茂兴地区葡萄花油层精细研究
|
摘要
葡萄花油层是茂兴地区的主力产油层之一,在油气勘探过程中获得了巨大突破,其巨大的潜力有待进一步勘探挖掘。以构造地质学、石油地质学、沉积学和层序地层学为指导,综合应用区域地质资料、地震资料、测井资料、岩心资料及前人的研究成果,对研究区进行了构造解释,分析了构造特征,结合砂体展布特征、油水分布特征及沉积相展布特征对研究区葡萄花油层进行了成藏模式研究。
以高分辨率三维地震资料为基础,层位和断层的精细解释技术,对研究区进行了构造精细解释,完成了茂兴地区葡萄花油层顶面构造图。通过对三维地震精细解释成果的分析,认为研究区的断层较发育,但是断层规模较小,基本上为南北向和东西向的正断层,断层断面较陡,断层剖面形态主要有板式、铲式两种,形成了阶梯状断层组合、“Y”字形断层组合、地堑与地垒组合。通过对构造演化分析认为,研究区断层主要形成于三个时期,主要为青山口沉积时期,而姚家组和嫩江组沉积时期发育的断层较少。
综合利用岩心、测井和地震资料,分析了葡萄花油层的层序地层和沉积特征,将葡萄花油层划分为3个中期旋回,以中期旋回为地层对比单元,进行了地层对比,建立了研究区的层序地层格架,在地层划分的基础上,进行了沉积特征的分析,分析认为葡萄花油层是在水进背景下形成的三角洲前缘亚相沉积,沉积时为水进期,湖面扩张,水体变深,在北部和西部物源控制下,沉积了三角洲前缘和滨浅湖亚相,相序完整,形成一个完整的向上变细的正旋回。三角洲前缘亚相可划分为水下分流河道、河口坝、席状砂、水下分流间湾和水下决口扇五种微相。
在分析研究区的成藏条件和油气藏类型的基础上,利用构造解释的成果,结合砂体展布特征、沉积相展布特征、油水分布特征,对研究区的成藏模式进行了研究。
Pupaohua oil layer is one of the main producting layers in Maoxing area, and great breakthroughs have been made on it during the exploration process. It has great potential for further exploration. The thesis is guided by structural geology, petroleum geology, sedimentology and sequence stratigraphy, synthetically utlizing regional geological data, seismic data, logging data, core data as well as the research achievements of former researchers, and the thesis makes tectonic explanation. Besides, combined with the distribution features of sand bodies, oil-water distribution features and sedimentary facies distribution features, the thesis analyses the structural characteristics and predicts the effective zones of Pupaohua oil layer.
The interpretation is based on high definition 3-D seismic data. With the help of section interpretation and fault interpretation, the thesis has completed the map of top structure of Putaohua oil layer. Through the analysis of 3-D seismic interpretaion, faults were well developed in the target area. However the faults are small in size, and most of them are south-north and east-west normal faults with steep fault plane. The morphologies of fault plane are basically plate and shovel, which formed the step faults and Y faults combination and graben and horst combination. The faults in the target area were formed mainly in three periods, in which most faults form dure Qingshankou depositional period, while faults develop in Yaojia and Nenjiang periods were relatively less.
After synthetically utlizing core, logging and seismic data and analysing the sequence stratigraphy and sedimentary characteristics of Putaohua oil layer, the thesis then divides the Putaohua oil layer into three middle-term stratigraphic base level circles. The research uses middle-term stratigraphic base level circle as stratigraphic correlation unit to correlate formations, then sets up layer sequence stratigraphic framework of th research area. On the basis of stratigraphic division, the thesis analyses sedimentary characteristics of Putaohua oil layer, which is the delta front facies formed in transient regression of the whole transgression setting. During the depositional stage the lake expansed, and the water deepened, the research area deposited delta front subfacies and offshore-shallow lake subfacies, which is an integrated sequence with an entire fining-upward sequence. The delta front subfacies can be further divided into five microfacies:underwater distributary channel, mouth bar, sand sheet, underwater distributary between bay and underwater crevasse-splays.
