Sequence stratigraphy and sedimentary filling evolution of fluvial facies of the Neogene of gentle slope belt in Huanghua Depression,Bohai Bay Basin
Chen Rong1, Wang Feng2, Li Yong3
1 Museum of Chengdu University of Technology,Chengdu 610059, Sichuan; 2 Institute of Sedimentary Geology, Chengdu University of Technology,Chengdu 610059, Sichuan; 3 College of Energy Resources of Chengdu University of Technology,Chengdu 610059, Sichuan
Abstract The Neogene of gentle slope belt in Huanghua Depression of Bohai Bay Basin is mainly composed of continental fluvial sediments. To explore the lithologic-stratigraphic reservoirs by using the theories of sequence stratigraphy is the current focus. The Minghuazhen Formation and Guantao Formation of Neogene in Huanghua Depression are the research objects. Based on the existing core, drilling and seismic data, together with the sequence interface recognition, the high-resolution sequence stratigraphic framework in the study area was established, including one super long-term cycle sequence, seven long-term cycle sequence and a number of middle-term and short-term cycle sequence. Filled by superposed sand bodies of braided river, the sequence stratigraphic model of multi-fault gentle slope with the structure of unsymmetric type, which only retained the rising stage of base level cycles, was developed in the Guantao Formation. The sequence stratigraphic model of stable slope with the sequence structure of uncompletely symmetrical type, which was mainly composed of rising stage of base level cycles, was developed in the Minghuazhen Formation. The composite sand bodies of braided river on the inside of multi-fault slope break in the early stage of sequence development is the most favorable reservoir sand body in the study area.
Corresponding Authors:
Wang Feng, born in 1977,associate professor,got his doctor??s degree of Chengdu University of Technology in 2007. He is engaged in sequence stratigraphy and lithofacies palaeogeography. E-mail: wangfeng07@cudt.cn.
About author: Chen Rong,born in 1982,with a Ph.D. degree obtained from Chengdu University of Technology,is an associate professor. She is engaged in sedimentology and stratigraphy. E-mail: chenrong07@cdut.cn.
Cite this article:
Chen Rong,Wang Feng,Li Yong. Sequence stratigraphy and sedimentary filling evolution of fluvial facies of the Neogene of gentle slope belt in Huanghua Depression,Bohai Bay Basin[J]. JOPC, 2016, 18(6): 976-985.
Chen Rong,Wang Feng,Li Yong. Sequence stratigraphy and sedimentary filling evolution of fluvial facies of the Neogene of gentle slope belt in Huanghua Depression,Bohai Bay Basin[J]. JOPC, 2016, 18(6): 976-985.
[1] 陈留勤,郭福生,梁伟. 2014. 河流相层序地层学研究现状及发展方向. 地层学杂志,38(2):227-235. [Chen L Q,Guo F S,Liang W. 2014. A review of terrestrial sequence stratigraphy. Journal of Stratigraphy,38(2):227-235] [2] 陈蓉,李勇,丘东洲. 2009. 埕宁隆起北坡新近纪沉积特征及发育模式. 沉积与特提斯地质,29(2):8-14. [Chen R,Li Y,Qiu D Z. 2009. Sedimentary facies types and models for the Neogene deposits on the northern slope of the Chengning uplift. Sedimentary Geology and Tethyan Geology,29(2):8-14.] [3] 邓宏文,王洪亮,李小孟. 1997. 高分辨率层序地层对比在河流相中的应用. 石油与天然气地质,18(2):90-95. [Deng H W,Wang H L,Li X M. 1997. Application of high-resolution sequence stratigraphic correlation to fluvial facies. Oil & Gas Geology,18(2):90-95] [4] 邓宏文,王洪亮,祝永军. 2002. 高分辨率层序地层学原理及应用. 北京:地质出版社,16-24. [Deng H W,Wang H L,Zhu Y J. 2002. The Principle and Application of High Resolution Sequence Stratigraphy. Beijing: Geological Publishing House, 16-24] [5] 董春梅. 2006. 基于河水位变化的层序地层模式:以济阳坳陷孤东油田为例. 石油实验地质,28(3):249-252. [Dong C M. 2006. The sequence stratigraphic model based on the variance of river level: Take the Gudong oilfield in the jiyang depression as an example. Petroleum Geology & Experiment,28(3):249-252] [6] 房煦. 2014. 非近海河流相层序地层学探讨: 以济阳坳陷新近系为例. 