天然气地球科学

• 天然气勘探 • 上一篇    下一篇

塔中寒武系深层白云岩储层测井评价技术

肖承文,张承森,刘世伟,韩东春,吴兴能,张璋,居大海,单交义   

  1. 1.中国石油塔里木油田分公司勘探开发研究院,新疆 库尔勒 841000;
    2.中海油田服务股份有限公司,河北 燕郊 065201
  • 收稿日期:2014-10-20 修回日期:2015-01-14 出版日期:2015-07-10 发布日期:2015-07-10
  • 作者简介:肖承文(1968-),男,湖北潜江人,高级工程师,博士,主要从事测井理论方法与储层描述评价研究. E-mail:xiaocw-tlm@petrochina.com.cn.
  • 基金资助:

    国家科技重大专项“复杂储层油气测井解释理论方法与处理技术”(编号:2011ZX05020-008)资助.

Logging Evaluation Technology of Cambrian Deep Dolomite Reservoir in Tazhong Area

XIAO Cheng-wen,ZHANG Cheng-sen,LIU Shi-wei,HAN Dong-chun,WU Xing-neng,ZHANG Zhang,JU Da-hai,SHAN Jiao-yi   

  1. 1.Tarim Oilfield Company,PetroChina,Korla 841000,China; 
    2.China Oilfield Services Limited,Yanjiao 065201,China
  • Received:2014-10-20 Revised:2015-01-14 Online:2015-07-10 Published:2015-07-10

摘要:

塔中寒武系深层白云岩储层具有埋藏深、岩性复杂等特点,油气藏储集空间以次生溶蚀的孔洞为主,并伴有裂缝发育,导致储层非均质强,油水关系复杂,储层定量评价及流体性质判别困难。经过测井攻关研究及实际井的应用实践,文章首次提出一套适用于塔中地区寒武系深层白云岩储层测井评价技术|该技术充分依据微电阻率扫描成像、元素俘获、热中子及声波扫描成像等测井新技术资料,依靠以电成像视地层水电阻率谱为主的专利技术,精细刻画白云岩储层的孔、洞、缝特征,评价储层有效性,确定储层流体性质,支撑塔中寒武系深层白云岩油气藏的发现与评价,见到明显的地质效果。

关键词: 塔中地区, 寒武系深层白云岩, 测井评价, 电阻率谱

Abstract:

The Cambrian deep dolomite reservoir in Tazhong area is deeply buried and complex in lithology.The hydrocarbon pore volume mainly consists of secondary erosional vugs accompanied with fractures.This may cause strong reservoir heterogeneity and complex oil-water relationship.This makes reservoir quantification and fluid identification difficult.A logging evaluation technology which suits Cambrian deep dolomite reservoir in Tazhong area is proposed after researching and practicing.This technology is based on MESI,ECS,APS,Sonic Scanner and combined with MESI Apparent Formation Water Resistivity Spectrum.It can not only finely describe the feature of vugs and fractures developed in dolomite reservoir,but also play well in effectiveness evaluating and fluid confirming of reservoir and plays an important role in discovery and evaluation of Cambrian deep dolomite reservoir.

Key words: Tazhong area;Cambrian deep dolomite, Logging evaluation technology, Resistivity spectrum

中图分类号: 