On the basis of the analysis of the accumulation conditions and reservoir types of the research area, the thesis uses the achievements of structural explanation and seismic oil and gas detective techonologies, uniting with sandbodies distribution features, sedimentary facies distribution features, oil-water distribution features and trap conditions, then studied Reservoiring Pattern in Maoxing area.
以高分辨率三维地震资料为基础,层位和断层的精细解释技术,对研究区进行了构造精细解释,完成了茂兴地区葡萄花油层顶面构造图。通过对三维地震精细解释成果的分析,认为研究区的断层较发育,但是断层规模较小,基本上为南北向和东西向的正断层,断层断面较陡,断层剖面形态主要有板式、铲式两种,形成了阶梯状断层组合、“Y”字形断层组合、地堑与地垒组合。通过对构造演化分析认为,研究区断层主要形成于三个时期,主要为青山口沉积时期,而姚家组和嫩江组沉积时期发育的断层较少。
综合利用岩心、测井和地震资料,分析了葡萄花油层的层序地层和沉积特征,将葡萄花油层划分为3个中期旋回,以中期旋回为地层对比单元,进行了地层对比,建立了研究区的层序地层格架,在地层划分的基础上,进行了沉积特征的分析,分析认为葡萄花油层是在水进背景下形成的三角洲前缘亚相沉积,沉积时为水进期,湖面扩张,水体变深,在北部和西部物源控制下,沉积了三角洲前缘和滨浅湖亚相,相序完整,形成一个完整的向上变细的正旋回。三角洲前缘亚相可划分为水下分流河道、河口坝、席状砂、水下分流间湾和水下决口扇五种微相。
在分析研究区的成藏条件和油气藏类型的基础上,利用构造解释的成果,结合砂体展布特征、沉积相展布特征、油水分布特征,对研究区的成藏模式进行了研究。
Pupaohua oil layer is one of the main producting layers in Maoxing area, and great breakthroughs have been made on it during the exploration process. It has great potential for further exploration. The thesis is guided by structural geology, petroleum geology, sedimentology and sequence stratigraphy, synthetically utlizing regional geological data, seismic data, logging data, core data as well as the research achievements of former researchers, and the thesis makes tectonic explanation. Besides, combined with the distribution features of sand bodies, oil-water distribution features and sedimentary facies distribution features, the thesis analyses the structural characteristics and predicts the effective zones of Pupaohua oil layer.
The interpretation is based on high definition 3-D seismic data. With the help of section interpretation and fault interpretation, the thesis has completed the map of top structure of Putaohua oil layer. Through the analysis of 3-D seismic interpretaion, faults were well developed in the target area. However the faults are small in size, and most of them are south-north and east-west normal faults with steep fault plane. The morphologies of fault plane are basically plate and shovel, which formed the step faults and Y faults combination and graben and horst combination. The faults in the target area were formed mainly in three periods, in which most faults form dure Qingshankou depositional period, while faults develop in Yaojia and Nenjiang periods were relatively less.
After synthetically utlizing core, logging and seismic data and analysing the sequence stratigraphy and sedimentary characteristics of Putaohua oil layer, the thesis then divides the Putaohua oil layer into three middle-term stratigraphic base level circles. The research uses middle-term stratigraphic base level circle as stratigraphic correlation unit to correlate formations, then sets up layer sequence stratigraphic framework of th research area. On the basis of stratigraphic division, the thesis analyses sedimentary characteristics of Putaohua oil layer, which is the delta front facies formed in transient regression of the whole transgression setting. During the depositional stage the lake expansed, and the water deepened, the research area deposited delta front subfacies and offshore-shallow lake subfacies, which is an integrated sequence with an entire fining-upward sequence. The delta front subfacies can be further divided into five microfacies:underwater distributary channel, mouth bar, sand sheet, underwater distributary between bay and underwater crevasse-splays.
