Research on Structures Controlling the Development of Deep Sand Bodies in Dongying Depression

WU Kong-you; QIN Lei; TAN Ming-you; WANG Yue-yang

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Article Navigation > Acta Sedimentologica Sinica > 2014 > 32(5): 893-900

WU Kong-you, QIN Lei, TAN Ming-you, WANG Yue-yang. Research on Structures Controlling the Development of Deep Sand Bodies in Dongying Depression[J]. Acta Sedimentologica Sinica, 2014, 32(5): 893-900.

Citation:

WU Kong-you, QIN Lei, TAN Ming-you, WANG Yue-yang. Research on Structures Controlling the Development of Deep Sand Bodies in Dongying Depression[J]. Acta Sedimentologica Sinica, 2014, 32(5): 893-900.

Research on Structures Controlling the Development of Deep Sand Bodies in Dongying Depression

1.
School of Geosciences, China University of Petroleum, Qingdao, Shandong 266580;
2.
Geophysical Research Institute of SINOPEC, Shengli Oilfield Company, Dongying, Shandong 257022

Received Date: 2013-09-10
Rev Recd Date: 2014-04-04
Publish Date: 2014-10-10

Abstract

Faults and ancient valley-troughs controlled the development of deep sand bodies in Dongying depression by analyzing borehole data, seismic data and previous conclusion. The fault is key element to control the distribution of sand bodies in the northern part of Dongying depression. The sandstone distributes along downthrown side of main faults like skirt sides. The intensity of the faults activity decided the thickness of sandstone, the changing trend line of the fault throw is consistent with the thickness of sandbodies. The intensity of the faults activity also controlled the facies type of sandbodies. The deep faults activity gradually intensified from north to south in Dongying depression due to the northern-faulted and southern-overlapped structural setting, so the facies type of sandbodies are changed from nearshore subaqueous fans in the northern part to braided river deltas in the middle part and to fan deltas in the southern part. The ancient valley-troughs which include the fault troughs and the incised valley with extensive development obviously controlled the distribution of sandbodies in the southern part of Dongying depression as a result of the lack of the deep-large faults. The developing succession of the ancient valley-troughs resulted in the vertical superposition of sand bodies from Sha 4 member to Sha 3 member. At last, the formation patterns of deep sandbodies in Dongying depression were set up according to controlling factors.
- the deep bed of Dongying depression,
- faults controlling sand,
- valley-troughs controlling fan,
- formation patterns of sand bodies

