鄂尔多斯盆地中部气田断层发现及其意义
|
摘要
以往研究中对鄂尔多斯盆地中部气田是否存在断层一直未有定论。随着开发的深入和资料的完善,在地层对比和地震资料解释工作中,发现气田内部存在北东和北西向2组小断距剪切断层,其组合模式有4种,即正逆断层共存断阶式组合、相同倾向正逆断层组合、同倾向正断层系列组合及背向式逆断层组合。研究表明这2组小断距剪切断层是燕山期、喜马拉雅期构造强烈改造的结果,其性质和分布特征与区域构造应力场相吻合。断层周边伴生的微裂缝对储集层渗透性有极大改善作用,并对低渗气藏的开发具有重要意义,与气井产能对应分析表明,80%高产井位于断块圈闭范围内,表明断块区对油气富集控制作用明显。图6表3参34
In the past,researchers could not make sure whether there were faults in the Mid Gasfield in Ordos Basin.With the progress in development and more available data,two groups of shear faults with NE direction and NW direction in the gasfield were found during the formation comparison and seismic data interpretation.There are four kinds of combination forms,namely,faulted-steps combination with co-existence of normal and reverse faults,same-dip normal and reverse faults combination,same-dip normal faults combination,and back-folding reverse faults combination.These two groups of faults were generated due to the strong tectonic movement during the Yanshan and Himalayan periods.Their properties and distribution features are consistent with the regional structural field.The associated micro-fractures around the faults greatly improve the permeability of the reservoir and have a great significance for developing the gas reservoir with low permeability.Production capacity analysis of relevant gas producers indicates that 80% of the productive gas producers are located in the faulted-block trap,showing the obvious effect of faulted-block on gas/oil accumulation.
In the past,researchers could not make sure whether there were faults in the Mid Gasfield in Ordos Basin.With the progress in development and more available data,two groups of shear faults with NE direction and NW direction in the gasfield were found during the formation comparison and seismic data interpretation.There are four kinds of combination forms,namely,faulted-steps combination with co-existence of normal and reverse faults,same-dip normal and reverse faults combination,same-dip normal faults combination,and back-folding reverse faults combination.These two groups of faults were generated due to the strong tectonic movement during the Yanshan and Himalayan periods.Their properties and distribution features are consistent with the regional structural field.The associated micro-fractures around the faults greatly improve the permeability of the reservoir and have a great significance for developing the gas reservoir with low permeability.Production capacity analysis of relevant gas producers indicates that 80% of the productive gas producers are located in the faulted-block trap,showing the obvious effect of faulted-block on gas/oil accumulation.
引文
[1]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 discoveryand exploration of marine fields in China(Part 2):Jingbian gasfield,Ordos Basin[J].Marine Origin Petroleum Geology,2005,10(2):37-44.
[2]代金友,何顺利.鄂尔多斯盆地中部气田奥陶系古地貌研究[J].石油学报,2005,26(3):37-39.Dai Jinyou,He Shunli.Ordovician paleokarst landformof centralgas fieldin Ordos Basin[J].Acta Petrolei Sinica,2005,26(3):37-39.
[3]郑秀才,任玉秀.鄂尔多斯盆地主力产气层溶蚀孔洞特征[J].江汉石油学院学报,1998,20(1):7-12.Zheng Xiucai,Ren Yuxiu.Denudation pores and cavities in amain gas-producing formation in Ordos Basin[J].Journal ofJianghan PetroleumInstitute,1998,20(1):7-12.
[4]王文炯.陕甘宁盆地中部大气田成藏条件分析[J].断块油气田,1995,2(1):10-15.Wang Wenjiong.Astudy onthe conditions of forming reservoir atthe center of the great gas fieldin Shan’ganning Basin[J].Fault-Block Oil&Gas Field,1995,2(1):10-15.
[5]周树勋,马振芳.鄂尔多斯盆地中东部奥陶系不整合面成藏组合及其分布规律[J].石油勘探与开发,1998,25(5):14-18.Zhou Shuxun,Ma Zhenfang.Study on the play and thedistribution of Ordovician unconformity in central east OrdosBasin[J].Petroleum Exploration and Development,1998,25(5):14-18.
[6]马振芳,陈安宁,王景.鄂尔多斯盆地中部古风化壳气藏成藏条件研究[J].天然气工业,1998,18(1):9-13.Ma Zhenfang,Chen Anning,Wang Jing.A study on theconditions of forming the fossil weathered residuum gas reservoirin the centre of Ordos Basin[J].Natural Gas Industry,1998,18(1):9-13.