On the basis of the analysis of the accumulation conditions and reservoir types of the research area, the thesis uses the achievements of structural explanation and seismic oil and gas detective techonologies, uniting with sandbodies distribution features, sedimentary facies distribution features, oil-water distribution features and trap conditions, then studied Reservoiring Pattern in Maoxing area.
引文
[1]牟智全,周立宏,张彦湘等.地震—地质综合储层预测技术在大庆油田G533区块的应用[J].石油地球物理勘探,2009,44(3):323~330
[2]张进铎.地震解释技术现状及发展趋势[J].地球物理学进展,2006,21(2):578-587.
[3]陈凤云,张宝水.相干体解释技术在三维地震勘探中的应用[J].煤田地质与勘探,2005,33(2):63-64.
[4]蔡刚,孙东,裴明利.相干体技术及其在油气勘探中的应用[J].天然气地球科学,2006,17(4):510-513.
[6]曹雪峰,梁会兰,肖伟等.地震资料解释技术在大港滩海极浅海区的应用[J].中国海上油气(地质),2001,15(4):276-279.
[7]陈同俊,崔若飞,郎玉泉.煤田采区三维地震精细构造解释方法[J].地球物理学进展,2007,22(2):573-578.
[8]汤祥武,宋中应.三维地震勘探小断层的解释方法及应用[J].沉积学报,2001,19(2):250-255.
[9]刘丽峰,杨怀义,蒋多元.三维精细构造解释的方法流程和关键技术[J].地球物理学进展,2006,21(3):864-871.
[10]陈双庆,陈昌武,王树敏.小断层的分辨识别与反射波特征[J].山东科技大学学报(自然科学版),2005,24(4):51-54.
[11]双文,赵建,谷跃民等.准噶尔盆地莫北凸起莫7、莫n井区三维地震资料构造精细解释技术[J].兰州大学学报(自然科学版),2008,41(1):1-5.
[12]孙志华,郑俊茂,甘嫦华等.地震解释技术在N50井区的应用[J].石油地球物理勘探,2003,38(6):687-689.
[13]张军华,王月英,赵勇. C3相干体在断层和裂缝识别中的应用[J].地震学报,2004,26(5):560-564.
[14]佘德平,曹辉,郭全仕.应用三维相干技术进行精细地震解释[J].石油物探,2000,39(2):83-88.
[15]王咸斌,曹辉,郭全仕等.真(全)三维构造解释技术初探[J].石油物探,2000,39(2):89~94
[16]朱巍,居春荣,夏步余等.地震综合解释技术在WZ地区的应用[J].江汉石油学院学报,2002,24(3):15-17.
[17]张延章,李淑恩,黄国平等.地震切片的分类及应用价值[J].油气地质与采收率,2002,9(3):67-69.
[18]许辉群,桂志先.边缘检测技术砂体边界识别方法研究[J].石油天然气学报,2009,31(5):75-77.
[19]周晶,张延庆,李建华.边缘检测技术探测盐丘[J].天然气工业,1996,27(增刊A):177-184.
[20]李红星,刘财,陶春辉.图像边缘检测方法在地震剖面同相轴自动检测中的应用研究[J].地球物理学进展,2007,22(5):1607-1610.
[21]关达,付强.地震解释技术新进展[J].勘探地球物理进展,2003,26(5-6):367-373.
[22]李洋,唐建华.三维可视化技术在准噶尔盆地地震解释中的应用[J].新疆石油地质,2000,21(3):235-237.
[23]吴东胜,陈华军,刘少华等.三维可视化技术在隐蔽油气藏勘探中的应用[J].石油物探,2005,44(1):44-46.
[24]孟德萍,龚洪春. Landmark软件在溱潼凹陷MS地区的应用[J].江苏地质,2003,27(4):216-219.
