磨溪气田嘉陵江组二段陆表海台地高频层序发育特征及对储层的控制

doi:10.11743/ogg20160511

石油与天然气地质 ›› 2016, Vol. 37 ›› Issue (5): 713-720.doi: 10.11743/ogg20160511

磨溪气田嘉陵江组二段陆表海台地高频层序发育特征及对储层的控制

刘宏¹, 王高峰¹, 刘南³, 乔琳⁴, 丁伟⁴, 丁熊¹, 段宏臻⁵, 谭秀成¹

1. 西南石油大学地球科学与技术学院天然气地质四川省重点实验室, 四川成都 610500;
2. 西南石油大学中国石油碳酸盐岩储层重点实验室沉积与成藏分室, 四川成都 610500;
3. 中海石油(中国)有限公司深圳分公司, 广东广州510240;
4. 中国石油西南油气田分公司勘探事业部, 四川成都 610041;
5. 中国石油集团测井有限公司青海事业部, 甘肃敦煌 736202

收稿日期:2015-05-20 修回日期:2016-06-15 出版日期:2016-10-08 发布日期:2016-11-07
第一作者简介:刘宏(1981-),男,博士、副教授,碳酸盐岩储层地质学与地震地层学。E-mail:nd123@163.com。
基金项目:
国家自然科学基金项目（41472099）；中国石油科技创新基金项目（2015D-5006-0107）。

Characterization of high-frequency sequences in the epicontinental carbonate platform of Jia 2 member in Moxi gas field and its controls over reservoirs

Liu Hong¹, Wang Gaofeng¹, Liu Nan³, Qiao Lin⁴, Ding Wei⁴, Ding Xiong¹, Duan Hongzhen⁵, Tan Xiucheng¹

1. Sichuan Province Key Laboratory of Natural Gas Geology, School of Geoscience and Technology, Southwest Petroleum University, Chengdu, Sichuan 610500, China;
2. PetroChina Deposition and Accumulation Department of Key Laboratory of Carbonate Reservoirs, Southwest Petroleum University, Chengdu, Sichuan 610500, China;
3. Shenzhen Branch Company, CNOOC, Guangzhou, Guangdong 510240, China;
4. Exploration Department of Southwest Oil & Gas Field Company, PetroChina, Chengdu, Sichuan 610041, China;
5. CNPC Logging Qinghai Business Division, Dunhuang, Gansu 736202, China

Received:2015-05-20 Revised:2016-06-15 Online:2016-10-08 Published:2016-11-07

摘要/Abstract

摘要： 高频层序是由海平面高频振动变化而形成的地层记录，一般形成于具有稳定沉降背景的盆地中，可与米兰科维奇天文周期旋回相对应。作为非海岸沉积环境的陆表海台，其高频层序发育具有一定的特殊性和代表性。在大量岩心观察、薄片分析、测井相研究的基础上，按能量环境、海平面升降及海水咸化旋回以及相序组合等特征，并考虑高频层序格架下储集层成因类型，将川中磨溪气田嘉二段陆表海碳酸盐台地高频层序划分为3类：台坪型、台内浅滩型与潟湖型。以膏质岩类、颗粒岩类广泛发育为特征，常见各种暴露标志，总体表现为向上变浅序列的多种岩性组合。高频层序地层格架内各级层序界面特征清晰，岩性组合稳定，可对比性强。同时，探讨了高频层序格架下早期储层成因机制，指出稳定沉积陆表海台地背景下的高频层序控制了岩相发育序列及同生岩溶作用，进而控制了不同成因类型储集层发育。

关键词: 高频层序, 碳酸盐岩, 嘉陵江组, 陆表海台地, 磨溪气田

Abstract: High-frequency sequences,generally formed in basins with stable subsidence settings and correspond well to astronomical Milankovitch cycles,are vivid records of high-frequency eustatic flucturation.Such sequences developed in epicontinental platforms of non-coastal sedimentary environment are both representative and special in certain ways.By combining core observations,thin section analyses and logging facies studies with such factors as energy environment,eustatic fluctuation and sea water salinity cycle as well as reservoir genesis types under high-frequency sequential framework,we classified high-frequency sequences in the epicontinental carbonate platform of the Jia 2 member of the Moxi gas field into the following three types:platform flat type,intraplatform shoal type and lagoon type.The sequences are found to be characterized by widely-distributed gypsiferous rocks and grainstone with all kinds of exposure marks.As a whole,they consist of stratigraphic assemblages of shallowing upwards sequences.Within the framework,sequences are separated by clear boundaries and stratigraphic assemblages are stable and highly comparable.The paper also discussed the mechanisms behind the formation of early reservoirs in the high-frequency sequence framework and proposed that the high-frequency sequences controlled the order of lithofacies development and the syngenetic karstification,and thus controlled the development of different genetic types of reservoirs.