[7]李道燧,张宗林,徐晓蓉.鄂尔多斯盆地中部古地貌与构造对气藏的控制作用[J].石油勘探与开发,1994,21(3):9-14.Li Daosui,Zhang Zonglin,Xu Xiaorong.Paleogeomorphologyand paleostructure controlling the gas fieldin the center of OrdosBasin[J].Petroleum Exploration and Development,1994,21(3):9-14.
[8]吴智勇,郑秀才,张尚峰.鄂尔多斯盆地中部马五14碳酸盐岩的成岩作用[J].江汉石油学院学报,1995,17(2):15-20.Wu Zhiyong,Zheng Xiucai,Zhang Shangfeng.Carbonatediagenesis of Majiagou Formation(Lower Ordovician)in thecentral Ordos Basin[J].Journal of Jianghan PetroleumInstitute,1995,17(2):15-20.
[9]柳广第,郝石生.鄂尔多斯盆地区古生界生烃史和排烃史的模拟[J].石油大学学报(自然科学版),1996,20(1):13-18.Liu Guangdi,Hao Shisheng.Modelling of generation andexpulsion histories of Paleozoic source rock in Ordos region[J].Journal of the University of Petroleum,China(Edition of NaturalScience),1996,20(1):13-18.
[10]郑秀才.鄂尔多斯盆地中部马五4亚段成岩作用及储集性能[J].西安地质学院学报,1996,18(1):43-49.Zheng Xiucai.Carbonate diagenesis and reservoir features of thesub-member No.4 from O1M5in the central Ordos Basin[J].Journal of Xi’an College of Geology,1996,18(1):43-49.
[11]吴冲龙,周江羽,王根发,等.鄂尔多斯古构造应力场与中部大气田的联系[J].石油与天然气地质,1997,18(4):267-275.Wu Chonglong,Zhou Jiangyu,Wang Genfa,et al.Relationshipbetween paleotectonic stress fields and major gas fields in OrdosBasin[J].Oil&Gas Geology,1997,18(4):267-275.
[12]孙少华,李小明,龚革联,等.鄂尔多斯盆地构造热事件研究[J].科学通报,1997,42(3):306-308.Sun Shaohua,Li Xiaoming,Gong Gelian,et al.A study oftectonic thermal event in Ordos Basin[J].Chinese ScienceBulletin,1997,42(3):306-308.
[13]王彩丽,孙六一,王宏.长庆气田马五1储层裂缝类型及特征[J].天然气工业,1999,19(4):8-12.Wang Caili,Sun Liuyi,Wang Hong.Fracture types andcharacteristics of the Ma51reservoir in Changqing gas field[J].Natural Gas Industry,1999,19(4):8-12.
[14]蒲仁海,姚宗慧,张艳春.鄂尔多斯盆地古构造演化在气田形成中的作用及意义[J].天然气工业,2000,20(6):27-30.Pu Renhai,Yao Zonghui,Zhang Yanchun.Significance and effectof palaeostructural evolution on gas fieldformationin Ordos Basin[J].Natural Gas Industry,2000,20(6):27-30.
[15]杨华,张军,王飞雁,等.鄂尔多斯盆地古生界含气系统特征[J].天然气工业,2000,20(6):7-11.Yang Hua,Zhang Jun,Wang Feiyan,et al.Characteristics ofPaleozoic gas systemin Ordos Basin[J].Natural Gas Industry,2000,20(6):7-11.
[16]张宗林,王宏,秦志宝,等.长庆气田下古生界马五段碳酸盐岩储层类别测井识别方法研究[J].天然气工业,2000,20(3):44-46.Zhang Zonglin,Wang Hong,Qin Zhibao,et al.A research onthe method of logidentifyingthe type of O1m5carbonate reservoirof lower Palaeozoic in Changqing gas field[J].Natural GasIndustry,2000,20(3):44-46.
[17]马振芳,于忠平,周树勋,等.鄂尔多斯盆地中东部奥陶系古风化壳储集层的分形及灰色系统评价[J].石油勘探与开发,2000,27(1):32-34.Ma Zhenfang,Yu Zhongping,Zhou Shuxun,et al.Fractal andgrey system evaluation of Ordovician paleocrust of weatheredreservoir in central-eastern Ordos Basin[J].PetroleumExploration and Development,2000,27(1):32-34.
