鄂尔多斯盆地中部奥陶系马四段天然气成藏主控因素

doi:10.3969/j.issn.1006-6535.2021.02.004

特种油气藏 ›› 2021, Vol. 28 ›› Issue (2): 27-33.DOI: 10.3969/j.issn.1006-6535.2021.02.004

鄂尔多斯盆地中部奥陶系马四段天然气成藏主控因素

任海姣^1,2, 吴伟涛^2,3, 赵靖舟^2,3, 陈梦娜¹

1.中国石油新疆油田分公司,新疆克拉玛依 834000;
2.西安石油大学,陕西西安 710065;
3.陕西省油气成藏地质学重点实验室,陕西西安 710065

收稿日期:2020-06-03 修回日期:2021-01-09 出版日期:2021-04-25 发布日期:2022-02-16
通讯作者: 赵靖舟(1962—),男,教授,1983年毕业于西北大学地质学专业,2002年毕业于中国石油勘探开发研究院矿产普查与勘探专业,获博士学位,现从事油气成藏地质学、非常规油气地质与勘探研究工作。
作者简介:任海姣(1992—),女,助理工程师,2015年毕业于西安石油大学资源勘查工程专业,2019年毕业于该校矿产普查与勘探专业,获硕士学位,现从事油气成藏地质学研究工作。
基金资助:
陕西省教育厅重点科研计划项目“鄂尔多斯盆地中部奥陶系中组合天然气成藏富集规律研究”(2015JS094)

Key Controlling Factors of Natural Gas Accumulation in the Ordovician Ma Member 4 in the Central Ordos Basin

Ren Haijiao^1,2, Wu Weitao^2,3, Zhao Jingzhou^2,3, Chen Mengna¹

1. PetroChina Xinjiang Oilfield Company, Karamay, Xinjiang 834000, China;
2. Xi'an Shiyou University, Xi'an, Shaanxi 710065, China;
3. Shaanxi Key Laboratory of Petroleum Accumulation Geology, Xi'an, Shaanxi 710065, China

Received:2020-06-03 Revised:2021-01-09 Online:2021-04-25 Published:2022-02-16

摘要/Abstract

摘要： 鄂尔多斯盆地中部奥陶系马四段碳酸盐岩天然气具有一定的勘探潜力,但其天然气成藏主控因素尚不清楚,限制了该区勘探的深入,针对这一问题,利用钻井、测井、地球化学、试气等资料,分析奥陶系马四段天然气藏特征,从气源岩条件、储层特征、运移条件和遮挡条件等方面开展成藏主控因素研究。研究结果表明:马四段气藏类型主要为岩性气藏;气源岩条件控制着天然气的贫富,马四段天然气为上古生界煤系源岩和下古生界碳酸盐岩源岩生成的混合气,并以前者为主,由于气源条件不充足,整体产气量较少;储层特征导致天然气主要富集在物性中等的灰云坪相和云灰坪相;孔隙、裂缝与断层组成的三维网络系统为天然气运移提供通道;在灰岩遮挡条件控制下,天然气主要分布在厚层白云岩与灰岩岩性变化带以及厚层灰岩中部云质含量增加的部位。通过对马四段天然气成藏主控因素的认识,可为鄂尔多斯盆地海相碳酸盐岩勘探提供理论依据。

