天然气地球科学

• 天然气地质学 • 上一篇    下一篇

吐哈盆地北部逆冲构造带油气成藏模式与勘探方向

杨占龙1,2,吴青鹏1,2,黄云峰1,2,黄小鹏1,2   

  1. 1.中国石油勘探开发研究院西北分院,甘肃 兰州 730020;
    2.中国石油天然气集团公司油藏描述重点实验室,甘肃 兰州 730020
  • 收稿日期:2015-08-05 修回日期:2015-10-19 出版日期:2016-06-10 发布日期:2016-06-10
  • 作者简介:杨占龙(1970-),男,甘肃宁县人,高级工程师,博士,主要从事含油气盆地油气地质特征综合评价与岩性油气藏勘探研究. E-mail:yang_zl@petrochina.com.cn.
  • 基金资助:
    国家重大科技专项(编号:2011ZX05001);中国石油天然气集团公司重大专项(编号:2012E-0502)联合资助.

Hydrocarbon accumulation and exploration domain of northern thrust belts in Turpan-Kumul Basin

Yang Zhan-long1,2,Wu Qing-peng1,2,Huang Yun-feng1,2,Huang Xiao-peng1,2   

  1. 1.Northwest Branch,Research Institute of Petroleum Exploration and Development,PetroChina,Lanzhou 730020,China;
    2.Key Laboratory of Reservoir Description,PetroChina,Lanzhou 730020,China
  • Received:2015-08-05 Revised:2015-10-19 Online:2016-06-10 Published:2016-06-10

摘要: 针对吐哈再生型前陆盆地北部山前逆冲构造带油气富集规律研究的需要,结合山前带不同块体构造发育特征分析与已发现油气藏解剖,提出山前带主要发育以走滑断裂体系为主、逆冲断裂为辅的断裂输导体系和与输导砂体相配置的构造脊2类输导体系,发育2种主控因素各异的油气成藏模式,即有走滑断裂发育的构造块体油气输导体系主要受控于走滑断裂及与其配置的逆冲断裂体系,缺乏走滑断裂发育的构造块体油气运移主要受控于与输导砂体相配置的构造脊。结合已有油气勘探发现过程分析,受走滑断裂控制的构造块体的油气扩展方向为构造高点靠近走滑断裂一侧的低断块,预探方向为逆冲断裂带下盘,油藏主体位于构造高部位;缺乏走滑断裂发育的构造块体油气预探方向主要为逆冲断裂带下盘,油藏主体位于逆冲断裂带下盘靠近生烃洼陷的部位。

关键词: 输导体系, 成藏模式, 勘探方向, 逆冲构造带, 吐哈盆地

Abstract: To meet the need of regularity study for hydrocarbon accumulation of northern piedmont of superimposed regenerated foreland Turpan-Kumul Basin,combined the structure and discovered reservoir analysis of different blocks of northern piedmont,we proposed that there are two main types of conducting for petroleum migration system,which are the fault (mainly composed of strike-slip fault and thrust fault in second) and structural ridge conducting system and lead to two different hydrocarbon accumulation models on northern piedmont.The conducting system of block with strike-slip fault is mainly controlled by strike-slip fault and conjunction thrust fault;The block without strike-slip fault is mainly controlled by structural ridge and migration sand body.Combined the process of proved reservoir,the expand domain of blocks with strike-slip fault is the lower wing fault-blocks near the strike-slip fault and the exploration domain is the footwall of thrust fault,the main reservoir located at the high position of this type of block.The exploration domain of blocks without strike-slip fault is the footwall of main thrust fault,the main reservoir located at the footwall of thrust fault near source depression.