[25]李霞,王睿.地震综合解释技术在复杂断块勘探中的应用[J].石油天然气学报,2009,31(5):259-262.
[26]许慧华,王志高.地震属性分析及其在胜利探区的应用[J].石油仪器, 2002, 16 (5): 21-24.
[27]席党鹏,李罡,万晓樵等.松辽盆地东南区姚家组—嫩江组一段地层特征与湖泊演变[J].古生物学报,2009,48(3):556-568.
[28]舒巧,辛仁臣,章伟.松辽盆地他拉哈西地区下白垩统青山口组下部沉积微相分析[J].沉积与特提斯地质,2008,28(2):69-74.
[29]王佰长,张智礼,刘振文.松辽盆地泰康地区上白垩统姚家组沉积相[J].地层学杂志,2007,31(4):361-366.
[30]吴河勇,梁晓东,向才富等.松辽盆地向斜油藏特征及成藏机理探讨[J].中国科学,2007,37(2):185-191.
[31]闫晶晶,席党鹏,于涛等.松辽盆地青山口地区嫩江组下部生物地层及环境变化[J].地层学杂志,2007,31(3):296-301.
[32]胡望水.松辽盆地“T2”断层系及青山口早期伸展裂陷[J].石油勘探与开发,1995,22(2):8-12.
[33]舒良树,慕玉福,王伯长.松辽盆地含油气地层及其构造特征[J].地层学杂志,2003,27(4):340-347.
[34]李娟,舒良树.松辽盆地中、新生代构造特征及其演化[J].南京大学学报(自然科学),2002,38(4):525-531.
[35]卓弘春,林春明,李艳丽等.松辽盆地北部上白垩统青山口—姚家组沉积相及层序地层界面特征[J].沉积学报,2007,25(1):29-38.
[36]辛仁臣,蔡希源,王英民.松辽坳陷深水湖盆层序界面特征及低位域沉积模式[J].沉积学报,2004,22(3):387-392.
[37]辛仁臣,王英民.松辽盆地北部青山口—姚家组西部坡折带成因及演化[J].地球科学—中国地质大学学报,2004,29(5):621-624.
[38]朱建伟,刘招君,董清水等.松辽盆地层序地层格架及油气聚集规律[J].石油地球物理勘探,2001,36(3):339-344.
[39]马明侠,马金龙.松辽盆地两江地区沉积体系分布规律[J].地大庆石油地质与开发,2000,19(3):4-6.
[40]胡慧婷,李占东,苏书震等.松辽盆地长垣以西中浅层三级构造发育史及其对油气成藏的控制作用[J].上海地质,2008,(3):45-49.
[41]胡望水,吕炳全,张文军等.松辽盆地构造演化及成盆动力学探讨[J].地质科学,2005,40(1):16-31.
[42]韩晓东,楼章华,姚炎明等.松辽盆地湖泊浅水三角洲沉积动力学研究[J].矿物学报,2000,20(3):305-313.
[43]楼章华,袁笛,金爱民.松辽盆地北部浅水三角洲前缘砂体类型、特征与沉积动力学过程分析[J].浙江大学学报(理学版),2004,31(2):211-215.
[44]陈发景,赵海玲,陈昭年等.中国东部中、新生代伸展盆地构造特征及地球动力学背景[J].地球科学,1996,21(4):357-365.
[45]杨继良.中国中新生代盆地构造和演化[M].北京:科学出版社,1983.
[46] Nilsen T H. The Hilt Bed, an Upper Cretaceous compound basin-plain seismo-turbidite in the Hornbrook Forearc Basin of southern Oregon and northern California, USA [J]. Sedimentary Geology, 2000, 135: 51-63.
[47]盛滨洲.松辽盆地莫霍界面深度计算及其初步认识[J].石油地质开发研究,1979,(2):5-9.
