新疆乌什凹陷中生界沉积相及储层特征研究
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摘要
2003年乌参1井获得高产工业油气流,最近,神木1井白垩系又获重要发现,揭开了勘探开发乌什凹陷热潮的序幕。研究区资料控制十分有限,研究程度尚低,主要靠二维地震资料结合5口井的控制进行研究。对乌什凹陷来说,要尽快掌握储层分布范围及储层发育特征,尽快落实构造圈闭及其构造特征,同时提出下一步钻井优选目标,尽快展开对乌什凹陷的全区勘探开发。
通过钻井的vsp标定,从过井剖面出发,协助搭起该区地震解释剖面框架,对工区地震剖面资料进行构造解释;完成中新生界地层分布图、构造纲要图、重点圈闭局部等时图;确定乌什凹陷中生界构造特征。通过完成四口井的岩芯观察和描述,做出单井沉积相分析;做储层评价。继而进行平面沉积相分析及储层预测,结合构造圈闭探讨该区的油气前景。在landmark工作站上进行三维、部分二维地震资料的解释,应用高分辨率地震资料,对该区构造、层序演化有个新的认识,指导沉积相展布研究。
乌什凹陷是南天山与塔里木盆地北缘之间的中新生界前陆盆地。中生界主要分布在凹陷中东部,由南部边界古木别孜断裂系统控制中生界沉积,是一套砂岩、砾岩、泥岩及其过渡类型组成的陆相碎屑沉积,主要是扇三角洲-湖泊体系的沉积。在三叠、侏罗、白垩纪有湖盆扩张缩小和冲积扇、河流等沉积体的迁移及叠覆,亦有多次构造运动造成的削蚀。
该区储层主要白垩系舒善河组,主要为砂砾岩的粗碎屑岩沉积,磨圆次棱一次圆,分选中等一好,成分成熟度南北变化较大,结构成熟度总体中等。砂岩半—固结,主要是次生溶蚀孔,成岩阶段划分为早成岩B阶段。储层段总体上属于低孔低渗和特低孔特低渗储层,且非均质性强。为超深层油藏,储盖配置优良,物性较差,横向分布较稳定。已有油气显示,综合评价为中等储集层。有利区域为凹陷东北部中生界构造岩性圈闭发育区、南天山山前背斜构造带、西瓜地层圈闭和C_2-P_1礁灰岩。
Well Wucan 1 attained high yield flow of hot gas in 2003, and recently Well Shenmu 1 gains big indicating, which reveals the prelude of exploration and developing upsurge in Wushi Sag. Materials are really limited in research region, and research degree is still low, so we do studies generally basing on two dimensional seism data, as well as 5 wells. To Wushi Sag, it's important to master the distributing bounds of the strata and reservoir features, and to carry out the traps and their structural features, and to submit next optimized target, which help to comprehensively explore and develop Wushi Sag.
Through the VSP mark of the wells, and from the profiles through by the wells, we form the framework of seismic explaining profile in this area, and explain structural profiles of seismic profiles here. We finish strata distributing map of Mesozoic and Cenozoic Erathem, structure compendium map and isochronographs of major traps, and definite the structural features of Mesozoic Erathem in Wushi Sag. After observe and describe the cores of 4 wells, we analyze sedimentary facies of single wells and estimate the reservoir, and then complete the sedimentary facies plan and reservoir forecast, as well as discuss petroleum prospect in this region, combined to structural traps. Based on the explanation of three and two dimensional seism data on Landmark workstation, we got new realization on structure and sequence evolution, which direct the study of sedimentary facies distributing.
Wushi Sag is Mesozoic and Cenozoic Erathem foreland between South Tianshan and the northern Tarim Basin. Mesozoic Erathem presents mainly in the mid and east of Wushi Sag, whose sediments are controlled by Gumubiezi Fault, the south bound, and is series of sand, conglomerate, mudstone and their transitional rock types. It's continental debris sediments, generally fan delta-lake system. In Triassic, Jurassic, and Cretaceous period, the lake basin expanded and shrank, and the fan and the river moved and mantled, and also there were several structural erosions.
