东濮凹陷濮卫洼陷含盐层系沉积层序与油气聚集规律
|
摘要
世界上大多数含盐盆地同时也是含油气区，在含盐盆地的油气勘探中，人们发现盐岩与油气有千丝万缕的关系。对于盐岩的成因及盐源在不同盆地有不同的认识，并建立了各自的沉积模式，就是同一含盐沉积盆地或含盐沉积凹陷人们的认识依然分歧很大，关于盐岩在层序地层中的位置人们的认识依然不同，对这些问题的认识不清将极大的影响对人们含盐盆地的能源勘探开发水平，因此搞清盐岩的成因及其与油气聚集的关系具有重要意义。我国东部新生代渤海湾含油气盆地东濮凹陷濮卫洼陷古近系沙河街组发育有数套巨厚的盐韵律组，并蕴藏有大量的油气资源。以层序地层学与沉积学的基本理论和方法为指导，综合构造—地层分析、地球物理学、地球化学、盆地分析、含油气系统的理论和方法，通过钻、测井资料和地震资料的综合分析和详细解剖，对该洼陷盐岩的成因、盐源及其发育规律进行系统研究，并分析探讨该地区盐岩与油气聚集的关系，不仅具有实践价值，而且具有理论意义。
东濮凹陷位于渤海湾盆地临清坳陷西南端，东侧以兰聊断裂为界与鲁西隆起为邻，西侧以长垣断裂为界与内黄隆起相接，南以封丘北断层为界与与兰考凸起相邻，北以马陵断层为界与与莘县凹陷相望，是以古—中生界为基底，以新生界为盖层，古近纪形成的拉分走滑—裂谷型箕状断陷盆地。凹陷呈北北东向，南宽北窄，面积约5300km~2，在构造演化及沉积相带上具有明显的“南北分区、东西分带”的特征，控制凹陷内构造格局的北北东向和北西向两个断裂体系相互截切，将东濮凹陷自西向东分为西部斜坡带、西部洼陷带、中央隆起带、东部洼陷带和东部兰聊断阶陡坡带五个次级构造单元。
濮卫洼陷为东濮凹陷的一个次级洼陷，构造位置上处于东濮凹陷中央隆起带北部，夹持于濮城—陈营断裂系与卫东断裂系之间，为一负向次级构造单元，是东濮凹陷沙三段发育的主要生油洼陷之一，基底区域东倾，被多条反向断层复杂化，成为西高东低的箕状洼陷。根据控洼断裂带及局部构造的发育展布特征，濮卫洼陷自西向东可以被分为西部反向屋脊带、中央洼陷带和东部顺向断阶带三个更次级构造单元。
构造分析表明，濮卫洼陷东西两侧的濮城—陈营断裂带和卫东断裂带的作用过程控制了洼陷的发展演化。地震相干体分析结果显示这两个断裂带均是由一系列相互平行、近平行或雁列式排列的断裂组成，两断裂带在深层与浅层的发育有很大的不同。
根据东濮凹陷濮卫洼陷新生界层序地层的发育特征，建立了濮卫洼陷新生界层序地层格架，将濮卫洼陷新生界概括为一个盆地充填序列，包括古近系凹陷充填超层序组和新近系坳陷充填超层序组。古近系凹陷充填超层序组又可以分为三个超层序，分别是沙四段到沙三段萁状断陷超层序、沙二段到沙一段双断洼陷超层序和东营组收缩充填超层序。古近系箕状断陷超层序又可以划分为5个沉积层序，反映了5次明显的湖平面的变化旋回；古近系双断洼陷超层序又可以划分为3个三级沉积层序，反映了3次明显的湖平面的变化旋回。濮卫洼陷三级层序的发育特点为：低水位体系域发育厚度比较大，含盐层序低水位体系域发育期具高频四～六级湖平面变化，表现为盐岩、膏盐岩与泥页岩的中-薄互层；湖进体系域和高水位体系域一般发育比较薄；层序在洼陷内显示出东厚西薄的特点，反映了萁状断陷的特征。层序地层分析表明，含盐层系位于构造层序(超层序或超层序组)的水进体系域，盐韵律组和单个盐韵律位于三级层序或高频层序的低水位体系域。
濮卫洼陷主要储层段沙三中亚段沉积体系的研究表明，洼陷东侧的濮城断裂下降盘具明显的坡折带沉积特征，在低水位期以发育低水位三角洲沉积为主，水进及高水位期以发育湖底扇沉积为主；洼陷西侧以发育滨浅湖砂坝沉积为主；洼陷北侧以发育滨浅湖砂坝沉积和高位三角洲沉积为主；洼陷中央和南侧处于深洼之中，低水位期以发育浅水盐湖沉积为主，水进及高水位期以发育深湖—半深湖沉积为主，同时在水进体系域初期或高水位体系域晚期发
东横凹陷簇卫洼陷含盐层系沉积层序与油气聚集规律
屈红军
育偶发性的湖底扇沉积。
淮城断裂的作用过程控制了洼陷内沙三中亚段地层厚度与岩性、岩相变化，卫东断裂对
洼陷内盐岩、砂岩沉积分布也有一定的影响。淮卫洼陷沙三中亚段储集砂体的主要岩相组合
类型是湖底扇的水下河道，其次是三角洲前缘水下分流河道、湖底扇的叶状体及滨浅湖砂坝
沉积。砂体的时空展布受控于基准面旋回及可容空间的变化规律。由淮城同沉积断裂引起的
断层下降盘的坡折带，是沉积物优先沉积的地带，因而洼陷东侧坡折带附近砂体分布较厚，
向洼陷中央变薄，洼陷内砂体东厚西薄，坡折带砂体由北向南展布，不同砂层组砂体展布高
值区多位于水下河道与坡折带的交汇处。
以层序地层学理论为指导，在浪卫洼陷沙河街组划分出七个盐韵律组，其中I级盐韵律
组三个，自下而上分别是I沙三3盐、I沙三2盐、l沙一盐;11级盐韵律组四个，自下而上
分别是11沙三4盐、11沙三l盐、11沙二上盐、11沙二顶盐.在洼陷内盐岩的展布具有西厚东
薄，南厚北薄的特点，不同期的盐韵律组具有南北向来回迁移和逐渐东
Most of the salt-bearing basins are also oil and gas bearing areas. In the exploration of oil and gas in salt-bearing basins, it has been found that there are some close relationships between salt and oil & gas. With regard to the causes of formation and sources of salt, people have different point of views in different basins, and different depositional models are set up, even in one same basin there are also divergent view to exist Different opinions still exist on the position of the salt bearing strata in sequence stratigraphy. It will greatly influence the exploration level of resources in salt-bearing basin if the above doublts can not be made clear. In this way, it will be of great significance to make it clear about the above issues and the relationships about salt and oil & gas. Several thick beds of salt rocks are developed in Shahejie Formation, Eocene in Puwei sag, Dongpu depression of oil and gas bearing Bohaiwan basin, and huge amount of oil and gas are accumulated there. It will be both practical value and theoretical significance to systematically research the causes of formation, sources of salt, and development regulations of the thick beds of salt rocks in Puwei sag, and to probe into the relationship about salt and oil and gas accumulations, under the direction of sequence stratigraphy and sedimentology theorys and metheds, conbined with the analyses of the colligation of structures and strata, geophysics, geochemistry, basin analysis, and oil and gas bearing systems theorys and methods, on the basis of the synthesis analyses and dissections of cores, logs and seismic data.
With an area of 5300 km2, Dongpu depression is located in the southwest of Lin-qing depression, Bohaiwan basin, bounded with Lu-xi uplift by Lan-liao fault in the east, with Nei-huang uplift by Chang-yuan fault in the west, with Lan-kao heave by the north Feng-qiu fault in the south, with Xin country depression by Ma-ling fault in the north, while spreading along NNE defection, taking on the forms of being wide in the south, and narrow in the north. It is a rift fault depression basin with the characteristics of striking, with the basement being the Paleozoic and Mesozoic, and the capping beds being the Cenozoic. Tectonically controlled by the NNE and NW direction faults, it is divided into 5 subunit by the intercept of the NNE and NW direction faults, from west to east i. e. the west slope belt, the west sag belt, the central upheave, the east sag, the east Lan-liao fault steep stair belt Dongpu depression takes on the characteristics of being subarea northsouth, and being belt disparted westeast in the evolution of tectonics and forms of sedimentary facies.
Tectonically located in the north of the central upheave of Dongpu depression, being one of the major oil-generating sag in Sha-3 member, Puwei sag is a subunit sag of Dongpu depression, which is clamped between Pucheng-chenyin and Wei-dong fault. With the basement dipping east, and being complicated by several reverse fault, Puwei sag is a dustpan-like sag. Based on the characteristics of faults which controlled the sag and other structures, Puwei sag can be divided into 3 hypo-subunit i. e. the west reverse fault ridge belt, the central sag belt the east orderly fault steep stair belt.
Structure analysis indicates mat the tectonic evolution of Puwei sag is controlled by Pucheng-chenyin and Wei-dong fault. The seismic coherence cube makes it clear that the two faults are composed of a series of paralleling or approximately paralleling or wold goose line pattern fractures, with the deep and the shallow part of the two faults being much different.