[48]萧德铭,迟元林、蒙启安等.松辽盆地北部向斜区岩性油藏勘探认识与实践[M].北京:石油工业出版社,2005,5-21.
[49]郭巍,刘招君,董惠民等.松辽盆地层序地层特征及油气聚集规律[J].吉林大学学报(地球科学版),2004,34(2):216-221.
[50]吕晓光,李长山,蔡希源等.松辽大型浅水湖盆三角洲沉积特征及前缘相储层结构模型[J].沉积学报,1999,17(4):572-576.
[51]陈雷,马世忠,付宪第等.古龙凹陷高台子油田北部葡萄花油层油气富集主控因素[J].内蒙古石油化工,2010,(7):52-65.
[52]刘珍,等.化验员读本(上册)(第四版)[M].北京:化学工业出版社,2004.
[53]王国民,付广.古龙凹陷嫩一、二段泥岩盖层抑制浓度封闭有效性研究[J].石油天然气学报,2008,30(1):22-25.
[54]李如一,林铁锋.松辽盆地北部古龙地区葡萄花油层储层特征研究[J].大庆石油地质与开发,2008,27(3):32-35.
[55]齐林,薛海涛,李占东.松辽盆地古龙凹陷龙南鼻状构造葡萄花油层油气富集条件[J].内蒙古石油化工,2010,1:117-119.
[56]侯启军,冯志强,冯子辉等.松辽盆地陆相石油地质学[M].黑龙江大庆:石油工业出版社.
[57]侯启军,冯子辉,邹玉良.松辽盆地齐家—古龙凹陷油气成藏期次研究[J].石油实验地质,2005,27(4):390-393.
[58]大庆油田石油地质志编写组.中国石油地质志(卷二),大庆、吉林油田[M].黑龙江大庆:石油工业出版社,1987.
[59]王建功,王天琦,卫平生等.松辽盆地海坨子地区葡萄花油层沉积微相[J].岩性油气藏,2007,19(2):28-34.
[60]李延钧,陈义才,朱江.松辽盆地古龙地区葡萄花油层油气成因与凝析气藏形成分布[J].西南石油学院学报,1997,19(3):14-19.
[61]毕素萍,张庆龙,王良书等.地震—地质综合储层预测技术在大庆油田G533区块的应用[J].石油实验地质,2008,30(2):203-211.
[62]李航,苏耿.百色盆地那坤油田构造精细解释与储层预测[J].南方油气,2006,19(2-3):50-53.
[63] Khaled Fouad.Wave-shape classification and attribute analysis of the lower Miocene deep-water reservoirs in Laguna Madre Basin,offshore Mexico.American Association of Petroleum Geologists Bulletin,2005,73:125-142.
[64]张玉明.高精度三维地震解释技术及在孤家子气田的应用[J].石油物探,2001,40(2):56-62.
[65]邬兴威,王英民,赵永胜.地震技术在B27井区中的应用[J].四川地质学报,1998,18(2):157-160.
[66]张永华,贾曙光,杨春峰等.断层封堵性的应用研究[J].石油物探, 2001,40 (4): 83-88.
[67]张永华.三维地震资料综合解释方法探讨[J].石油物探,2004,43 (1):49-53.
[68]张永华.分步法解释技术在南阳张店油田高分辨率三维地震勘探中的应用[J].石油物探,2000,39(1):98-105.
[69]张世奇,纪友亮,高岭.平衡剖面分析技术在松辽盆地构造演化恢复中的应用[J].新疆地质,2003,21(4):489-490.
[70]钟建华,孙正贵,禚元杰等.高分辨率层序地层学的应用—以河125断层区沙三中亚段为例[J].地质找矿论丛,2009,24(3):243-247.
[71]杨斌,郭翔,刘洪彦等.三塘湖盆地马朗地区重矿物特征与物源分析[J].石油天然气学报,2008,30(3):57-59.
[72]赵红格,刘池洋.物源分析方法及研究进展[J].沉积学报,2003,21(3):409-415.