Shushanhe formation Cretaceous system is the main reservoir here, is generally thick sediments of sand- conglomerate degree, whose psephicity varies from subround to subangular, and mid-well sorted, and composition maturity differs quite greatly between north and south, and structure maturity is mid degree generally. The sandstone is solidified-subsolidified, and their voids are mainly secondary voids, and the diagenetic stage is Early B. The reservoir is mainly low void- low permeability and very low void- very low permeability types, and meanwhile with great anisotropism. Oil deposits here are extra-deep, with good reservoir-capping equipment, quite poor physical property, and quite stable extent. It has got oil indicatings, is comprehensively estimated as mid reservoir. The optimized areas are structure- lithologic traps of Mesozoic Erathem in the northeast of the sag, anticline belt in the front of South Tianshan, Xigua lithologic trap, and reef limestone of C_2-P_1.
通过钻井的vsp标定,从过井剖面出发,协助搭起该区地震解释剖面框架,对工区地震剖面资料进行构造解释;完成中新生界地层分布图、构造纲要图、重点圈闭局部等时图;确定乌什凹陷中生界构造特征。通过完成四口井的岩芯观察和描述,做出单井沉积相分析;做储层评价。继而进行平面沉积相分析及储层预测,结合构造圈闭探讨该区的油气前景。在landmark工作站上进行三维、部分二维地震资料的解释,应用高分辨率地震资料,对该区构造、层序演化有个新的认识,指导沉积相展布研究。
乌什凹陷是南天山与塔里木盆地北缘之间的中新生界前陆盆地。中生界主要分布在凹陷中东部,由南部边界古木别孜断裂系统控制中生界沉积,是一套砂岩、砾岩、泥岩及其过渡类型组成的陆相碎屑沉积,主要是扇三角洲-湖泊体系的沉积。在三叠、侏罗、白垩纪有湖盆扩张缩小和冲积扇、河流等沉积体的迁移及叠覆,亦有多次构造运动造成的削蚀。
该区储层主要白垩系舒善河组,主要为砂砾岩的粗碎屑岩沉积,磨圆次棱一次圆,分选中等一好,成分成熟度南北变化较大,结构成熟度总体中等。砂岩半—固结,主要是次生溶蚀孔,成岩阶段划分为早成岩B阶段。储层段总体上属于低孔低渗和特低孔特低渗储层,且非均质性强。为超深层油藏,储盖配置优良,物性较差,横向分布较稳定。已有油气显示,综合评价为中等储集层。有利区域为凹陷东北部中生界构造岩性圈闭发育区、南天山山前背斜构造带、西瓜地层圈闭和C_2-P_1礁灰岩。
Well Wucan 1 attained high yield flow of hot gas in 2003, and recently Well Shenmu 1 gains big indicating, which reveals the prelude of exploration and developing upsurge in Wushi Sag. Materials are really limited in research region, and research degree is still low, so we do studies generally basing on two dimensional seism data, as well as 5 wells. To Wushi Sag, it's important to master the distributing bounds of the strata and reservoir features, and to carry out the traps and their structural features, and to submit next optimized target, which help to comprehensively explore and develop Wushi Sag.
Through the VSP mark of the wells, and from the profiles through by the wells, we form the framework of seismic explaining profile in this area, and explain structural profiles of seismic profiles here. We finish strata distributing map of Mesozoic and Cenozoic Erathem, structure compendium map and isochronographs of major traps, and definite the structural features of Mesozoic Erathem in Wushi Sag. After observe and describe the cores of 4 wells, we analyze sedimentary facies of single wells and estimate the reservoir, and then complete the sedimentary facies plan and reservoir forecast, as well as discuss petroleum prospect in this region, combined to structural traps. Based on the explanation of three and two dimensional seism data on Landmark workstation, we got new realization on structure and sequence evolution, which direct the study of sedimentary facies distributing.
Wushi Sag is Mesozoic and Cenozoic Erathem foreland between South Tianshan and the northern Tarim Basin. Mesozoic Erathem presents mainly in the mid and east of Wushi Sag, whose sediments are controlled by Gumubiezi Fault, the south bound, and is series of sand, conglomerate, mudstone and their transitional rock types. It's continental debris sediments, generally fan delta-lake system. In Triassic, Jurassic, and Cretaceous period, the lake basin expanded and shrank, and the fan and the river moved and mantled, and also there were several structural erosions.