油气地质与采收率,21(6):10-14. [Fang X. 2014. Discussion on non-coastal fluvial facies sequence stratigraphy:An example from the Neogene in Jiyang depression. Petroleum Geology and Recovery Efficiency,21(6):10-14] [7] 顾家裕. 1995. 陆相盆地层序地层学格架概念及模式. 石油勘探与开发,22(4):6-10. [Gu J Y. 1995. Framework concepts and models of sequence stratigraphy in nonmarine petroliferous basin. Petroleum Exploration and Development,22(4):6-10] [8] 胡受权,郭文平,杨凤根,颜其彬,刘树根,童崇光. 2001. 试论控制断陷湖盆陆相层序发育的影响因素. 沉积学报,19(2):256-262. [Hu S Q,Guo W P,Yang F G,Yan Q B,Liu S G,Tong C G. 2001. Study on influential factors of terrigenous sequence formation and development in fault-depressed lacustrine basin. Acta Sedimentologica Sinica,19(2):256-262] [9] 刘招君,董清水,王嗣敏,朱建伟,郭巍. 2002. 陆相层序地层学导论与应用. 北京:石油工业出版社, 39-50. [Liu Z J,Dong Q S,Wang S M,Zhu J W,Guo W. 2002. The Introduction and Application of Continental Sequence Stratigraphy. Beijing:Petroleum Industry Press, 39-50] [10] 漆家福. 2004. 渤海湾新生代盆地的两种构造系统及其成因解释. 中国地质,31(1):15-22. [Qi J F. 2004. Two tectonic systems in the Cenozoic Bohai Bay basin and their genetic interpretation. Geology in China,31(1):15-22.] [11] 孙小霞,李勇,丘东洲,肖敦清,武站国,张连雪,陈蓉,赵瞻. 2006. 黄骅坳陷新近系馆陶组重矿物特征及物源区意义. 沉积与特提斯地质,26(3):61-66. [Sun X X,Li Y,Qiu D Z,Xiao D Q,Wu Z G,Zhang L X,Chen R,Zhao Z. 2006. The heavy minerals and provenances of the Neogene Guantao Formation in the Huanghua depression. Sedimentary Geology and Tethyan Geology,26(3):61-66] [12] 王德发,张服民. 1987. 黄骅坳陷第三系沉积相及沉积环境. 北京:地质出版社,122-133. [Wang D F,Zhang F M. 1987. Sedimentary Facies and Environment of Tertiary in Huanghua Depression.Beijing:Geological Publishing House,122-133] [13] 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. [Xue L Q. 1995. Currentstatus,methodology,and future directions of sequence statigraphy study. Petroleum Exploration and Development,22(5):8-13] [14] 张晨晨,张顺,魏巍,吴朝东,梁江平,牛文,杜锦霞,付秀丽,崔坤宁,王超,王辉. 2014. 松辽盆地嫩江组T-R 旋回控制下的层序结构与沉积响应. 中国科学:地球科学,44(12):2618-2636. [Zhang C C,Zhang S,Wei W,Wu C D,Liang J P,Niu W,Du J X,Fu X L,Cui K N,Wang C,Wang H. 2014. Sedimentary filling and sequence structure dominated by T-R cycles of the Nenjiang Formation in the Songliao Basin. Science China:Earth Sciences,57:278-296] [15] 张周良. 1996. 河流相地层的层序地层学与河流类型. 地质论评,42(3):188-193. [Zhang Z L. 1996. Fluvial sequence stratigraphy and river types. Geological Review,42(3):188-193] [16] 赵澄林,陈纯芳. 2003. 渤海湾早第三纪油区岩相古地理及储集层. 北京:石油工业出版社, 1-132. [Zhao C L,Chen C F. 2003. Lithofacies Paleogeography and Reservoirs in Oil Region of Early Teriary in Bohai Bay. Beijing:Petroleum Industry Press, 1-132] [17] 朱筱敏,康安,王贵文. 2003. 陆相坳陷型和断陷型湖盆层序地层样式探讨. 沉积学报,21(2):283-287. [Zhu X M,Kang A,Wang G W. 2003. Sequence stratigraphic models of depression and faulted-down lake basins. Acta Sedimentologica Sinica,21(2):283-287] [18] Cross T A. 2000. Stratigraphic controls on reservoir attributes in continental Strate. Earth Science Frontiers,7(4):322-350. [19] Holbrook J M,Scott R W,Oboh-Ikuenobe F E. 2006. Base-level buffers and buttresses:A model for upstream versus downstream control on fluvial geometry and architecture within sequences. Journal of Sedimentary Research,76:162-174. [20] Posamentier H W,Jervey M T,Vail P R. 1988. Eustatic controls on clastic deposition. Sea Level Changes an Integrated Approach,42:110-124. [21] Shanley K W,McCabe P J. 1993. Alluvial architecture in a sequence stratigraphic framework:A case history from the Upper Cretaceous of southern Utah,USA. In: Flint S, Bryant I(eds). The Geological Modeling of Hydrocarbon Reservoirs and Outcrop Analogues. International Association of Sedimentologists Special Publication 15:21-56. [22] Vail P R. 1987. Seismic stratigraphy interpretation using sequence stratigraphy. AAPG Bulletin,27:1-10. [23] Wright V P,Marriott S B. 1993. The sequence stratigraphy of fluvial depositional systems:The role of flood plain sediment storage. Sedimentary Geology,86(3-4):203-210.