细粒沉积物中不同级次高频层序划分及其地质意义——以东营凹陷沙三下—沙四上亚段泥页岩为例

杜学斌; 陆永潮; 刘惠民; 刘辉; 王勇; 熊仕鹏; 郭来源; 刘占红; 彭丽

doi:10.11781/sysydz201802244

文章导航 > 石油实验地质 > 2018 > 40(2): 244-252

杜学斌, 陆永潮, 刘惠民, 刘辉, 王勇, 熊仕鹏, 郭来源, 刘占红, 彭丽. 细粒沉积物中不同级次高频层序划分及其地质意义——以东营凹陷沙三下—沙四上亚段泥页岩为例[J]. 石油实验地质, 2018, 40(2): 244-252. doi: 10.11781/sysydz201802244

引用本文:

DU Xuebin, LU Yongchao, LIU Huimin, LIU Hui, WANG Yong, XIONG Shipeng, GUO Laiyuan, LIU Zhanhong, PENG Li. Division of high-frequency sequences of different orders in fine-grained deposits and its geologic significance: A case study of mud shale from the lower section of the third member to the upper section of the fourth member of Shahejie Formation in Dongying Sag, Bohai Bay Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2018, 40(2): 244-252. doi: 10.11781/sysydz201802244

Citation:

DU Xuebin, LU Yongchao, LIU Huimin, LIU Hui, WANG Yong, XIONG Shipeng, GUO Laiyuan, LIU Zhanhong, PENG Li. Division of high-frequency sequences of different orders in fine-grained deposits and its geologic significance: A case study of mud shale from the lower section of the third member to the upper section of the fourth member of Shahejie Formation in Dongying Sag, Bohai Bay Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2018, 40(2): 244-252. doi: 10.11781/sysydz201802244

引用本文:

Citation:

DU Xuebin, LU Yongchao, LIU Huimin, LIU Hui, WANG Yong, XIONG Shipeng, GUO Laiyuan, LIU Zhanhong, PENG Li. Division of high-frequency sequences of different orders in fine-grained deposits and its geologic significance: A case study of mud shale from the lower section of the third member to the upper section of the fourth member of Shahejie Formation in Dongying Sag, Bohai Bay Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2018, 40(2): 244-252. doi: 10.11781/sysydz201802244

细粒沉积物中不同级次高频层序划分及其地质意义——以东营凹陷沙三下—沙四上亚段泥页岩为例

doi: 10.11781/sysydz201802244

杜学斌^1,2,
陆永潮²,
刘惠民³,
刘辉⁴,
王勇³,
熊仕鹏^1,2,
郭来源^1,2,
刘占红^1,2,
彭丽^1,2

1.
中国地质大学(武汉) 海洋学院, 武汉 430074
2. 中国地质大学(武汉) 构造与油气资源教育部重点实验室, 武汉 430074
3. 中国石化胜利油田分公司地质科学研究院, 山东东营 257015
4. 湖北省宜昌市远安县国土资源局, 湖北远安 444200

基金项目: 国家重点基础研究发展计划（973计划）（2017CB239102）和国家科技重大专项（2016ZX05060004，2016ZX05034002003）资助。

详细信息

作者简介:
杜学斌(1977-),男,副教授,能源地质专业。E-mail:xbdu@cug.edu.cn。

中图分类号: TE121.34
计量
- 文章访问数: 1359
- HTML全文浏览量: 112
- PDF下载量: 173
- 被引次数: 0
出版历程
- 收稿日期: 2017-08-16
- 修回日期: 2018-01-25
- 刊出日期: 2018-03-28

Division of high-frequency sequences of different orders in fine-grained deposits and its geologic significance: A case study of mud shale from the lower section of the third member to the upper section of the fourth member of Shahejie Formation in Dongying Sag, Bohai Bay Basin

1.
College of Marine Science and Technology, China University of Geosciences(Wuhan), Wuhan, Hubei 430074, China
2. Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences(Wuhan), Wuhan, Hubei 430074, China
3. Geological Scientific Research Institute, SINOPEC Shengli Oilfield, Dongying, Shandong 257015, China
4. Yuan'an Land Resources Bureau, Yichang, Hubei 444200, China