On the basis of the characteristics of sequence stratigraphy of the Cenozoic in Puwei sag, Dongpu depression, the sequence stratigraphic framework of the Cenozoic is set up, including two supersequence sets which is fault depression filling supersequence sets of the Eocene, and depression filling supersequence sets of the Tertiary. The fault depression filling supersequence sets of the Eocene can be divided into 3 supersequ
东濮凹陷位于渤海湾盆地临清坳陷西南端，东侧以兰聊断裂为界与鲁西隆起为邻，西侧以长垣断裂为界与内黄隆起相接，南以封丘北断层为界与与兰考凸起相邻，北以马陵断层为界与与莘县凹陷相望，是以古—中生界为基底，以新生界为盖层，古近纪形成的拉分走滑—裂谷型箕状断陷盆地。凹陷呈北北东向，南宽北窄，面积约5300km~2，在构造演化及沉积相带上具有明显的“南北分区、东西分带”的特征，控制凹陷内构造格局的北北东向和北西向两个断裂体系相互截切，将东濮凹陷自西向东分为西部斜坡带、西部洼陷带、中央隆起带、东部洼陷带和东部兰聊断阶陡坡带五个次级构造单元。
濮卫洼陷为东濮凹陷的一个次级洼陷，构造位置上处于东濮凹陷中央隆起带北部，夹持于濮城—陈营断裂系与卫东断裂系之间，为一负向次级构造单元，是东濮凹陷沙三段发育的主要生油洼陷之一，基底区域东倾，被多条反向断层复杂化，成为西高东低的箕状洼陷。根据控洼断裂带及局部构造的发育展布特征，濮卫洼陷自西向东可以被分为西部反向屋脊带、中央洼陷带和东部顺向断阶带三个更次级构造单元。
构造分析表明，濮卫洼陷东西两侧的濮城—陈营断裂带和卫东断裂带的作用过程控制了洼陷的发展演化。地震相干体分析结果显示这两个断裂带均是由一系列相互平行、近平行或雁列式排列的断裂组成，两断裂带在深层与浅层的发育有很大的不同。
根据东濮凹陷濮卫洼陷新生界层序地层的发育特征，建立了濮卫洼陷新生界层序地层格架，将濮卫洼陷新生界概括为一个盆地充填序列，包括古近系凹陷充填超层序组和新近系坳陷充填超层序组。古近系凹陷充填超层序组又可以分为三个超层序，分别是沙四段到沙三段萁状断陷超层序、沙二段到沙一段双断洼陷超层序和东营组收缩充填超层序。古近系箕状断陷超层序又可以划分为5个沉积层序，反映了5次明显的湖平面的变化旋回；古近系双断洼陷超层序又可以划分为3个三级沉积层序，反映了3次明显的湖平面的变化旋回。濮卫洼陷三级层序的发育特点为：低水位体系域发育厚度比较大，含盐层序低水位体系域发育期具高频四～六级湖平面变化，表现为盐岩、膏盐岩与泥页岩的中-薄互层；湖进体系域和高水位体系域一般发育比较薄；层序在洼陷内显示出东厚西薄的特点，反映了萁状断陷的特征。层序地层分析表明，含盐层系位于构造层序(超层序或超层序组)的水进体系域，盐韵律组和单个盐韵律位于三级层序或高频层序的低水位体系域。
濮卫洼陷主要储层段沙三中亚段沉积体系的研究表明，洼陷东侧的濮城断裂下降盘具明显的坡折带沉积特征，在低水位期以发育低水位三角洲沉积为主，水进及高水位期以发育湖底扇沉积为主；洼陷西侧以发育滨浅湖砂坝沉积为主；洼陷北侧以发育滨浅湖砂坝沉积和高位三角洲沉积为主；洼陷中央和南侧处于深洼之中，低水位期以发育浅水盐湖沉积为主，水进及高水位期以发育深湖—半深湖沉积为主，同时在水进体系域初期或高水位体系域晚期发
东横凹陷簇卫洼陷含盐层系沉积层序与油气聚集规律
屈红军
育偶发性的湖底扇沉积。
淮城断裂的作用过程控制了洼陷内沙三中亚段地层厚度与岩性、岩相变化，卫东断裂对
洼陷内盐岩、砂岩沉积分布也有一定的影响。淮卫洼陷沙三中亚段储集砂体的主要岩相组合
类型是湖底扇的水下河道，其次是三角洲前缘水下分流河道、湖底扇的叶状体及滨浅湖砂坝
沉积。砂体的时空展布受控于基准面旋回及可容空间的变化规律。由淮城同沉积断裂引起的
断层下降盘的坡折带，是沉积物优先沉积的地带，因而洼陷东侧坡折带附近砂体分布较厚，
向洼陷中央变薄，洼陷内砂体东厚西薄，坡折带砂体由北向南展布，不同砂层组砂体展布高
值区多位于水下河道与坡折带的交汇处。
以层序地层学理论为指导，在浪卫洼陷沙河街组划分出七个盐韵律组，其中I级盐韵律
组三个，自下而上分别是I沙三3盐、I沙三2盐、l沙一盐;11级盐韵律组四个，自下而上
分别是11沙三4盐、11沙三l盐、11沙二上盐、11沙二顶盐.在洼陷内盐岩的展布具有西厚东
薄，南厚北薄的特点，不同期的盐韵律组具有南北向来回迁移和逐渐东
Most of the salt-bearing basins are also oil and gas bearing areas. In the exploration of oil and gas in salt-bearing basins, it has been found that there are some close relationships between salt and oil & gas. With regard to the causes of formation and sources of salt, people have different point of views in different basins, and different depositional models are set up, even in one same basin there are also divergent view to exist Different opinions still exist on the position of the salt bearing strata in sequence stratigraphy. It will greatly influence the exploration level of resources in salt-bearing basin if the above doublts can not be made clear. In this way, it will be of great significance to make it clear about the above issues and the relationships about salt and oil & gas. Several thick beds of salt rocks are developed in Shahejie Formation, Eocene in Puwei sag, Dongpu depression of oil and gas bearing Bohaiwan basin, and huge amount of oil and gas are accumulated there. It will be both practical value and theoretical significance to systematically research the causes of formation, sources of salt, and development regulations of the thick beds of salt rocks in Puwei sag, and to probe into the relationship about salt and oil and gas accumulations, under the direction of sequence stratigraphy and sedimentology theorys and metheds, conbined with the analyses of the colligation of structures and strata, geophysics, geochemistry, basin analysis, and oil and gas bearing systems theorys and methods, on the basis of the synthesis analyses and dissections of cores, logs and seismic data.
With an area of 5300 km2, Dongpu depression is located in the southwest of Lin-qing depression, Bohaiwan basin, bounded with Lu-xi uplift by Lan-liao fault in the east, with Nei-huang uplift by Chang-yuan fault in the west, with Lan-kao heave by the north Feng-qiu fault in the south, with Xin country depression by Ma-ling fault in the north, while spreading along NNE defection, taking on the forms of being wide in the south, and narrow in the north. It is a rift fault depression basin with the characteristics of striking, with the basement being the Paleozoic and Mesozoic, and the capping beds being the Cenozoic. Tectonically controlled by the NNE and NW direction faults, it is divided into 5 subunit by the intercept of the NNE and NW direction faults, from west to east i. e. the west slope belt, the west sag belt, the central upheave, the east sag, the east Lan-liao fault steep stair belt Dongpu depression takes on the characteristics of being subarea northsouth, and being belt disparted westeast in the evolution of tectonics and forms of sedimentary facies.
Tectonically located in the north of the central upheave of Dongpu depression, being one of the major oil-generating sag in Sha-3 member, Puwei sag is a subunit sag of Dongpu depression, which is clamped between Pucheng-chenyin and Wei-dong fault. With the basement dipping east, and being complicated by several reverse fault, Puwei sag is a dustpan-like sag. Based on the characteristics of faults which controlled the sag and other structures, Puwei sag can be divided into 3 hypo-subunit i. e. the west reverse fault ridge belt, the central sag belt the east orderly fault steep stair belt.
Structure analysis indicates mat the tectonic evolution of Puwei sag is controlled by Pucheng-chenyin and Wei-dong fault. The seismic coherence cube makes it clear that the two faults are composed of a series of paralleling or approximately paralleling or wold goose line pattern fractures, with the deep and the shallow part of the two faults being much different.
On the basis of the characteristics of sequence stratigraphy of the Cenozoic in Puwei sag, Dongpu depression, the sequence stratigraphic framework of the Cenozoic is set up, including two supersequence sets which is fault depression filling supersequence sets of the Eocene, and depression filling supersequence sets of the Tertiary. The fault depression filling supersequence sets of the Eocene can be divided into 3 supersequ
引文
Allen P A, Allen J R 著．盆地分析---原理及应用．陈全茂译．1995．北京：石油工业出版社，108-124
C．k．威尔格斯等编．徐怀大，魏魁生，洪卫东，等译．1993．层序地层学原理(海平面变化综合分析)．北京：石油工业出版社，526p．
Cross T．A 著，杜宁平 译．1996．据高分辨率层序地层学认识地层结构对比概念体积配分相分异和储层的间隔单元划分．国外油气勘探，8(3)：285-294
陈发亮，朱晖，李绪涛，等．2000．东濮凹陷下第三系沙河街组层序地层划分及盐岩成因探讨．沉积学报，18(3)：386-388
陈发景．1983．中国中新生代盆地构造与演化．北京：科学出版社，78-83