关键词: 天然气成藏, 主控因素, 气源条件, 碳酸盐岩, 沉积相, 海相沉积, 奥陶系马四段, 鄂尔多斯盆地

Abstract: There is certain potential of exploring the carbonate gas in the Ordovician Ma Member 4 in the Central Ordos Basin. However, the key controlling factors for natural gas accumulation are not clear, limiting the exploration in this area. In response to this problem, the gas reservoir characteristics of the Ordovician Ma Member 4 was analyzed with reference to drilling, logging, geochemistry, gas testing and other data. The key controlling factors of hydrocarbon accumulation were studied from the aspects of gas source rock conditions, reservoir characteristics, migration conditions, and shielding conditions. The results showed that the gas reservoirs of the Ordovician Ma Member 4 were mainly lithological gas reservoirs; the richness of natural gas was controlled by the gas-source rock conditions; the natural gas of the Ordovician Ma Member 4 was the gas mixture generated by the upper Paleozoic coal-bearing source rocks and the Lower Paleozoic carbonate source rocks, dominated by the former, and the overall gas produced was less due to insufficient gas source; the characteristics of the reservoir made the natural gas mainly accumulated in the lime dolomite flat facies and dolomite lime flat facies with medium physical properties; the three-dimensional network system composed of pores, fractures and faults provided channels for natural gas migration; under the control of limestone shielding conditions, the natural gas was mainly distributed in the section with lithologic change of thick dolomite and limestone, and the central section with increased dolomite content of thick limestone. The understanding of the key controlling factors of natural gas accumulation in the Ordovician Ma Member 4 can provide a theoretical foundation for the exploration of marine carbonate rocks in the Ordos Basin.

Key words: natural gas accumulation, key controlling factors, gas source conditions, carbonate rocks, sedimentary facies, marine facies, Ordovician Ma Member 4, Ordos Basin

中图分类号:

TE122.1

任海姣, 吴伟涛, 赵靖舟, 陈梦娜. 鄂尔多斯盆地中部奥陶系马四段天然气成藏主控因素[J]. 特种油气藏, 2021, 28(2): 27-33.

Ren Haijiao, Wu Weitao, Zhao Jingzhou, Chen Mengna. Key Controlling Factors of Natural Gas Accumulation in the Ordovician Ma Member 4 in the Central Ordos Basin[J]. Special Oil & Gas Reservoirs, 2021, 28(2): 27-33.