Shushanhe formation Cretaceous system is the main reservoir here, is generally thick sediments of sand- conglomerate degree, whose psephicity varies from subround to subangular, and mid-well sorted, and composition maturity differs quite greatly between north and south, and structure maturity is mid degree generally. The sandstone is solidified-subsolidified, and their voids are mainly secondary voids, and the diagenetic stage is Early B. The reservoir is mainly low void- low permeability and very low void- very low permeability types, and meanwhile with great anisotropism. Oil deposits here are extra-deep, with good reservoir-capping equipment, quite poor physical property, and quite stable extent. It has got oil indicatings, is comprehensively estimated as mid reservoir. The optimized areas are structure- lithologic traps of Mesozoic Erathem in the northeast of the sag, anticline belt in the front of South Tianshan, Xigua lithologic trap, and reef limestone of C_2-P_1.
引文
[1]戴启德,纪友亮.油气储层地质学[M].东营:石油大学出版社,1996.8
[2]梁狄刚,陈建平,张宝民,张水昌,王飞宇,赵孟军等.塔里木盆地库车凹陷陆相油气的生成[M].贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷六).北京:石油工业出版社,2004.1
[3]杜耀斌,曾庆才.塔里木盆地河南探区地震资料处理方法研究[J].新疆石油地质,2006.2,27(1):53-55
[4]高岩,赵秀岐,张玮,王小平,谷跃民,田兵.塔里木盆地层序地层特征与非构造圈闭勘探[M]_贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷九).北京:石油工业出版社,2004.1
[5]顾家裕.沉积相与油气[M].北京:石油工业出版社,1994.9
[6]顾家裕,朱筱敏,贾进华等.塔里木盆地沉积与储层[M].贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷四).北京:石油工业出版社,2004.1
[7]韩丹.库车西部巴什基奇克组-库姆格列木群物源体系、沉积相与储层特征[D].北京:中国地质大学,2006
[8]纪友亮.层序地层学[M].上海:同济大学出版社,2005.5
[9]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,1999.6,20(3):177-183
[10]贾承造.中国中西部前陆冲断带构造特征与天然气富集规律[J].石油勘探与开发,2005.8,32(4),9-15
[11]贾承造等.前陆冲断带油气勘探[M].北京:石油工业出版社,2000.10
[12]贾承造等.塔里木盆地板块构造与大陆动力学[M].贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷一).北京:石油工业出版社,2004.1
[13]贾承造等.塔里木盆地中新生代构造特征与油气[M].贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷二).北京:石油工业出版社,2004.1
[14]贾承造,卢华复等.库车-柯坪再生前陆冲断带油气聚集和勘探[M].北京:科学出版社,2004.3
[15]贾承造,宋岩,魏国齐,赵孟军,柳少波,李本亮.中国中西部前陆盆地的地质特征及油气聚集[J].地学前缘,2005.9,12(3),3-13
[16]贾进华,周东延,张立平,刘泽斌,周兴熙.塔里木盆地乌什凹陷石油地质特征[J].石油学报,2004.11,25(6):12-17
