冀中坳陷饶阳凹陷蠡县斜坡沙一下亚段地震沉积学
|
摘要
冀中坳陷饶阳凹陷蠡县斜坡因富含油气而备受关注,随着勘探程度的不断提高,岩性-地层油气藏成为蠡县斜坡增储上产的主要目标,明确砂体成因类型及其分布演化规律是油气高效勘探开发的关键。综合利用岩芯、测井和三维地震资料,开展了蠡县斜坡北段沙一下亚段地震沉积学研究。依据沙一下亚段顶、底界面T4和T42地震反射标志层以及内部T43地震反射标志层,将沙一下亚段划分为尾砂岩段和特殊岩性段。浅水三角洲成因的尾砂岩段可细分为浅水三角洲平原、浅水三角洲前缘(内前缘和外前缘)及前浅水三角洲等3种亚相类型;特殊岩性段以滩坝-湖泊沉积为特征,砂体类型主要为砂质碎屑岩滩坝,碳酸盐岩滩坝次之。尾砂岩段沉积时期,浅水三角洲体系在平面上表现出明显的分带性,浅水三角洲内前缘水下分流河道砂体分布范围广,最大推进距离达15km,是研究区的主力储层;从早到晚,伴随着湖平面逐步上升,西南部物源逐步占据主导地位,而北部物源影响范围减小。特殊岩性段沉积时期,湖平面迅速上升,浅水三角洲体系完全退出蠡县斜坡北段,沉积体系以滨浅湖—半深湖和滩坝沉积为特征,砂体类型主要为砂质碎屑岩滩坝,分布在研究区东部(面积约12km2),大多平行于湖岸线呈条带状展布。根据沉积学和地震沉积学研究,分别建立了研究区尾砂岩段和特殊岩性段时期的沉积模式,为下一步储层预测和油气勘探开发提供参考。
The Lixian slope of Raoyang sag in Jizhong depression has received numerous attentions because of its richness in oil and gas production.With the improvement of petroleum exploration and exploitation,the lithologic-stratigraphic reservoirs are becoming an important target forpetroleum promotion,and identifying the genetic types and distribution and evolution of sand bodies is the key of efficient petroleum exploration and exploitation.The seismic sedimentology of the lower part of the first member of Shahejie Formation in Lixian slope was studied based on core,well logging and three-dimensional seismic data.The study interval corresponds to a set of a fourth-order sequence,which is bounded by T4 and T42seismic markers,respectively,and the seismic marker of T43 is also identified internally;thus,the lower part of the first member of Shahejie Formation can be subdivided into the bottom sandstone section and the special lithologic section.The bottom sandstone section related to the shallow-water deltaic origin can be subdivided into three sub-facies types,including shallow-water delta plain,shallow-water delta front(inner front and outer front)and pro-shallow-water delta;the special lithologic section is characterized by lacustrine beach-bar deposits,and the types of the associated sand bodies are predominantly constituted by sandy clastic beach-bar,followed by carbonate beach-bar.During the sedimentary period of bottom sandstone section,the shallow-water delta system shows obvious zonation in plane,and the underwater distributary channel sandstones in the inner front of the shallow-water delta has a wide distribution range with a maximum transport distance of 15 km,which are proven good reservoirs in the study area;from early to late,with the lake level rising gradually,the sediments provided by the southwestern provenance gradually become predominant,while the supply from the northern provenance system shrinks.During the sedimentary period of special lithologic section,the lake level rises abruptly.Consequently,the shallow-water delta system almost withdraws from the study area,and the shallow lake to deep lake together with beach-bar deposits become dominated,and the main type of the associated sand bodies is sandy clastic beach-bar,which is located in the eastern part of the study area(the area is about 12km2)with paralleling to the lake shoreline in a strip geometry.Based on sedimentology and seismic sedimentology,the depositional models of the bottom sandstone section and the special lithologic section are established,which can provide potential references for reservoirs prediction and petroleum exploration and exploitation in the future.