池英柳，张万选，张厚福，等．1996．陆相断陷盆地层序成因初探．石油学报，17(5)：19-26
池秋鄂，龚福华．2001．层序地层学基础及应用．北京：石油工业出版社，229p．
蔡雄飞．1994．古气候是盆地分析不可缺少的因素．岩相古地理，14(2)：42-46
邓宏文．1995．美国层序地层研究中的新学派—高分辨率层序地层学．石油天然气地质，16(2)：90-97
邓宏文，王红亮，宁宁．2000．沉积物体积分配原理—高分辨率层序地层学的理论基础．地学前缘，7(4)：305-313
邓宏文，王洪亮，翟爱军，等．1999．中国陆源碎屑盆地层序地层与储层展布．石油与天然气地质，20(2)：108-114
邓宏文，王洪亮，李熙韶．1996．层序地层基准面的识别、对比技术及应用．石油与天然气地质，17(3)：177-184
邓宏文，王洪亮，祝永军，等．2002．高分辨率层序地层学—原理及应用．北京：地质出版社，178p．
樊太亮，郭齐军，吴贤顺．1999．鄂尔多斯盆地北部上古生界层序地层特征与储层发育规律．现代地质，13(1)：32-36
樊太亮，吕建仓，丁明华．2000．层序地层体制中的陆相储层发育规律．地学前缘，7(4)：315-321
樊太亮，李卫东．1999．层序地层应用于陆相油藏预测的成功实例．石油学报，20(2)：12-17
樊太亮．1997．沉积基准面变化分析技术及应用．石油与天然气地质，18(2)：120-127
冯有良，李思田．2001．东营凹陷沙河街组三段层序低位域砂体沉积特征．地质论评，47(3)：278-286
冯有良，李思田，解习农．2000．陆相断陷盆地层序形成动力学及层序地层模式．地学前缘，7(3)：119-131
顾家裕．1986．东濮凹陷形成环境．石油实验地质，8(1)：22-28
顾家裕．1995．陆相盆地层序地层格架概念及模式．石油勘探与开发，22(4)：6-10
顾家裕．1984．中国东部古代扇—三角洲沉积．石油与天然气地质，5(3)：236-244
郭建华，宫少波，吴东胜．1998．陆相断陷湖盆T-R旋回沉积层序与研究实例．沉积学报，16(1)：8-14
郭建华，郭成贤，翟永红，等．1996．东濮凹陷前梨园地区Es_3~4-Es_3~3亚段沉积旋回与沉积体系．石油实验地质，18(4)：377-384
侯读杰，王铁冠，张一伟，等．1997．中国东部第三系的陆相沉积中的甲藻甾烷：海侵指相的标志物?地质论评，43(5)：524-528
何承全，朱神照，靳广兴，等，1989．东濮地区早第三纪沟鞭藻及其它的藻类．北京：石油工业出版社．15-21
郝诒纯，李蕙生．1984．渤海沿岸地区及邻近地区第三纪钙质超微化石地发现．科学通报，29(12)：741-745
胡受权，郭文平．2001．论陆相层序地层学理论体系及其研究思路．断块油气田，8(5)：1-7．
胡受权，颜其彬，张永贵．1999．断陷湖盆陡坡带陆相层序体系域与油气藏成藏类型．石油勘探与开发，26(1)：13-17
姜在兴，赵澄林，刘孟慧．1990．东濮凹陷西部湖相风暴沉积的初步研究．沉积学报，8(1)：107-113
姜在兴，李华启．1996．层序地层学原理及应用．北京：石油工业出版社，162p．
金强，黄醒汉．1985．东濮凹陷早第三纪盐湖成因探讨．华东石油学院学报，(1)：1-13
纪友亮，张世奇．1996．陆相断陷湖盆层序地层学．北京：石油工业出版社，127p．
刘立，胡春燕．1991．砂岩中主要碎屑成分的物源意义．岩相古地理，(6)：48-53
刘明义．1984．东濮凹陷油气聚集模式．石油学报，5(4)：19-25
刘星利．1987．渤海地区构造展布特征与油气分析．石油与天然气地质，8(1)：45-55
刘池洋．1990．从渤海湾盆地的地壳厚度变化论地壳双层差异扩张原理．见：赵重远，刘池洋著．华北克拉通沉积盆地形成与演化及其油气赋存．西安：西北大学出版社，43-53
刘招君，董清水，王嗣敏，等．2000．陆相层序地层学导论与应用．北京：石油工业出版社，253p．
李守军．1998．渤海湾盆地早第三纪水平面升降和全球海平面升降的不一致性．地质论评，44(1)：31-34
李德生．1979．渤海湾含油气盆地的构造格局．石油勘探与开发，6(2)：1-10
李德生，薛叔浩．1983．中国东部中新生代盆地与油气分布．地质学报，57(3)：224-234
李任伟．1988．高盐环境和生油．中国科学，3期：303-313
李任伟，辛茂安．1989．东濮盆地蒸发岩的成因．沉积学报，7(4)：141-148
李思田，杨士恭．1992．论沉积盆地的等时地层和基本建造单元，沉积学报，10(4)：11-22
李思田，潘元林，陆永潮，等．2002．断陷湖盆隐蔽油藏预测及勘探的关键技术--高精度地震探测基础上的层序地层学研究．地球科学—中国地质大学学报．27(5)：592-598
李思田，林畅松，解习农，等．1995．大型陆相盆地层序地层学研究---以鄂尔多斯中生代盆地为例．地学前缘，2(3-4)：133-136
李思田．1996．含能源盆地沉积体系—中国内陆和近海主要沉积体系类型的典型分析，武汉：中国地质大学出版社，117-137
李文厚，屈红军，魏红红，等．2003．内蒙古苏里格庙地区晚古生代层序地层学研究．地层学杂志，27(1)：41-44
李文厚．1997．吐-哈盆地台北凹陷侏罗系层序地层学研究．石油与天然气地质，18(3)：210-215
李文厚．1997．苏红图-银根盆地下白垩统层序地层学研究．沉积学报，15(3)：18-22
林又玲，吴贤涛，潘结南，等．2000．东濮凹陷老第三系沙河街组盐类沉积模式新见．古地理学报；2(4)：66-75
林畅松，刘景彦，张燕梅．1988．沉积盆地动力学与模拟研究．地学前缘，5：119-125
林畅松，张燕梅，刘景彦，等．2000．高精度层序地层学和储层预测．地学前缘，7(3)：
111-117
林畅松，潘元林，肖建新，等．2000．“构造坡折带”---断陷盆地层序分析和油气预测的重要概念．地球科学—中国地质大学学报，25(3)：260-265
林舸．1991．东濮凹陷及邻区卫星影像特征及其地质意义．北京：石油工业出版社．12-45
蔺殿忠．1984．渤海湾盆地断块体扭转翘倾及其形成机制的探讨．石油勘探与开发，3期：26-31
陆荣生，赵春元，陈树文，等．1993．中国石油地质志(卷7，中原油田)．北京：石油工业出版社，7-70
马新华，华爱刚，李景明，等．2000．含盐油气盆地．北京：石油工业出版社，1-4
马杏垣，刘和甫，王维襄．1983．中东部中新代裂陷作用和伸展构造．地质学报，57(1)：22-31
梅志超．1993．层序地层学．西安：西北大学出版社，99p
彭立才，杨平，濮人龙．1999．陆相咸化湖泊沉积硫酸岩盐硫同位素组成及其地质意义[J]．矿物岩石地球化学通报，18(2)：99-102
齐兴宇．1988．东濮凹陷油气藏类型及分布．石油学报，9(2)：28-36
齐兴宇，黄先雄，寿建峰，等．1992．东濮凹陷盐岩与油气．石油学报，13(1)：23-29
漆家福，张一伟，陆克政，等．1995．渤海湾新生代裂陷盆地的伸展构造模式及其构造动力学过程．石油实验地质，17(4)：316-323
强祖基，张立人．1983．中国第四纪活动断裂分区与地震活动性．地质学报，57(4)：358-368
屈红军，李文厚，何希鹏，等．2003．六盘山盆地下白垩统沉积层序与含油气系统．西北大学学报(自然科学版)，33(1)：70-73
屈红军，李文厚，苗建宇，等．2003．东濮凹陷濮卫洼陷盐岩发育规律及其成因探讨．中国地质，已录用(待刊)
任来义，林桂芳，赵志清，等．2000．东濮凹陷早第三系的海侵事件．古生物学报，39(4)：553-557
任来义．2001．东濮凹陷下第三系生物地层及隐蔽油气藏勘探研究．西安：西北大学硕士学位论文，80p
孙镇城，杨藩，张技焕，等．1997．中国中新生代咸化湖泊沉积环境与油气生成．北京：石油工业出版社，142-149
童崇光．1980．中国东部裂谷系统的地质特征．石油学报，1(4)：19-26
覃建雄，陈洪德，田景春．2001．层序地层作为沉积盆地识别标志的研究．古地理学报，3(2)：72-81
唐祥华．1986．东濮凹陷渐新世早期成盐环境及古生态的探讨．微体古生物学报，3(1)：51-58
吴贤涛，林又玲，等．1999．东濮凹陷沙河街组痕迹相及其对应的测井图型．古地理学报，1(3)：50-64
吴贤涛，张庆智，张国成，等．1999．东濮凹陷北部下第三系沙四段沉积期海水入侵前后生物痕迹特征及其意义．见：沉积学及岩相古地理学新进展．北京：石油工业出版社．1995，273-277
吴因业，顾家裕，2000．油气层序地层学．北京：石油工业出版社，470p．
王鸿桢，史晓颖．1998．沉积层序及海平面旋回的分类级别—旋回周期的成因讨论．现代地质，12(1)：1-16
王鸿祯，史晓颖，王训练，等，2000．中国层序地层研究．广州：广东科技出版社，
434p．
王红亮，邓宏文．2000．东濮凹陷濮卫环洼带层序划分与沉积体系，古地理学报，2(1)：49-53
王涛．1997．中国东部裂谷盆地油气藏地质．北京：石油工业出版社，1-53
王新运，辛茂安，1989．东濮凹陷油气藏形成条件及油气富集规律．石油与天燃气地质，10(4)：407-417
王德仁，焦大庆，任来义，等．1998．东濮凹陷与盐岩有关的岩性油气藏特征．见：潘元林，孔凡仙，杨申镳，等主编．中国隐蔽油气藏．北京：地质出版社，57-66
王东坡，刘立．1994．大陆裂谷盆地层序地层学的研究．岩相古地理，14(3)：1-9
魏魁生，徐怀大．1993．冀中地区早第三纪海泛特征及其层序地层学意义．现代地质，7(3)：274-283
魏魁生，徐怀大．1993．华北典型箕状断陷盆地层序地层学模式及其与油气的赋集．地球科学，18(2)：139-149
魏魁生，徐怀大，王淑芬．1997．松辽盆地白垩系高分辨率层序地层格架．石油与天然气地质，18(1)：7-13
汪时成，周庆凡．2000．含油气系统概念的由来及内涵．石油与天然气地质，21(3)：279-282．
许靖华．1985．地中海盐度突变地历史．见何起祥等译：大地构造与沉积作用．北京：地质出版社，382-410
徐强，姜烨，董伟良，等．2003．中国层序地层研究现状和发展方向．21(1)：155-167
徐怀大．1997．陆相地层研究中的某些问题．石油与天然气地质，18(2)：83-88
薛良清．2000．成因层序地层学的回顾与展望．沉积学报，18(3)：484-488
薛良清．1995．层序地层学研究现状、方法与前景，石油勘探与开发，22(5)：8-13
薛良清．1990．层序地层学在湖相盆地中的应用探讨，石油勘探与开发，17(6)：29-34，40
解习农，程守田，陆永潮．1996．陆相盆地幕式构造旋回与层序构造．地球科学—中国地质大学学报，21(1)：27-33
杨香华，陈开远，石万忠，等．2002．东濮凹陷盐湖层序结构与隐藏油气藏．石油与天然气地质，23(2)：139-142
姚益民，梁鸿德，蔡治国，等．1994．中国油气区第三系(Ⅳ)—渤海湾盆地油气区分册．北京：石油工业出版社，240p．
尹太举．2002．高分辨率层序地层学及其在濮城油田开发中的应用．北京：中国地质大学博士学位论文，134p
阎敦实，王尚文，唐智．1980．渤海湾含油气盆地断块活动与古潜山油气田的形成．石油学报，1(2)：1-9
岳文浙，丁保良，魏乃颐．2000．陆盆层序地层研究的思路．地质论评，46(4)：347-354
郑荣才，吴朝容，叶茂才．2000．浅谈陆相盆地高分辨率层序地层研究思路．成都理工学院学报，27(3)：241-244
郑荣才，吴朝容．1999．西部凹陷深层沙河街组生储盖组合的层序分析．成都理工学院学报，26(4)：348-356
郑荣才，尹世民，彭军．2000．基准面旋回结构与叠加样式的沉积动力学分析．沉积学报，18(3)：369-375
郑鸿稳．2002．东濮凹陷下第三系层序地层模式．石油学报，23<4)：24-28
郑浚茂，王德发．1984．东濮断陷盐湖盆地下第三系砂岩体类型及沉积模式．沉积学报，2(2)：17-28
张建军，李治，刘贤武．1998．东濮凹陷沙河街组盐岩成因研究．断块油气田．5(5)：18-22
张永才．1992．东濮凹陷早第三纪含盐地层．石油学报，13(2)：232-239
张世奇，纪友亮．1996．陆相断陷湖盆层序地层学模式探讨．石油勘探与开发，23(5)：20-23
张文昭．1997．中国陆相大油田．北京：石油工业出版社，216-233，702-742
张功成，蔡希源，周章保，等．1996．裂陷盆地分析原理和方法—以松辽盆地为例．北京：石油工业出版社，293p．
张洪安，李继东．2003．白庙构造油气成藏特征．石油与天然气地质，24(1)：45-49
赵重远，刘池洋．1990．华北克拉通沉积盆地形成与演化及其油气赋存．西安：西北大学出版社，1-74
赵良金，张子贤．1997．濮城西沙二气顶油藏．北京：石油工业出版社，191p．
赵政璋．2000．储层预测技术及应用实例．石油工业出版社，P．95-147
赵澄林，刘孟慧．1988．湖相沉积中的同生变形构造及其地质意义．岩石学报，4(4)：14-21
赵澄林，刘孟慧．1984．湖底扇相模式及其在油气预测中应用．华东石油学院学报，4期：1-11
赵澄林，刘孟慧，纪友亮．1992．东濮凹陷下第三系碎屑岩沉积体系与成岩作用．北京：石油工业出版社，1-55
赵澄林，刘孟慧，姜在兴，等．1991．渤海湾早第三纪断陷盆地含油气岩系沉积学及沉积相的基本特征．石油学报，12(2)：8-32
赵澄林，姜在兴，刘孟慧．1989．东濮凹陷西部下第三系的遗迹相．石油大学学报，13(1)：1-8
赵志清，吕红玉．1988．东濮凹陷晚始新世生物群及其古环境探讨．微体古生物学报，5(3)：315-322
朱夏．1965．我国陆相中新生界含油气盆地的大地构造特征及有关大地构造问题．北京：科学出版社，10-15
朱夏，陈焕疆，孙肇才，等．1983．中国新生代构造与含油气盆地．地质学报，57(3)：235-241
朱浩然．1979．山东滨县下第三系沙河街组的藻类化石．古生物学报，18(4)：327-340
朱家蔚，辛茂安，许化政．1991．东濮凹陷油气生成特征．见：中原石油勘探局．东濮凹陷油气生成地球化学特征．北京：石油工业出版社，1-48
朱筱敏．1998．层序地层学原理及应用．北京：石油工业出版社，106p．
曾允孚，覃建雄．1999．沉积学发展现状与前瞻．成都理工学院学报，26(1)：1-7
钟筱春，钟石兰，费轩冬，等．1988．渤海湾盆地沙河街组一段颗石藻化石及其沉积环境．微体古生物学报，5(2)：145-151
周章保，陶国强，汪新文．2000．东濮凹陷变换构造初析．断块油气田，7(增刊)：3-6
甄维胜，吕新华，胡望水，等．2001．复杂断块油田非均质油藏精细描述．北京：石油工业出版社，159p．
中原石油勘探局．1991．东濮凹陷油气生成地球化学研究-北京：石油工业出版社，181p．
中原石油勘探局勘探开发研究院，中科院南京地质古生物研究所．1989．东濮地区早第三纪介形类．北京：石油工业出版社，72p．