Key words: Conducting system, Accumulation model, Exploration domain, Thrust belt, Turpan-Kumul Basin

中图分类号: 

  • TE122.2

[1]
Yuan Mingsheng,Liang Shijun,Yan Liecan,et al,Petroleum Geology and Exploration Practice of Turpan-Kumul Basin[M].Beijing:Press of Petroleum Industry,2002:5-38.[袁明生,梁世君,燕列灿,等.吐哈盆地油气地质与勘探实践[M].北京:石油工业出版社,2002:5-38.]
[2]Liu Bo,Huang Zhilong,Tu Xiaoxian,et al,Structural styles and hydrocarbon accumulation of the northern piedmont belt in the Taibei Sag,Turpan-hami Basin[J].Petroleum Exploration and Development,2011,38(2):152-158.[柳波,黄志龙,涂小仙,等.吐哈盆地台北凹陷北部山前带构造样式与油气成藏[J].石油勘探与开发,2011,38(2):152-158.]
[3]Jia Chengzao,Song Yan,Wei Guoqi,et al.Geological features and petroleum accumulation in the foreland basins in central and western China[J].Earth Science Frontiers,2005,12(3):3-13.[贾承造,宋岩,魏国齐,等.中国中西部前陆盆地的地质特征及油气聚集[J].地学前缘,2005,12(3):3-13.]
[4]Yang Zhanlong,Huang Yunfeng,Wu Qingpeng,et al.Buried giant arc-shape structure system and petroleum exploration in Turpan-kumul Basin[J].Natural Gas Geoscience,2014,25(8):1156-1164.[杨占龙,黄云峰,吴青鹏,等.隐伏巨型弧形构造体系与吐鲁番坳陷油气勘探[J].天然气地球科学,2014,25(8):1156-1164.]
[5]Wu Qingpeng,Guo Jingyi,Li Hongzhe,et al.Analysis of main control factors and accumulation patterns of gas reservoirs in Shanle structural procince[J].Natural Gas Geoscience,2006,17(1):97-101.[吴青鹏,郭精义,李红哲,等.鄯勒构造带油气成藏主控因素和成藏规律[J].天然气地球科学,2006,17(1):97-101.]
[6]Wu Chonglong,Lin Zhongmin,Mao Xiaoping,et al.Concept,research status and trend of “hydrocarbon pooling patterns”[J].Oil & Gas Geology,2009,30(6):673-683.[吴冲龙,林忠民,毛小平,等.“油气成藏模式”的概念、研究现状和发展趋势[J].石油天然气地质,2009,30(6):673-683.]
[7]Yang Zhanlong,Liu Zhenhua,Huang Yunfeng,et al.Hydrocarbon accumulation conditions of footwall exploration domain within a thrust fault system in Turpan Depression[J].Journal of Lanzhou University:Natural Science Edition,2014,50(6):795-801.[杨占龙,刘震华,黄云峰,等.吐鲁番坳陷逆掩断裂带下盘油气勘探领域成藏条件分析[J].兰州大学学报:自然科学版,2014,50(6):795-801.]
[8]Liang Huishe,Zhang Jianzhen,Xia Yiping.Balanced Section Technique and Its Application for Exploration Zctivity[M].Beijing: Seismic Press,2002.[梁慧社,张建珍,夏义平.平衡剖面技术及其在油气勘探中的应用[M].北京:地震出版社,2002.]
[9]Wang Lei,Lv Shuangbin,Zhu Yingkang.Structural pattern of thrust-fold zone in southern Junggar foreland basin and effect on the formation of traps[J].Journal of Daqing Petroleum Institute,2007,31(6):24-31.[王磊,吕双兵,朱映康.准噶尔盆地南缘的构造样式与圈闭作用[J].大庆石油学院学报,2007,31(6):24-31.]
[10]Guan Shuwei,Chen Zhuxin,Li Benliang,et al.Discussion on the character and interpretation model of Kelasu deep structures in the Kuqa area[J].Petroleum Exploration and Development,2010,37(5):531-536,551.[管树巍,陈竹新,李本亮,等.再论库车克拉苏深部构造的性质与解释模型[J].石油勘探与开发,2010,37(5):531-536,551.]