The Lixian slope of Raoyang sag in Jizhong depression has received numerous attentions because of its richness in oil and gas production.With the improvement of petroleum exploration and exploitation,the lithologic-stratigraphic reservoirs are becoming an important target forpetroleum promotion,and identifying the genetic types and distribution and evolution of sand bodies is the key of efficient petroleum exploration and exploitation.The seismic sedimentology of the lower part of the first member of Shahejie Formation in Lixian slope was studied based on core,well logging and three-dimensional seismic data.The study interval corresponds to a set of a fourth-order sequence,which is bounded by T4 and T42seismic markers,respectively,and the seismic marker of T43 is also identified internally;thus,the lower part of the first member of Shahejie Formation can be subdivided into the bottom sandstone section and the special lithologic section.The bottom sandstone section related to the shallow-water deltaic origin can be subdivided into three sub-facies types,including shallow-water delta plain,shallow-water delta front(inner front and outer front)and pro-shallow-water delta;the special lithologic section is characterized by lacustrine beach-bar deposits,and the types of the associated sand bodies are predominantly constituted by sandy clastic beach-bar,followed by carbonate beach-bar.During the sedimentary period of bottom sandstone section,the shallow-water delta system shows obvious zonation in plane,and the underwater distributary channel sandstones in the inner front of the shallow-water delta has a wide distribution range with a maximum transport distance of 15 km,which are proven good reservoirs in the study area;from early to late,with the lake level rising gradually,the sediments provided by the southwestern provenance gradually become predominant,while the supply from the northern provenance system shrinks.During the sedimentary period of special lithologic section,the lake level rises abruptly.Consequently,the shallow-water delta system almost withdraws from the study area,and the shallow lake to deep lake together with beach-bar deposits become dominated,and the main type of the associated sand bodies is sandy clastic beach-bar,which is located in the eastern part of the study area(the area is about 12km2)with paralleling to the lake shoreline in a strip geometry.Based on sedimentology and seismic sedimentology,the depositional models of the bottom sandstone section and the special lithologic section are established,which can provide potential references for reservoirs prediction and petroleum exploration and exploitation in the future.
引文
[1]ZENG H L,HENRY S C,RIOLA J P.Stratal Sicing Part II:Real 3-D Seismic Data[J].Geophysics,1998,63(2):514-522.
[2]ZENG H L,HENTZ T F.High-frequency Sequence Stratigraphy from Seismic Sedimentology Applied to Miocene Vermilio Block 50Tiger Shoal Area Offshore Louisiana[J].AAPG Bulletin,2004,88(2):153-174.
[3]ZENG H L,BACKUS M M.Interpretive Advantages of 90°-phase Wavelets:Part I,Modeling[J].Geophysics,2005,70(3):7-15.
[4]ZHU X M,ZENG H L,LI S L,et al.Sedimentary Characteristics and Seismic Geomorphologic Responses of a Shallow-water Delta in the Qingshankou Formation from the Songliao Basin,China[J].Marine and Petroleum Geology,2017,79(4):131-148.
[5]董艳蕾,朱筱敏,曾洪流,等.歧南凹陷地震沉积学研究[J].中国石油大学学报(自然科学版),2008,32(4):7-12.DONG Yan-lei,ZHU Xiao-min,ZENG Hong-liu,et al.Study of Seismic Sedimentology in Qinan Sag[J].Journal of China University of Petroleum(Edition of Natural Science),2008,32(4):7-12.
[6]朱筱敏,董艳蕾,胡廷惠,等.精细层序地层格架与地震沉积学研究:以泌阳凹陷核桃园组为例[J].石油与天然气地质,2011,32(4):615-624.ZHU Xiao-min,DONG Yan-lei,HU Ting-hui,et al.Seismic Sedimentology Study of Fine Sequence Stratigraphic Framework:A Case Study of the Hetaoyuan Formation in the Biyang Sag[J].Oil and Gas Geology,2011,32(4):615-624.
