DEPOSITIONAL FILLING MODEL AND EVOLUTION OF THE SAG IN LACUSTRINE BASIN:A CASE STUDY FROM SHAHEJIE FORMATION IN MAXI SAG, RAOYANG DEPRESSION

ZHANG Yi-ming; LI Sheng-li; LI Min; YU Xing-he; ZHANG Wan-fu; TIAN Qian-qian; FANG Xin-xin

Volume 18 Issue 4

Dec. 2012

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Article Navigation > Journal of Geomechanics > 2012 > 18(4): 379-388

ZHANG Yi-ming, LI Sheng-li, LI Min, et al., 2012. DEPOSITIONAL FILLING MODEL AND EVOLUTION OF THE SAG IN LACUSTRINE BASIN:A CASE STUDY FROM SHAHEJIE FORMATION IN MAXI SAG, RAOYANG DEPRESSION. Journal of Geomechanics, 18 (4): 379-388.

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DEPOSITIONAL FILLING MODEL AND EVOLUTION OF THE SAG IN LACUSTRINE BASIN:A CASE STUDY FROM SHAHEJIE FORMATION IN MAXI SAG, RAOYANG DEPRESSION

1.
PetroChina Huabei Oilfield Company, Renqiu 062550, China
2.
School of Energy Resources, China University of Geosciences, Beijing 100083, China
3.
Fracturing & Acidizing Technology Research Institute, GWDC Fracturing Company, Panjin 124107, China
4.
Geological Research Center, Bureau of Geophysical Prospecting, Zhuozhou 072751, China

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Abstract

Abstract

Sag is an important part of the rift lacustrine basin and is the main occurrence area of hydrocarbon source rocks. But in terms of its unique characteristics of sedimentary filling, the buried depth and the reservoir development, the exploratory degree of petroleum in a sag is usually low. Maxi sag is located at Raoyang depression, Jizhong sub-basin and this paper is to discuss the sedimentary filling model and evolution law of Shahejie Formation which is one of the main petroleum exploration intervals. The differences of sedimentary facies type and the depositional model between the steep slope and gentle slope of the sag area were delineated. Furthermore, the depositional characteristics of the Shahejie Formation, the depositional filling models of different tectonic evolution periods of the sag area were analyzed. The sag area of rift basin had the depositional conditions of the reservoir existence, and it's the favorable area for the stratigraphic reservoirs. Therefore, the sag area could be an important area for future petroleum exploration of deep strata in the rift basin.
- sag in rift lacustrine basin,
- Maxi sag,
- depositional filling model,
- sedimentary evolution