Key words: high-frequency sequence, carbonate rock, Jialinjiang Formation, epicontinental sea platform, Moxi gas field

中图分类号:

TE121.3

刘宏,王高峰,刘南,等. 磨溪气田嘉陵江组二段陆表海台地高频层序发育特征及对储层的控制[J]. 石油与天然气地质, 2016, 37(5): 713-720. doi: 10.11743/ogg20160511 Liu Hong,Wang Gaofeng,Liu Nan,et al. Characterization of high-frequency sequences in the epicontinental carbonate platform of Jia 2 member in Moxi gas field and its controls over reservoirs[J]. Oil & Gas Geology, 2016, 37(5): 713-720. doi: 10.11743/ogg20160511

参考文献

[1] Goodwin P,W & Anderson E J.Punctuated aggradational cycles:a general hypothesis of episodic stratigraphic accumulation[J].Journal of Geology,1985,93:515-533.
[2] Van Wagoner J C,Posamentier H W,Mitchum R M,et al.An overview of sequence stratigraphy and key definitions,[C]//Wilgus C K,Hastings B S,Kendall C G,et al.Sea level changes:an integrated approach.SEPM(Special Publication),1988,42:39-45.
[3] Van Wagoner J C,Mitchum R M,Campion K M,et al.Siliciclastic sequence stratigraphy in well logs,coresand outcrops:concepts for high resolution correlation of time and facies[J].AAPG,1990,7:1-55.
[4] Mitchum R M,Van Wagoner J C.High-frequency sequences and their stacking patterns:sequence stratigraphic evidence of high-frequency eustatic cycles[J].Sedimentary Geology,1991,70:131-147.
[5] 梅冥相.从旋回的有序叠加形式到层序的识别和划分:层序地层学进展之三[J].古地理学报,2011,13(1):37-54. Mei Mingxiang.From vertical stacking patern of cycles to discerning and division of sequences:The third advance in sequence sratigraphy[J].Journal of Palaeogeography,2011,13(1):37-54.
[6] 赵玉光,许效松,刘宝珺.上扬子台地西缘峨眉地区三叠纪高频层序与海平面振荡研究[J].岩相古地理,1996,16(1):1-18. Zhao Yuguang,Xu Xiaosong,Liu Baojun.High-frequency sequences and sea-level oscillations in the Emei area on the western margin of the upper Yzngtze platform[J].Sedimentary Facies and Palaeogeography,1996,16(1):1-18.
[7] 陈洪德,彭军,田景春,等.上扬子克拉通南缘中泥盆统-石炭系高频层序及复合海平面变化[J].沉积学报,2000,18(2):181-189. Cheng Hongde,Peng Jun,Tian Jingchun,et al.The Middle Devonian to Carboniferous high-frequency sequences and composite sea-level changes on the southern margin of the upper Yzngtze Craon basic[J].Acta Sedimentlolgica Sinica,2000,18(2):181-189.
[8] 梅冥相,徐德斌,周洪瑞.米级旋回层序的成因类型及其相序组构特征[J].沉积学报,2000,18(1):43-49. Mei Mingxiang,Xu Debin,Zhou Hongrui.Geneic types of Meter-Scale Cyclic sequences and their fabric features of facies-succession[J].Acta Sedimentlolgica Sinica,2000,18(1):43-49
[9] 梅冥相,高金汉,孟庆芬,等.天津蓟县中元古界雾迷山组微指状叠层石及其对1250Ma±叠层石衰减事件的响应[J].古地理学报,2008,05:495-509. Mei Mingxiang,Gao Jinhan,Meng Qingfen,et al.Microdigital stromatolites and their response to stromatolite decline at 1250,Ma+ for the Mesoproterozoic Wunishan formation at Jixian section in Tianjin[J].Journal of Palaeogeography,,2008,05:495-509.