[7]朱筱敏,刘长利,张义娜,等.地震沉积学在陆相湖盆三角洲砂体预测中的应用[J].沉积学报,2009,27(5):915-921.ZHU Xiao-min,LIU Chang-li,ZHANG Yi-na,et al.Seismic Sedimentology of Lacustrine Deltaic Deposition Systems[J].Acta Sedimentologica Sinica,2009,27(5):915-921.
[8]洪忠,刘化清,苏明军,等.地震沉积学在复杂岩性地区的应用:以歧北凹陷沙二段为例[J].岩性油气藏,2012,24(4):40-44.HONG Zhong,LIU Hua-qing,SU Ming-jun,et al.Application of Seismic Sedimentology in the Area with Complex Lithologies:A Case from the Second Member of Shahejie Formation in Qibei Sag[J].Lithologic Reservoirs,2012,24(4):40-44.
[9]张闻亭,潘树新,刘震华,等.地震沉积学在坳陷湖盆滩坝砂体预测中的应用:以酒西盆地Y区块间泉子段为例[J].岩性油气藏,2016,28(6):109-116.ZHANG Wen-ting,PAN Shu-xin,LIU Zhen-hua,et al.Application of Seismic Sedimentology to Prediction of Beach and Bar Sand Bodies in Lacustrine Basin:ACase Study of Jianquanzi Member in Y Block,Jiuxi Basin[J].Lithologic Reservoirs,2016,28(6):109-116.
[10]刘建平,鲜本忠,王璐,等.渤海湾盆地东营凹陷始新世三角洲供给型重力流地震沉积学研究[J].古地理学报,2016,18(6):961-974.LIU Jian-ping,XIAN Ben-zhong,WANG Lu,et al.Seismic Sedimentology of Delta-fed Turbidites of the Eocene in Dongying Sag,Bohai Bay Basin[J].Journal of Palaeogeography,2016,18(6):961-974.
[11]张峰,李胜利,黄杰,等.华北蠡县斜坡油气藏分布、成藏模式及主控因素探讨[J].岩性油气藏,2015,27(5):189-195.ZHANG Feng,LI Sheng-li,HUANG Jie,et al.Hydrocarbon Reservoir Distribution,Accumulation Models and Main Controlling Factors in Lixian Slope,North China[J].Lithologic Reservoirs,2015,27(5):189-195.
[12]崔周旗,李文厚,李莉,等.冀中饶阳凹陷蠡县斜坡古近系沙河街组沙二段及沙一段下亚段沉积相与隐蔽油藏[J].古地理学报,2005,7(3):373-381.CUI Zhou-qi,LI Wen-hou,LI Li,et al.Sedimentary Facies and Subtle Petroleum Reservoir of the Member2and Lower Submember of Member 1of Shahejie Formation of Paleogene on Lixian Slope of Raoyang Sag,Central Hebei Province[J].Journal of Palaeogeography,2005,7(3):373-381.
[13]杨帆,于兴河,李胜利,等.冀中坳陷蠡县斜坡油藏分布规律与主控因素研究[J].石油天然气学报,2010,32(4):37-41.YANG Fan,YU Xing-he,LI Sheng-li,et al.Rules of Reservoir Distribution of Lixian Slope and Its Critical Controlling Factors in Jizhong Depression[J].Journal of Oil and Gas Technology,2010,32(4):37-41.
[14]杨帆,邹才能,侯连华,等.坳陷湖盆浅水三角洲沉积特征与油气成藏研究:以饶阳凹陷蠡县斜坡为例[J].特种油气藏,2012,19(3):26-31.YANG Fan,ZOU Cai-neng,HOU Lian-hua,et al.Sedimentary Characteristics and Hydrocarbon Accumulation in Shallow-water Delta of Depression Lake Basin:A Case Study with Lixian Slope in Raoyang Depression[J].Special Oil and Gas Reservoirs,2012,19(3):26-31.