[18]何自新,郑聪斌,陈安宁.长庆气田奥陶系古沟槽展布及其对气藏的控制[J].石油学报,2001,22(4):35-38.He Zixin,Zheng Congbin,Chen Anning.Distributiveconfiguration of ancient valley-trough on Ordovician erosionsurface in Changqing gas field and its control over gasaccumulations[J].Acta Petrolei Sinica,2001,22(4):35-38.
[19]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 isotopiccomposition and gas sourcein giant gas fields of Ordos Basin[J].Acta Petrolei Sinica,2005,26(1):18-26.
[20]王雪莲,王长陆,陈振林,等.鄂尔多斯盆地奥陶系风化壳岩溶储层研究[J].特种油气藏,2005,12(3):32-35.Wang Xuelian,Wang Changlu,Chen Zhenlin,et al.Study ofOrdovician weathering crust karst reservoirs in Ordos Basin[J].Special Oil and Gas Reservoirs,2005,12(3):32-35.
[21]王欣,李振宏,郑聪斌.鄂尔多斯盆地奥陶系储层演化与油气运聚[J].天然气地球科学,2006,17(1):114-118.Wang Xin,Li Zhenhong,Zheng Congbin.The evolution ofOrdovician reservoir and movement-gathering of oil-gas in OrdosBasin[J].Natural Gas Geoscience,2006,17(1):114-118.
[22]席胜利,李振宏,王欣,等.鄂尔多斯盆地奥陶系储层展布及勘探潜力[J].石油与天然气地质,2006,17(1):405-412.Xi Shengli,Li Zhenhong,Wang Xin,et al.Distribution andexploration potential of Ordovician reservoir in Ordos Basin[J].Oil&Gas Geology,2006,17(1):405-412.
[23]张福礼.鄂尔多斯盆地早古生代复合的古构造体系与天然气[J].地质力学学报,2002,8(3):193-200.Zhang Fuli.Compound ancient tectonic systemand natural gas ofearly paleozoic in Ordos Basin[J].Journal of Geomechanics,2002,8(3):193-200.
[24]包洪平,杨承运.鄂尔多斯东部奥陶系马家沟组微相分析[J].古地理学报,2000,2(1):31-41.Bao Hongping,Yang Chengyun.Study on microfacies ofMajiagou Formation,Lower Ordovician,eastern Ordos,NorthChina[J].Journal of Palaeogeography,2000,2(1):31-41.
[25]冯增昭,鲍志东.鄂尔多斯奥陶纪马家沟期岩相古地理[J].沉积学报,1999,17(1):1-8.Feng Zengzhao,Bao Zhidong.Lithofacies paleogeography ofMajiagou Age of Ordovician in Ordos Basin[J].ActaSedi mentologica Sinica,1999,17(1):1-8.
[26]郭英海,刘焕杰,权彪,等.鄂尔多斯地区晚古生代沉积体系及古地理演化[J].沉积学报,1998,16(3):44-50.Guo Yinghai,Liu Huanjie,Quan Biao,et al.Late Paleozoicsedi mentary system and paleogrographic evolution of Ordos area[J].Acta Sedi mentologica Sinica,1998,16(3):44-50.
[27]付金华,郑聪斌.鄂尔多斯盆地奥陶纪华北海和祁连海演变及岩相古地理特征[J].古地理学报,2001,3(4):25-33.Fu Jinhua,Zheng Congbin.Evolution between north China seaand Qilian sea of the Ordovician and the characteristics oflithofacies palaeogeography in Ordos Basin[J].Journal ofPalaeogeography,2001,3(4):25-33.
[28]张福礼.鄂尔多斯盆地天然气地质[M].北京:地质出版社,1994.Zhang Fuli.Natural gas geology in Ordos Basin[M].Beijing:Geological Publishing House,1994.
[29]张福礼.多旋回与鄂尔多斯盆地石油天然气[J].石油实验地质,2004,26(2):138-142.Zhang Fuli.Relation of multicycles to oil and natural gas in theOrdos Basin[J].Petroleum Geology and Experi ment,2004,26(2):138-142.
[30]孙肇才.简论鄂尔多斯盆地地质构造风格及其油气潜力———纪念朱夏院士逝世10周年[J].石油实验地质,2000,22(4):291-296.Sun Zhaocai.Geotectonic style and oil/gas potential of OrdosBasin:On the 10thanniversary for passing away of academicianZhu Xia[J].Petroleum Geology and Experi ment,2000,22(4):291-296.