References

[1]	李理, 钟大赉, 时秀朋. 鲁西隆起和济阳坳陷新生代隆坳耦合关系[J]. 地质学报, 2007, 81(9):1215-1225[Li Li, Zhong Dalai, Shi Xiupeng. Cenozoic uplifting/subsidence coupling between the west Shandong rise and the Jiyang depression, Northern China[J]. Acta Geologica Sinica, 2007, 81(9): 1215-1225]
[2]	杨辉, 程军, 王宜昌. 重新认识东营凹陷的深层构造[J]. 石油地球物理勘探, 2005, 40(3):360-365[Yang Hui, Cheng Jun, Wang Yichang. Renewing knowledge of deep structures of Dongying depression[J]. Oil Geophysical Prospecting, 2005, 40(3): 360-365]
[3]	任建业, 于建国, 张俊霞. 济阳坳陷深层构造及其对中新生代盆地发育的控制作用[J]. 地学前缘, 2009, 16(4):117-137[Ren Jianye, Yu Jianguo, Zhang Junxia. Structures of deep bed in Jiyang sag and their control over the development of Mesozoic and Cenozoic basins[J]. Earth Science Frontiers, 2009, 16(4): 117-137]
[4]	贾红义, 于建国, 王金铎. 东营凹陷深层构造剖析及其地质意义[J]. 油气地球物理, 2007, 5(1):59-64[Jia Hongyi, Yu Jianguo, Wang Jinduo.The analysis and geologic significance of the deep structures in Dongying sag[J]. Petroleum Geophysics, 2007, 5(1): 59-64]
[5]	贾红义, 于建国, 王金铎. 济阳坳陷深层构造层序划分[J]. 油气地球物理, 2007, 5(3):45-50[Jia Hongyi, Yu Jianguo, Wang Jinduo. Compartmentalization of deep structural sequence in Jiyang depression[J]. Petroleum Geophysics, 2007, 5(3): 45-50]
[6]	王健, 操应长, 刘惠民, 等. 东营凹陷沙四下亚段沉积环境特征及沉积充填模式[J]. 沉积学报, 2012, 30(2):274-282[Wang Jian, Cao Yingchang, Liu Huimin, et al. Characteristics of sedimentary environment and filling model of the lower submember of the fourth member of Shahejie Formation, Dongying depression[J]. Acta Sedimentologica Sinica, 2012, 30(2): 274-282]
[7]	姜华, 王建波, 张磊, 等. 南堡凹陷西南庄断层分段活动性及其对沉积的控制作用[J]. 沉积学报, 2010, 28(6):1047-1053[Jiang Hua, Wang Jianbo, Zhang Lei, et al. Segment activity of Xi'nanzhuang fault in Nanpu sag and its controlling on sedimentary process[J]. Acta Sedimentologica Sinica, 2010, 28(6): 1047-1053]
[8]	刘震, 李运振, 赵阳, 等. 济阳坳陷古近系多级控砂机制分析[J]. 地质学报, 2007, 81(5):701-711[Liu Zhen, Li Yunzhen, Zhao Yang, et al. Analysis of multi grade controlling of formation and distribution on Paleogene sand bodies in the Jiyang depression, Bohai Bay Basin[J]. Acta Geologica Sinica, 2007, 81(5): 701-711]
[9]	路智勇. 渤海湾盆地车镇凹陷古近系构造样式对沉积及储集层的影响[J]. 古地理学报, 2008, 10(3):276-285[Lu Zhiyong. Influence of the Paleogene structural styles on deposition and reservoir in Chezhen sag, Bohai Bay Basin[J]. Journal of Palaeogeography, 2008, 10(3): 276-285]
[10]	李勤英, 罗凤芝, 苗翠芝. 断层活动速率研究方法及应用探讨[J]. 断块油气田, 2000, 7(2):14-17[Li Qinying, Luo Fengzhi, Miao Cuizhi. Research on fault activity ratio and its application[J]. Fault-Block Oil & Gas Field, 2000, 7(2): 14-17]
[11]	王燮培. 石油勘探构造分析[M]. 北京:石油工业出版社, 1990:1-128[Wang Xiepei. Structural Analysis of Hydrocarbon Exploration[M]. Beijing: Petroleum Industry Press, 1990: 1-128]
[12]	张善文, 隋风贵, 王永诗. 济阳坳陷下第三系陡岸沉积模式[J]. 沉积学报, 2001, 19(2):219-222[Zhang Shanwen, Sui Fenggui, Wang Yongshi. Depositional models on the steep slope of Paleogene, Jiyang Sub-basin[J]. Acta Sedimentologica Sinica, 2001, 19(2): 219-222]
[13]	李桂范, 李建平, 王根照, 等. 渤中坳陷青东凹陷古近系沙三下亚段构造—古地貌对沉积的控制[J]. 石油与天然气地质, 2009, 30(4):425-430[Li Guifan, Li Jianping, Wang Genzhao, et al. Control of structure-paleogeomorphology on the deposition of the lower part of the third member of the Paleogene Shahejie Formation in the Qingdong sag of the Bozhong depression[J]. Oil & Gas Geology, 2009, 30(4): 425-430]
[14]	陶晓风, 刘登忠, 朱利东. 陆相盆地沉积作用与构造作用的关系[J]. 沉积学报, 2001, 19(3):410-414[Tao Xiaofeng, Liu Dengzhong, Zhu Lidong. Relationship between sedimentary process in terrestrial basin and tectonic process[J]. Acta Sedimentologica Sinica, 2001, 19(3): 410-414]
[15]	林畅松, 刘景彦, 胡博. 构造活动盆地沉积层序形成过程模拟——以断陷和前陆盆地为例[J]. 沉积学报, 2010, 28(5):868-874[Lin Changsong, Liu Jingyan, Hu Bo. Computer simulation on the formation of depositional sequences in tectonic active basin: Case study on rift and foreland basins[J]. Acta Sedimentologica Sinica, 2010, 28(5): 868-874]
[16]	林畅松, 潘元林, 肖建新, 等. 构造坡折带——断陷盆地层序分析和油气预测的重要概念[J]. 地球科学, 2000, 25(3):260-265[Lin Changsong, Pan Yuanlin, Xiao Jianxin, et al. Structural slope-break zone: key concept for stratigraphic sequence analysis and petroleum forecasting in fault subsidence basins[J]. Earth Science, 2000, 25(3): 260-265]
[17]	冯有良. 东营凹陷下第三系层序地层格架及盆地充填模式[J]. 地球科学, 1999, 24 (6):635-642[Feng Youliang. Lower Tertiary sequence stratigraphic framework and basin filling model in Dongying depression[J]. Earth Science, 1999, 24 (6): 635-642]
[18]	孔凡仙. 东营凹陷北带砂砾岩扇体勘探技术与实践[J]. 石油学报, 2000, 21(5):27-31[Kong Fanxian. Exploration technique and practice of sandy-conglomeratic fans in the northern part of Dongying depression[J]. Acta Petrolei Sinica, 2000, 21(5): 27-31]
[19]	操应长. 断陷湖盆中强制湖退沉积作用及其成因机制[J]. 沉积学报, 2005, 23(1):84-90[Cao Yingzhang. Sedimentation and its forming mechanism of the forced lacustrine regression in the rift lacustrine basin[J]. Acta Sedimentologica Sinica, 2005, 23(1): 84-90]
[20]	Gawthorpe R L, Hurst J M. Transfer zones in extensional basins: their structural style and influence on drainage development and stratigraphy[J]. Journal of Geology Society, 1993, 150(6): 1137-1152
[21]	Withjack M O, Islam Q T, La Pointe P R. Normal faults and their hanging-wall deformation: an experimental study[J]. AAPG Bulletin, 1995, 79(1): 1-18