[15]刘建,任莹,王丹蕾,等.蠡县斜坡北段储层流体包裹体特征及成藏时期[J].地质科技情报,2016,35(1):53-58.LIU Jian,REN Ying,WANG Dan-lei,et al.Fluid Inclusions Characteristics and Hydrocarbon Accumulation Period of the Reservoir in the Northern Section,Lixian Slope[J].Geological Science and Technology Information,2016,35(1):53-58.
[16]国景星,袭著纲,赵晓颖,等.蠡县斜坡中北部沙二段-沙一段层序地层研究[J].西南石油大学学报(自然科学版),2010,32(6):33-40.GUO Jing-xing,XI Zhu-gang,ZHAO Xiao-ying,et al.Study on the Sequence Stratigraphy of the Member 2-member 1of Shahejie Formation in the North-central Part of Lixian Slope[J].Journal of Southwest Petroleum University(Science and Technology Edition),2010,32(6):33-40.
[17]纪友亮,杜金虎,赵贤正,等.饶阳凹陷下第三系层序类型及发育模式[J].沉积学报,2007,25(1):1-9.JI You-liang,DU Jin-hu,ZHAO Xian-zheng,et al.Sequence Stratigraphy Models and Controlling Factors of Eocene in Raoyang Depression[J].Acta Sedimentologica Sinica,2007,25(1):1-9.
[18]陈贺贺,朱筱敏,黄捍东,等.基于碎屑锆石定年的饶阳凹陷蠡县斜坡沙河街组物源分析[J].地球科学,2017,42(11):1955-1971.CHEN He-he,ZHU Xiao-min,HUANG Han-dong,et al.Sediment Provenance of Shahejie Formation in Lixian Slope of Raoyang Depression Based on the Detrital Zircon Dating Analysis[J].Earth Science,2017,42(11):1955-1971.
[19]陈骥,徐凤强,刘超,等.蠡县斜坡沙三上亚段与沙一下亚段沉积特征及有利储层分布[J].岩性油气藏,2016,28(5):91-98.CHEN Ji,XU Feng-qiang,LIU Chao,et al.Sedimentary Characteristics and Favorable Reservoir Distribution of the Upper Submember of the Third Member and the Lower Submember of the First Member of Shahejie Formation in Lixian Slope[J].Lithologic Reservoirs,2016,28(5):91-98.
[20]刘金龙,李胜利,梁星如,等.冀中坳陷蠡县斜坡古近系沙一段下亚段沉积物源分析[J].古地理学报,2016,18(5):809-817.LIU Jin-long,LI Sheng-li,LIANG Xing-ru,et al.Provenance Analysis of the Lower Part of Member 1of Paleogene Shahejie Formation in Lixian Slope,Central Hebei Depression[J].Journal of Palaeogeography,2016,18(5):809-817.
[21]栗宝鹃,董春梅,林承焰,等.不同期次浊积扇体地震沉积学研究:以车西洼陷缓坡带车40-44块沙三上亚段为例[J].吉林大学学报(地球科学版),2016,46(1):65-79.LI Bao-juan,DONG Chun-mei,LIN Cheng-yan,et al.Seismic Sedimentology Research on Turbidite Fan Body of Different Stages:In Case of the Gentle Slope Belt of Chexi Depression's Che40-44Area of Upper Submember of Es3[J].Journal of Jilin University(Earth Science Edition),2016,46(1):65-79.
[22]杨勇强,邱隆伟,姜在兴,等.陆相断陷湖盆滩坝沉积模式:以东营凹陷古近系沙四上亚段为例[J].石油学报,2011,32(3):417-423.YANG Yong-qiang,QIU Long-wei,JIANG Zai-xing,et al.A Depositional Pattern of Beach Bar in Continental Rift Lake Basins:A Case Study on the Upper Part of the Fourth Member of the Shahejie Formation in the Dongying Sag[J].Acta Petrolei Sinica,2011,32(3):417-423.
