天然气地球科学

• 天然气地质学 • 上一篇    下一篇

塔北西部玉东地区奥陶系油气成藏条件与勘探潜力

周俊峰,张虎权,余建平,朱永峰,姚清洲,袁玉春   

  1. (1.中国石油勘探开发研究院西北分院,甘肃 兰州730020;
    2.中国石油塔里木油田公司勘探开发研究院,新疆 库尔勒 841000)
  • 收稿日期:2015-05-26 修回日期:2015-08-16 出版日期:2015-09-20 发布日期:2015-09-20
  • 作者简介:周俊峰(1979-),男,湖北钟祥人,工程师,硕士,主要从事石油地质综合研究. E-mail:cug1118@sina.com.cn.
  • 基金资助:

    中国石油集团重大专项(编号:2011ZX05004-04)资助.

Analysis of the Hydrocarbon Accumulation Conditions and Exploration Potential in the Ordovician in Yudong Area of West Tabei Uplift

ZHOU Jun-feng,ZHANG Hu-quan,YU Jian-ping,ZHU Yong-feng,YAO Qing-zhou,YUAN Yu-chun   

  1. (1.Research Institute of Exploration and Development-Northwest,PetroChina,Lanzhou 730020,China;
    2.Exploration and Development Research Institute,Tarim Oilfield Company,PetroChina,Korla 841000,China)
  • Received:2015-05-26 Revised:2015-08-16 Online:2015-09-20 Published:2015-09-20

摘要:

塔北西部玉东地区奥陶系未获得油气突破。对该区油气成藏条件认识不明确,其勘探潜力不落实。通过对玉东地区构造、成藏演化分析,明确了鹰山组碳酸盐岩岩溶储集体在晚海西期形成准层状古油藏,后期的构造抬升仅造成构造高点油藏破坏,对分布于围斜部位缝洞型油藏影响不大。通过对源岩条件、储盖组合及圈闭条件等成藏因素综合评价,估算了奥陶系碳酸盐岩的油气勘探潜力,明确玉东地区是塔里木盆地重要的油气战略接替区。

关键词: 勘探潜力, 成藏条件, 玉东地区, 塔里木盆地

Abstract:

In the Ordovician there has been no discovery and break through of oil and gas in Yudong area of western Tabei.Previous studies suggested that there is no accumulation,or reservoir has been destroyed in the Yudong area,and there is no exploration potential.To further explore the hydrocarbon potential of carbonate rocks in the Karayulgun structural belt of west Tabei Uplift,according to the question in previous studies,this research carries out detailed analysis of the Ordovician oil-gas accumulation conditions in the Yudong area based on the relationship between structure and accumulation of hydrocarbon.On the basis of the analysis of fine structure interpretaion and evolution,it is clear that the Yudong structure was mainly formed in Late Hercynian.Affected by the Karayulgun fault sustained activity,the Yudong tectonic uplifted,the strata have suffered variable degrees of erosion.The analytical results of reservoir formation conditions show that the karst reservoirs in the Yingshan Formation could capture oil and gas generated in Late Hercynian,and form quasi-layered oil deposits distributing along the Ordovician reservoir.Reservoirs in the high position were eroded during the later stages of tectonic uplifting,but other lower structural positions relative to the Yudong 2 were still relatively high area.They not only avoided the erosion during the later stages of tectonic uplifting,but alsowere in a favorable position during the later adjustment of the reservoir.Considering the source rock condition,structure,reservoir cap assemblage and igneous influence,the authors think Yudong has similar reservoir conditions as Yingmai 2,and both are quasi-layered reservoir controlled by fracture and cave karst reservoir with great exploration potential.