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通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

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Research on Structures Controlling the Development of Deep Sand Bodies in Dongying Depression

1. School of Geosciences, China University of Petroleum, Qingdao, Shandong 266580;

2. Geophysical Research Institute of SINOPEC, Shengli Oilfield Company, Dongying, Shandong 257022

Received Date: 2013-09-10

Rev Recd Date: 2014-04-04

Publish Date: 2014-10-10

Key words:

Abstract: Faults and ancient valley-troughs controlled the development of deep sand bodies in Dongying depression by analyzing borehole data, seismic data and previous conclusion. The fault is key element to control the distribution of sand bodies in the northern part of Dongying depression. The sandstone distributes along downthrown side of main faults like skirt sides. The intensity of the faults activity decided the thickness of sandstone, the changing trend line of the fault throw is consistent with the thickness of sandbodies. The intensity of the faults activity also controlled the facies type of sandbodies. The deep faults activity gradually intensified from north to south in Dongying depression due to the northern-faulted and southern-overlapped structural setting, so the facies type of sandbodies are changed from nearshore subaqueous fans in the northern part to braided river deltas in the middle part and to fan deltas in the southern part. The ancient valley-troughs which include the fault troughs and the incised valley with extensive development obviously controlled the distribution of sandbodies in the southern part of Dongying depression as a result of the lack of the deep-large faults. The developing succession of the ancient valley-troughs resulted in the vertical superposition of sand bodies from Sha 4 member to Sha 3 member. At last, the formation patterns of deep sandbodies in Dongying depression were set up according to controlling factors.