参考文献

[1] 戚家振,过敏.鄂尔多斯盆地东北部奥陶系马家沟组成藏主控因素分析[J].特种油气藏,2017,24(4):54-59.
QI Jiazhen,GUO Min.Analysis of major controlling factor for hydrocarbon accumulation in Ordovician Majiagou Formation in northeastern Ordos Basin[J].Special Oil & Gas Reservoirs,2017,24(4):54-59.
[2] 何自新,郑聪斌,王彩丽,等.中国海相油气田勘探实例之二:鄂尔多斯盆地靖边气田的发现与勘探[J].海相油气地质,2005,10(2):37-44.
HE Zixin,ZHENG Congbin,WANG Caili,et al.Cases of discovery and exploration of marine fields in China(Part 2):Jingbian Gas Field, Ordos Basin[J].Marine Origin Petroleum Geology,2005,10(2):37-44.
[3] 傅锁堂,黄建松,闫小雄.鄂尔多斯盆地古生界海相碳酸盐岩勘探新领域[J].天然气工业,2002,22(6):17-21.
FU Suotang,HUANG Jiansong,YAN Xiaoxiong.New exploration realm of Paleozoic marine carbonate rocks in E'Erduosi Basin[J].Natural Gas Industry,2002,22(6):17-21.
[4] 于洲,丁振纯,吴东旭,等.鄂尔多斯盆地中东部奥陶系马家沟组沉积相演化模式研究[J].海相油气地质,2017,22(3):12-22.
YU Zhou,DING Zhenchun,WU Dongxu,et al.Sedimentary facies evolution model of Ordovician Majiagou Formation,central-Eastern Ordos Basin[J].Marine Origin Petroleum Geology,2017,22(3):12-22
[5] 包洪平,杨帆,蔡郑红,等.鄂尔多斯盆地奥陶系白云岩成因及白云岩储层发育特征[J].天然气工业,2017,37(1):32-45.
BAO Hongping,YANG Fan,CAI Zhenghong,et al.Origin and reservoir characteristics of Ordovician dolostones in the Ordos Basin[J].Natural Gas Industry,2017,37(1):32-45.
[6] 史基安,邵毅,张顺存,等.鄂尔多斯盆地东部地区奥陶系马家沟组沉积环境与岩相古地理研究[J].天然气地球科学,2009,20(3):316-324.
SHI Ji'an,SHAO Yi,ZHANG Shuncun,et al.Lithofacies paleogeography and sedimentary environment in Ordovician Majiagou Formation,eastern Ordos Basin[J].Natural Gas Geoscience,2009,20(3):316-324.
[7] 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.
SU Zhongtang,CHEN Hongde,XU Fenyan,et al.Geochemistry and dolomitization mechanism of Majiagou dolomites in Ordovician,Ordos,China[J].Acta Petrologica Sinica,2011,27(8):2230-2238.
[8] 时保宏,刘亚楠,武春英,等.鄂尔多斯盆地古隆起东侧奥陶系马家沟组中组合成藏地质条件[J].石油与天然气地质,2013,34(5):610-618.
SHI Baohong,LIU Yanan,WU Chunying,et al.Geological conditions for hydrocarbon accumulation in middle reservoir-source rock combination of the Ordovician Majiagou Formation on the east side of the paleo-uplift in Ordos Basin[J].Oil & Gas Geology,2013,34(5):610-618.
[9] 吴伟涛,赵靖舟,孙六一,等.鄂尔多斯盆地西部奥陶系克里摩里组天然气成藏特征[J].天然气地球科学,2015,26(10):1862-1872.
WU Weitao,ZHAO Jingzhou,SUN Liuyi,et al.Accumulation characteristics of natural gas from the Ordovician Kelimoli Formation,western Ordos Basin[J].Natural Gas Geoscience,2015,26(10):1862-1872.
[10] 谢锦龙,吴兴宁,孙六一,等.鄂尔多斯盆地奥陶系马家沟组五段岩相古地理及有利区带预测[J].海相油气地质,2013,18(4):23-32.
XIE Jinlong,WU Xingning,SUN Liuyi,et al.Lithofacies palaeogeography and potential zone prediction of Ordovician Majiagou Member-5 in Ordos Basin[J].Marine Origin Petroleum Geology,2013,18(4):23-32.
[11] 关德师,张文正,裴戈,等.鄂尔多斯盆地中部气田奥陶系产层的油气源[J].石油与天然气地质,1993,14(3):191-199.
GUAN Deshi,ZHANG Wenzheng,PEI Ge,et al.Oil-gas sources of Ordovician reservoir in gas field of central Ordos Basin[J].Oil & Gas Geology,1993,14(3):191-199.
[12] 戴金星,李剑,罗霞,等.鄂尔多斯盆地大气田的烷烃气碳同位素组成特征及其气源对比[J].石油学报,2005,26(1):18-26.
DAI Jinxing,LI Jian,LUO Xia,et al.Alkane carbon isotopic composition and gas source in giant gas fields of Ordos Basin[J].Acta Petrolei Sinica,2005,26(1):18-26.
[13] 黄第藩,熊传武,杨俊杰,等.鄂尔多斯盆地中部气田气源判识和天然气成因类型[J].天然气工业,1996,16(6):1-6.
HUANG Difan,XIONG Chuanwu,YANG Junjie,et al.Gas source discrimination and natural gas genetic types of central gas field in E'erduosi Basin[J].Natural Gas Industry,1996,16(6):1-6.
[14] 王传刚,王毅,许化政,等.论鄂尔多斯盆地下古生界烃源岩的成藏演化特征[J].石油学报,2009,30(1):38-44.
WANG Chuangang,WANG Yi,XU Huazheng,et al.Discussion on evolution of source rocks in Lower Paleozoic of Ordos Basin[J].Acta Petrolei Sinica,2009,30(1):38-44.
[15] 李军,赵靖舟,王大兴,等.鄂尔多斯盆地中央古隆起东侧奥陶系中组合天然气成因与来源[J].石油学报,2016,37(7):821-831.
LI Jun,ZHAO Jingzhou,WANG Daxing,et al.Genesis and source of the Ordovician mid-assemblage natural gas in the east side of the central paleo-uplift, Ordos Basin[J].Acta Petrolei Sinica,2016,37(7):821-831.
[16] 赵靖舟,王大兴,孙六一,等.鄂尔多斯盆地西北部奥陶系气源及其成藏规律[J].石油与天然气地质,2015,36(5):711-720.
ZHAO Jingzhou,WANG Daxing,SUN Liuyi,et al.Origin of the Ordovician gas and its accumulation patterns in northwestern Ordos Basin[J].Oil & Gas Geology,2015,36(5):711-720.
[17] ZHAO Zilong,ZHAO Jingzhou,REN Haijiao,et al.Characteriza-tion and formation mechanisms of fractures and their significance to hydrocarbon accumulation:a case study of Lower Ordovician mid-assemblage Formations in central Ordos Basin,China[J].Journal of Central South University,2018,25(11):2766-2784.