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[1]	Soreghan M J, Cohen A S. Textural and compositional variability across littoral segments of Lake Tanganyika:The effect of asymmetric basin structure on sedimentation in large rift lakes[J]. AAPG Bulletin, 1996, 80(3):382~409. http://www.osti.gov/scitech/biblio/213052-textural-compositional-variability-across-littoral-segments-lake-tanganyika-effect-asymmetric-basin-structure-sedimentation-large-rift-lakes
[2]	朱筱敏.层序地层学[M].东营:中国石油大学出版社, 2000. ZHU Xiao-min. Sequence stratigraphy[M]. Dongying:China University of Petroleum Press, 2000.
[3]	Lambiase J J. A model for tectonic control of lacustrine stratigraphic sequences in continental rift basins[C]//Katz B J. Lacustrine basin exploration:Case studies and modern analogs. Tulsa:American Association of Petroleum Geologists, 1990:265~276.
[4]	林畅松, 李思田, 任建业.断陷湖盆层序地层学研究和计算机模拟——以二连盆地乌里雅斯太断陷为例[J].地学前缘, 1995, 2(3~4):124~132. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY503.017.htm LIN Chang-song, LI Si-tian, REN Jian-ye. Sequence architecture and depositional systems of Erlian lacustrine fault basins, north China[J]. Earth Science Frontiers, 1995, 2(3~4):124~132. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY503.017.htm
[5]	李金良, 樊太亮, 张岳桥.二连盆地白音查干凹陷层序地层及其油气勘探意义[J].地质力学学报, 2007, 13(1):60~69. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20070108&journal_id=dzlxxb LI Jin-liang, FAN Tai-liang, ZHANG Yue-qiao. Sequence stratigraphy of the Bayan Qagan subbasin in the Eren basin and applications for petrobleum exploration[J].Journal of Geomechanics, 2007, 13(1):60~69. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20070108&journal_id=dzlxxb
[6]	Ravnas R, Steel R J. Architecture of marine rift-basin successions[J]. AAPG Bulletin, 1998, 82(1):110~146. http://aapgbull.geoscienceworld.org/content/82/1/110
[7]	汤良杰, 金之钧, 贾承造, 等.叠合盆地构造解析几点思考[J].石油实验地质, 2001, 23(3):251~255. doi: 10.11781/sysydz200103251 TANG Liang-jie, JIN Zhi-jun, JIA Cheng-zao, et al. Tectonic analysis of superimposed basins[J]. Petroleum Geology and Experiment, 2001, 23(3):251~255. doi: 10.11781/sysydz200103251
[8]	刘刚, 董树文.前陆盆地层序地层与油气聚集[J].地质力学学报, 2007, 13(1):51~59. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20070107&journal_id=dzlxxb LIU Gang, DONG Shu-wen.Sequence stratigraphy and petroleum accumulation in foreland basins[J].Journal of Geomechanics, 2007, 13(1):51~59. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20070107&journal_id=dzlxxb
[9]	Carroll A R, Bohacs K M. Stratigraphic classification of ancient lakes:Balancing tectonic and climatic controls[J]. Geology, 1999, 27(2):99~102. doi: 10.1130/0091-7613(1999)027<0099:SCOALB>2.3.CO;2
[10]	邓宏文, 王红亮, ,宁宁.沉积物体积分配原理——高分辨率层序地层学的理论基础[J].地学前缘, 2000, 7(4):305~313. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200004000.htm DENG Hong-wen, WANG Hong-liang, NING Ning. Sediment volume partition principle:Theory basis for high-resolution sequence stratigraphy[J]. Earth Science Frontiers, 2000, 7(4):305~313. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200004000.htm
[11]	赵贤正, 金凤鸣, 王权, 等.华北探区断陷洼槽区油气藏形成与分布[J].中国石油勘探, 2008, 13(2):1~8. http://www.cnki.com.cn/Article/CJFDTOTAL-KTSY200802003.htm ZHAO Xian-zheng, JIN Feng-ming, WANG Quan, et al. Oil and gas reservoir formation and distribution in sags of fault depressions in Huabei exploration area[J]. China Petroleum Exploration, 2008, 13(2):1~8. http://www.cnki.com.cn/Article/CJFDTOTAL-KTSY200802003.htm
[12]	洪月英, 杜远生, 邓述全, 等.马西洼槽中南部区带综合评价[J].石油地球物理勘探, 2006, 41(增刊):86~93. http://www.cnki.com.cn/Article/CJFDTOTAL-SYDQ2006S1018.htm HONG Yue-ying, DU Yuan-sheng, DENG Shu-quan, et al. Comprehensive evaluation on the area of central south Maxi sag[J]. Oil Geophysical Prospecting, 2006, 41(Supp.) 86~93. http://www.cnki.com.cn/Article/CJFDTOTAL-SYDQ2006S1018.htm
[13]	崔殿, 查明, 高长海, 等.饶阳凹陷马西断层封闭性评价[J].科技导报, 2010, 28(19):30~35. http://www.cnki.com.cn/Article/CJFDTOTAL-KJDB201019017.htm CUI Dian, ZHA Ming, GAO Chang-hai, et al. Study on fault sealing of the Maxi fault in the Raoyang depression[J]. Science and Technology Review, 2010, 28(19):30~35. http://www.cnki.com.cn/Article/CJFDTOTAL-KJDB201019017.htm
[14]	吴孔友, 李继岩, 崔世凌, 等.断层成岩封闭及其应用[J].地质力学学报, 2011, 17(4):350~360. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLX201104006.htm WU Kong-you, LI Ji-yan, CUI Shi-ling, et al. Diagenetic sealing characteristics of faulting zone and its application[J].Journal of Geomechanics, 2011, 17(4):350~360. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLX201104006.htm
[15]	邹伟宏, 戴俊生, 王余泉, 等.饶阳凹陷构造成因分析[J].新疆石油地质, 2010, 31(5):463~466. http://www.cnki.com.cn/Article/CJFDTOTAL-XJSD201005008.htm ZOU Wei-hong, DAI Jun-sheng, WANG Yu-quan, et al. Analysis of structural genesis in Raoyang sag[J]. Xinjiang Petroleum Geology, 2010, 31(5):463~466. http://www.cnki.com.cn/Article/CJFDTOTAL-XJSD201005008.htm
[16]	于兴河, 姜辉, 李胜利, 等.中国东部中、新生代陆相断陷盆地沉积充填模式及其控制因素:以济阳坳陷东营凹陷为例[J].岩性油气藏, 2007, 19(1):39~45. http://www.cnki.com.cn/Article/CJFDTOTAL-YANX200701008.htm YU Xing-he, JIANG Hui, LI Sheng-li, et al. Depositional filling models and controlling factors on Mesozoic and Cenozoic fault basins of terrestrial facies in eastern China:A case study of Dongying sag of Jiyang depression[J]. Lithologic Reservoirs, 2007, 19(1):39~45. http://www.cnki.com.cn/Article/CJFDTOTAL-YANX200701008.htm
[17]	林宗满.论中国东部中、新生代大地构造的基本特征[J].地质力学学报, 2010, 16(3):246~259. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLX201003004.htm LIN Zong-man. General characteristics of the Mesozoic-Cenozoic tectonics in eastern China[J].Journal of Geomechanics, 2010, 16(3):246~259. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLX201003004.htm