The Provenance Transformation and Sedimentary Filling Response of Paleogene Dongying Formation in Western Slope of Bozhong Sag

LI Huan; YANG XiangHua; ZHU HongTao; ZHOU XinHuai; LI JianPing

doi:10.14027/j.cnki.cjxb.2015.01.004

Volume 33 Issue 1

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LI Huan, YANG XiangHua, ZHU HongTao, ZHOU XinHuai, LI JianPing. The Provenance Transformation and Sedimentary Filling Response of Paleogene Dongying Formation in Western Slope of Bozhong Sag[J]. Acta Sedimentologica Sinica, 2015, 33(1): 36-48. doi: 10.14027/j.cnki.cjxb.2015.01.004

Citation:

LI Huan, YANG XiangHua, ZHU HongTao, ZHOU XinHuai, LI JianPing. The Provenance Transformation and Sedimentary Filling Response of Paleogene Dongying Formation in Western Slope of Bozhong Sag[J]. Acta Sedimentologica Sinica, 2015, 33(1): 36-48. doi: 10.14027/j.cnki.cjxb.2015.01.004

The Provenance Transformation and Sedimentary Filling Response of Paleogene Dongying Formation in Western Slope of Bozhong Sag

doi: 10.14027/j.cnki.cjxb.2015.01.004

1.
Key Laboratory of Tectonics and Petroleum Resources of the Ministry of Education, China University of Geosciences, Wuhan 430074;
2.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074;
3.
China National Offshore Oil Corporation Limited-Tianjin, Tianjin 300452

Received Date: 2013-10-28
Rev Recd Date: 2014-04-09
Publish Date: 2015-02-10

Abstract

Through comprehensive analysis of U-Pb age analysis of detrital zircons in sandstones, change of the content of tephra component, seismic multi-attributes analysis, sequence stratigraphic framework and sedimentary filling, considering that in the Donger member sedimentary period, the provenance supply mode, the sequence stratigraphic framework and sedimentary filling characteristics of the west of Bozhong sag changed obviously. In the sedimentation of SQd_2L and it's earlier stage, lake basin was in the intense rift stage, structure activities were intense, basin was interphase concave-convex, sedimentation rate of the basin was accelerated, depth of water deepened, stratum deposited thickly as a whole, lithology were mainly gray-dark grey mudstones conainning lamina medium-fine sandstones and siltstones, granularity was fine as a whole, provenance was mainly the local provenance like Shijiutuo uplift and Shaleitian uplift and Mesozoic igneous rock basement inside the basin, et al, content of tephra in sandstones was high, Mesozoic zircons were also rich, seismic multi-attributes ichnography show that sandstones in the Shijiutuo uplift and Shaleitian uplift two sides were rich, area of red zone is large, sedimentary sequence was obviously controlled by the lower uplifts inside the basin and faults around them, sequence characteristics have remarkable differences between the direction parallel and perpendicular to the provenance, in the direction parallel to the provenance, sequence at Shaleitian side was ansymmetrical cycle which took declining half cycle as principal, it's GR electrical characteristics were smooth finger, the braided river delta sand bodies which distributed approximately to EW were developed, however, sequence at Shijiutuo uplift side took LST which was rising half cycle as principal, it's GR electrical characteristics were infundibulate and box combination, multi-phase fan delta lobes were developed, in the seismic section passing the fan along the provenance direction at the two uplifts, typical foreset features were visible. In the direction perpendicular to the provenance, however, there mainly no significant difference, sequence was ansymmetrical cycle which took declining half cycle mainly, it's GR electrical characteristics were medium-high amplitude finger, shore shallow lake-braided river delta facies were developed; After the sedimentation of SQd_2L, lake basin was in the fault depression-depression transition period, area of lake basin was large, depth of water was shallow, fault activities around the lower uplifts inside the basin weakened obviously, stratum was thin as a whole, lithology were primarily conglomeratic sandstones, medium-fine sandstones and siltstones, monolithic granularity was fine, clastics inside basin were mainly came from Yanshan tectonic belt (regional provenance) in the northwest part of the sag, content of tephra in sandstones reduced visibly, detrital zircons in sandstones were primarily Proterozoic zircons, seismic multi-attributes ichnography show that distribution area of red zone decreased obviously, depositional sequence overlapped toward low uplifts inside basin, sequence characeristics have little differences between the direction parallel and perpendicular to the provenance, sequence was primarily ansymmetrical cycle which took declining half cycle chiefly, it's GR electrical characteristics were low amplitude finger and dentation, proximal fan delta sand bodies transformed gradually to distal braided river delta sand bodies, at the same time, broad shore shallow lake environment was developed. In Paleogene sedimentary filling process of the western slope of Bozhong sag, the consistent changes of the stratigraphic pattern, sedimentary mode and provenance supply mode reflect the inherent law of filling evolution of the rifted basin, provide new clues for evolution and division of rift-subsidence cycles of the rifted basins in the eastern part of our country.
- western slope of Bozhong sag,
- Dongying member,
- provenance transformation,
- sequence stratigraphic framework,
- sedimentary filling