[73]高瑞祺,蔡希源.松辽盆地油气田形成条件与分布规律[M].山东东营:石油工业出版社,1997.
[74]郭耀华,谢昕.地震油气检测技术在宁东油田的应用[J].成都理工学院学报,2008,30(1):66-70.
[2]张进铎.地震解释技术现状及发展趋势[J].地球物理学进展,2006,21(2):578-587.
[3]陈凤云,张宝水.相干体解释技术在三维地震勘探中的应用[J].煤田地质与勘探,2005,33(2):63-64.
[4]蔡刚,孙东,裴明利.相干体技术及其在油气勘探中的应用[J].天然气地球科学,2006,17(4):510-513.
[6]曹雪峰,梁会兰,肖伟等.地震资料解释技术在大港滩海极浅海区的应用[J].中国海上油气(地质),2001,15(4):276-279.
[7]陈同俊,崔若飞,郎玉泉.煤田采区三维地震精细构造解释方法[J].地球物理学进展,2007,22(2):573-578.
[8]汤祥武,宋中应.三维地震勘探小断层的解释方法及应用[J].沉积学报,2001,19(2):250-255.
[9]刘丽峰,杨怀义,蒋多元.三维精细构造解释的方法流程和关键技术[J].地球物理学进展,2006,21(3):864-871.
[10]陈双庆,陈昌武,王树敏.小断层的分辨识别与反射波特征[J].山东科技大学学报(自然科学版),2005,24(4):51-54.
[11]双文,赵建,谷跃民等.准噶尔盆地莫北凸起莫7、莫n井区三维地震资料构造精细解释技术[J].兰州大学学报(自然科学版),2008,41(1):1-5.
[12]孙志华,郑俊茂,甘嫦华等.地震解释技术在N50井区的应用[J].石油地球物理勘探,2003,38(6):687-689.
[13]张军华,王月英,赵勇. C3相干体在断层和裂缝识别中的应用[J].地震学报,2004,26(5):560-564.
[14]佘德平,曹辉,郭全仕.应用三维相干技术进行精细地震解释[J].石油物探,2000,39(2):83-88.
[15]王咸斌,曹辉,郭全仕等.真(全)三维构造解释技术初探[J].石油物探,2000,39(2):89~94
[16]朱巍,居春荣,夏步余等.地震综合解释技术在WZ地区的应用[J].江汉石油学院学报,2002,24(3):15-17.
[17]张延章,李淑恩,黄国平等.地震切片的分类及应用价值[J].油气地质与采收率,2002,9(3):67-69.
[18]许辉群,桂志先.边缘检测技术砂体边界识别方法研究[J].石油天然气学报,2009,31(5):75-77.
[19]周晶,张延庆,李建华.边缘检测技术探测盐丘[J].天然气工业,1996,27(增刊A):177-184.
[20]李红星,刘财,陶春辉.图像边缘检测方法在地震剖面同相轴自动检测中的应用研究[J].地球物理学进展,2007,22(5):1607-1610.
[21]关达,付强.地震解释技术新进展[J].勘探地球物理进展,2003,26(5-6):367-373.
[22]李洋,唐建华.三维可视化技术在准噶尔盆地地震解释中的应用[J].新疆石油地质,2000,21(3):235-237.
[23]吴东胜,陈华军,刘少华等.三维可视化技术在隐蔽油气藏勘探中的应用[J].石油物探,2005,44(1):44-46.
[24]孟德萍,龚洪春. Landmark软件在溱潼凹陷MS地区的应用[J].江苏地质,2003,27(4):216-219.
[25]李霞,王睿.地震综合解释技术在复杂断块勘探中的应用[J].石油天然气学报,2009,31(5):259-262.
[26]许慧华,王志高.地震属性分析及其在胜利探区的应用[J].石油仪器, 2002, 16 (5): 21-24.