[17]贾进华,周东延,张立平,周兴熙,刘泽斌.塔里木盆地乌什凹陷石油地质与勘探早期评价[R].北京:中国石油勘探开发研究院,2004.2
[18]解释系统使用手册(landmark部分)[R].涿州:石油地球物理勘探局,1998.10
[19]金之钧,吕修祥,王毅,刘国臣,鲍志东.塔里木盆地波动过程及其控油规律[M].贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷十二).北京:石油工业出版社,2004.1
[20]雷燕平.库车坳陷西部库姆格列木组高精度层序格架和储层预测[D].北京:中国地质大学,2005
[21]刘林玉,柳益群,陈刚.吐鲁番坳陷中-上侏罗统碎屑岩中的自生粘土矿物特征及其成岩意义[J].岩石学报,1998.5,14(2):258-268
[22]罗金海,周新源,邱斌,杨芝林,尹宏,尚新璐.塔里木盆地西部喀什凹陷褶皱冲断带的构造特征[J].石油与天然气地质,2004.4,25(2):199-203
[23]罗金海,周新源,邱斌,尹宏,李建立.塔里木盆地西部中、新生代5次构造事件及其石油地质学意义[J].石油勘探与开发,2005.2,32(1):18-22
[24]吕锡敏,皮学军,任战利,刘全新,蔡振忠,丁兆海.库车前陆盆地含油气系统的地质特征[J].天然气地球科学,2004.6,15(3):214-217
[25]吕修祥,金之钧,周新源,杨明慧,马玉杰,张存.塔里木盆地乌什凹陷-温宿凸起油气勘探前景[J].中国石油大学学报(自然科学版),2006.2,30(1):17-21
[26]梅志超.沉积相与古地理重建[M].西安:西北大学出版社,1994.11
[27]苗继军,贾承造,戴金星,王招明,张君峰.南天山前陆冲断带中段乌什-温宿地区构造分析与油气成藏[J].天然气地球科学,2005.8,16(4):428-432
[28]裘亦楠,薛叔浩等.油气储层评价技术[M].北京:石油工业出版社,1997.5
[29]邵龙义,何志平,顾家裕,罗文林,贾进华,刘永福,张丽娟,张鹏飞.塔里木盆地古近纪岩相古地理[J].古地理学报,2006.8,8(3):353-364
[30]宋岩,王喜双.新构造运动对天然气晚期成藏的控制作用[J].天然气地球科学,2003.4,14(2),103-106
[31]孙凤华,陈祥,王振平.泌阳凹陷安棚深层系成岩作用与成岩阶段划分[J].西安石油大学学报(自然科学版),2004.1,19(1):24-37
[32]孙龙德,周新源,王国林.塔里木盆地石油地质研究新进展和油气勘探主攻方向[J].地质科学,2005.4,40(2):167-178
[33]孙永传,李蕙生.碎屑岩沉积相和沉积环境[M].北京:地质出版社,1986.12
[34]田作基,胡见义,宋建国.塔里木库车前陆盆地构造格架和含油气系统[J].新疆石油地质,2000.10,21(5):379-383
[35]田作基,宋建国,罗志立,罗蛰潭,彭大钧,于汇津.塔里木阿瓦提前陆盆地构造特征及油 气远景[J].新疆石油地质,1999.6,20(3):193-198
[36]田作基,胡见义,宋建国,罗志立.塔里木库车陆内前陆盆地及其勘探意义[J].地质科学,2002.11,37(增刊):105-112
[37]田作基,宋建国.塔里木库车新生代前陆盆地构造特征及形成演化[J].石油学报,1999.7,20(4):7-13
[38]田作基,张光亚,邹华耀,李启明,皮学军.塔里木库车含油气系统油气成藏的主控因素及成藏模式[J].石油勘探与开发,2001.10,28(5):12-16
[39]童晓光等.塔里木盆地石油地质研究新进展[M].北京:科学出版社,1996.8
[40]童晓光,何登发.油气勘探原理和方法[M].北京:石油工业出版社,2001.3
[41]王红军,周东延,张光亚,李洪辉,胡云杨,彭红雨,苗继军,李宏兵,刘桂侠,李涛,杨文静,彭更新,雷刚林,张国伟,周历,叶林,马玉杰.塔里木盆地库车西南部(含乌什凹陷)成藏条件及勘探目标优选[R].北京:中国石油勘探开发研究院,2005.1
[42]王良忱,张金亮.沉积环境和沉积相[M].北京:石油工业出版社,1996.6
[43]王庭斌.天然气与石油成藏条件差异及中国气田成藏模式[J].天然气地球科学,2003.4,14(2),79-86
[44]王筱荣.柯坪块体的地震活动特征[J].西北地震学报,2001.12,23(4):382-388
[45]王招明等.塔里木盆地油气勘探与实践[M].贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷十一).北京:石油工业出版社,2004.1
[46]王招明,李曰俊,周黎霞,夏维书,李道善,汪新,赵孟军.塔里木盆地第十三区块圈闭评价与目标选择研究报告[R].库尔勒:中国石油天然气股份有限公司塔里木油田分公司,1999.12