[10] 武法东,苏新,周平,等.东海陆架盆地下第三系高频层序分析[J].地质论评,2001,47(1):47-52. Wu Fadong,Su Xin,Zhou Ping,et al.Analysis ofpaleogene high-frequency sequences in the east China sea shelf basin[J].Geological Review,2001,47(1):47-52.
[11] 刘宏,孙振,李卓沛,等.三叠纪嘉陵江期华蓥山同沉积断层的沉积、储层响应[J].地层学杂志,2010,03:312-320. Liu Hong,Sun Zhen,Li Zhuopei,et al.Syndepositionaltectonic activities in the HuaYingShan Fracture belt during the Triassic JiaLing River phase and its impact on sedimentation and reservoir development[J].Journal of Stratigraphy,2010,03:312-320.
[12] 谭秀成,邹娟,李凌,等磨溪气田嘉二段陆表海型台地内沉积微相研究[J].石油学报,2008,29(2):219-225. Tan Xiucheng,Zou Juan,Li Ling,et al.Research on sedimentary microfacies of the epicontinental sea platform of Jia 2 member in Moxi gas field[J].Acta Petrolei Sinica,2008,29(2):219-225.
[13] 王鸿祯.中国古地理图集[M].北京:中国地图出版社,1985:1-283. Wang Hongzhen.Atlas of the Palaeogeography of China[M].Beijing:China Cartographic Publishing House,1985:1-283.
[14] 王宓君,包茨,肖明德,等.中国石油地质志(卷十)四川油气区[M].北京:石油工业出版社,1989:1-516 Wang Mijun,Bao Ci,Xiao Mingde,et al.Petroleum Geology of China (vol.10) Sichuan hydrocarbon provinces[M].Beijing:Petroleum Industry Press,1989:1-516.
[15] Einsele G, Seilacher A.Cyclic and event stratification[M].England:Springer-Verlag,1982.1-306.
[16] Masetti D, Nero C,Bosellini A.Deep-water say-mmetric cycles and progradation of carbonate platforms governed by high-frequence eustatic oscillations[J].Geology,1991,19:336-339.
[17] Osleger D.Subtidal carbonate cycles:implications for allocyclic vs.autocyclic controls[J].Geology,1991,19:917-920.
[18] Read J F.Carbonate platform facies models[J].American Assocation Petrology Geology Bulletim.1985,69:1~21.
[19] 胡明毅,魏国齐,李思田,等.四川盆地嘉陵江组层序-岩相古地理特征和储层预测[J].沉积学报,2010,28(6):1145-1152. Hu Mingyi,Wei Guoqi,Li Sitian,et al.Characterisics of sequence-based lithofacies and paleogeography,and reservior predicion of the Jialingjiang formation in Sichuan basin[J].Acta Sedimenologica Sinica,2010,28(6):1145-1152.
[20] 谭秀成,刘晓光,陈景山,等.磨溪气田嘉二段陆表海碳酸盐岩台地内滩体发育规律[J].沉积学报,2009,27(5):995-1001. Tan Xiucheng,Liu Xiaoguang,Chen Jingshan,et al.Shoal development within the epicontinental carbonate platform,Jia 2 member,Lower Triassic,Moxi gas field,central Sichuan basin[J].Acta Sedimenologica Sinica,2009,27(5):995-1001.
[21] 刘宏,谭秀成,周彦,等.颗粒碳酸盐岩测井相及其对滩相储层的指示意义[J].天然气地球科学,2007,18(4):527-530. Liu Hong,Tan Xiucheng,Zhou Yan,et al.Logging facies of granular carbonate rocks and its implication on reservoir evaluation[J].Natural Gas Geoscience,2007,18(4):527-530.
[22] 雷克辉,朱广生,毛宁波,等.在小波时频域中研究沉积旋回[J].石油地球物理勘探,1998,S1:72-78,177. Lei Kehui,Zhu Guangsheng,Mao Ningbo,et al.Frequency study sedimentary cycles in Wavelet Time-Frequency domain[J].Oil Geophysical Prospecting,1998,S1:72-78,177.