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Reference (21)

[1]	李理, 钟大赉, 时秀朋. 鲁西隆起和济阳坳陷新生代隆坳耦合关系[J]. 地质学报, 2007, 81(9):1215-1225[Li Li, Zhong Dalai, Shi Xiupeng. Cenozoic uplifting/subsidence coupling between the west Shandong rise and the Jiyang depression, Northern China[J]. Acta Geologica Sinica, 2007, 81(9): 1215-1225]
[2]	杨辉, 程军, 王宜昌. 重新认识东营凹陷的深层构造[J]. 石油地球物理勘探, 2005, 40(3):360-365[Yang Hui, Cheng Jun, Wang Yichang. Renewing knowledge of deep structures of Dongying depression[J]. Oil Geophysical Prospecting, 2005, 40(3): 360-365]
[3]	任建业, 于建国, 张俊霞. 济阳坳陷深层构造及其对中新生代盆地发育的控制作用[J]. 地学前缘, 2009, 16(4):117-137[Ren Jianye, Yu Jianguo, Zhang Junxia. Structures of deep bed in Jiyang sag and their control over the development of Mesozoic and Cenozoic basins[J]. Earth Science Frontiers, 2009, 16(4): 117-137]
[4]	贾红义, 于建国, 王金铎. 东营凹陷深层构造剖析及其地质意义[J]. 油气地球物理, 2007, 5(1):59-64[Jia Hongyi, Yu Jianguo, Wang Jinduo.The analysis and geologic significance of the deep structures in Dongying sag[J]. Petroleum Geophysics, 2007, 5(1): 59-64]
[5]	贾红义, 于建国, 王金铎. 济阳坳陷深层构造层序划分[J]. 油气地球物理, 2007, 5(3):45-50[Jia Hongyi, Yu Jianguo, Wang Jinduo. Compartmentalization of deep structural sequence in Jiyang depression[J]. Petroleum Geophysics, 2007, 5(3): 45-50]
[6]	王健, 操应长, 刘惠民, 等. 东营凹陷沙四下亚段沉积环境特征及沉积充填模式[J]. 沉积学报, 2012, 30(2):274-282[Wang Jian, Cao Yingchang, Liu Huimin, et al. Characteristics of sedimentary environment and filling model of the lower submember of the fourth member of Shahejie Formation, Dongying depression[J]. Acta Sedimentologica Sinica, 2012, 30(2): 274-282]
[7]	姜华, 王建波, 张磊, 等. 南堡凹陷西南庄断层分段活动性及其对沉积的控制作用[J]. 沉积学报, 2010, 28(6):1047-1053[Jiang Hua, Wang Jianbo, Zhang Lei, et al. Segment activity of Xi'nanzhuang fault in Nanpu sag and its controlling on sedimentary process[J]. Acta Sedimentologica Sinica, 2010, 28(6): 1047-1053]
[8]	刘震, 李运振, 赵阳, 等. 济阳坳陷古近系多级控砂机制分析[J]. 地质学报, 2007, 81(5):701-711[Liu Zhen, Li Yunzhen, Zhao Yang, et al. Analysis of multi grade controlling of formation and distribution on Paleogene sand bodies in the Jiyang depression, Bohai Bay Basin[J]. Acta Geologica Sinica, 2007, 81(5): 701-711]
[9]	路智勇. 渤海湾盆地车镇凹陷古近系构造样式对沉积及储集层的影响[J]. 古地理学报, 2008, 10(3):276-285[Lu Zhiyong. Influence of the Paleogene structural styles on deposition and reservoir in Chezhen sag, Bohai Bay Basin[J]. Journal of Palaeogeography, 2008, 10(3): 276-285]
[10]	李勤英, 罗凤芝, 苗翠芝. 断层活动速率研究方法及应用探讨[J]. 断块油气田, 2000, 7(2):14-17[Li Qinying, Luo Fengzhi, Miao Cuizhi. Research on fault activity ratio and its application[J]. Fault-Block Oil & Gas Field, 2000, 7(2): 14-17]
[11]	王燮培. 石油勘探构造分析[M]. 北京:石油工业出版社, 1990:1-128[Wang Xiepei. Structural Analysis of Hydrocarbon Exploration[M]. Beijing: Petroleum Industry Press, 1990: 1-128]