[23]曾洪流,朱筱敏,朱如凯,等.陆相坳陷型盆地地震沉积学研究规范[J].石油勘探与开发,2012,39(3):275-284.ZENG Hong-liu,ZHU Xiao-min,ZHU Ru-kai,et al.Guidelines for Seismic Sedimentologic Study in Nonmarine Post Rift Basins[J].Petroleum Exploration and Development,2012,39(3):275-284.
[24]朱筱敏,李洋,董艳蕾,等.地震沉积学研究方法和歧口凹陷沙河街组沙一段实例分析[J].中国地质,2013,40(1):152-162.ZHU Xiao-min,LI Yang,DONG Yan-lei,et al.The Program of Seismic Sedimentology and Its Application to Shahejie Formation in Qikou Depression of North China[J].Geology in China,2013,40(1):152-162.
[25]张兆辉,刘化清,苏明军.基于地层切片的小尺度沉积相定量解释方法[J].吉林大学学报(地球科学版),2016,46(3):893-899.ZHANG Zhao-hui,LIU Hua-qing,SU Ming-jun.Quantitative Interpretation Method of Small-scale Sedimentary Facies Based on Strata Slice[J].Journal of Jilin University(Earth Science Edition),2016,46(3):893-899.
[2]ZENG H L,HENTZ T F.High-frequency Sequence Stratigraphy from Seismic Sedimentology Applied to Miocene Vermilio Block 50Tiger Shoal Area Offshore Louisiana[J].AAPG Bulletin,2004,88(2):153-174.
[3]ZENG H L,BACKUS M M.Interpretive Advantages of 90°-phase Wavelets:Part I,Modeling[J].Geophysics,2005,70(3):7-15.
[4]ZHU X M,ZENG H L,LI S L,et al.Sedimentary Characteristics and Seismic Geomorphologic Responses of a Shallow-water Delta in the Qingshankou Formation from the Songliao Basin,China[J].Marine and Petroleum Geology,2017,79(4):131-148.
[5]董艳蕾,朱筱敏,曾洪流,等.歧南凹陷地震沉积学研究[J].中国石油大学学报(自然科学版),2008,32(4):7-12.DONG Yan-lei,ZHU Xiao-min,ZENG Hong-liu,et al.Study of Seismic Sedimentology in Qinan Sag[J].Journal of China University of Petroleum(Edition of Natural Science),2008,32(4):7-12.
[6]朱筱敏,董艳蕾,胡廷惠,等.精细层序地层格架与地震沉积学研究:以泌阳凹陷核桃园组为例[J].石油与天然气地质,2011,32(4):615-624.ZHU Xiao-min,DONG Yan-lei,HU Ting-hui,et al.Seismic Sedimentology Study of Fine Sequence Stratigraphic Framework:A Case Study of the Hetaoyuan Formation in the Biyang Sag[J].Oil and Gas Geology,2011,32(4):615-624.
[7]朱筱敏,刘长利,张义娜,等.地震沉积学在陆相湖盆三角洲砂体预测中的应用[J].沉积学报,2009,27(5):915-921.ZHU Xiao-min,LIU Chang-li,ZHANG Yi-na,et al.Seismic Sedimentology of Lacustrine Deltaic Deposition Systems[J].Acta Sedimentologica Sinica,2009,27(5):915-921.
[8]洪忠,刘化清,苏明军,等.地震沉积学在复杂岩性地区的应用:以歧北凹陷沙二段为例[J].岩性油气藏,2012,24(4):40-44.HONG Zhong,LIU Hua-qing,SU Ming-jun,et al.Application of Seismic Sedimentology in the Area with Complex Lithologies:A Case from the Second Member of Shahejie Formation in Qibei Sag[J].Lithologic Reservoirs,2012,24(4):40-44.
[9]张闻亭,潘树新,刘震华,等.地震沉积学在坳陷湖盆滩坝砂体预测中的应用:以酒西盆地Y区块间泉子段为例[J].岩性油气藏,2016,28(6):109-116.ZHANG Wen-ting,PAN Shu-xin,LIU Zhen-hua,et al.Application of Seismic Sedimentology to Prediction of Beach and Bar Sand Bodies in Lacustrine Basin:ACase Study of Jianquanzi Member in Y Block,Jiuxi Basin[J].Lithologic Reservoirs,2016,28(6):109-116.