[47]王子煜.库车坳陷西部中新生代地层岩石物理和力学性质[J].地球物理学进展,2002.9,17(3):399-405
[48]温声明,王贵重,程明华,王志勇.南天山山前冲断带的构造样式及成因探讨[J].新疆地质,2006.3,24(1):24-29
[49]向奎.塔里木盆地西南边缘压扭构造体系及其石油地质意义[J].古地理学报,2006.5,8(2):233-240
[50]肖序常,汤耀庆,冯益民,朱宝清,李锦轶,赵民.新疆北部及其邻区大地构造[M].北京:地质出版社,1992.11
[51]新疆石油管理局南疆石油勘探指挥部地质研究所,北京师范大学地理系新生代古地理研究室.古特提斯海北支塔里木古海湾岩相古地理[M].北京:科学出版社,1989.2
[52]杨庚,钱祥麟,郭华.塔里木北缘库车陆内挠曲盆地构造演化与油气远景评价[M].北京:地质出版社,2003
[53]杨仁超.储层地质学研究新进展[J].特种油气藏,2006.8,13(4):1-5
[54]张丽娟,李多丽,孙玉善,程明.库车坳陷西部古近系-白垩系沉积储层特征分析[J].天然气地球科学,2006.6,17(3):355-360
[55]张明山,姚宗惠,陈发景.塑性岩体与逆冲构造变形关系讨论--库车坳陷西部实例分析[J].地学前缘,2002.10,9(4):371-376
[56]张师本,黄智斌,朱怀诚等.塔里木盆地覆盖区显生宙地层[M].贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷三).北京:石油工业出版社,2004.1
[57]张水昌,梁狄刚,张宝民,王飞宇,边立曾,赵孟军等.塔里木盆地海相油气的生成[M].贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷七).北京:石油工业出版社,2004.1
[58]张振红,吕修祥,王国林,马玉杰.塔里木盆地乌什凹陷-温宿凸起油气运聚过程模拟实验研究[J].西安石油大学学报(自然科学版),2005.11,20(6):16-20
[59]张振红,吕修祥,杨明慧,张存.塔里木盆地乌什凹陷石油地质特征[J].西安石油大学学报(自然科学版),2004.7,19(4):29-65
[60]赵靖舟,李启明等.塔里木盆地油气藏形成与分布规律[M].贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷八).北京:石油工业出版社,2004.1
[61]赵孟军,卢双舫,王庭栋,付广,田作基,张宝民.塔里木盆地天然气成藏与勘探[M].贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷十).北京:石油工业出版社,2004.1[62]赵文智,何登发等.石油地质综合研究导论[M].北京:石油工业出版社,1999.4
[63]郑浚茂,庞明.碎屑储集岩的成岩作用研究[M].武汉:中国地质大学出版社,1989.10
[64]周新源,王福焕,晁重阳.塔里木盆地周缘凹陷带含油气特征及勘探前景[J].中国石油勘探,2002.9,7(3),25-31
[65]周兴熙.塔里木盆地发现深成无机气的踪迹[J].天然气地球科学,1998.12,9(6):40-41
[66]周兴熙,贾进华,周东延,张立平.库车坳陷乌什凹陷东部成藏作用初步研究[J].石油勘探与开发,2006.4,33(2):184-188
[67]朱筱敏.层序地层学[M].东营:石油大学出版社,2000.4
[68]朱筱敏,顾家裕,贾进华等.塔里木盆地重点层系储盖层评价[M].贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷五).北京:石油工业出版社,2004.1
[69]Allen M.Band,Vincent S J.Structural features of northern Tarim basin:Implications for regional tectonics and petroleum traps: Discussion [J]. AAPG Bulletin, 1999, 83(8): 1279-1283
[70] Burtman V S, Skobelev S F, Molnar P. Late Cenozoic slip on the Talas - Ferghana fault, the Tien Shan, central Asia[J]. Gel. Soc. Am. Bull., 1996,108:1004-1021
[71] Cermak V, Bordi L. A heat production model of the crust and upper mantle [J] . Tectonophysics, 1991, 194: 307-323