Key words: Exploration potential, Reservoir forming conditions, Yudong, Tarim Basin

中图分类号: 

  • TE122.3

[1]An Haiting,Li Haiyin,Wang Jianzhong.Tecton ic 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.塔北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.]
[2]Zhang Shuichang,Liang Digang,Zhang Baoming.Generation of Marine Oil and Gas inTarim Basin[M].Beijing:Petroleum Industry Press,2004.[张水昌,梁狄刚,张宝民.塔里木盆地海相油气的生成[M].北京:石油工业出版社,2004.]
[3]Sun Longde.Marine carbonate rocks and hydrocarbon in Tarim Basin[J].Marine Origin Petroleum Geology,2007,12(4):10-15.[孙龙德.塔里木盆地海相碳酸盐岩与油气[J].海相油气地质,2007,12(4):10-15.]
[4]Zhang Shuichang,Zhang Baomin,Wang Feiyu,et al.Two sets ofmarine source rocks in Tarim Basin:The characteristics of organicmatter,development environment and control factors[J].Progress in Chinese Science,2001,11(3):261-268.[张水昌,张宝民,王飞宇,等.塔里木盆地两套海相烃源岩:有机质性质、发育环境及控制因素[J].自然科学进展,2001,11(3):261-268.]
[5]Jia Chengzao.Structural characteristics and oil/gas accumulative regularity in Tarim Basin[J].Xinjiang Petroleum Geology,1999,20(3):177-183.[贾承造.塔里木盆地构造特征与油气聚集规律[J].新疆石油地质,1999,20(3):177-183.]
[6]Wei Guoqi,Jia Chenzao,Shi Yangshen.Characteristics of the Meso Cenozoic torsional fault system in northern north Tarim Uprift[J].Acta Petrolei Sinica,2001,22(1):20-24.[魏国齐,贾承造,施央申.塔北隆起北部中新生界扭性断裂系统特征[J].石油报,2001,22(1):20-24.]
[7]Cui Zehong,Wang Zhixin,Tang Liangjie.Characteristics of overlapped faults in the noth of the Tarbei Uplift and anaysis of genetic setting[J].Geology in China,2005,32(3):378-385.[崔泽宏,王志欣,汤良杰.塔北隆起北部叠加断裂构造特征与成因背景分析[J].中国地质,2005,32(3):378-385.]
[8]Li Yuejun,Yang Haijun,Zhao Yan.Tectonic framework and evolution of south Tianshan[J].Geotectonica et Metallogenia,2009,33(1):94-104.[李曰俊,杨海军,赵岩.南天山区域大地构造与演化[J].大地构造与成学,2009,33(1):94-104.]
[9]Zhou Junfeng,Zhang Huquan,Liu Jianxin.Ananysis of the Paleozoic fault characteristics and its formation mechanism of YM 1-2 work district in Tabei Uplift[J].Natural Gas Geoscience,2012,23(2):237-243.[周俊峰,张虎权,刘建新.塔北隆起YM1-2构造带古生界断裂特征及成因机制分析[J].天然气地球科学,2012,23(2):237-243.]
[10]Zhu Guangyou,Liu Xingwang,Zhu Yongfeng.The characteristics and the accumulation mechanism of complex reservoirsin the Hanilcatam area Tarim Basin[J].Bulletin of Miner-alogy,Petrology and Geochemistry,2013,32(2):231-242.[朱光有,刘星旺,朱永峰.塔里木盆地哈拉哈塘地区复杂油气藏特征及其成藏机制[J].矿物岩石地球化学通报,2013,32(2):231-242.]
[11]Cheng Bin,Wang Tieguan,Chang Xiangchun.Application of C5-C7light hydrocarbons in geochemical studies:A case study of Ordovician crude oils from the Halahatang Depression,Ta-bei Uplift[J].Natural Gas Geoscience,2013,24(2):398-405.[程斌,王铁冠,常象春.C5—C7轻烃在原油地球化学研究中的应用——以塔北隆起哈拉哈塘凹陷奥陶系原油为例[J].天然气地球科学,2013,24(2):398-405.]
[12]Zhang Shuichang,Gao Zhiyong,Li Jianjun.Identification and distribution of marine hydro-carbon source rocks in the Ordovician and Cambrian of the Tarim Basin[J].Petroleum Exploration and Development,2012,39(3):285-294.[张水昌,高志勇,李建军.塔里木盆地寒武系—奥陶系海相烃源岩识别与分布预测[J].石油勘探与开发,2012,39(3):285-294.]