[31]杨遂正,金文化,李振宏.鄂尔多斯多旋回叠合盆地形成与演化[J].天然气地球科学,2006,17(4):494-498.Yang Suizheng,Jin Wenhua,Li Zhenhong.Multicyclesuperi mposed basin form and evolution of Ordos Basin[J].Natural Gas Geoscience,2006,17(4):494-498.
[32]张义楷,周立发,党D,等.鄂尔多斯盆地中新生代构造应力场与油气聚集[J].石油实验地质,2006,28(3):215-219.Zhang Yikai,Zhou Lifa,Dang Ben,et al.Relationship betweenthe Mesozoic and Cenozoic tectonic stress fields and thehydrocarbon accumulation in the Ordos Basin[J].PetroleumGeology and Experi ment,2006,28(3):215-219.
[33]邸领军,张东阳,王宏科.鄂尔多斯盆地喜山期构造运动与油气成藏[J].石油学报,2003,24(2):34-37.Di Lingjun,Zhang Dongyang,Wang Hongke.Pri mary discussionon Hi malayan tectonic movement and petroleum reservoir inOrdos Basin[J].Acta Petrolei Sinica,2003,24(2):34-37.
[34]邓起东,程绍平,闵伟,等.鄂尔多斯块体新生代构造活动和动力学的讨论[J].地质力学学报,1999,5(3):13-20.Deng Qidong,Cheng Shaoping,Min Wei,et al.Discussion onCenozoic tectonics and dynamics of Ordos Block[J].Journal ofGeomechanics,1999,5(3):13-20.
[2]代金友,何顺利.鄂尔多斯盆地中部气田奥陶系古地貌研究[J].石油学报,2005,26(3):37-39.Dai Jinyou,He Shunli.Ordovician paleokarst landformof centralgas fieldin Ordos Basin[J].Acta Petrolei Sinica,2005,26(3):37-39.
[3]郑秀才,任玉秀.鄂尔多斯盆地主力产气层溶蚀孔洞特征[J].江汉石油学院学报,1998,20(1):7-12.Zheng Xiucai,Ren Yuxiu.Denudation pores and cavities in amain gas-producing formation in Ordos Basin[J].Journal ofJianghan PetroleumInstitute,1998,20(1):7-12.
[4]王文炯.陕甘宁盆地中部大气田成藏条件分析[J].断块油气田,1995,2(1):10-15.Wang Wenjiong.Astudy onthe conditions of forming reservoir atthe center of the great gas fieldin Shan’ganning Basin[J].Fault-Block Oil&Gas Field,1995,2(1):10-15.
[5]周树勋,马振芳.鄂尔多斯盆地中东部奥陶系不整合面成藏组合及其分布规律[J].石油勘探与开发,1998,25(5):14-18.Zhou Shuxun,Ma Zhenfang.Study on the play and thedistribution of Ordovician unconformity in central east OrdosBasin[J].Petroleum Exploration and Development,1998,25(5):14-18.
[6]马振芳,陈安宁,王景.鄂尔多斯盆地中部古风化壳气藏成藏条件研究[J].天然气工业,1998,18(1):9-13.Ma Zhenfang,Chen Anning,Wang Jing.A study on theconditions of forming the fossil weathered residuum gas reservoirin the centre of Ordos Basin[J].Natural Gas Industry,1998,18(1):9-13.
[7]李道燧,张宗林,徐晓蓉.鄂尔多斯盆地中部古地貌与构造对气藏的控制作用[J].石油勘探与开发,1994,21(3):9-14.Li Daosui,Zhang Zonglin,Xu Xiaorong.Paleogeomorphologyand paleostructure controlling the gas fieldin the center of OrdosBasin[J].Petroleum Exploration and Development,1994,21(3):9-14.
[8]吴智勇,郑秀才,张尚峰.鄂尔多斯盆地中部马五14碳酸盐岩的成岩作用[J].江汉石油学院学报,1995,17(2):15-20.Wu Zhiyong,Zheng Xiucai,Zhang Shangfeng.Carbonatediagenesis of Majiagou Formation(Lower Ordovician)in thecentral Ordos Basin[J].Journal of Jianghan PetroleumInstitute,1995,17(2):15-20.
[9]柳广第,郝石生.鄂尔多斯盆地区古生界生烃史和排烃史的模拟[J].石油大学学报(自然科学版),1996,20(1):13-18.Liu Guangdi,Hao Shisheng.Modelling of generation andexpulsion histories of Paleozoic source rock in Ordos region[J].Journal of the University of Petroleum,China(Edition of NaturalScience),1996,20(1):13-18.