References

[1]	Klemme H D. Petroleum basins-classifications and characteristics[J]. Journal of Petroleum Geology, 1980, 3(2):187-207.
[2]	焦养泉,周海民,刘少峰,等. 断陷盆地多层次幕式裂陷作用与沉积充填响应—以南堡老第三纪断陷盆地为例[J]. 地球科学,1996,21(6):633-636. [Jiao Yangquan, Zhou Haimin, Liu Shaofeng, et al. Multistage episodic rifting and its controls on filling in rift basin: Taking the Eogene Nanpu rift basin as an example[J]. Earth Science, 1996, 21(6): 633-636.]
[3]	廖计华,王华,肖军,等. 琼东南盆地古近纪幕式裂陷及构造、层序和沉积的综合响应过程[J]. 吉林大学学报:地球科学版,2012,42(4):970-983. [Liao Jihua, Wang Hua, Xiao Jun, et al. Episodic rifting and integrated response process of tectonic, sequence stratigraphy and sedimentary filling in Paleogene of Qiongdongnan Basin, South China Sea[J]. Journal of Jilin University: Earth Science Edition, 2012, 42(4): 970-983.]
[4]	林畅松,张燕梅,李思田,等. 中国东部中新生代断陷盆地幕式裂陷过程的动力学响应和模拟模型[J]. 地球科学,2004,29(5):583-588. [Lin Changsong, Zhang Yanmei, Li Sitian, et al. Episodic rifting dynamic process and quantitative model of Mesozoic-Cenozoic faulted basins in eastern China [J]. Earth Science, 2004, 29(5): 583-588.]
[5]	李敏. 渤中凹陷西斜坡古近系东营组沉积物源体系研究[D]. 武汉:中国地质大学(武汉),2012.[Li Min. Sediment provenance system analysis of Paleogene Dongying Formation in western slope of Bozhong sag, Bohai Bay Basin[D]. Wuhan: China University of Geosciences(Wuhan), 2012.]
[6]	吴崇筠,薛书浩. 中国含油气盆地沉积学[M]. 北京:石油工业出版社,1992. [Wu Chongjun, Xue Shuhao. Sedimentology of Petroliferous Basin in China[M]. Beijing: Petroleum Industry Press, 1992.]
[7]	胡望水,王家林. 松辽裂陷盆地伸展构造演化与油气[J]. 石油勘探与开发,1996,23(3):30-33. [Hu Wangshui, Wang Jialin. Extensional tectonic evolution and petroleum accumulation in Songliao rift Basin[J]. Petroleum Exploration and Development, 1996, 23(3): 30-33.]
[8]	郭少斌. 陆相断陷盆地层序地层模式[J]. 石油勘探与开发,2006,33(5):548-552. [Guo Shaobin. Sequence stratigraphy pattern of the terrestrial rifted basin[J]. Petroleum Exploration and Development, 2006, 33(5): 548-552.]
[9]	单敬福, 葛黛薇, 乐江华,等. 松辽盆地东南缘层序地层与沉积体系配置及演化——以梨树断陷西北部营城组地层为例[J]. 沉积学报,2013,31(1):67-76. [Shan Jingfu, Ge Daiwei, Le Jianghua, et al. Framework of sequence stratigraphy, sedimentary system and evolution of southeastern Songliao Basin: An example from Yingcheng Formation in Lishu fault depression[J]. Acta Sedimentologica Sinica, 2013, 31(1): 67-76.]
[10]	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. [Yu Xinghe, Jiang Hui, Li Shengli, 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.]
[11]	池英柳,赵文智. 渤海湾盆地新生代走滑构造与油气聚集[J]. 石油学报,2000,21(2):14-20. [Chi Yingliu, Zhao Wenzhi. Strike-slip deformation during the Cenozoic and its influence on hydrocarbon accumulation in Bohai Bay Basin[J]. Acta Petrolei Sinica, 2000, 21(2): 14-20.]