[13][KG*7/8]Zhao Zongju,Zhou Xinyuan,Zheng Xingping,et al.Evidences of chief source rock in Tarim Basin[J].Acta Petrolei Sinica,2005,26(3):10-15.[赵宗举,周新源,郑兴平,等.塔里木盆地主力烃源岩的诸多证据[J].石油学报,2005,26(3):10-15.]
[14][KG*6/7]Mi Jingkui,Zhang Shuichang,Chen Jianping,et al.Carbon isotopiccompositions and effect factors of oil from northern Tarim Basin[J].Petroleum Exploration and Development,2010,37(1):21-25.[米敬奎,张水昌,陈建平,等.塔北地区原油碳同位素组成特征及影响因素[J].石油勘探与开发,2010,37(1):21-25.]
[15]Zhang Chaojun,Jia Chengzao,Li Benliang,et al.Ancient karsts and hydrocarbon accumulation in the middle and western parts of the north Tarim Uplift,NW China[J].Petroleum Exploration and Development,2010,37(3):263-269.[张朝军,贾承造,李本亮,等.塔北隆起中西部地区古岩溶与油气聚集[J].石油勘探与开发,2010,37(3):263-269.]
[16]Shi Shuyuan,Hu Suyun,Liu Wei,et al.Ordovician paleokarst cave system and it′s controlling factor in Xekar,Tarim Basin[J].Natural Gas Geoscience,2014,25(2):167-177.[石书缘,胡素云,刘伟,等.塔里木盆地西克尔地区奥陶系溶洞系统特征及控制因素[J].天然气地球科学,2014,25(2):167-177.]
[17]Wang Huanhuan,Zhu Guangyou,Xue Haitao.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):183-191.[王欢欢,朱光有,薛海涛.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):183-191.]
[18]Lv Xiuxiang,Jin Zhijun.Ananysis on reservoir formation procession in Yangtake strcuturel belt of Tabe Uplift[J].Journal of the University of Petroleum,China,2000,24(1):48-52.[吕修祥,金之钧.塔北隆起羊塔克构造带油气成藏分析[J].石油大学学报:自然科学版,2000,24(1):47-52.]
[19]Sang Hong,Zhang Wei,Wang Yueran,et al.Characteristics of Permian volcanic rock reservoir in north Tarim Basin[J].Natural Gas Geoscience,2012,23(3):450-460.[桑洪,张巍,王月然,等.塔北地区二叠系火山岩储层特征研究[J].天然气地球科学,2012,23(3):450-460.]
[20]Zhang Nianchun,Cuihai-feng,Teng Tuanyu.Features of carbonate buried hill oil and gas reservoir in Yingmaili-Yaha region,Tarim Basin[J].Natural Gas Geoscience,2010,21(5):763-771.[张年春,崔海峰,滕团余.塔里木盆地英买力—牙哈地区碳酸盐岩潜山油气藏特征研究[J].天然气地球科学,2010,21(5):763-771.]
[21]Wang Zongli,Xu Xiaofeng,Li Jun.Reservoir forming patterns and exploration analysis of new area and new field in Tarim Basin[J].Natural Gas Geoscience,2011,22(1):73-80.[王宗礼,徐晓峰,李君.塔里木盆地油气成藏模式及新区新领域勘探方向分析[J].天然气地球科学,2011,22(1):73-80.]

[1] 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.
[2] 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.
[3] 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.
[4] 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.
[5] 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.
[6] 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.
[7] 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.
[8] 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.
[9] 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.
[10] 张文,李玉宏,王利,赵峰华,韩伟,宋昌贵. 渭河盆地氦气成藏条件分析及资源量预测[J]. 天然气地球科学, 2018, 29(2): 236-244.
[11] 于京都, 郑民, 李建忠, 吴晓智, 郭秋麟. 我国深层天然气资源潜力、勘探前景与有利方向[J]. 天然气地球科学, 2018, 29(10): 1398-1408.
[12] 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.
[13] 王彬, 张强, 吕福亮, 杨涛涛, 杨志力, 孙国忠, 吴敬武, . 南海海域新生界沉积盆地天然气成藏条件及资源前景[J]. 天然气地球科学, 2018, 29(10): 1542-1552.
[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   
No Suggested Reading articles found!