Allen, P. A.,and J. R. Allen, 1990． Basin analysis principles and applications. Blackwell Scientific Pub. Oxford, 451 p.
Anstey N A, 1982． Simple seismics: International Human Resources Development Corporation, Boston, 168p.
Bahorich M and Farmer S. 1995． The coherence cube. The Leading Edge, P. 1053-1058
Busson, G, and Schreiber, B. C. (eds.), 1997． Sedimentary deposition in rift and foreland basins in France and Spain : Columbia University Press, New York, 479 p.
Biddle K T, Wielchowshy C C. 1994． Hydrocarbon traps. In: Magoon L B, Dow W G, eds. The petroleum system-from source to trap. AAPG Memoir, 60 :219-235
Brown L F Jr, Benson J M, Brink G J, et al. 1995． Sequence stratigraphy in Offshore South African divergent basin. AAPG Studies in Geology, 41:1-184
Carter, R. M., T. R. Nash, M. Ito, and B. J. Pillans (eds.), 1998． Sequence stratigraphy in the Plio-Pleistocene: An evaluation: Sedimentary Geology, v. 122, 288 p. [Special Issue]
Christie-Bilker K, G S. Mountain, and K. G Miller, 1990, Seismic stratigraphic record of sea-level change, in Revelle, R. R. et al. (eds.). Sea level change, National Research Council Studies in Geophysics, National Academy Press, Washington, D. C., p. 116-140
Cloetingh S C. 1986． Intraplate stresses: a new tectonic mechanism for fluctuations of relative sea level. Geology, 14:617-620
Cross T A. 1994, Genetic Stratigraphy Research Group Colorado School of Mines Annual Report on Research Projects and Industry Collagborations. 1-28
Cross T A. 1994． High-resolution stratigraphic correlation from the perspective of base-level cycles and sediment accommodation. In: Proceedings of Northwestern Europian Sequence Stratigraphy Congress, 105-123
Cross, T.A., and Lessenger, M.A., 1998． Sediment volume partitioning: rational for stratigraphic model evaluation and high-resolution stratigraphic correlation, in F.M. Gradstein. K.O. Sandvik, and N.J. Milton, eds., Sequence Stratigraphy Cross, T.A., and Lessenger, M.A., 1999． Construction and application of a stratigraphic inverse model, in J.W. Harbaugh, W.L. Watney, E.C. Rankey, R. Slingerland, R.H. Goldstein, E.K. Franseen, eds, SEPM Special Publication 62 Numerical Experiments in Stratigraphy: Recent Advances in Stratigraphic and Sedimentologic Computer Simulations: SEPM (Society for Sedimentary Geology), p. 69-83．
Demaison G. 1984． The generative basin concept In: Denmaison G. Murris R J. eds. Petroleum geochemistry and basin evaluation. AAPG Memoir,35: 1-14
Dickinson, R. W., et al., 1983． Provenance of North American Phancrozoic sandstones in relation to tectonic setting: Geol. Soc. America Bull., V. 94, p. 223
Emery, D., and K. J. Meyers (eds.), 1996． Sequence stratigraphy: Blackwell Science Ltd., Oxford, 297 p.
Eschard R, Lemouzy P, Bacchiuna, et al. 1998． Combining sequence stratigraphy, geostatistical simulations and production data for modeling a fluvial reservoir in the chauchoy field (Triassic, France). AAPG Bulletin, 82(4) : 545-568
Galloway W E. 1989a. Genetic stratigraphic sequences in basin analysis I : architecture and genesis of flooding-surface bounded depositional units. AAPG Bulletin, 73: 125-142
Galloway W E. 1989b.Genetic stratigraphic sequences in basin analysis II: application to northwest Gulf of Mexico Cenozoic basin. AAPG Bulletin, 73: 143-154
Galloway W E. 1998． Geologic Column-Clastic Depositional Systems and Sequences: Applications to Reservoir Prediction, Delineation, and Characterizatoion. The Leading Edge, 17(2) , 173-176,178-180
Hallam, 1992． Phanerozoic sea-level changes: Columbia University Press, New York, 266 p.
Hallam, A., 1998, Interpreting sea level, in Doyle, P. and M.R. Bennett (eds.). Unlocking the stratigraphyical record: Advances in modern stratigraphy: John Wiley & Sons, Ltd., Chichester, p.
421-439
Halbouty M T. 1982． The deliberate search for the subtle trap. AAPG Memior, 32 : 351
Haq, B. U. (ed.), 1995． Sequence stratigraphy and depositional response to eustatic, tectonic and climatic forcing: Kluwer Academic Publishers, Dordrecht, 381 p.
Haq.B U, Hardenbol J, Vail P R. 1988． Mesozoic and Cenozoic chronostratigraphy and cycles of sea level change. In: Wilgus C K, et al. eds. Sea level changes: an integrated approach. SEPM, Special Publication 42:71-108
Holser W. 1979． Trace elements and isotopes in evaporites. Mineralogical society of erica short course notes, 6: 295-346
Johnson, Klapper J G, Sandberg C A. 1995, Devonian eustatic fluctuations in euramerica. Gololgical Society of America Bulletin, 79(5) : 567-587
Kendall AC. 1979． Subaqueous evaporates. In: Walker G G (ed.), Facies models: Geoscience Canada Reorent Ser. 1,170
Kendall A C. 1992． Evaporates. In: Walker R G, and James N P (ed.), Facies models-Response to sea level change: Geol. Assoc, Canada, 375-409
Levorsen A I. 1967． Geology of petroleum. 2nd ed. San Francisco : Freeman W H and Co, 724
Lin C S, Eriksson K, Li S T, et al. 2000． Sequence architecture , depositional systems, and controls on development of lacustrine basin fills in part of the Erlian basin, Northeast China. AAPG Bulletin, 85(11) : 2017-2043
Loutit T S, Hardenbol J, Vail P R, Baum G R. 1988． Condensed sections: the key to age determination and correlation of continental margin sequences. In: Wilgus C K, Hastings B S, Kendall C G St C. et al., ed. Sea level changes:an intergrated approach. Soc. Econ Paleontol. Mineral spec, publ., 42:183-213．
Lu Yongchao, Xie Xinong, Jiao Yangquan, et al. 1997． Depositional responding to tectonic evolution of East China Sea. shelf basin. Journal of China University of Geosciences, 8(1) : 56-61
MacDonald, D. I. M., 1991． Sedimentation, tectonics and eustasy: Sea-level changes at active margins: Internal. Assoc. Sedimentologists Spec. Pub. 12, Blackwell, Oxford, 518 p.
Magoon L B, Dow W G 1994． The petroleum system. In: Magoon L B, Dow W G. The petroleum system-from source to trap.AAPG Memoir,60:3-22．
Marfurt K J and R. L Kirlin, 1998． 3-D Seismic attributes using a semblance-based coherency algorithm, Geophysics, Vol.63, No.4, P.1150-1165
Marfurt K J and V Sudhaker, 1999． Coherency calculations in the presence of structural dip, Geophysics, Vol. 64, No. 1, P. 104-111
Meissner F F. 1984． Petroleum geology of the Bakken Formation., Williston basin, North Dakota and Montana. In: Demaison G, Murris R J,eds. Petroleum geochemistry and basin evaluation. AAPG Memoir, 35:159-179
Melvin J. L. (ed.), 1991． Evaporites, petroleum, and mineral resources: Elsevier, Amsterdam, 556 p.