[12]	杨运海. 物源分析的几种方法[J]. 内江科技,2009(12):21-21. [Yang Yunhai. Several methods of provenance analysis[J]. Neijiang Science & Technology, 2009(12): 21-21.]
[13]	赵红格,刘池洋. 物源分析方法及研究进展[J]. 沉积学报,2003,21(3):409-415. [Zhao Hongge, Liu Chiyang. Approaches and prospects of provenance analysis [J]. Acta Sedimentologica Sinica, 2003, 21(3): 409-415.]
[14]	吴元保,郑永飞. 锆石成因矿物学研究及其对U-Pb年龄解释的制约[J]. 科学通报,2004,49(16):1589-1604. [Wu Yuanbao, Zheng Yongfei. Genetic mineralogy research of zircon and its constraint on explanation of U-Pb age[J]. Chinese Science Bulletin, 2004, 49(16): 1589-1604.]
[15]	闫义,林舸,李自安. 利用锆石形态、成分组成及年龄分析进行沉积物源区示踪的综合研究[J]. 大地构造与成矿学,2003,27(2):184-190. [Yan Yi, Lin Ge, Li Zian. Provenance tracing of sediments by means of synthetic study of shape, composition and chronology of zircon[J]. Geotectonica et Metallogenia, 2003, 27(2): 184-190.]
[16]	周剑雄,陈振宇. 锆石等测年矿物的电子探针及阴极射线致发光综合研究新方法[J]. 地质论评,2002,48(增刊4):31-35. [Zhou Jianxiong, Chen Zhenyu. A new Integrated method for dating minerals like zircon using electron microprobe and cathodoluminescence[J]. Geological Review, 2002, 48(Suppl.4): 31-35.]
[17]	Corfu F, Hanchar J M, Hoskin P W O, et al. Atlas of zircon textures[J]. Reviews in Mineralogy & Geochemistry, 2003, 53(1): 469-500.
[18]	移根旺. 锆石成因矿物学研究[J]. 中国水运,2008,8(6):259-260. [Yi Genwang. Genetic mineralogy research of zircon[J]. China Water Transport, 2008, 8(6): 259-260.]
[19]	陈道公,李彬贤,夏群科,等. 变质岩中锆石U-Pb计时问题评述——兼论大别造山带锆石定年[J]. 岩石学报,2001,17(1):129-138. [Chen Daogong, Li Binxian, Xia Qunke, et al. An evaluation of zircon U-Pb dating for metamorphic rocks and comments on zircon ages of Dabie orogen[J]. Acta Petrologica Sinica, 2001, 17(1): 129-138.]
[20]	Liu Yongsheng, Hu Zhaochu, Gao Shan, et al. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard[J]. Chemical Geology, 2008, 257(1/2): 34-43.
[21]	Liu Yongsheng, Gao Shan, Hu Zhaochu, et al. Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans-North China Orogen: U-Pb dating, Hf isotopes and trace elements in zircons of mantle xenoliths[J]. Journal of Petrology, 2010, 51(1/2): 537-571.
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[25]	朱红涛,杨香华,周心怀,等. 基于层序地层学和地震沉积学的高精度三维沉积体系——以渤中凹陷西斜坡BZ3-1区块东营组为例[J]. 地球科学,2011,36(6):1073-1084. [Zhu Hongtao, Yang Xianghua, Zhou Xinhuai, et al. High resolution three-dimensional facies architecture delineation using sequence stratigraphy, seismic sedimentology: Example from Dongying Formation in BZ3-1 block of western slope of Bozhong sag, Bohai Bay Basin[J]. Earth Science, 2011, 36(6): 1073-1084.]