[27]席党鹏,李罡,万晓樵等.松辽盆地东南区姚家组—嫩江组一段地层特征与湖泊演变[J].古生物学报,2009,48(3):556-568.
[28]舒巧,辛仁臣,章伟.松辽盆地他拉哈西地区下白垩统青山口组下部沉积微相分析[J].沉积与特提斯地质,2008,28(2):69-74.
[29]王佰长,张智礼,刘振文.松辽盆地泰康地区上白垩统姚家组沉积相[J].地层学杂志,2007,31(4):361-366.
[30]吴河勇,梁晓东,向才富等.松辽盆地向斜油藏特征及成藏机理探讨[J].中国科学,2007,37(2):185-191.
[31]闫晶晶,席党鹏,于涛等.松辽盆地青山口地区嫩江组下部生物地层及环境变化[J].地层学杂志,2007,31(3):296-301.
[32]胡望水.松辽盆地“T2”断层系及青山口早期伸展裂陷[J].石油勘探与开发,1995,22(2):8-12.
[33]舒良树,慕玉福,王伯长.松辽盆地含油气地层及其构造特征[J].地层学杂志,2003,27(4):340-347.
[34]李娟,舒良树.松辽盆地中、新生代构造特征及其演化[J].南京大学学报(自然科学),2002,38(4):525-531.
[35]卓弘春,林春明,李艳丽等.松辽盆地北部上白垩统青山口—姚家组沉积相及层序地层界面特征[J].沉积学报,2007,25(1):29-38.
[36]辛仁臣,蔡希源,王英民.松辽坳陷深水湖盆层序界面特征及低位域沉积模式[J].沉积学报,2004,22(3):387-392.
[37]辛仁臣,王英民.松辽盆地北部青山口—姚家组西部坡折带成因及演化[J].地球科学—中国地质大学学报,2004,29(5):621-624.
[38]朱建伟,刘招君,董清水等.松辽盆地层序地层格架及油气聚集规律[J].石油地球物理勘探,2001,36(3):339-344.
[39]马明侠,马金龙.松辽盆地两江地区沉积体系分布规律[J].地大庆石油地质与开发,2000,19(3):4-6.
[40]胡慧婷,李占东,苏书震等.松辽盆地长垣以西中浅层三级构造发育史及其对油气成藏的控制作用[J].上海地质,2008,(3):45-49.
[41]胡望水,吕炳全,张文军等.松辽盆地构造演化及成盆动力学探讨[J].地质科学,2005,40(1):16-31.
[42]韩晓东,楼章华,姚炎明等.松辽盆地湖泊浅水三角洲沉积动力学研究[J].矿物学报,2000,20(3):305-313.
[43]楼章华,袁笛,金爱民.松辽盆地北部浅水三角洲前缘砂体类型、特征与沉积动力学过程分析[J].浙江大学学报(理学版),2004,31(2):211-215.
[44]陈发景,赵海玲,陈昭年等.中国东部中、新生代伸展盆地构造特征及地球动力学背景[J].地球科学,1996,21(4):357-365.
[45]杨继良.中国中新生代盆地构造和演化[M].北京:科学出版社,1983.
[46] Nilsen T H. The Hilt Bed, an Upper Cretaceous compound basin-plain seismo-turbidite in the Hornbrook Forearc Basin of southern Oregon and northern California, USA [J]. Sedimentary Geology, 2000, 135: 51-63.
[47]盛滨洲.松辽盆地莫霍界面深度计算及其初步认识[J].石油地质开发研究,1979,(2):5-9.
[48]萧德铭,迟元林、蒙启安等.松辽盆地北部向斜区岩性油藏勘探认识与实践[M].北京:石油工业出版社,2005,5-21.
[49]郭巍,刘招君,董惠民等.松辽盆地层序地层特征及油气聚集规律[J].吉林大学学报(地球科学版),2004,34(2):216-221.