Miall AD. 1991． Stratigraphic sequences and their chronostratigraphic correlation. Journal of Sedimentary Petrology, 61:497-506
Miall, A. D., 1992． Alluuvial deposits, in Walker, R.G and N. P. James (eds.), Facies models: Response to sea level changes, Geol. Assoc. Canada, p. 119-142
Miall, A. D., 1994, Sequence stratigraphy and chronostratigaphy: problems of definition and precision in correlation, and their implication for global eustasy: Geoscience Canada, v. 21, p. 1-26
Miall, A. D., 1997． The geology of Stratigraphic sequences: Springer-Verlag, Berlin, 433 p.
Miall, A. D., 1990． Principles of sedimentary basin analysis, 2 nd ed.: Springer-Verlag, New York, 668 p.
Miall, A. D., 1991． Exxon global cycle chart: An event for every occasion ? Geology, v, 20, p. 790-797
Miall, A. D., 1996． The geology of fluvial deposits: Springer-verlag, Berlin, 582p.
Middleton G V, 1973． Johannes Walther's Law of the Correlation of Facies: Geol. Soc. America Bull., v. 84, p.979-988．
Middleton G V, 1978． Facies, in Fail-bridge R W and J Bourgeois(eds.), Encyclopedia of sedimentology: Dowden, Hutchinson and Ross, Stroudsburg, PA, p. 323-325．
Mutti, E., 1985． Turbidite systems and their relations to depositional sequences, in Zuffa, G. G. (ed.). Provenance of arenites: D. Riedel, Dordrecht, p. 65-93
Nummedal, D., O. H. Pilkey, and J. D. Howard (eds.), 1987． Sea-level tluctuation and coastal evolution: Soc. Econ. Paleontologists and Mineralogists Spec. Pub. 41,267 p.
Payton. C. E. (ed.), 1977． Seismic stratigraphy-Applications to hydrocarbon exploration: Am. Assoc. Petroleum Geologists Memoir 26, Tulsa, OK, 516 p.
Peper T, Beeknan F, Cloetingh S. 1992． Consequences of thrusting and intraplate stress fluctuations for vertical motions in foreland basins and peripheral areas. Geophysical Journal International, 111: 104-126
Perlmutter M A., Matthews M D, 1989． Global Cyclostratigrahy-A Model. In: Cross T. A. (ed.), Quantitative Dynamic Stratigraphy. Prentice Hail, p.233-260
Perrodon A. 1980． Geodynamique petroliere . Cenese et repartition desgisements d' hydrocarbures: Paris, Masson-Elf Aquitaine, 381．
Posamentier H W, Vail P R. 1988． Eustatic controls on clastic deposition II-Seqence and system stract models. In: Wilgus C K, Hastings B S, Kendall C G St C. et al., ed. Sea level changes: an intergrated approach. Soc. Econ Paleontol. Mineral spec, publ., 42: 109-124．
Posamentier, H. W., C. P. Summerhayes, B. U. Haq, and G. P. Allen (eds.), 1993． Sequence stratigraphy and factes associations: International Association Sedimentoiogists Spec. Pub. 18, Blackwell Scientific Publications, Oxford, 644 p.
Posamentier, H. W. 1993． Variability of the Sequence Stratigraphic Model: Effects of Local Basin Factors. Sedimentary Geology, 86: 91-109
Posamentier, H. W., Allen G P., James D.P. et al., 1992, Forced regressions in a sequence Stratigraphic framenwork: concepts, examples and exploration significance. AAPG Bulletin v. 76, p. 1687-1709
Posamentier H. W et al. 1992． High Resolution Sequence Stratigraphy-the East Coulee Delta Alberta. Journal of Sedimentary Petrology, 62 (2) : 310-317
Posamentier H.W et al . 1993． Siliciclastic Sequence Stratigraphy and petroleum Geology-Where to From Here ?. AAPG Bulletin. 77(5) : 731-742．
Revelle. R. R. (ed.), 1990． Sea level change: National Research Council Studies in Geophysics. National Academy Press, Washington, D. C., 234 p.
Rittenhause G.1972． Stratigraphic trap classification. In: King R E, ed. Stratigraphic oil and gas fields-classification, exploration methods, and case histories. AAPG Memoir, 16 : 14-28
Schreiber, B. C. (ed.), 1988． Evaporites and hydrocarbons : Columbia University Press, New York, 475 p.
Sangree, J. B., Vail, P. R. & Mitchum, R. M., 1991． Summary of exploration applications of sequence stratigraphy. In : Sequence Stratigraphy as an Explo ration Tool : concepts and Practices from the Gulf Coast (ed. By J. M. Armentrout & B. F. Perkins). Eleventh Annual Research Conference Gulf Coast Section. Society of Economic Paleontologists and Mineralogists, pp. 321-327
Sam Boggs J. 2001． Principles of sedimendology and stratigraphy, 3thd ed.: Prentice Hall, Upper Saddle River, New Jersey, 215-217,442-448
Shanley K W, McCabe P J. 1994． Perspective on the Sequence stratigraphy of continental strata.AAPG Bulletin, 78(4) : 544-568
Sonnenfeld P and Kendall G C St C. 1989． Marine evaporates: genesis, alteration, and associated deposits: Penrose Conference Report, Geology, 17: 573-574
Strecke Uwe, Stridtmarm J R., Smithson. 1999． A conceptual tectonostratigraphic model for seismic fades migration in a fluvio-lacustrine extensional basion. AAPG Bulletin, 83(1) : 43-61
Swift D J P, Phillips S. Thorne J A. 1991． Sedimentation on continental margins. V: parasequence. In: Swift D J P, et al. eds. Shelf sand and sandstone bodies: geometry, facies and sequence stratigraphy. International Association of Sedimentologists, Special Publication 12: 153-187
Tung-yilee, Lawrence A. 1995． Lawver Cenozoic plate reconstruction of Southeast Asia. Tectonics, 251:85-138
Ulmishek G 1986． Stratigraphic aspects of petroleum resource assessment.ln: Rice D D, ed. Oil and gas assessment-metheds and applications. AAPG Studies in Geology, 21:59-68．
Magoon L B. 1987． The petroleum system-a classification scheme for research, resource assessment, and exploration (abs). AAPG Bull,71 (5) :587．
Vail P R et al. 1977． Seismic stratigraphy and global changes of sea level. Seismic stratigraphy-Applications to Hydrocarbon Exploration. AAPG, 26(2) : 199-206
Vail P R. et al., 1991． The Stratigraphic Signatures of Tectonics, Eustasy and Sedimentology-an Overview, Cycles and Events in Stratigraphy. Berlin Heidlberg: Springer-Verlag. 167-695
Van Wagoner J.C., 1985． Reservoir facies distribution as controlled by sea-level change: Abstract and Poster Session, Society of Economic Paleontologists and Mineralologisls Mid-year Meeting, Golden, Colorado, P. 91-92
Van Wagoner, et al. 1990． Silicistic Sequence stratigraphy in well logs, cores, and outcrops: Concept for high-resolution correlation of time and facies. AAPG Methods in Exploration series No.7,55:1-57
Van Wagoner J.C. 1995． Sequence stratigraphy and marine to nonmarine facies architecture of forland basin strata. AAPG Memoir, 64: 137-223
Van Wagoner, J. C., R. M. Mitchum, K.M. Campion, and V.D. Rahmanian, 1990． Siliciclastic sequence stratigraphy in well logs, cores, and outcrops: Concepts for high-resolution correlation of time and facies: AAPG Methods in Exploration Series, No. 7, Am. Assoc. petroleum Geologists, Tula, OK, 55 p.
Vincent, S. J., D. M. Macdonald, and P. Gutteridge, 1998, Sequence stratigraphy, in Doyle, P. and M. R. Bennett (eds.), Unlocking the stratigraphical record: Advances in modern stratigraphy: John Wiley & Sons, Ltd., Chichester, p. 299-350
Walker, R. G., 1990． Facies modeling and sequence stratigraphy: Jour. Sedimentary Petrology, v. 60, p. 777-786
Walker, R. G, and N. P. James (eds.), 1992． Facies models Response to sea level change: Geol. Assoc. Canada, 409 p.
Warren, J. K., 1989． Evaporite sedimentology : Prentice Hall, Englewood Cliffs, N. J., 285 p.
Warren, J., 1999． Evaporites : Blackwell Science Ltd., 438 P.
Weimer. P., and H. Posamentier (eds.), 1993． Siliciclastic sequence stratigraphy: Recent developments and applications: Am. Assoc. petroleum Geologists Memoir 58． Tulsa, OK, 492 p.