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The Provenance Transformation and Sedimentary Filling Response of Paleogene Dongying Formation in Western Slope of Bozhong Sag

1. Key Laboratory of Tectonics and Petroleum Resources of the Ministry of Education, China University of Geosciences, Wuhan 430074;

2. Faculty of Earth Resources, China University of Geosciences, Wuhan 430074;

3. China National Offshore Oil Corporation Limited-Tianjin, Tianjin 300452

Received Date: 2013-10-28

Rev Recd Date: 2014-04-09

Publish Date: 2015-02-10

Key words:

Abstract: Through comprehensive analysis of U-Pb age analysis of detrital zircons in sandstones, change of the content of tephra component, seismic multi-attributes analysis, sequence stratigraphic framework and sedimentary filling, considering that in the Donger member sedimentary period, the provenance supply mode, the sequence stratigraphic framework and sedimentary filling characteristics of the west of Bozhong sag changed obviously. In the sedimentation of SQd_2L and it's earlier stage, lake basin was in the intense rift stage, structure activities were intense, basin was interphase concave-convex, sedimentation rate of the basin was accelerated, depth of water deepened, stratum deposited thickly as a whole, lithology were mainly gray-dark grey mudstones conainning lamina medium-fine sandstones and siltstones, granularity was fine as a whole, provenance was mainly the local provenance like Shijiutuo uplift and Shaleitian uplift and Mesozoic igneous rock basement inside the basin, et al, content of tephra in sandstones was high, Mesozoic zircons were also rich, seismic multi-attributes ichnography show that sandstones in the Shijiutuo uplift and Shaleitian uplift two sides were rich, area of red zone is large, sedimentary sequence was obviously controlled by the lower uplifts inside the basin and faults around them, sequence characteristics have remarkable differences between the direction parallel and perpendicular to the provenance, in the direction parallel to the provenance, sequence at Shaleitian side was ansymmetrical cycle which took declining half cycle as principal, it's GR electrical characteristics were smooth finger, the braided river delta sand bodies which distributed approximately to EW were developed, however, sequence at Shijiutuo uplift side took LST which was rising half cycle as principal, it's GR electrical characteristics were infundibulate and box combination, multi-phase fan delta lobes were developed, in the seismic section passing the fan along the provenance direction at the two uplifts, typical foreset features were visible. In the direction perpendicular to the provenance, however, there mainly no significant difference, sequence was ansymmetrical cycle which took declining half cycle mainly, it's GR electrical characteristics were medium-high amplitude finger, shore shallow lake-braided river delta facies were developed; After the sedimentation of SQd_2L, lake basin was in the fault depression-depression transition period, area of lake basin was large, depth of water was shallow, fault activities around the lower uplifts inside the basin weakened obviously, stratum was thin as a whole, lithology were primarily conglomeratic sandstones, medium-fine sandstones and siltstones, monolithic granularity was fine, clastics inside basin were mainly came from Yanshan tectonic belt (regional provenance) in the northwest part of the sag, content of tephra in sandstones reduced visibly, detrital zircons in sandstones were primarily Proterozoic zircons, seismic multi-attributes ichnography show that distribution area of red zone decreased obviously, depositional sequence overlapped toward low uplifts inside basin, sequence characeristics have little differences between the direction parallel and perpendicular to the provenance, sequence was primarily ansymmetrical cycle which took declining half cycle chiefly, it's GR electrical characteristics were low amplitude finger and dentation, proximal fan delta sand bodies transformed gradually to distal braided river delta sand bodies, at the same time, broad shore shallow lake environment was developed. In Paleogene sedimentary filling process of the western slope of Bozhong sag, the consistent changes of the stratigraphic pattern, sedimentary mode and provenance supply mode reflect the inherent law of filling evolution of the rifted basin, provide new clues for evolution and division of rift-subsidence cycles of the rifted basins in the eastern part of our country.

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Reference (25)