  • TE122.3+5

[1]Huang Qingyu,Zhang Shaonan,Zhang Siyang,et al.Textural control on the development of dolomite reservoir:A study from the Cambrian-Ordovician dolimite,central Tarim Basin,NW China[J].Natural Gas Geoscience,2014,25(3):341-350,470.[黄擎宇,张哨楠,张斯杨,等.白云岩结构对储集空间发育的控制作用——以塔里木盆地中央隆起区寒武系—奥陶系白云岩为例[J].天然气地球科学,2014,25(3):341-350,470.] 
[2]Zhu Dongya,Meng Qingqiang,Jin Zhijun,et al.Carbonate reservoir rock of composite genesis and its dynamic developing process:An example from Tahe carbonate reservoir[J].Natural Gas Geoscience,2012,23(1):26-35.[朱东亚,孟庆强,金之钧,等.复合成因碳酸盐岩储层及其动态发育过程——以塔河地区奥陶系碳酸盐岩为例[J].天然气地球科学,2012,23(1):26-35.]
[3]Chen Yongquan,Zhou Xinyuan,Yang Wenjing.Genesis of Cambrian dolostone and the reservoir evaluation in Tarim Basin[J].Marine Origin Petroleum Geology,2009,14(4):10-17.[陈永权,周新源,杨文静.塔里木盆地寒武系白云岩的主要成因及其储层评价[J].海相油气地质,2009,14(4):10-17.]
[4]Zhao Xuefeng,Zhu Guangyou,Liu Qinfu,et al.Main control factors of pore development in deep marine carbonate reservoirs[J].Natural Gas Geoscience,2007,18(4):514-521.[赵雪凤,朱光有,刘钦甫,等.深部海相碳酸盐岩储层孔隙发育的主控因素研究[J].天然气地球科学,2007,18(4):514-521.]
[5]Huang Sijing,Qing Hairuo,Hu Zuowei,et al.The diagenesis and dolomitization of the Feixianguan carbonates of Triassic in NE Sichuan Basin:An overview[J].Advances in Earth Science,2007,22(5):495-503.[黄思静,Hairuo Qing,胡作维,等.四川盆地东北部三叠系飞仙关组碳酸盐岩成岩作用和白云岩成因的研究现状和存在问题[J].地球科学进展,2007,22(5):495-503.]
[6]Sun Longde,Zou Caineng,Zhu Rukai,et al.Formation,distribution and potential of deep hydrocarbon resources in China[J].Petroleum Exploration and Development,2013,40(6):641-649.[孙龙德,邹才能,朱如凯,等.中国深层油气形成、分布与潜力分析[J].石油勘探与开发,2013,40(6):641-649.]
[7]Wang Yu,Su Jin,Wang Kai,et al.Distribution and accumulation of global deep oil and gas[J].Natural Gas Geoscience,2012,23(3):526-534.[王宇,苏劲,王凯,等.全球深层油气分布特征及聚集规律[J].天然气地球科学,2012,23(3):526-534.]
[8]Zhao Jingzhou,Wang Qinghua,Shi Baohong,et al.Marine hydrocarbon enrichment rules and palaeouplift-controlling hydrocarbon theory for the Paleozoic Tarim Craton Basin[J].Oil & Gas Geology,2007,28(6):703-712.[赵靖舟,王清华,时保宏,等.塔里木古生界克拉通盆地海相油气富集规律与古隆起控油气论[J].石油与天然气地质,2007,28(6):703-712.]
[9]Zhang Bin,Zhu Guangyou,Gu  Qiaoyuan,et al.Research progress in marine oil & gas reservoirs of the Tarim Basin:A review of the conference on “complex oil & gas pool formation,adjustment and re-accumulation mechanism of the typical superimposed basin in the west of China” and discussionon hydrocarbon accumulation of the Tarim Basin[J].Natural Gas Geoscience,2009,20(5):664-669.[张斌,朱光有,顾乔元,等.塔里木盆地海相油气成藏研究进展——“中国西部典型叠合盆地复杂油气藏形成改造再聚集机制”课题进展交流暨塔里木盆地油气成藏学术研讨会综述[J].天然气地球科学,2009,20(5):664-669.]
[10]Liu Yongfu,Yin Jun,Sun Xiongwei,et al.Cambrian sedimentary characteristics and origin of high-quality dolomite reservoirs in eastern Tarim Basin[J].Natural Gas Geoscience,2008,19(1):126-132.[刘永福,殷军,孙雄伟,等.塔里木盆地东部寒武系沉积特征及优质白云岩储层成因[J].天然气地球科学,2008,19(1):126-132.]
[11]Zheng Jianfeng,Shen Anjiang,Liu Yongfu,et al.Multi-parameter comprehensive identification of the genesis of LowerPaleozoic dolomite in Tarim Basin,China[J].Acta Petrolei Sinica,2012,33(S2):145-153.[郑剑锋,沈安江,刘永福,等.多参数综合识别塔里木盆地下古生界白云岩成因[J].石油学报,2012,33(S2):145-153.]