[12]	张善文, 隋风贵, 王永诗. 济阳坳陷下第三系陡岸沉积模式[J]. 沉积学报, 2001, 19(2):219-222[Zhang Shanwen, Sui Fenggui, Wang Yongshi. Depositional models on the steep slope of Paleogene, Jiyang Sub-basin[J]. Acta Sedimentologica Sinica, 2001, 19(2): 219-222]
[13]	李桂范, 李建平, 王根照, 等. 渤中坳陷青东凹陷古近系沙三下亚段构造—古地貌对沉积的控制[J]. 石油与天然气地质, 2009, 30(4):425-430[Li Guifan, Li Jianping, Wang Genzhao, et al. Control of structure-paleogeomorphology on the deposition of the lower part of the third member of the Paleogene Shahejie Formation in the Qingdong sag of the Bozhong depression[J]. Oil & Gas Geology, 2009, 30(4): 425-430]
[14]	陶晓风, 刘登忠, 朱利东. 陆相盆地沉积作用与构造作用的关系[J]. 沉积学报, 2001, 19(3):410-414[Tao Xiaofeng, Liu Dengzhong, Zhu Lidong. Relationship between sedimentary process in terrestrial basin and tectonic process[J]. Acta Sedimentologica Sinica, 2001, 19(3): 410-414]
[15]	林畅松, 刘景彦, 胡博. 构造活动盆地沉积层序形成过程模拟——以断陷和前陆盆地为例[J]. 沉积学报, 2010, 28(5):868-874[Lin Changsong, Liu Jingyan, Hu Bo. Computer simulation on the formation of depositional sequences in tectonic active basin: Case study on rift and foreland basins[J]. Acta Sedimentologica Sinica, 2010, 28(5): 868-874]
[16]	林畅松, 潘元林, 肖建新, 等. 构造坡折带——断陷盆地层序分析和油气预测的重要概念[J]. 地球科学, 2000, 25(3):260-265[Lin Changsong, Pan Yuanlin, Xiao Jianxin, et al. Structural slope-break zone: key concept for stratigraphic sequence analysis and petroleum forecasting in fault subsidence basins[J]. Earth Science, 2000, 25(3): 260-265]
[17]	冯有良. 东营凹陷下第三系层序地层格架及盆地充填模式[J]. 地球科学, 1999, 24 (6):635-642[Feng Youliang. Lower Tertiary sequence stratigraphic framework and basin filling model in Dongying depression[J]. Earth Science, 1999, 24 (6): 635-642]
[18]	孔凡仙. 东营凹陷北带砂砾岩扇体勘探技术与实践[J]. 石油学报, 2000, 21(5):27-31[Kong Fanxian. Exploration technique and practice of sandy-conglomeratic fans in the northern part of Dongying depression[J]. Acta Petrolei Sinica, 2000, 21(5): 27-31]
[19]	操应长. 断陷湖盆中强制湖退沉积作用及其成因机制[J]. 沉积学报, 2005, 23(1):84-90[Cao Yingzhang. Sedimentation and its forming mechanism of the forced lacustrine regression in the rift lacustrine basin[J]. Acta Sedimentologica Sinica, 2005, 23(1): 84-90]
[20]	Gawthorpe R L, Hurst J M. Transfer zones in extensional basins: their structural style and influence on drainage development and stratigraphy[J]. Journal of Geology Society, 1993, 150(6): 1137-1152
[21]	Withjack M O, Islam Q T, La Pointe P R. Normal faults and their hanging-wall deformation: an experimental study[J]. AAPG Bulletin, 1995, 79(1): 1-18

Research on Structures Controlling the Development of Deep Sand Bodies in Dongying Depression

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