摘要

摘要: 泥页岩地层中层序划分是目前基础研究中的难点与热点之一。在充分借鉴国外研究成果的基础上，提出了基于多种敏感性指标、依托GR曲线，借助改进后的T-R旋回理论指导，开展泥页岩层段四-五级层序地层划分的方案；同时，提出在连续测试数据支持下，借助天文旋回理论，利用偏心率、斜率、岁差等天文参数，建立泥页岩层段的天文标尺，从而建立六-七级层序单元。在此基础上，借助天文标尺，将渤海湾盆地东营凹陷A井沙四纯上段划分出4个沉积过程，并将各个沉积过程进行定量化计算。利用上述系列方法，将东营凹陷沙三下-沙四上泥岩段划分为8个四级层序，31个五级层序，并通过对沉积过程的定量分析，认为沙四上段第二个准层序组沉积期最有利于生物发育。
- 自然伽马曲线 /
- T-R旋回 /
- 高频层序 /
- 泥页岩 /
- 东营凹陷 /
- 渤海湾盆地
Abstract: The sequence division of mud shale is a focus in basic research. Based on lots of sensitivity parameters, using the natural gamma curves (GR) and the improved TR cycle theory, it was classified in this paper the fourth and fifth orders of sequences in mud shale. Moreover, using continuous testing data, based on the astronomical cycle theory, some parameters such as eccentricity, slope and precession were used to establish an astronomical scale for mud shale in the study area, by which the sixth and seventh orders of sequence units can be identified. Four deposition processes were concluded in the upper section of the fourth member of Shahejie Formation in well A in the Dongying Sag, Bohai Bay Basin, and quantitative calculations were made for each process to estimate the deposition rates in different units. We divided the strata from the lower section of the third member to the upper section of the fourth member of Shahejie Formation into eight fourth order and 31 fifth order units. The quantitative analyses of deposition process showed that the deposition period of the second quasisequence in the upper section of the fourth member of Shahejie Formation was the most conducive to biological development.
- natural gamma curve (GR) /
- T-R cycle /
- high resolution sequence /
- mud shale /
- Dongying Sag /
- Bohai Bay Basin

HTML全文

参考文献(23)