[12]Wang Huanhuan,Zhu Guangyou,Xue Haitao,et al.Formation and controlling factors of effective weathered crust carbonate reservoirs:Taking the Yingmaili-Yaha area of Tarim Basin as an example[J].Natural Gas Geoscience,2009,20(2):182-191.[王欢欢,朱光有,薛海涛,等.碳酸盐岩风化壳型有效储层的形成与控制因素研究——以塔里木盆地英买力—牙哈地区为例[J].天然气地球科学,2009,20(2):182-191.]
[13]Wang Fuhuan,Wang Zhaoming,Han Jianfa,et al.Geological conditions of oil and gas enrichment in carbonate reservoirs of Tazhong area,Tarim Basin[J].Natural Gas Geoscience,2009,20(5):695-702.[王福焕,王招明,韩剑发,等.塔里木盆地塔中地区碳酸盐岩油气富集的地质条件[J].天然气地球科学,2009,20(5):695-702.]
[14]Sun Chonghao,Yu Hongfeng,Wang Huaisheng,et al.Vugular formation of carbonates in Ordovician Yingshan reservior in Tazhong northern slope of Tarim Basin[J].Natural Gas Geoscience,2012,23(2):230-236.[孙崇浩,于红枫,王怀盛,等.塔里木盆地塔中地区奥陶系鹰山组碳酸盐岩孔洞发育规律研究[J].天然气地球科学,2012,23(2):230-236.]
[15]Song Wenyan,Liu Liqing,Gan Xueqi,et al.Weathering crust karstification in Leikoupo Formation in central Sichuan area[J].Natural Gas Geoscience,2012,23(6):1019-1024.[宋文燕,刘利清,甘学启,等.川中地区雷口坡组风化壳岩溶作用研究[J].天然气地球科学,2012,23(6):1019-1024.]
[16]Yao Jingli,Wang Lanping,Zhang Qing,et al.Controlling factor and distribution of Paleo-karst development in Ordovician of southern Ordos Basin[J].Natural Gas Geoscience,2011,22(1):56-65.[姚泾利,王兰萍,张庆,等.鄂尔多斯盆地南部奥陶系古岩溶发育控制因素及展布[J].天然气地球科学,2011,22(1):56-65.]
[17]Hu Ruibo,Chang Jingchun,Zhang Wensheng,et al.On lithology identification of limnetic facies carbonate reservoir in Qikou Sag and its reservoir types[J].Well Logging Technology,2012,36(2):179-182.[胡瑞波,常静春,张文胜,等.歧口凹陷湖相碳酸盐岩储层岩性识别及储集类型研究[J].测井技术,2012,36(2):179-182.]
[18]Li Ling,Tan Xiucheng,Chen Jingshan,et al.Characteristics and origin of dolostones in Yingshan Formation,Lower  and  Middle Ordovician,north of central Tarim Basin[J].Journal of Southwest Petroleum University,2007,29(1):34-36.[李凌,谭秀成,陈景山,等.塔中北部中下奥陶统鹰山组白云岩特征及成因[J].西南石油大学学报,2007,29(1):34-36.]
[19]Zhong Guangfa,Ma Zaitian.Sedimentary structures identified from high-resolution borehole micro-resistivity image logs[J].Journal of Tongji Utiversity,2001,29(5):576-580.[钟广法,马在田.利用高分辨率成像测井技术识别沉积构造[J].同济大学学报,2001,29(5):576-580.]
[20]Qi Xingzhong,Liu Xingli,Fu Haicheng,et al.Research and application of the quantitative processing methods of electric imaging log data[J].Natural Gas Industry,2005,25(6):32-34.[祁兴中,刘兴礼,傅海成,等.电成像测井资料定量处理方法研究及应用[J].天然气工业,2005,25(6):32-34.]
[21]Kang Wei,Cheng Jiubing.Pseudo-acoustic wave equations for reverse-time migration in TI media[J].Chinese  Journal.Geophys.(in Chinese),2012,55(3):1033-1045.[康玮,程玖兵.横向各向同性介质拟声波方程及其在逆时偏移中的应用[J].地球物理学报,2012,55(3):1033-1045.]
[22]Zhang Hongying.Judging reservoir fluid property with P1/2 method[J].Journal of Oil and Gas Technology(J.JPI),2007,29(5):106-107,140-141.[张红英.利用P1/2法判别储层流体性质[J].石油天然气学报:江汉石油学院学报,2007,29(5):106-107,140-141.]
[23]Wu Xingneng,Xiao Chengwen,Xin Yi,et al.Interpretation method for fractures with FMI/ XRMI images in carbonate horizontal well and its application[J].Well Logging Technology,2009,33(5):431-464.[吴兴能,肖承文,信毅,等.利用FMI/XRMI解释水平井中碳酸盐岩储层裂缝的方法及其应用[J].测井技术,2009,33(5):431-464.]
[24]Xiao Chengwen,Liu Ruilin,Yang Haijun,et al.A Method of Apparent Formation Water Resistivity Spectrum and Parameter Calculation based on micro-resistivity image calibrated point by point:China,ZL 201010522233.X[P].2010-10-22.[肖承文,刘瑞林,杨海军,等.一种逐点刻度电成像资料计算视地层水电阻率谱及参数的方法:中国,ZL 201010522233.X[P].2010-10-22.]