[10]郑秀才.鄂尔多斯盆地中部马五4亚段成岩作用及储集性能[J].西安地质学院学报,1996,18(1):43-49.Zheng Xiucai.Carbonate diagenesis and reservoir features of thesub-member No.4 from O1M5in the central Ordos Basin[J].Journal of Xi’an College of Geology,1996,18(1):43-49.
[11]吴冲龙,周江羽,王根发,等.鄂尔多斯古构造应力场与中部大气田的联系[J].石油与天然气地质,1997,18(4):267-275.Wu Chonglong,Zhou Jiangyu,Wang Genfa,et al.Relationshipbetween paleotectonic stress fields and major gas fields in OrdosBasin[J].Oil&Gas Geology,1997,18(4):267-275.
[12]孙少华,李小明,龚革联,等.鄂尔多斯盆地构造热事件研究[J].科学通报,1997,42(3):306-308.Sun Shaohua,Li Xiaoming,Gong Gelian,et al.A study oftectonic thermal event in Ordos Basin[J].Chinese ScienceBulletin,1997,42(3):306-308.
[13]王彩丽,孙六一,王宏.长庆气田马五1储层裂缝类型及特征[J].天然气工业,1999,19(4):8-12.Wang Caili,Sun Liuyi,Wang Hong.Fracture types andcharacteristics of the Ma51reservoir in Changqing gas field[J].Natural Gas Industry,1999,19(4):8-12.
[14]蒲仁海,姚宗慧,张艳春.鄂尔多斯盆地古构造演化在气田形成中的作用及意义[J].天然气工业,2000,20(6):27-30.Pu Renhai,Yao Zonghui,Zhang Yanchun.Significance and effectof palaeostructural evolution on gas fieldformationin Ordos Basin[J].Natural Gas Industry,2000,20(6):27-30.
[15]杨华,张军,王飞雁,等.鄂尔多斯盆地古生界含气系统特征[J].天然气工业,2000,20(6):7-11.Yang Hua,Zhang Jun,Wang Feiyan,et al.Characteristics ofPaleozoic gas systemin Ordos Basin[J].Natural Gas Industry,2000,20(6):7-11.
[16]张宗林,王宏,秦志宝,等.长庆气田下古生界马五段碳酸盐岩储层类别测井识别方法研究[J].天然气工业,2000,20(3):44-46.Zhang Zonglin,Wang Hong,Qin Zhibao,et al.A research onthe method of logidentifyingthe type of O1m5carbonate reservoirof lower Palaeozoic in Changqing gas field[J].Natural GasIndustry,2000,20(3):44-46.
[17]马振芳,于忠平,周树勋,等.鄂尔多斯盆地中东部奥陶系古风化壳储集层的分形及灰色系统评价[J].石油勘探与开发,2000,27(1):32-34.Ma Zhenfang,Yu Zhongping,Zhou Shuxun,et al.Fractal andgrey system evaluation of Ordovician paleocrust of weatheredreservoir in central-eastern Ordos Basin[J].PetroleumExploration and Development,2000,27(1):32-34.
[18]何自新,郑聪斌,陈安宁.长庆气田奥陶系古沟槽展布及其对气藏的控制[J].石油学报,2001,22(4):35-38.He Zixin,Zheng Congbin,Chen Anning.Distributiveconfiguration of ancient valley-trough on Ordovician erosionsurface in Changqing gas field and its control over gasaccumulations[J].Acta Petrolei Sinica,2001,22(4):35-38.
[19]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 isotopiccomposition and gas sourcein giant gas fields of Ordos Basin[J].Acta Petrolei Sinica,2005,26(1):18-26.
[20]王雪莲,王长陆,陈振林,等.鄂尔多斯盆地奥陶系风化壳岩溶储层研究[J].特种油气藏,2005,12(3):32-35.Wang Xuelian,Wang Changlu,Chen Zhenlin,et al.Study ofOrdovician weathering crust karst reservoirs in Ordos Basin[J].Special Oil and Gas Reservoirs,2005,12(3):32-35.
[21]王欣,李振宏,郑聪斌.鄂尔多斯盆地奥陶系储层演化与油气运聚[J].天然气地球科学,2006,17(1):114-118.Wang Xin,Li Zhenhong,Zheng Congbin.The evolution ofOrdovician reservoir and movement-gathering of oil-gas in OrdosBasin[J].Natural Gas Geoscience,2006,17(1):114-118.