[23] 李庆谋,刘少华.地球物理测井序列的小波波谱方法[J].地球物理学进展,2002,01:78-83,101. Li Qingmou,Liu Shaohua.Waveletscalogram and application for geophysical well[J].Progress in Geophysics,2002,01:78-83,101.
[24] 余继峰,李增学,王明镇,等.鲁西-济阳C-P陆表海沉积测井层序对比分析[J].中国矿业大学学报,2007,01:85-90. Yu Jifeng,Li Zengxue,Wang Mingzhen,et al.Correlaion andanalysis of well-log sequences of epicontinental sea sediments of Permo-carboniferous in Luxi and Jiyang[J].Journal of China University of Mining & Technology,2007,01:85-90.
[25] Schwarzacher W.Sedimentary moelsand quantitative stratigraphy[M].Amserdam:Elsevier,1975,1-225.
[26] 乔占峰,李国蓉,李弢,等.泸州古隆起地区嘉陵江组层序特征及其对碳酸盐岩储层的控制[J].沉积学报,2008,01:92-99,110. Qiao Zhanfeng,Li Guorong,Li Tao,et al.Sequence-stratigraphic features and their controlson carbonate reservoirs for the Triassic Jialingjiang formation of the Luzhou Paleohigh in Sichuan basin[J].Acta Sedimenologica Sinica,2008,01:92-99,110.
[27] 马永生,储昭宏.普光气田台地建造过程及其礁滩储层高精度层序地层学研究[J].石油与天然气地质,2008,05:548-556. Ma Yongsheng,Chu Zhaohong.Building-up process of carbonate platform and high-resoluion sequence straigraphy of reservoirs of reef and oolitic shoal facies in Puguang gas field[J].Oil & Gas Geology,2008,05:548-556.
[28] 刘嘉庆,李忠,韩银学,等.塔里木盆地塔中上奥陶统碳酸盐台地高频层序控制的早期成岩作用及其对储层分布的影响[J].岩石学报,2010,12:3629-3640. Liu Jiaqing,Li Zhong,Han Yinxue,et al.Early diagenesis in high-frequency sequence framework of the Upper Ordovician carbonate platform in Tazhong,Tarim basin and its influence on reservoir distribution[J].Acta Petrologica Sinica,2010,12:3629-3640.
[29] 刘宏,谭秀成,李凌,等.孔隙型碳酸盐岩储集层特征及主控因素_以川西南嘉陵江组嘉_5段为例[J].石油勘探与开发,201138(3)275-281. Liu Hong,Tan Xiucheng,Li Ling,et al.Characteristics and main controlling factors of porous carbonate reservoirs:A case from the Jia 5 Member of the Jialingjiang formation,southwest Sichuan basin[J].Petroleum Exploration and Development,201138(3)275-281.
[30] 周彦,谭秀成,刘宏,等.四川盆地磨溪构造嘉二段孔隙型碳酸盐岩储层的评价[J].石油学报,2009,30(3):372-377. Zhou Yan,Tan Xiucheng,Liu Hong,et al.Evaluation of porous carbonate reservoir of Jia 2 Member in Moxi structure of Sichuan basin[J].Acta Petrolei Sinica,2009,30(3):372-377.
[31] 何治亮,高志前,张军涛,等.层序界面类型及其对优质碳酸盐岩储层形成与分布的控制[J].石油与天然气地质,2014,35(6):853-859. He Zhiliang,Gao Zhiqian,Zhang Juntao,et al.Types of sequence boundaries and their control over formation and distribution of quality carbonate reservoirs[J].Oil & Gas Geology,2014,35(6):853-859.
[32] 马宏霞,孙辉,邵大力,等.缅甸若开盆地上中新统-上新统深水沉积层序地层划分及控制因素[J].石油与天然气地质,2015,36(1):136-141. Ma Hongxia,Sun Hui,Shao Dali,et al.Sequence stratigraphy of the Upper Miocene-Pliocene deepwater deposits and its controlling factors in Rakhine Basin,Myanmar[J].Oil & Gas Geology,2014,35(6):136-141.