[1] 彭真,秦臻,潘和平,纪扬,郭博,徐伟,孙立洲. 杭锦旗地区低阻气层成因及测井评价方法[J]. 天然气地球科学, 2016, 27(11): 2054-2063.
[2] 尹帅,丁文龙,黄昌杰,肖子亢,周学慧. 非饱和致密砂岩储层含气饱和度测井评价[J]. 天然气地球科学, 2016, 27(1): 156-165.
[3] 李霞,程相志,周灿灿,李潮流,刘忠华. 页岩油气储层测井评价技术及应用[J]. 天然气地球科学, 2015, 26(5): 904-914.
[4] 陈君青,庞雄奇,姜振学,庞宏. 塔里木盆地塔中地区上奥陶统油气相态及其控制因素[J]. 天然气地球科学, 2014, 25(12): 1913-1924.
[5] 杨少春,王娜,李明瑞,喻建. 鄂尔多斯盆地崇信地区三叠系延长组烃源岩测井评价[J]. 天然气地球科学, 2013, 24(3): 470-476.
[6] 周新平,徐怀民,牛玉杰,李猛,黄娅,李辉,黄素,苏芮. 塔中地区西北部CⅢ油组含砾砂岩段沉积相研究[J]. 天然气地球科学, 2013, 24(2): 292-299.
[7] 孙崇浩,于红枫,王怀盛,刘虎,张正红,韩杰,罗新生. 塔里木盆地塔中地区奥陶系鹰山组碳酸盐岩孔洞发育规律研究[J]. 天然气地球科学, 2012, 23(2): 230-236.
[8] 张琴, 唐玄, 杨镱婷, 葛明娜. 塔中地区泥盆系东河砂岩石油运聚方向研究[J]. 天然气地球科学, 2011, 22(6): 996-1000.
[9] 金涛, 高日胜, 高彩霞, 罗强, 王建. 从烃源岩测井评价结果看冀中坳陷饶阳凹陷勘探前景[J]. 天然气地球科学, 2010, 21(3): 406-412.
[10] 李鹏春, 陈广浩, 孟庆任, 谈玉明, 郝加良, 唐春燕, 龙利平, 张渊. 塔中地区奥陶系天然气地球化学及成因与分布特征[J]. 天然气地球科学, 2010, 21(2): 321-330.
[11] 郭振华, 赵彦超. 大牛地气田盒2段致密砂岩气层测井评价[J]. 天然气地球科学, 2010, 21(1): 87-94.
[12] 刘俊田, 焦立新, 张日供, 覃新平, 闫立纲, 刘媛萍. 三塘湖盆地牛东区块石炭系火山岩储集层测井评价[J]. 天然气地球科学, 2009, 20(4): 518-524.
[13] 吴章武,张敏,张俊, 冯敏. 塔里木盆地塔中地区石炭系油气运移和聚集特征――以对塔中4号构造原油非烃地球化学研究说明[J]. 天然气地球科学, 2003, 14(6): 480-483.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!