鄂尔多斯盆地中部奥陶系马四段天然气成藏主控因素

Key Controlling Factors of Natural Gas Accumulation in the Ordovician Ma Member 4 in the Central Ordos Basin

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

本文评价

[1]	赵辉, 齐怀彦, 王凯, 蔡涛, 孟利华, 周兵. 致密砂岩油藏测井响应特征及有利区评价[J]. 特种油气藏, 2023, 30(5): 35-41.
[2]	钟红利, 卓自敏, 张凤奇, 张佩, 陈玲玲. 鄂尔多斯盆地甘泉地区长7页岩油储层非均质性及其控油规律[J]. 特种油气藏, 2023, 30(4): 10-18.
[3]	秦迎峰. 松辽盆地三肇凹陷葡萄花油层油气成藏主控因素及成藏模式[J]. 特种油气藏, 2023, 30(4): 28-34.
[4]	郭琪琪, 耳闯, 赵靖舟, 滕云玺, 谭诗锦, 沈聪敏. 鄂尔多斯盆地大宁—吉县地区盒8段储层特征与优质储层控制因素[J]. 特种油气藏, 2023, 30(3): 19-28.
[5]	汪如军, 冯建伟, 李世银, 昌伦杰, 杜赫, 邓兴梁. 塔北—塔中隆起奥陶系富油气三角带断裂特征及控藏分析[J]. 特种油气藏, 2023, 30(2): 26-35.
[6]	昝春景, 季汉成, 赵忠波, 施尚明. 长春岭南区块浅层气成藏条件及其主控因素[J]. 特种油气藏, 2023, 30(2): 36-43.
[7]	杨浩, 阳波, 石伟, 林丽, 方燕, 朱玉双. 鄂尔多斯盆地华庆地区长9油藏富集特征及潜力区预测[J]. 特种油气藏, 2023, 30(2): 78-85.
[8]	庞兰苏, 王杨, 蒋薇, 王永生, 高国海, 王欣. 基于机器学习的短生产周期碳酸盐岩气井产量预测研究[J]. 特种油气藏, 2023, 30(2): 134-141.
[9]	邱文波, 蔡秦秦, 张雪锐, 蒋少龙, 郭龙, 袁子琦. 二连盆地大庙凹陷油气富集规律及有利目标优选[J]. 特种油气藏, 2023, 30(1): 50-56.
[10]	黄董, 曾德铭, 王兴志, 谢圣阳, 张芮, 张少敏, 郭奕浩. 川中地区侏罗系大安寨段沉积相及有利岩石组合分析[J]. 特种油气藏, 2023, 30(1): 65-73.
[11]	王容, 李隆新, 刘晓旭, 罗瑜, 张娜. 深层碳酸盐岩气藏改建储气库注采能力预测方法及应用[J]. 特种油气藏, 2023, 30(1): 126-133.
[12]	李浩, 冯玉福. 考虑黏滞性低渗透油藏数值模拟应用研究[J]. 特种油气藏, 2023, 30(1): 134-138.
[13]	单俊峰, 吴炳伟, 金科, 董德胜, 刘媛媛, 崔晓磊, 迟润龙, 聂文彬. 鄂尔多斯盆地宜川-黄龙地区上古生界储层特征及其对天然气成藏的影响[J]. 特种油气藏, 2022, 29(6): 29-38.
[14]	韩珊, 车明光, 苏旺, 肖毓祥, 吴忠宝, 陈建阳, 汪莉彬. 四川盆地威远区块页岩气单井产量预测方法及应用[J]. 特种油气藏, 2022, 29(6): 141-149.
[15]	周晓龙. 辽河西部凹陷牛心坨地区沙四段储层特征及主控因素[J]. 特种油气藏, 2022, 29(5): 49-56.