[1]	ABOUELRESH M O,SLATT R M.Lithofacies and sequence stratigraphy of the Barnett shale in east-central Fort Worth Basin,Texas[J].AAPG Bulletin,2012,96(1):1-22.
[2]	KINLEY T J,COOK L W,BREYER J A,et al.,Hydrocarbon potential of the Barnett shale (Mississippian),Delaware Basin,west Texas and southeastern New Mexico[J].AAPG Bulletin,2009,93(8):967-991.
[3]	LOUCKS R G,RUPPEL S C.Mississippian Barnett shale:Lithofacies and depositional setting of a deep-water shale-gas succession in the Fort Worth Basin,Texas[J].AAPG Bulletin,2007,91(4):579-601.
[4]	SINGH P,SLATT R,BORGES G,et al..Reservoir characterization of unconventional gas shale reservoirs:Example from the Barnett shale,Texas,U.S.A[J].Earth Sciences Research Journal,2009,60(1):15-31.
[5]	王艳忠,操应长,远光辉.小波分析在深水砂砾岩和泥页岩地层层序划分中的应用[J].天然气地球科学,2012,23(2):251-258. WANG Yanzhong,CAO Yingchang,YUAN Guanghui.Application of wavelet analysis in sequence division of deepwater glutenite and shale layer[J].Natural Gas Geosciences,2012,23(2):251-258.
[6]	朱德燕,王学军,郝雪峰,等.东营凹陷泥页岩层序地层划分[J].油气地质与采收率,2016,23(2):52-56. ZHU Deyan,WANG Xuejun,HAO Xuefeng,et al.Study on sequence stratigraphic division of oil shale in Dongying Sag[J].Petroleum Geology and Recovery Efficiency,2016,23(2):52-56.
[7]	杜学斌,刘辉,刘惠民,等.细粒沉积物层序地层划分方法初探:以东营凹陷樊页1井沙三下-沙四上亚段泥页岩为例[J].地质科技情报,2016,35(4):1-11. DU Xuebin,LIU Hui,LIU Huimin,et al.Methods of sequence stratigraphy in the fine-grained sediments:A case from the upper fourth sub-member and the lower third sub-member of the Shahejie Formation in well Fanye 1 of Dongying Depression[J].Geological Science and Technology Information,2016,35(4):1-11.
[8]	纪友亮.层序地层学[M].上海:同济大学出版社,2005:89-112. JI Youliang.Sequence stratigraphy[M].Shanghai:Tongji University Press,2005:89-112.
[9]	王华.层序地层学基本原理、方法与应用[M].武汉:中国地质大学出版社,2007:1-3. WANG Hua.The basic principles and application methods of sequence stratigraphy[M].Wuhan:China University of Geosciences Press,2007:1-3.
[10]	郭建华,宫少波,吴东胜.陆相断陷湖盆T-R旋回沉积层序与研究实例[J].沉积学报,1998,16(1):8-14. GUO Jianhua,GONG Shaobo,WU Dongsheng.Sedimentary sequence of the T-R cycle and a studied example in the continental fault lacustrine basin[J].Acta Sedimentologica Sinica,1998,16(1):8-14.
[11]	刘招君,孙平昌,贾建亮,等.陆相深水环境层序识别标志及成因解释:以松辽盆地青山口组为例[J].地学前缘,2011,18(4):171-180. LIU Zhaojun,SUN Pingchang,JIA Jianliang,et al.Distinguishing features and their genetic interpretation of stratigraphic sequences in continental deep water setting:A case from Qingshankou Formation in Songliao Basin[J].Earth Science Frontiers,2011,18(4):171-180.
[12]	张美玲,李建明,郭战峰,等.涪陵焦石坝地区五峰组-龙马溪组富有机质泥页岩层序地层与沉积相研究[J].长江大学学报(自然科学版),2015,12(11):17-21. ZHANG Meiling,LI Jianming,GUO Zhanfeng,et al.Study on sequence stratigraphy and sedimentary facies of rich organic mud shale of Wufeng-Longmaxi Formation in Fuling Jiaoshiba area[J].Journal of Yangtze University (Natural Science Edition),2015,12(11):17-21.
[13]	吴松涛,邹才能,朱如凯,等.鄂尔多斯盆地上三叠统长7段泥页岩储集性能[J].地球科学(中国地质大学学报),2015,40(11):1810-1823. WU Songtao,ZOU Caineng,ZHU Rukai,et al.Reservoir quality characterization of Upper Triassic Chang 7 shale in Ordos Basin[J].Earth Science(Journal of China University of Geosciences),2015,40(11):1810-1823.
[14]	曾翔,蔡进功,董哲,等.泥页岩沉积特征与生烃能力:以东营凹陷沙河街组三段中亚段-沙河街组四段上亚段为例[J].石油学报,2017,38(1):31-43. ZENG Xiang,CAI Jingong,DONG Zhe,et al.Sedimentary characteristics and hydrocarbon generation potential of mudstone and shale:A case study of middle submember of member 3 and upper submember of member 4 in Shahejie Formation in Dong-ying Sag[J].Acta Petrolei Sinica,2017,38(1):31-43.
[15]	王勇.济阳陆相断陷湖盆泥页岩细粒沉积层序初探[J].西南石油大学学报(自然科学版),2016,38(6):61-69. WANG Yong.A study on fine sedimentary sequence of shale in the continental rift basin of Jiyang Depression[J].Journal of Southwest Petroleum University (Science & Technology Edition),2016,38(6):61-69.
[16]	WANG Yong,WANG Xuejun,SONG Guoqi,et al.Genetic connection between mud shale lithofacies and shale oil enrichment in Jiyang Depression,Bohai Bay Basin[J].Petroleum Exploration and Development,2016,43(5):759-768.
[17]	DEHAIRS F,CHESSELET R,JEDWAB J.Discrete suspended particles of barite and the barium cycle in the Open Ocean[J].Earth and Planetary Science Letters,1980,49(2):528-550.
[18]	DYMOND J,SUESS E,LYLE M.Barium in deep-sea sediment:A geochemical proxy for paleoproductivity[J].Paleoceano-graphy,1992,7(2):163-181.
[19]	HUERTA-DIA M A,MORSE J W.A quantitative method for determination of trace metal concentrations in sedimentary pyrite[J].Marine Chemistry,1990,29:119-144.
[20]	TRIBOVILLARD N,ALGEO T J,LYONS T,et al.Trace metals as paleoredox and paleoproductivity proxies:An update[J].Chemical Geology,2006,232(1/2):12-32.
[21]	黄春菊.旋回地层学和天文年代学及其在中生代的研究现状[J].地学前缘,2014,21(2):48-66. HUANG Chunju.The current status of cyclostratigraphy and astrochronology in the Mesozoic[J].Earth Science Frontiers,2014,21(2):48-66.
[22]	王起琮.天文周期约束下的基准面旋回层序划分方法[J].新疆石油地质,2009,30(4):499-514. WANG Qicong.The method for astronomical period-restricted datum-cycle sequence classification[J].Xinjiang Petroleum Geology,2009,30(4):499-514.
[23]	徐伟,解习农.基于米兰科维奇周期的沉积速率计算新方法:以东营凹陷牛38井沙三中为例[J].石油实验地质,2012,34(2):207-214. XU Wei,XIE Xinong.A new method to calculate sedimentary rates based on Milankovitch Cycles:A case study on middle section of 3rd member of Shahejie Formation in well Niu38,Dongying Sag,Bohai Bay Basin[J].Petroleum Geology & Experiment,2012,34(2):207-214.