Wheeler H E. 1964． Base level, lithosphere surface and time-stratigraphy. Bull Geol Soc. 75: 599-610
Wilgus, C. K., B. S. Hastings, C. G. St. C. Kendall. H. W. Posamentier, C. A. Rosss, and J. C. Van Wagoner (eds.), 1989． Sea-level changes: An integrated approach: Socity of Economic Paleontologists and Mineralogists Spec. Pub.42, Tulsa. OK, 407 p
Wilson, R. C. L. ,1991, Sequence stratigraphy: An introduction: Geoscientist, v. 1, p. 13-23
C．k．威尔格斯等编．徐怀大，魏魁生，洪卫东，等译．1993．层序地层学原理(海平面变化综合分析)．北京：石油工业出版社，526p．
Cross T．A 著，杜宁平 译．1996．据高分辨率层序地层学认识地层结构对比概念体积配分相分异和储层的间隔单元划分．国外油气勘探，8(3)：285-294
陈发亮，朱晖，李绪涛，等．2000．东濮凹陷下第三系沙河街组层序地层划分及盐岩成因探讨．沉积学报，18(3)：386-388
陈发景．1983．中国中新生代盆地构造与演化．北京：科学出版社，78-83
池英柳，张万选，张厚福，等．1996．陆相断陷盆地层序成因初探．石油学报，17(5)：19-26
池秋鄂，龚福华．2001．层序地层学基础及应用．北京：石油工业出版社，229p．
蔡雄飞．1994．古气候是盆地分析不可缺少的因素．岩相古地理，14(2)：42-46
邓宏文．1995．美国层序地层研究中的新学派—高分辨率层序地层学．石油天然气地质，16(2)：90-97
邓宏文，王红亮，宁宁．2000．沉积物体积分配原理—高分辨率层序地层学的理论基础．地学前缘，7(4)：305-313
邓宏文，王洪亮，翟爱军，等．1999．中国陆源碎屑盆地层序地层与储层展布．石油与天然气地质，20(2)：108-114
邓宏文，王洪亮，李熙韶．1996．层序地层基准面的识别、对比技术及应用．石油与天然气地质，17(3)：177-184
邓宏文，王洪亮，祝永军，等．2002．高分辨率层序地层学—原理及应用．北京：地质出版社，178p．
樊太亮，郭齐军，吴贤顺．1999．鄂尔多斯盆地北部上古生界层序地层特征与储层发育规律．现代地质，13(1)：32-36
樊太亮，吕建仓，丁明华．2000．层序地层体制中的陆相储层发育规律．地学前缘，7(4)：315-321
樊太亮，李卫东．1999．层序地层应用于陆相油藏预测的成功实例．石油学报，20(2)：12-17
樊太亮．1997．沉积基准面变化分析技术及应用．石油与天然气地质，18(2)：120-127
冯有良，李思田．2001．东营凹陷沙河街组三段层序低位域砂体沉积特征．地质论评，47(3)：278-286
冯有良，李思田，解习农．2000．陆相断陷盆地层序形成动力学及层序地层模式．地学前缘，7(3)：119-131
顾家裕．1986．东濮凹陷形成环境．石油实验地质，8(1)：22-28
顾家裕．1995．陆相盆地层序地层格架概念及模式．石油勘探与开发，22(4)：6-10
顾家裕．1984．中国东部古代扇—三角洲沉积．石油与天然气地质，5(3)：236-244
郭建华，宫少波，吴东胜．1998．陆相断陷湖盆T-R旋回沉积层序与研究实例．沉积学报，16(1)：8-14
郭建华，郭成贤，翟永红，等．1996．东濮凹陷前梨园地区Es_3~4-Es_3~3亚段沉积旋回与沉积体系．石油实验地质，18(4)：377-384
侯读杰，王铁冠，张一伟，等．1997．中国东部第三系的陆相沉积中的甲藻甾烷：海侵指相的标志物?地质论评，43(5)：524-528
何承全，朱神照，靳广兴，等，1989．东濮地区早第三纪沟鞭藻及其它的藻类．北京：石油工业出版社．15-21
郝诒纯，李蕙生．1984．渤海沿岸地区及邻近地区第三纪钙质超微化石地发现．科学通报，29(12)：741-745
胡受权，郭文平．2001．论陆相层序地层学理论体系及其研究思路．断块油气田，8(5)：1-7．
胡受权，颜其彬，张永贵．1999．断陷湖盆陡坡带陆相层序体系域与油气藏成藏类型．石油勘探与开发，26(1)：13-17
姜在兴，赵澄林，刘孟慧．1990．东濮凹陷西部湖相风暴沉积的初步研究．沉积学报，8(1)：107-113
姜在兴，李华启．1996．层序地层学原理及应用．北京：石油工业出版社，162p．
金强，黄醒汉．1985．东濮凹陷早第三纪盐湖成因探讨．华东石油学院学报，(1)：1-13
纪友亮，张世奇．1996．陆相断陷湖盆层序地层学．北京：石油工业出版社，127p．
刘立，胡春燕．1991．砂岩中主要碎屑成分的物源意义．岩相古地理，(6)：48-53
刘明义．1984．东濮凹陷油气聚集模式．石油学报，5(4)：19-25
刘星利．1987．渤海地区构造展布特征与油气分析．石油与天然气地质，8(1)：45-55
刘池洋．1990．从渤海湾盆地的地壳厚度变化论地壳双层差异扩张原理．见：赵重远，刘池洋著．华北克拉通沉积盆地形成与演化及其油气赋存．西安：西北大学出版社，43-53
刘招君，董清水，王嗣敏，等．2000．陆相层序地层学导论与应用．北京：石油工业出版社，253p．
李守军．1998．渤海湾盆地早第三纪水平面升降和全球海平面升降的不一致性．地质论评，44(1)：31-34
李德生．1979．渤海湾含油气盆地的构造格局．石油勘探与开发，6(2)：1-10
李德生，薛叔浩．1983．中国东部中新生代盆地与油气分布．地质学报，57(3)：224-234
李任伟．1988．高盐环境和生油．中国科学，3期：303-313
李任伟，辛茂安．1989．东濮盆地蒸发岩的成因．沉积学报，7(4)：141-148
李思田，杨士恭．1992．论沉积盆地的等时地层和基本建造单元，沉积学报，10(4)：11-22
李思田，潘元林，陆永潮，等．2002．断陷湖盆隐蔽油藏预测及勘探的关键技术--高精度地震探测基础上的层序地层学研究．地球科学—中国地质大学学报．27(5)：592-598
李思田，林畅松，解习农，等．1995．大型陆相盆地层序地层学研究---以鄂尔多斯中生代盆地为例．地学前缘，2(3-4)：133-136
李思田．1996．含能源盆地沉积体系—中国内陆和近海主要沉积体系类型的典型分析，武汉：中国地质大学出版社，117-137
李文厚，屈红军，魏红红，等．2003．内蒙古苏里格庙地区晚古生代层序地层学研究．地层学杂志，27(1)：41-44
李文厚．1997．吐-哈盆地台北凹陷侏罗系层序地层学研究．石油与天然气地质，18(3)：210-215
李文厚．1997．苏红图-银根盆地下白垩统层序地层学研究．沉积学报，15(3)：18-22
林又玲，吴贤涛，潘结南，等．2000．东濮凹陷老第三系沙河街组盐类沉积模式新见．古地理学报；2(4)：66-75
林畅松，刘景彦，张燕梅．1988．沉积盆地动力学与模拟研究．地学前缘，5：119-125
林畅松，张燕梅，刘景彦，等．2000．高精度层序地层学和储层预测．地学前缘，7(3)：
111-117
林畅松，潘元林，肖建新，等．2000．“构造坡折带”---断陷盆地层序分析和油气预测的重要概念．地球科学—中国地质大学学报，25(3)：260-265
林舸．1991．东濮凹陷及邻区卫星影像特征及其地质意义．北京：石油工业出版社．12-45
蔺殿忠．1984．渤海湾盆地断块体扭转翘倾及其形成机制的探讨．石油勘探与开发，3期：26-31
陆荣生，赵春元，陈树文，等．1993．中国石油地质志(卷7，中原油田)．北京：石油工业出版社，7-70
马新华，华爱刚，李景明，等．2000．含盐油气盆地．北京：石油工业出版社，1-4
马杏垣，刘和甫，王维襄．1983．中东部中新代裂陷作用和伸展构造．地质学报，57(1)：22-31
梅志超．1993．层序地层学．西安：西北大学出版社，99p
彭立才，杨平，濮人龙．1999．陆相咸化湖泊沉积硫酸岩盐硫同位素组成及其地质意义[J]．矿物岩石地球化学通报，18(2)：99-102
齐兴宇．1988．东濮凹陷油气藏类型及分布．石油学报，9(2)：28-36
齐兴宇，黄先雄，寿建峰，等．1992．东濮凹陷盐岩与油气．石油学报，13(1)：23-29
漆家福，张一伟，陆克政，等．1995．渤海湾新生代裂陷盆地的伸展构造模式及其构造动力学过程．石油实验地质，17(4)：316-323
强祖基，张立人．1983．中国第四纪活动断裂分区与地震活动性．地质学报，57(4)：358-368
屈红军，李文厚，何希鹏，等．2003．六盘山盆地下白垩统沉积层序与含油气系统．西北大学学报(自然科学版)，33(1)：70-73
屈红军，李文厚，苗建宇，等．2003．东濮凹陷濮卫洼陷盐岩发育规律及其成因探讨．中国地质，已录用(待刊)
任来义，林桂芳，赵志清，等．2000．东濮凹陷早第三系的海侵事件．古生物学报，39(4)：553-557
任来义．2001．东濮凹陷下第三系生物地层及隐蔽油气藏勘探研究．西安：西北大学硕士学位论文，80p
孙镇城，杨藩，张技焕，等．1997．中国中新生代咸化湖泊沉积环境与油气生成．北京：石油工业出版社，142-149
童崇光．1980．中国东部裂谷系统的地质特征．石油学报，1(4)：19-26
覃建雄，陈洪德，田景春．2001．层序地层作为沉积盆地识别标志的研究．古地理学报，3(2)：72-81
唐祥华．1986．东濮凹陷渐新世早期成盐环境及古生态的探讨．微体古生物学报，3(1)：51-58
吴贤涛，林又玲，等．1999．东濮凹陷沙河街组痕迹相及其对应的测井图型．古地理学报，1(3)：50-64
吴贤涛，张庆智，张国成，等．1999．东濮凹陷北部下第三系沙四段沉积期海水入侵前后生物痕迹特征及其意义．见：沉积学及岩相古地理学新进展．北京：石油工业出版社．1995，273-277
吴因业，顾家裕，2000．油气层序地层学．北京：石油工业出版社，470p．
王鸿桢，史晓颖．1998．沉积层序及海平面旋回的分类级别—旋回周期的成因讨论．现代地质，12(1)：1-16
王鸿祯，史晓颖，王训练，等，2000．中国层序地层研究．广州：广东科技出版社，
434p．
王红亮，邓宏文．2000．东濮凹陷濮卫环洼带层序划分与沉积体系，古地理学报，2(1)：49-53
王涛．1997．中国东部裂谷盆地油气藏地质．北京：石油工业出版社，1-53
王新运，辛茂安，1989．东濮凹陷油气藏形成条件及油气富集规律．石油与天燃气地质，10(4)：407-417
王德仁，焦大庆，任来义，等．1998．东濮凹陷与盐岩有关的岩性油气藏特征．见：潘元林，孔凡仙，杨申镳，等主编．中国隐蔽油气藏．北京：地质出版社，57-66
王东坡，刘立．1994．大陆裂谷盆地层序地层学的研究．岩相古地理，14(3)：1-9
魏魁生，徐怀大．1993．冀中地区早第三纪海泛特征及其层序地层学意义．现代地质，7(3)：274-283
魏魁生，徐怀大．1993．华北典型箕状断陷盆地层序地层学模式及其与油气的赋集．地球科学，18(2)：139-149
魏魁生，徐怀大，王淑芬．1997．松辽盆地白垩系高分辨率层序地层格架．石油与天然气地质，18(1)：7-13
汪时成，周庆凡．2000．含油气系统概念的由来及内涵．石油与天然气地质，21(3)：279-282．
许靖华．1985．地中海盐度突变地历史．见何起祥等译：大地构造与沉积作用．北京：地质出版社，382-410
徐强，姜烨，董伟良，等．2003．中国层序地层研究现状和发展方向．21(1)：155-167
徐怀大．1997．陆相地层研究中的某些问题．石油与天然气地质，18(2)：83-88
薛良清．2000．成因层序地层学的回顾与展望．沉积学报，18(3)：484-488
薛良清．1995．层序地层学研究现状、方法与前景，石油勘探与开发，22(5)：8-13
薛良清．1990．层序地层学在湖相盆地中的应用探讨，石油勘探与开发，17(6)：29-34，40
解习农，程守田，陆永潮．1996．陆相盆地幕式构造旋回与层序构造．地球科学—中国地质大学学报，21(1)：27-33
杨香华，陈开远，石万忠，等．2002．东濮凹陷盐湖层序结构与隐藏油气藏．石油与天然气地质，23(2)：139-142
姚益民，梁鸿德，蔡治国，等．1994．中国油气区第三系(Ⅳ)—渤海湾盆地油气区分册．北京：石油工业出版社，240p．
尹太举．2002．高分辨率层序地层学及其在濮城油田开发中的应用．北京：中国地质大学博士学位论文，134p
阎敦实，王尚文，唐智．1980．渤海湾含油气盆地断块活动与古潜山油气田的形成．石油学报，1(2)：1-9
岳文浙，丁保良，魏乃颐．2000．陆盆层序地层研究的思路．地质论评，46(4)：347-354
郑荣才，吴朝容，叶茂才．2000．浅谈陆相盆地高分辨率层序地层研究思路．成都理工学院学报，27(3)：241-244
郑荣才，吴朝容．1999．西部凹陷深层沙河街组生储盖组合的层序分析．成都理工学院学报，26(4)：348-356
郑荣才，尹世民，彭军．2000．基准面旋回结构与叠加样式的沉积动力学分析．沉积学报，18(3)：369-375
郑鸿稳．2002．东濮凹陷下第三系层序地层模式．石油学报，23<4)：24-28
郑浚茂，王德发．1984．东濮断陷盐湖盆地下第三系砂岩体类型及沉积模式．沉积学报，2(2)：17-28
张建军，李治，刘贤武．1998．东濮凹陷沙河街组盐岩成因研究．断块油气田．5(5)：18-22
张永才．1992．东濮凹陷早第三纪含盐地层．石油学报，13(2)：232-239
张世奇，纪友亮．1996．陆相断陷湖盆层序地层学模式探讨．石油勘探与开发，23(5)：20-23
张文昭．1997．中国陆相大油田．北京：石油工业出版社，216-233，702-742
张功成，蔡希源，周章保，等．1996．裂陷盆地分析原理和方法—以松辽盆地为例．北京：石油工业出版社，293p．
张洪安，李继东．2003．白庙构造油气成藏特征．石油与天然气地质，24(1)：45-49
赵重远，刘池洋．1990．华北克拉通沉积盆地形成与演化及其油气赋存．西安：西北大学出版社，1-74
赵良金，张子贤．1997．濮城西沙二气顶油藏．北京：石油工业出版社，191p．
赵政璋．2000．储层预测技术及应用实例．石油工业出版社，P．95-147