[11]Wang Xinwei,Wang Xinwen,Ma Yongsheng.Characteristics of structure transform zones in the fold-thrust belts on the southern margin of Junggar Basin,northwest China[J].Oil & Gas Geology,2007,28(3):345-354.[汪新伟,汪新文,马永生.准噶尔盆地南缘褶皱_冲断带的构造变换带特征[J].石油与天然气地质,2007,28(3):345-354.]
[12]Li Bin,Song Yan,Meng Zifang,et al.Hydrocarbon accumulation pattern and types in the southern Junggar Foreland Basin[J].Petroleum Geology & Experiment,2007,29(5):452-456.[李斌,宋岩,孟自芳,等.准南前陆盆地油藏类型与成藏模式[J].石油实验地质,2007,29(5):452-456.]
[13]Song Yongdong,Dai Junsheng,Wu Kongyou.Study on the structural features and hydrocarbon accumulation of Wuxia fault belt in the northwest margin of Junggar Basin[J].Journal of Xi’an Shiyou University:Natural Science Edition,2009,24(3):17-20.[宋永东,戴俊生,吴孔友.准噶尔盆地西北缘乌夏断裂带构造特征与油气成藏模式[J].西安石油大学学报:自然科学版,2009,24(3):17-20.]
[14]Tang Jiguang,Li Qi.Tectonic deformation and hydrocarbon accumulation model of foreland thrust belts in central and western of China[J].Petroleum Geology and Recovery Efficiency,2008,15(3):1-5.[汤济广,李祺.中国中西部前陆冲断带构造变形与油气成藏模式[J].油气地质与采收率,2008,15(3):1-5.]
[15]Wang Qiang,Cheng Xubin,Zhang Weibi,et al.Approach to hydrocarbon accumulation in piedmont of Zagros Forelanf Basin,Iran[J].Xinjiang Petroleum Geology,2011,32(2):204-206.[王强,程绪彬,张玮璧,等.扎格罗斯前陆盆地山前带油气成藏探讨[J].新疆石油地质,2011,32(2):204-206.]
[16]Wang Zongli ,Xu Xiaofeng,Li Jun,et al.Reservoir forming pattern 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,等.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.]
[17]Yu Yixin,Tang Liangjie,Wang Qinghua,et al.Salt structures and forming models of hydrocarbon pools in the Kuaq Depression[J].Coal Geology and Exploration,2005,33(6):5-9.[余一欣,汤良杰,王清华,等.库车坳陷盐构造与相关成藏模式[J].煤田地质与勘探,2005,33(6):5-9.]
[18]Zhou Shengyou,Yang Xiumei,Ma Yan,et al.Forming condition for hydrocarbon accumulation and hydrocarbon accumulation pattern in the northern part of Pre-Caspian basin[J].Journal of Northwest University:Natural Science Edition,2010,40(2):304-308.[周生友,杨秀梅,马艳,等.滨里海盆地北部盐下油气成藏条件与模式研究[J].西北大学学报:自然科学版,2010,40(2):304-308.]
[19]Liu Yundong,Deng Yong,Wang Zhijiang,et al.Analysis on geologic framework and hydrocarbon potential prediction of west mountain front in northern Tuha Basin[J].Petroleum Geology and Engineering,2008,22(4):27-32.[刘云冬,邓勇,王志江,等.吐哈盆地北部山前带西段地质结构分析与油气远景预测[J].石油地质与工程,2008,22(4):27-32.]
[20]Yuan Mingsheng,Niu Renjie,Jiao Lixin,et al.Geology characteristic and exploration of foreland thrust belt in Tuha Basin[J].Xinjiang Petroleum Geology,2002,23(5):376-379.[袁明生,牛仁杰,焦立新,等.吐哈盆地前陆冲断带地质特征及勘探成果[J].新疆石油地质,2002,23(5):376-379.]

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