[10]刘建平,鲜本忠,王璐,等.渤海湾盆地东营凹陷始新世三角洲供给型重力流地震沉积学研究[J].古地理学报,2016,18(6):961-974.LIU Jian-ping,XIAN Ben-zhong,WANG Lu,et al.Seismic Sedimentology of Delta-fed Turbidites of the Eocene in Dongying Sag,Bohai Bay Basin[J].Journal of Palaeogeography,2016,18(6):961-974.
[11]张峰,李胜利,黄杰,等.华北蠡县斜坡油气藏分布、成藏模式及主控因素探讨[J].岩性油气藏,2015,27(5):189-195.ZHANG Feng,LI Sheng-li,HUANG Jie,et al.Hydrocarbon Reservoir Distribution,Accumulation Models and Main Controlling Factors in Lixian Slope,North China[J].Lithologic Reservoirs,2015,27(5):189-195.
[12]崔周旗,李文厚,李莉,等.冀中饶阳凹陷蠡县斜坡古近系沙河街组沙二段及沙一段下亚段沉积相与隐蔽油藏[J].古地理学报,2005,7(3):373-381.CUI Zhou-qi,LI Wen-hou,LI Li,et al.Sedimentary Facies and Subtle Petroleum Reservoir of the Member2and Lower Submember of Member 1of Shahejie Formation of Paleogene on Lixian Slope of Raoyang Sag,Central Hebei Province[J].Journal of Palaeogeography,2005,7(3):373-381.
[13]杨帆,于兴河,李胜利,等.冀中坳陷蠡县斜坡油藏分布规律与主控因素研究[J].石油天然气学报,2010,32(4):37-41.YANG Fan,YU Xing-he,LI Sheng-li,et al.Rules of Reservoir Distribution of Lixian Slope and Its Critical Controlling Factors in Jizhong Depression[J].Journal of Oil and Gas Technology,2010,32(4):37-41.
[14]杨帆,邹才能,侯连华,等.坳陷湖盆浅水三角洲沉积特征与油气成藏研究:以饶阳凹陷蠡县斜坡为例[J].特种油气藏,2012,19(3):26-31.YANG Fan,ZOU Cai-neng,HOU Lian-hua,et al.Sedimentary Characteristics and Hydrocarbon Accumulation in Shallow-water Delta of Depression Lake Basin:A Case Study with Lixian Slope in Raoyang Depression[J].Special Oil and Gas Reservoirs,2012,19(3):26-31.
[15]刘建,任莹,王丹蕾,等.蠡县斜坡北段储层流体包裹体特征及成藏时期[J].地质科技情报,2016,35(1):53-58.LIU Jian,REN Ying,WANG Dan-lei,et al.Fluid Inclusions Characteristics and Hydrocarbon Accumulation Period of the Reservoir in the Northern Section,Lixian Slope[J].Geological Science and Technology Information,2016,35(1):53-58.
[16]国景星,袭著纲,赵晓颖,等.蠡县斜坡中北部沙二段-沙一段层序地层研究[J].西南石油大学学报(自然科学版),2010,32(6):33-40.GUO Jing-xing,XI Zhu-gang,ZHAO Xiao-ying,et al.Study on the Sequence Stratigraphy of the Member 2-member 1of Shahejie Formation in the North-central Part of Lixian Slope[J].Journal of Southwest Petroleum University(Science and Technology Edition),2010,32(6):33-40.
[17]纪友亮,杜金虎,赵贤正,等.饶阳凹陷下第三系层序类型及发育模式[J].沉积学报,2007,25(1):1-9.JI You-liang,DU Jin-hu,ZHAO Xian-zheng,et al.Sequence Stratigraphy Models and Controlling Factors of Eocene in Raoyang Depression[J].Acta Sedimentologica Sinica,2007,25(1):1-9.