[50]吕晓光,李长山,蔡希源等.松辽大型浅水湖盆三角洲沉积特征及前缘相储层结构模型[J].沉积学报,1999,17(4):572-576.
[51]陈雷,马世忠,付宪第等.古龙凹陷高台子油田北部葡萄花油层油气富集主控因素[J].内蒙古石油化工,2010,(7):52-65.
[52]刘珍,等.化验员读本(上册)(第四版)[M].北京:化学工业出版社,2004.
[53]王国民,付广.古龙凹陷嫩一、二段泥岩盖层抑制浓度封闭有效性研究[J].石油天然气学报,2008,30(1):22-25.
[54]李如一,林铁锋.松辽盆地北部古龙地区葡萄花油层储层特征研究[J].大庆石油地质与开发,2008,27(3):32-35.
[55]齐林,薛海涛,李占东.松辽盆地古龙凹陷龙南鼻状构造葡萄花油层油气富集条件[J].内蒙古石油化工,2010,1:117-119.
[56]侯启军,冯志强,冯子辉等.松辽盆地陆相石油地质学[M].黑龙江大庆:石油工业出版社.
[57]侯启军,冯子辉,邹玉良.松辽盆地齐家—古龙凹陷油气成藏期次研究[J].石油实验地质,2005,27(4):390-393.
[58]大庆油田石油地质志编写组.中国石油地质志(卷二),大庆、吉林油田[M].黑龙江大庆:石油工业出版社,1987.
[59]王建功,王天琦,卫平生等.松辽盆地海坨子地区葡萄花油层沉积微相[J].岩性油气藏,2007,19(2):28-34.
[60]李延钧,陈义才,朱江.松辽盆地古龙地区葡萄花油层油气成因与凝析气藏形成分布[J].西南石油学院学报,1997,19(3):14-19.
[61]毕素萍,张庆龙,王良书等.地震—地质综合储层预测技术在大庆油田G533区块的应用[J].石油实验地质,2008,30(2):203-211.
[62]李航,苏耿.百色盆地那坤油田构造精细解释与储层预测[J].南方油气,2006,19(2-3):50-53.
[63] Khaled Fouad.Wave-shape classification and attribute analysis of the lower Miocene deep-water reservoirs in Laguna Madre Basin,offshore Mexico.American Association of Petroleum Geologists Bulletin,2005,73:125-142.
[64]张玉明.高精度三维地震解释技术及在孤家子气田的应用[J].石油物探,2001,40(2):56-62.
[65]邬兴威,王英民,赵永胜.地震技术在B27井区中的应用[J].四川地质学报,1998,18(2):157-160.
[66]张永华,贾曙光,杨春峰等.断层封堵性的应用研究[J].石油物探, 2001,40 (4): 83-88.
[67]张永华.三维地震资料综合解释方法探讨[J].石油物探,2004,43 (1):49-53.
[68]张永华.分步法解释技术在南阳张店油田高分辨率三维地震勘探中的应用[J].石油物探,2000,39(1):98-105.
[69]张世奇,纪友亮,高岭.平衡剖面分析技术在松辽盆地构造演化恢复中的应用[J].新疆地质,2003,21(4):489-490.
[70]钟建华,孙正贵,禚元杰等.高分辨率层序地层学的应用—以河125断层区沙三中亚段为例[J].地质找矿论丛,2009,24(3):243-247.
[71]杨斌,郭翔,刘洪彦等.三塘湖盆地马朗地区重矿物特征与物源分析[J].石油天然气学报,2008,30(3):57-59.
[72]赵红格,刘池洋.物源分析方法及研究进展[J].沉积学报,2003,21(3):409-415.
[73]高瑞祺,蔡希源.松辽盆地油气田形成条件与分布规律[M].山东东营:石油工业出版社,1997.
[74]郭耀华,谢昕.地震油气检测技术在宁东油田的应用[J].成都理工学院学报,2008,30(1):66-70.