赵澄林，刘孟慧．1988．湖相沉积中的同生变形构造及其地质意义．岩石学报，4(4)：14-21
赵澄林，刘孟慧．1984．湖底扇相模式及其在油气预测中应用．华东石油学院学报，4期：1-11
赵澄林，刘孟慧，纪友亮．1992．东濮凹陷下第三系碎屑岩沉积体系与成岩作用．北京：石油工业出版社，1-55
赵澄林，刘孟慧，姜在兴，等．1991．渤海湾早第三纪断陷盆地含油气岩系沉积学及沉积相的基本特征．石油学报，12(2)：8-32
赵澄林，姜在兴，刘孟慧．1989．东濮凹陷西部下第三系的遗迹相．石油大学学报，13(1)：1-8
赵志清，吕红玉．1988．东濮凹陷晚始新世生物群及其古环境探讨．微体古生物学报，5(3)：315-322
朱夏．1965．我国陆相中新生界含油气盆地的大地构造特征及有关大地构造问题．北京：科学出版社，10-15
朱夏，陈焕疆，孙肇才，等．1983．中国新生代构造与含油气盆地．地质学报，57(3)：235-241
朱浩然．1979．山东滨县下第三系沙河街组的藻类化石．古生物学报，18(4)：327-340
朱家蔚，辛茂安，许化政．1991．东濮凹陷油气生成特征．见：中原石油勘探局．东濮凹陷油气生成地球化学特征．北京：石油工业出版社，1-48
朱筱敏．1998．层序地层学原理及应用．北京：石油工业出版社，106p．
曾允孚，覃建雄．1999．沉积学发展现状与前瞻．成都理工学院学报，26(1)：1-7
钟筱春，钟石兰，费轩冬，等．1988．渤海湾盆地沙河街组一段颗石藻化石及其沉积环境．微体古生物学报，5(2)：145-151
周章保，陶国强，汪新文．2000．东濮凹陷变换构造初析．断块油气田，7(增刊)：3-6
甄维胜，吕新华，胡望水，等．2001．复杂断块油田非均质油藏精细描述．北京：石油工业出版社，159p．
中原石油勘探局．1991．东濮凹陷油气生成地球化学研究-北京：石油工业出版社，181p．
中原石油勘探局勘探开发研究院，中科院南京地质古生物研究所．1989．东濮地区早第三纪介形类．北京：石油工业出版社，72p．
Allen, P. A.,and J. R. Allen, 1990． Basin analysis principles and applications. Blackwell Scientific Pub. Oxford, 451 p.
Anstey N A, 1982． Simple seismics: International Human Resources Development Corporation, Boston, 168p.
Bahorich M and Farmer S. 1995． The coherence cube. The Leading Edge, P. 1053-1058
Busson, G, and Schreiber, B. C. (eds.), 1997． Sedimentary deposition in rift and foreland basins in France and Spain : Columbia University Press, New York, 479 p.
Biddle K T, Wielchowshy C C. 1994． Hydrocarbon traps. In: Magoon L B, Dow W G, eds. The petroleum system-from source to trap. AAPG Memoir, 60 :219-235
Brown L F Jr, Benson J M, Brink G J, et al. 1995． Sequence stratigraphy in Offshore South African divergent basin. AAPG Studies in Geology, 41:1-184
Carter, R. M., T. R. Nash, M. Ito, and B. J. Pillans (eds.), 1998． Sequence stratigraphy in the Plio-Pleistocene: An evaluation: Sedimentary Geology, v. 122, 288 p. [Special Issue]
Christie-Bilker K, G S. Mountain, and K. G Miller, 1990, Seismic stratigraphic record of sea-level change, in Revelle, R. R. et al. (eds.). Sea level change, National Research Council Studies in Geophysics, National Academy Press, Washington, D. C., p. 116-140
Cloetingh S C. 1986． Intraplate stresses: a new tectonic mechanism for fluctuations of relative sea level. Geology, 14:617-620
Cross T A. 1994, Genetic Stratigraphy Research Group Colorado School of Mines Annual Report on Research Projects and Industry Collagborations. 1-28
Cross T A. 1994． High-resolution stratigraphic correlation from the perspective of base-level cycles and sediment accommodation. In: Proceedings of Northwestern Europian Sequence Stratigraphy Congress, 105-123
Cross, T.A., and Lessenger, M.A., 1998． Sediment volume partitioning: rational for stratigraphic model evaluation and high-resolution stratigraphic correlation, in F.M. Gradstein. K.O. Sandvik, and N.J. Milton, eds., Sequence Stratigraphy
Demaison G. 1984． The generative basin concept In: Denmaison G. Murris R J. eds. Petroleum geochemistry and basin evaluation. AAPG Memoir,35: 1-14
Dickinson, R. W., et al., 1983． Provenance of North American Phancrozoic sandstones in relation to tectonic setting: Geol. Soc. America Bull., V. 94, p. 223
Emery, D., and K. J. Meyers (eds.), 1996． Sequence stratigraphy: Blackwell Science Ltd., Oxford, 297 p.
Eschard R, Lemouzy P, Bacchiuna, et al. 1998． Combining sequence stratigraphy, geostatistical simulations and production data for modeling a fluvial reservoir in the chauchoy field (Triassic, France). AAPG Bulletin, 82(4) : 545-568
Galloway W E. 1989a. Genetic stratigraphic sequences in basin analysis I : architecture and genesis of flooding-surface bounded depositional units. AAPG Bulletin, 73: 125-142
Galloway W E. 1989b.Genetic stratigraphic sequences in basin analysis II: application to northwest Gulf of Mexico Cenozoic basin. AAPG Bulletin, 73: 143-154
Galloway W E. 1998． Geologic Column-Clastic Depositional Systems and Sequences: Applications to Reservoir Prediction, Delineation, and Characterizatoion. The Leading Edge, 17(2) , 173-176,178-180
Hallam, 1992． Phanerozoic sea-level changes: Columbia University Press, New York, 266 p.
Hallam, A., 1998, Interpreting sea level, in Doyle, P. and M.R. Bennett (eds.). Unlocking the stratigraphyical record: Advances in modern stratigraphy: John Wiley & Sons, Ltd., Chichester, p.
421-439
Halbouty M T. 1982． The deliberate search for the subtle trap. AAPG Memior, 32 : 351
Haq, B. U. (ed.), 1995． Sequence stratigraphy and depositional response to eustatic, tectonic and climatic forcing: Kluwer Academic Publishers, Dordrecht, 381 p.
Haq.B U, Hardenbol J, Vail P R. 1988． Mesozoic and Cenozoic chronostratigraphy and cycles of sea level change. In: Wilgus C K, et al. eds. Sea level changes: an integrated approach. SEPM, Special Publication 42:71-108
Holser W. 1979． Trace elements and isotopes in evaporites. Mineralogical society of erica short course notes, 6: 295-346
Johnson, Klapper J G, Sandberg C A. 1995, Devonian eustatic fluctuations in euramerica. Gololgical Society of America Bulletin, 79(5) : 567-587
Kendall AC. 1979． Subaqueous evaporates. In: Walker G G (ed.), Facies models: Geoscience Canada Reorent Ser. 1,170
Kendall A C. 1992． Evaporates. In: Walker R G, and James N P (ed.), Facies models-Response to sea level change: Geol. Assoc, Canada, 375-409
Levorsen A I. 1967． Geology of petroleum. 2nd ed. San Francisco : Freeman W H and Co, 724
Lin C S, Eriksson K, Li S T, et al. 2000． Sequence architecture , depositional systems, and controls on development of lacustrine basin fills in part of the Erlian basin, Northeast China. AAPG Bulletin, 85(11) : 2017-2043
Loutit T S, Hardenbol J, Vail P R, Baum G R. 1988． Condensed sections: the key to age determination and correlation of continental margin sequences. In: Wilgus C K, Hastings B S, Kendall C G St C. et al., ed. Sea level changes:an intergrated approach. Soc. Econ Paleontol. Mineral spec, publ., 42:183-213．
Lu Yongchao, Xie Xinong, Jiao Yangquan, et al. 1997． Depositional responding to tectonic evolution of East China Sea. shelf basin. Journal of China University of Geosciences, 8(1) : 56-61
MacDonald, D. I. M., 1991． Sedimentation, tectonics and eustasy: Sea-level changes at active margins: Internal. Assoc. Sedimentologists Spec. Pub. 12, Blackwell, Oxford, 518 p.
