -81 .
[7] 刘玉梅;邓泽进;孙广伯;曹宏涛;. 板桥断裂构造带油气成藏组合特征[J]. 天然气地球科学, 2003, 14(4): 275 -278 .
[8] 朱维耀;宋洪庆; 何东博;王明 ;贾爱林;胡永乐 . 含水低渗气藏低速非达西渗流数学模型及产能方程研究[J]. 天然气地球科学, 2008, 19(05): 685 -689 .
[9] 金惠, 魏国齐, 杨威, 朱秋影, 谢增业, 施振生, 刘满仓, 沈珏红. 安岳—潼南地区须家河组地震相模式及其地质意义[J]. 天然气地球科学, 2009, 20(4): 544 -548 .
[10] 白斌, 邹才能, 朱如凯, 翟文亮, 刘柳红, 戴朝成, 张健, 杜红权, 毛治国. 利用露头、自然伽玛、岩石地球化学和测井地震一体化综合厘定层序界面——以四川盆地上三叠统须家河组为例[J]. 天然气地球科学, 2010, 21(1): 78 -86 .