[72] Fernandez M, Ranalli G. The role of rheology in extensional basin formation modeling [J]. Tectonophysics, 1997,282:129-145
[73] Jia Dong, Lu Huafu, Cai Dongsheng, Wu Shimin, Shi Yangshen, Chen Chuming. Structural features of northern Tarim basin: Implications for regional tectonics and petroleum traps [J]. AAPG Bulletin, 1999,82(1):147-159
[74] Jia Dong, Lu Huafu, Jia Chengzao, Wei Guoqi. Structural features of northern Tarim basin: Implications for regional tectonics and petroleum traps: Reply [J]. AAPG Bulletin, 1999, 83(8): 1284-1286
[2]梁狄刚,陈建平,张宝民,张水昌,王飞宇,赵孟军等.塔里木盆地库车凹陷陆相油气的生成[M].贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷六).北京:石油工业出版社,2004.1
[3]杜耀斌,曾庆才.塔里木盆地河南探区地震资料处理方法研究[J].新疆石油地质,2006.2,27(1):53-55
[4]高岩,赵秀岐,张玮,王小平,谷跃民,田兵.塔里木盆地层序地层特征与非构造圈闭勘探[M]_贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷九).北京:石油工业出版社,2004.1
[5]顾家裕.沉积相与油气[M].北京:石油工业出版社,1994.9
[6]顾家裕,朱筱敏,贾进华等.塔里木盆地沉积与储层[M].贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷四).北京:石油工业出版社,2004.1
[7]韩丹.库车西部巴什基奇克组-库姆格列木群物源体系、沉积相与储层特征[D].北京:中国地质大学,2006
[8]纪友亮.层序地层学[M].上海:同济大学出版社,2005.5
[9]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,1999.6,20(3):177-183
[10]贾承造.中国中西部前陆冲断带构造特征与天然气富集规律[J].石油勘探与开发,2005.8,32(4),9-15
[11]贾承造等.前陆冲断带油气勘探[M].北京:石油工业出版社,2000.10
[12]贾承造等.塔里木盆地板块构造与大陆动力学[M].贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷一).北京:石油工业出版社,2004.1
[13]贾承造等.塔里木盆地中新生代构造特征与油气[M].贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷二).北京:石油工业出版社,2004.1
[14]贾承造,卢华复等.库车-柯坪再生前陆冲断带油气聚集和勘探[M].北京:科学出版社,2004.3
[15]贾承造,宋岩,魏国齐,赵孟军,柳少波,李本亮.中国中西部前陆盆地的地质特征及油气聚集[J].地学前缘,2005.9,12(3),3-13
[16]贾进华,周东延,张立平,刘泽斌,周兴熙.塔里木盆地乌什凹陷石油地质特征[J].石油学报,2004.11,25(6):12-17
[17]贾进华,周东延,张立平,周兴熙,刘泽斌.塔里木盆地乌什凹陷石油地质与勘探早期评价[R].北京:中国石油勘探开发研究院,2004.2
[18]解释系统使用手册(landmark部分)[R].涿州:石油地球物理勘探局,1998.10
[19]金之钧,吕修祥,王毅,刘国臣,鲍志东.塔里木盆地波动过程及其控油规律[M].贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷十二).北京:石油工业出版社,2004.1
[20]雷燕平.库车坳陷西部库姆格列木组高精度层序格架和储层预测[D].北京:中国地质大学,2005
[21]刘林玉,柳益群,陈刚.吐鲁番坳陷中-上侏罗统碎屑岩中的自生粘土矿物特征及其成岩意义[J].岩石学报,1998.5,14(2):258-268
[22]罗金海,周新源,邱斌,杨芝林,尹宏,尚新璐.塔里木盆地西部喀什凹陷褶皱冲断带的构造特征[J].石油与天然气地质,2004.4,25(2):199-203