[22]席胜利,李振宏,王欣,等.鄂尔多斯盆地奥陶系储层展布及勘探潜力[J].石油与天然气地质,2006,17(1):405-412.Xi Shengli,Li Zhenhong,Wang Xin,et al.Distribution andexploration potential of Ordovician reservoir in Ordos Basin[J].Oil&Gas Geology,2006,17(1):405-412.
[23]张福礼.鄂尔多斯盆地早古生代复合的古构造体系与天然气[J].地质力学学报,2002,8(3):193-200.Zhang Fuli.Compound ancient tectonic systemand natural gas ofearly paleozoic in Ordos Basin[J].Journal of Geomechanics,2002,8(3):193-200.
[24]包洪平,杨承运.鄂尔多斯东部奥陶系马家沟组微相分析[J].古地理学报,2000,2(1):31-41.Bao Hongping,Yang Chengyun.Study on microfacies ofMajiagou Formation,Lower Ordovician,eastern Ordos,NorthChina[J].Journal of Palaeogeography,2000,2(1):31-41.
[25]冯增昭,鲍志东.鄂尔多斯奥陶纪马家沟期岩相古地理[J].沉积学报,1999,17(1):1-8.Feng Zengzhao,Bao Zhidong.Lithofacies paleogeography ofMajiagou Age of Ordovician in Ordos Basin[J].ActaSedi mentologica Sinica,1999,17(1):1-8.
[26]郭英海,刘焕杰,权彪,等.鄂尔多斯地区晚古生代沉积体系及古地理演化[J].沉积学报,1998,16(3):44-50.Guo Yinghai,Liu Huanjie,Quan Biao,et al.Late Paleozoicsedi mentary system and paleogrographic evolution of Ordos area[J].Acta Sedi mentologica Sinica,1998,16(3):44-50.
[27]付金华,郑聪斌.鄂尔多斯盆地奥陶纪华北海和祁连海演变及岩相古地理特征[J].古地理学报,2001,3(4):25-33.Fu Jinhua,Zheng Congbin.Evolution between north China seaand Qilian sea of the Ordovician and the characteristics oflithofacies palaeogeography in Ordos Basin[J].Journal ofPalaeogeography,2001,3(4):25-33.
[28]张福礼.鄂尔多斯盆地天然气地质[M].北京:地质出版社,1994.Zhang Fuli.Natural gas geology in Ordos Basin[M].Beijing:Geological Publishing House,1994.
[29]张福礼.多旋回与鄂尔多斯盆地石油天然气[J].石油实验地质,2004,26(2):138-142.Zhang Fuli.Relation of multicycles to oil and natural gas in theOrdos Basin[J].Petroleum Geology and Experi ment,2004,26(2):138-142.
[30]孙肇才.简论鄂尔多斯盆地地质构造风格及其油气潜力———纪念朱夏院士逝世10周年[J].石油实验地质,2000,22(4):291-296.Sun Zhaocai.Geotectonic style and oil/gas potential of OrdosBasin:On the 10thanniversary for passing away of academicianZhu Xia[J].Petroleum Geology and Experi ment,2000,22(4):291-296.
[31]杨遂正,金文化,李振宏.鄂尔多斯多旋回叠合盆地形成与演化[J].天然气地球科学,2006,17(4):494-498.Yang Suizheng,Jin Wenhua,Li Zhenhong.Multicyclesuperi mposed basin form and evolution of Ordos Basin[J].Natural Gas Geoscience,2006,17(4):494-498.
[32]张义楷,周立发,党D,等.鄂尔多斯盆地中新生代构造应力场与油气聚集[J].石油实验地质,2006,28(3):215-219.Zhang Yikai,Zhou Lifa,Dang Ben,et al.Relationship betweenthe Mesozoic and Cenozoic tectonic stress fields and thehydrocarbon accumulation in the Ordos Basin[J].PetroleumGeology and Experi ment,2006,28(3):215-219.
[33]邸领军,张东阳,王宏科.鄂尔多斯盆地喜山期构造运动与油气成藏[J].石油学报,2003,24(2):34-37.Di Lingjun,Zhang Dongyang,Wang Hongke.Pri mary discussionon Hi malayan tectonic movement and petroleum reservoir inOrdos Basin[J].Acta Petrolei Sinica,2003,24(2):34-37.
[34]邓起东,程绍平,闵伟,等.鄂尔多斯块体新生代构造活动和动力学的讨论[J].地质力学学报,1999,5(3):13-20.Deng Qidong,Cheng Shaoping,Min Wei,et al.Discussion onCenozoic tectonics and dynamics of Ordos Block[J].Journal ofGeomechanics,1999,5(3):13-20.
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心