磨溪气田嘉陵江组二段陆表海台地高频层序发育特征及对储层的控制

Characterization of high-frequency sequences in the epicontinental carbonate platform of Jia 2 member in Moxi gas field and its controls over reservoirs

PDF (PC)

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

[1]	丁文龙, 李云涛, 韩俊, 黄诚, 王来源, 孟庆修. 碳酸盐岩储层高精度构造应力场模拟与裂缝多参数分布预测方法及其应用[J]. 石油与天然气地质, 2024, 45(3): 827-851.
[2]	杨德彬, 鲁新便, 鲍典, 曹飞, 汪彦, 王明, 谢润成. 塔里木盆地北部奥陶系海相碳酸盐岩断溶体油藏成因类型及特征再认识[J]. 石油与天然气地质, 2024, 45(2): 357-366.
[3]	张赫驿, 杨帅, 张玺华, 彭瀚霖, 李乾, 陈聪, 高兆龙, 陈安清. 川东地区中二叠统茅口组沉积微相与环境演变[J]. 石油与天然气地质, 2024, 45(2): 457-470.
[4]	江同文, 邓兴梁, 曹鹏, 常少英. 塔里木盆地富满断控破碎体油藏储集类型特征与注水替油效果[J]. 石油与天然气地质, 2024, 45(2): 542-552.
[5]	屈海洲, 郭新宇, 徐伟, 李文皓, 唐松, 邓雅霓, 何仕鹏, 张云峰, 张兴宇. 碳酸盐岩微孔隙的分类、成因及对岩石物理性质的影响[J]. 石油与天然气地质, 2023, 44(5): 1102-1117.
[6]	史今雄, 赵向原, 潘仁芳, 曾联波, 朱正平. 川中地区震旦系灯影组碳酸盐岩天然裂缝特征及其对气井产能影响[J]. 石油与天然气地质, 2023, 44(2): 393-405.
[7]	邹才能, 谢增业, 李剑, 张璐, 杨春龙, 崔会英, 王晓波, 郭泽清, 潘松圻. 典型碳酸盐岩大气田规模聚集差异性及其主控因素[J]. 石油与天然气地质, 2023, 44(1): 1-15.
[8]	张涛, 张亚雄, 金晓辉, 周雁, 张军涛, 谷宁, 张威, 王濡岳, 鲁锴. 鄂尔多斯盆地奥陶系马家沟组碳酸盐岩-蒸发岩层系层序地层模式及其对源-储的控制作用[J]. 石油与天然气地质, 2023, 44(1): 110-124.
[9]	刘建章, 蔡忠贤, 滕长宇, 张恒, 陈诚. 塔里木盆地顺北地区克拉通内走滑断裂带中-下奥陶统储集体方解石脉形成及其与油气充注耦合关系[J]. 石油与天然气地质, 2023, 44(1): 125-137.
[10]	何治亮, 赵向原, 张文彪, 吕心瑞, 朱东亚, 赵峦啸, 胡松, 郑文波, 刘彦锋, 丁茜, 段太忠, 胡向阳, 孙建芳, 耿建华. 深层-超深层碳酸盐岩储层精细地质建模技术进展与攻关方向[J]. 石油与天然气地质, 2023, 44(1): 16-33.
[11]	丁茜, 王静彬, 杨磊磊, 朱东亚, 江文滨, 何治亮. 基于模拟实验探讨断裂-流体-岩石体系中的矿物溶解-沉淀过程[J]. 石油与天然气地质, 2023, 44(1): 164-177.
[12]	李剑, 杨春龙, 谢武仁, 芮宇润, 王晓波, 张璐, 谢增业, 郭泽清. 四川盆地安岳气田震旦系台缘带和台内地区天然气成藏差异性及勘探领域[J]. 石油与天然气地质, 2023, 44(1): 34-45.
[13]	钱一雄, 武恒志, 周凌方, 董少峰, 王琼仙, 宋晓波, 邓美洲, 李勇. 深埋条件下微生物碳酸盐岩成岩作用与孔隙演化——以四川盆地西部中三叠统雷口坡组为例[J]. 石油与天然气地质, 2023, 44(1): 55-74.
[14]	吕心瑞, 邬兴威, 孙建芳, 夏东领, 李彦普, 丁炎志, 王斌. 深层碳酸盐岩储层溶洞垮塌物理模拟及分布预测[J]. 石油与天然气地质, 2022, 43(6): 1505-1514.
[15]	胡安平, 沈安江, 张杰, 吴东旭, 付小东, 蒙绍兴. 碳酸盐岩-膏盐岩高频沉积旋回组合生-储特征[J]. 石油与天然气地质, 2022, 43(4): 943-956.