[23]罗金海,周新源,邱斌,尹宏,李建立.塔里木盆地西部中、新生代5次构造事件及其石油地质学意义[J].石油勘探与开发,2005.2,32(1):18-22
[24]吕锡敏,皮学军,任战利,刘全新,蔡振忠,丁兆海.库车前陆盆地含油气系统的地质特征[J].天然气地球科学,2004.6,15(3):214-217
[25]吕修祥,金之钧,周新源,杨明慧,马玉杰,张存.塔里木盆地乌什凹陷-温宿凸起油气勘探前景[J].中国石油大学学报(自然科学版),2006.2,30(1):17-21
[26]梅志超.沉积相与古地理重建[M].西安:西北大学出版社,1994.11
[27]苗继军,贾承造,戴金星,王招明,张君峰.南天山前陆冲断带中段乌什-温宿地区构造分析与油气成藏[J].天然气地球科学,2005.8,16(4):428-432
[28]裘亦楠,薛叔浩等.油气储层评价技术[M].北京:石油工业出版社,1997.5
[29]邵龙义,何志平,顾家裕,罗文林,贾进华,刘永福,张丽娟,张鹏飞.塔里木盆地古近纪岩相古地理[J].古地理学报,2006.8,8(3):353-364
[30]宋岩,王喜双.新构造运动对天然气晚期成藏的控制作用[J].天然气地球科学,2003.4,14(2),103-106
[31]孙凤华,陈祥,王振平.泌阳凹陷安棚深层系成岩作用与成岩阶段划分[J].西安石油大学学报(自然科学版),2004.1,19(1):24-37
[32]孙龙德,周新源,王国林.塔里木盆地石油地质研究新进展和油气勘探主攻方向[J].地质科学,2005.4,40(2):167-178
[33]孙永传,李蕙生.碎屑岩沉积相和沉积环境[M].北京:地质出版社,1986.12
[34]田作基,胡见义,宋建国.塔里木库车前陆盆地构造格架和含油气系统[J].新疆石油地质,2000.10,21(5):379-383
[35]田作基,宋建国,罗志立,罗蛰潭,彭大钧,于汇津.塔里木阿瓦提前陆盆地构造特征及油 气远景[J].新疆石油地质,1999.6,20(3):193-198
[36]田作基,胡见义,宋建国,罗志立.塔里木库车陆内前陆盆地及其勘探意义[J].地质科学,2002.11,37(增刊):105-112
[37]田作基,宋建国.塔里木库车新生代前陆盆地构造特征及形成演化[J].石油学报,1999.7,20(4):7-13
[38]田作基,张光亚,邹华耀,李启明,皮学军.塔里木库车含油气系统油气成藏的主控因素及成藏模式[J].石油勘探与开发,2001.10,28(5):12-16
[39]童晓光等.塔里木盆地石油地质研究新进展[M].北京:科学出版社,1996.8
[40]童晓光,何登发.油气勘探原理和方法[M].北京:石油工业出版社,2001.3
[41]王红军,周东延,张光亚,李洪辉,胡云杨,彭红雨,苗继军,李宏兵,刘桂侠,李涛,杨文静,彭更新,雷刚林,张国伟,周历,叶林,马玉杰.塔里木盆地库车西南部(含乌什凹陷)成藏条件及勘探目标优选[R].北京:中国石油勘探开发研究院,2005.1
[42]王良忱,张金亮.沉积环境和沉积相[M].北京:石油工业出版社,1996.6
[43]王庭斌.天然气与石油成藏条件差异及中国气田成藏模式[J].天然气地球科学,2003.4,14(2),79-86
[44]王筱荣.柯坪块体的地震活动特征[J].西北地震学报,2001.12,23(4):382-388
[45]王招明等.塔里木盆地油气勘探与实践[M].贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷十一).北京:石油工业出版社,2004.1
[46]王招明,李曰俊,周黎霞,夏维书,李道善,汪新,赵孟军.塔里木盆地第十三区块圈闭评价与目标选择研究报告[R].库尔勒:中国石油天然气股份有限公司塔里木油田分公司,1999.12
[47]王子煜.库车坳陷西部中新生代地层岩石物理和力学性质[J].地球物理学进展,2002.9,17(3):399-405
[48]温声明,王贵重,程明华,王志勇.南天山山前冲断带的构造样式及成因探讨[J].新疆地质,2006.3,24(1):24-29
[49]向奎.塔里木盆地西南边缘压扭构造体系及其石油地质意义[J].古地理学报,2006.5,8(2):233-240
[50]肖序常,汤耀庆,冯益民,朱宝清,李锦轶,赵民.新疆北部及其邻区大地构造[M].北京:地质出版社,1992.11
[51]新疆石油管理局南疆石油勘探指挥部地质研究所,北京师范大学地理系新生代古地理研究室.古特提斯海北支塔里木古海湾岩相古地理[M].北京:科学出版社,1989.2
[52]杨庚,钱祥麟,郭华.塔里木北缘库车陆内挠曲盆地构造演化与油气远景评价[M].北京:地质出版社,2003
[53]杨仁超.储层地质学研究新进展[J].特种油气藏,2006.8,13(4):1-5
[54]张丽娟,李多丽,孙玉善,程明.库车坳陷西部古近系-白垩系沉积储层特征分析[J].天然气地球科学,2006.6,17(3):355-360