[18]陈贺贺,朱筱敏,黄捍东,等.基于碎屑锆石定年的饶阳凹陷蠡县斜坡沙河街组物源分析[J].地球科学,2017,42(11):1955-1971.CHEN He-he,ZHU Xiao-min,HUANG Han-dong,et al.Sediment Provenance of Shahejie Formation in Lixian Slope of Raoyang Depression Based on the Detrital Zircon Dating Analysis[J].Earth Science,2017,42(11):1955-1971.
[19]陈骥,徐凤强,刘超,等.蠡县斜坡沙三上亚段与沙一下亚段沉积特征及有利储层分布[J].岩性油气藏,2016,28(5):91-98.CHEN Ji,XU Feng-qiang,LIU Chao,et al.Sedimentary Characteristics and Favorable Reservoir Distribution of the Upper Submember of the Third Member and the Lower Submember of the First Member of Shahejie Formation in Lixian Slope[J].Lithologic Reservoirs,2016,28(5):91-98.
[20]刘金龙,李胜利,梁星如,等.冀中坳陷蠡县斜坡古近系沙一段下亚段沉积物源分析[J].古地理学报,2016,18(5):809-817.LIU Jin-long,LI Sheng-li,LIANG Xing-ru,et al.Provenance Analysis of the Lower Part of Member 1of Paleogene Shahejie Formation in Lixian Slope,Central Hebei Depression[J].Journal of Palaeogeography,2016,18(5):809-817.
[21]栗宝鹃,董春梅,林承焰,等.不同期次浊积扇体地震沉积学研究:以车西洼陷缓坡带车40-44块沙三上亚段为例[J].吉林大学学报(地球科学版),2016,46(1):65-79.LI Bao-juan,DONG Chun-mei,LIN Cheng-yan,et al.Seismic Sedimentology Research on Turbidite Fan Body of Different Stages:In Case of the Gentle Slope Belt of Chexi Depression's Che40-44Area of Upper Submember of Es3[J].Journal of Jilin University(Earth Science Edition),2016,46(1):65-79.
[22]杨勇强,邱隆伟,姜在兴,等.陆相断陷湖盆滩坝沉积模式:以东营凹陷古近系沙四上亚段为例[J].石油学报,2011,32(3):417-423.YANG Yong-qiang,QIU Long-wei,JIANG Zai-xing,et al.A Depositional Pattern of Beach Bar in Continental Rift Lake Basins:A Case Study on the Upper Part of the Fourth Member of the Shahejie Formation in the Dongying Sag[J].Acta Petrolei Sinica,2011,32(3):417-423.
[23]曾洪流,朱筱敏,朱如凯,等.陆相坳陷型盆地地震沉积学研究规范[J].石油勘探与开发,2012,39(3):275-284.ZENG Hong-liu,ZHU Xiao-min,ZHU Ru-kai,et al.Guidelines for Seismic Sedimentologic Study in Nonmarine Post Rift Basins[J].Petroleum Exploration and Development,2012,39(3):275-284.
[24]朱筱敏,李洋,董艳蕾,等.地震沉积学研究方法和歧口凹陷沙河街组沙一段实例分析[J].中国地质,2013,40(1):152-162.ZHU Xiao-min,LI Yang,DONG Yan-lei,et al.The Program of Seismic Sedimentology and Its Application to Shahejie Formation in Qikou Depression of North China[J].Geology in China,2013,40(1):152-162.
[25]张兆辉,刘化清,苏明军.基于地层切片的小尺度沉积相定量解释方法[J].吉林大学学报(地球科学版),2016,46(3):893-899.ZHANG Zhao-hui,LIU Hua-qing,SU Ming-jun.Quantitative Interpretation Method of Small-scale Sedimentary Facies Based on Strata Slice[J].Journal of Jilin University(Earth Science Edition),2016,46(3):893-899.