Magoon L B, Dow W G 1994． The petroleum system. In: Magoon L B, Dow W G. The petroleum system-from source to trap.AAPG Memoir,60:3-22．
Marfurt K J and R. L Kirlin, 1998． 3-D Seismic attributes using a semblance-based coherency algorithm, Geophysics, Vol.63, No.4, P.1150-1165
Marfurt K J and V Sudhaker, 1999． Coherency calculations in the presence of structural dip, Geophysics, Vol. 64, No. 1, P. 104-111
Meissner F F. 1984． Petroleum geology of the Bakken Formation., Williston basin, North Dakota and Montana. In: Demaison G, Murris R J,eds. Petroleum geochemistry and basin evaluation. AAPG Memoir, 35:159-179
Melvin J. L. (ed.), 1991． Evaporites, petroleum, and mineral resources: Elsevier, Amsterdam, 556 p.
Miall AD. 1991． Stratigraphic sequences and their chronostratigraphic correlation. Journal of Sedimentary Petrology, 61:497-506
Miall, A. D., 1992． Alluuvial deposits, in Walker, R.G and N. P. James (eds.), Facies models: Response to sea level changes, Geol. Assoc. Canada, p. 119-142
Miall, A. D., 1994, Sequence stratigraphy and chronostratigaphy: problems of definition and precision in correlation, and their implication for global eustasy: Geoscience Canada, v. 21, p. 1-26
Miall, A. D., 1997． The geology of Stratigraphic sequences: Springer-Verlag, Berlin, 433 p.
Miall, A. D., 1990． Principles of sedimentary basin analysis, 2 nd ed.: Springer-Verlag, New York, 668 p.
Miall, A. D., 1991． Exxon global cycle chart: An event for every occasion ? Geology, v, 20, p. 790-797
Miall, A. D., 1996． The geology of fluvial deposits: Springer-verlag, Berlin, 582p.
Middleton G V, 1973． Johannes Walther's Law of the Correlation of Facies: Geol. Soc. America Bull., v. 84, p.979-988．
Middleton G V, 1978． Facies, in Fail-bridge R W and J Bourgeois(eds.), Encyclopedia of sedimentology: Dowden, Hutchinson and Ross, Stroudsburg, PA, p. 323-325．
Mutti, E., 1985． Turbidite systems and their relations to depositional sequences, in Zuffa, G. G. (ed.). Provenance of arenites: D. Riedel, Dordrecht, p. 65-93
Nummedal, D., O. H. Pilkey, and J. D. Howard (eds.), 1987． Sea-level tluctuation and coastal evolution: Soc. Econ. Paleontologists and Mineralogists Spec. Pub. 41,267 p.
Payton. C. E. (ed.), 1977． Seismic stratigraphy-Applications to hydrocarbon exploration: Am. Assoc. Petroleum Geologists Memoir 26, Tulsa, OK, 516 p.
Peper T, Beeknan F, Cloetingh S. 1992． Consequences of thrusting and intraplate stress fluctuations for vertical motions in foreland basins and peripheral areas. Geophysical Journal International, 111: 104-126
Perlmutter M A., Matthews M D, 1989． Global Cyclostratigrahy-A Model. In: Cross T. A. (ed.), Quantitative Dynamic Stratigraphy. Prentice Hail, p.233-260
Perrodon A. 1980． Geodynamique petroliere . Cenese et repartition desgisements d' hydrocarbures: Paris, Masson-Elf Aquitaine, 381．
Posamentier H W, Vail P R. 1988． Eustatic controls on clastic deposition II-Seqence and system stract models. In: Wilgus C K, Hastings B S, Kendall C G St C. et al., ed. Sea level changes: an intergrated approach. Soc. Econ Paleontol. Mineral spec, publ., 42: 109-124．
Posamentier, H. W., C. P. Summerhayes, B. U. Haq, and G. P. Allen (eds.), 1993． Sequence stratigraphy and factes associations: International Association Sedimentoiogists Spec. Pub. 18, Blackwell Scientific Publications, Oxford, 644 p.
Posamentier, H. W. 1993． Variability of the Sequence Stratigraphic Model: Effects of Local Basin Factors. Sedimentary Geology, 86: 91-109
Posamentier, H. W., Allen G P., James D.P. et al., 1992, Forced regressions in a sequence Stratigraphic framenwork: concepts, examples and exploration significance. AAPG Bulletin v. 76, p. 1687-1709
Posamentier H. W et al. 1992． High Resolution Sequence Stratigraphy-the East Coulee Delta Alberta. Journal of Sedimentary Petrology, 62 (2) : 310-317
Posamentier H.W et al . 1993． Siliciclastic Sequence Stratigraphy and petroleum Geology-Where to From Here ?. AAPG Bulletin. 77(5) : 731-742．
Revelle. R. R. (ed.), 1990． Sea level change: National Research Council Studies in Geophysics. National Academy Press, Washington, D. C., 234 p.
Rittenhause G.1972． Stratigraphic trap classification. In: King R E, ed. Stratigraphic oil and gas fields-classification, exploration methods, and case histories. AAPG Memoir, 16 : 14-28
Schreiber, B. C. (ed.), 1988． Evaporites and hydrocarbons : Columbia University Press, New York, 475 p.
Sangree, J. B., Vail, P. R. & Mitchum, R. M., 1991． Summary of exploration applications of sequence stratigraphy. In : Sequence Stratigraphy as an Explo ration Tool : concepts and Practices from the Gulf Coast (ed. By J. M. Armentrout & B. F. Perkins). Eleventh Annual Research Conference Gulf Coast Section. Society of Economic Paleontologists and Mineralogists, pp. 321-327
Sam Boggs J. 2001． Principles of sedimendology and stratigraphy, 3thd ed.: Prentice Hall, Upper Saddle River, New Jersey, 215-217,442-448
Shanley K W, McCabe P J. 1994． Perspective on the Sequence stratigraphy of continental strata.AAPG Bulletin, 78(4) : 544-568
Sonnenfeld P and Kendall G C St C. 1989． Marine evaporates: genesis, alteration, and associated deposits: Penrose Conference Report, Geology, 17: 573-574
Strecke Uwe, Stridtmarm J R., Smithson. 1999． A conceptual tectonostratigraphic model for seismic fades migration in a fluvio-lacustrine extensional basion. AAPG Bulletin, 83(1) : 43-61
Swift D J P, Phillips S. Thorne J A. 1991． Sedimentation on continental margins. V: parasequence. In: Swift D J P, et al. eds. Shelf sand and sandstone bodies: geometry, facies and sequence stratigraphy. International Association of Sedimentologists, Special Publication 12: 153-187
Tung-yilee, Lawrence A. 1995． Lawver Cenozoic plate reconstruction of Southeast Asia. Tectonics, 251:85-138
Ulmishek G 1986． Stratigraphic aspects of petroleum resource assessment.ln: Rice D D, ed. Oil and gas assessment-metheds and applications. AAPG Studies in Geology, 21:59-68．
Magoon L B. 1987． The petroleum system-a classification scheme for research, resource assessment, and exploration (abs). AAPG Bull,71 (5) :587．
Vail P R et al. 1977． Seismic stratigraphy and global changes of sea level. Seismic stratigraphy-Applications to Hydrocarbon Exploration. AAPG, 26(2) : 199-206
Vail P R. et al., 1991． The Stratigraphic Signatures of Tectonics, Eustasy and Sedimentology-an Overview, Cycles and Events in Stratigraphy. Berlin Heidlberg: Springer-Verlag. 167-695
Van Wagoner J.C., 1985． Reservoir facies distribution as controlled by sea-level change: Abstract and Poster Session, Society of Economic Paleontologists and Mineralologisls Mid-year Meeting, Golden, Colorado, P. 91-92
Van Wagoner, et al. 1990． Silicistic Sequence stratigraphy in well logs, cores, and outcrops: Concept for high-resolution correlation of time and facies. AAPG Methods in Exploration series No.7,55:1-57
Van Wagoner J.C. 1995． Sequence stratigraphy and marine to nonmarine facies architecture of forland basin strata. AAPG Memoir, 64: 137-223
Van Wagoner, J. C., R. M. Mitchum, K.M. Campion, and V.D. Rahmanian, 1990． Siliciclastic sequence stratigraphy in well logs, cores, and outcrops: Concepts for high-resolution correlation of time and facies: AAPG Methods in Exploration Series, No. 7, Am. Assoc. petroleum Geologists, Tula, OK, 55 p.
Vincent, S. J., D. M. Macdonald, and P. Gutteridge, 1998, Sequence stratigraphy, in Doyle, P. and M. R. Bennett (eds.), Unlocking the stratigraphical record: Advances in modern stratigraphy: John Wiley & Sons, Ltd., Chichester, p. 299-350
Walker, R. G., 1990． Facies modeling and sequence stratigraphy: Jour. Sedimentary Petrology, v. 60, p. 777-786
Walker, R. G, and N. P. James (eds.), 1992． Facies models Response to sea level change: Geol. Assoc. Canada, 409 p.
Warren, J. K., 1989． Evaporite sedimentology : Prentice Hall, Englewood Cliffs, N. J., 285 p.
Warren, J., 1999． Evaporites : Blackwell Science Ltd., 438 P.
Weimer. P., and H. Posamentier (eds.), 1993． Siliciclastic sequence stratigraphy: Recent developments and applications: Am. Assoc. petroleum Geologists Memoir 58． Tulsa, OK, 492 p.
Wheeler H E. 1964． Base level, lithosphere surface and time-stratigraphy. Bull Geol Soc. 75: 599-610
Wilgus, C. K., B. S. Hastings, C. G. St. C. Kendall. H. W. Posamentier, C. A. Rosss, and J. C. Van Wagoner (eds.), 1989． Sea-level changes: An integrated approach: Socity of Economic Paleontologists and Mineralogists Spec. Pub.42, Tulsa. OK, 407 p
Wilson, R. C. L. ,1991, Sequence stratigraphy: An introduction: Geoscientist, v. 1, p. 13-23