[55]张明山,姚宗惠,陈发景.塑性岩体与逆冲构造变形关系讨论--库车坳陷西部实例分析[J].地学前缘,2002.10,9(4):371-376
[56]张师本,黄智斌,朱怀诚等.塔里木盆地覆盖区显生宙地层[M].贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷三).北京:石油工业出版社,2004.1
[57]张水昌,梁狄刚,张宝民,王飞宇,边立曾,赵孟军等.塔里木盆地海相油气的生成[M].贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷七).北京:石油工业出版社,2004.1
[58]张振红,吕修祥,王国林,马玉杰.塔里木盆地乌什凹陷-温宿凸起油气运聚过程模拟实验研究[J].西安石油大学学报(自然科学版),2005.11,20(6):16-20
[59]张振红,吕修祥,杨明慧,张存.塔里木盆地乌什凹陷石油地质特征[J].西安石油大学学报(自然科学版),2004.7,19(4):29-65
[60]赵靖舟,李启明等.塔里木盆地油气藏形成与分布规律[M].贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷八).北京:石油工业出版社,2004.1
[61]赵孟军,卢双舫,王庭栋,付广,田作基,张宝民.塔里木盆地天然气成藏与勘探[M].贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷十).北京:石油工业出版社,2004.1[62]赵文智,何登发等.石油地质综合研究导论[M].北京:石油工业出版社,1999.4
[63]郑浚茂,庞明.碎屑储集岩的成岩作用研究[M].武汉:中国地质大学出版社,1989.10
[64]周新源,王福焕,晁重阳.塔里木盆地周缘凹陷带含油气特征及勘探前景[J].中国石油勘探,2002.9,7(3),25-31
[65]周兴熙.塔里木盆地发现深成无机气的踪迹[J].天然气地球科学,1998.12,9(6):40-41
[66]周兴熙,贾进华,周东延,张立平.库车坳陷乌什凹陷东部成藏作用初步研究[J].石油勘探与开发,2006.4,33(2):184-188
[67]朱筱敏.层序地层学[M].东营:石油大学出版社,2000.4
[68]朱筱敏,顾家裕,贾进华等.塔里木盆地重点层系储盖层评价[M].贾承造主编.塔里木盆地石油地质与勘探丛书[C](卷五).北京:石油工业出版社,2004.1
[69]Allen M.Band,Vincent S J.Structural features of northern Tarim basin:Implications for regional tectonics and petroleum traps: Discussion [J]. AAPG Bulletin, 1999, 83(8): 1279-1283
[70] Burtman V S, Skobelev S F, Molnar P. Late Cenozoic slip on the Talas - Ferghana fault, the Tien Shan, central Asia[J]. Gel. Soc. Am. Bull., 1996,108:1004-1021
[71] Cermak V, Bordi L. A heat production model of the crust and upper mantle [J] . Tectonophysics, 1991, 194: 307-323
[72] Fernandez M, Ranalli G. The role of rheology in extensional basin formation modeling [J]. Tectonophysics, 1997,282:129-145
[73] Jia Dong, Lu Huafu, Cai Dongsheng, Wu Shimin, Shi Yangshen, Chen Chuming. Structural features of northern Tarim basin: Implications for regional tectonics and petroleum traps [J]. AAPG Bulletin, 1999,82(1):147-159
[74] Jia Dong, Lu Huafu, Jia Chengzao, Wei Guoqi. Structural features of northern Tarim basin: Implications for regional tectonics and petroleum traps: Reply [J]. AAPG Bulletin, 1999, 83(8): 1284-1286