[1]	Klemme H D. Petroleum basins-classifications and characteristics[J]. Journal of Petroleum Geology, 1980, 3(2):187-207.
[2]	焦养泉,周海民,刘少峰,等. 断陷盆地多层次幕式裂陷作用与沉积充填响应—以南堡老第三纪断陷盆地为例[J]. 地球科学,1996,21(6):633-636. [Jiao Yangquan, Zhou Haimin, Liu Shaofeng, et al. Multistage episodic rifting and its controls on filling in rift basin: Taking the Eogene Nanpu rift basin as an example[J]. Earth Science, 1996, 21(6): 633-636.]
[3]	廖计华,王华,肖军,等. 琼东南盆地古近纪幕式裂陷及构造、层序和沉积的综合响应过程[J]. 吉林大学学报:地球科学版,2012,42(4):970-983. [Liao Jihua, Wang Hua, Xiao Jun, et al. Episodic rifting and integrated response process of tectonic, sequence stratigraphy and sedimentary filling in Paleogene of Qiongdongnan Basin, South China Sea[J]. Journal of Jilin University: Earth Science Edition, 2012, 42(4): 970-983.]
[4]	林畅松,张燕梅,李思田,等. 中国东部中新生代断陷盆地幕式裂陷过程的动力学响应和模拟模型[J]. 地球科学,2004,29(5):583-588. [Lin Changsong, Zhang Yanmei, Li Sitian, et al. Episodic rifting dynamic process and quantitative model of Mesozoic-Cenozoic faulted basins in eastern China [J]. Earth Science, 2004, 29(5): 583-588.]
[5]	李敏. 渤中凹陷西斜坡古近系东营组沉积物源体系研究[D]. 武汉:中国地质大学(武汉),2012.[Li Min. Sediment provenance system analysis of Paleogene Dongying Formation in western slope of Bozhong sag, Bohai Bay Basin[D]. Wuhan: China University of Geosciences(Wuhan), 2012.]
[6]	吴崇筠,薛书浩. 中国含油气盆地沉积学[M]. 北京:石油工业出版社,1992. [Wu Chongjun, Xue Shuhao. Sedimentology of Petroliferous Basin in China[M]. Beijing: Petroleum Industry Press, 1992.]
[7]	胡望水,王家林. 松辽裂陷盆地伸展构造演化与油气[J]. 石油勘探与开发,1996,23(3):30-33. [Hu Wangshui, Wang Jialin. Extensional tectonic evolution and petroleum accumulation in Songliao rift Basin[J]. Petroleum Exploration and Development, 1996, 23(3): 30-33.]
[8]	郭少斌. 陆相断陷盆地层序地层模式[J]. 石油勘探与开发,2006,33(5):548-552. [Guo Shaobin. Sequence stratigraphy pattern of the terrestrial rifted basin[J]. Petroleum Exploration and Development, 2006, 33(5): 548-552.]
[9]	单敬福, 葛黛薇, 乐江华,等. 松辽盆地东南缘层序地层与沉积体系配置及演化——以梨树断陷西北部营城组地层为例[J]. 沉积学报,2013,31(1):67-76. [Shan Jingfu, Ge Daiwei, Le Jianghua, et al. Framework of sequence stratigraphy, sedimentary system and evolution of southeastern Songliao Basin: An example from Yingcheng Formation in Lishu fault depression[J]. Acta Sedimentologica Sinica, 2013, 31(1): 67-76.]
[10]	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. [Yu Xinghe, Jiang Hui, Li Shengli, 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.]
[11]	池英柳,赵文智. 渤海湾盆地新生代走滑构造与油气聚集[J]. 石油学报,2000,21(2):14-20. [Chi Yingliu, Zhao Wenzhi. Strike-slip deformation during the Cenozoic and its influence on hydrocarbon accumulation in Bohai Bay Basin[J]. Acta Petrolei Sinica, 2000, 21(2): 14-20.]
[12]	杨运海. 物源分析的几种方法[J]. 内江科技,2009(12):21-21. [Yang Yunhai. Several methods of provenance analysis[J]. Neijiang Science & Technology, 2009(12): 21-21.]
[13]	赵红格,刘池洋. 物源分析方法及研究进展[J]. 沉积学报,2003,21(3):409-415. [Zhao Hongge, Liu Chiyang. Approaches and prospects of provenance analysis [J]. Acta Sedimentologica Sinica, 2003, 21(3): 409-415.]
[14]	吴元保,郑永飞. 锆石成因矿物学研究及其对U-Pb年龄解释的制约[J]. 科学通报,2004,49(16):1589-1604. [Wu Yuanbao, Zheng Yongfei. Genetic mineralogy research of zircon and its constraint on explanation of U-Pb age[J]. Chinese Science Bulletin, 2004, 49(16): 1589-1604.]
[15]	闫义,林舸,李自安. 利用锆石形态、成分组成及年龄分析进行沉积物源区示踪的综合研究[J]. 大地构造与成矿学,2003,27(2):184-190. [Yan Yi, Lin Ge, Li Zian. Provenance tracing of sediments by means of synthetic study of shape, composition and chronology of zircon[J]. Geotectonica et Metallogenia, 2003, 27(2): 184-190.]
[16]	周剑雄,陈振宇. 锆石等测年矿物的电子探针及阴极射线致发光综合研究新方法[J]. 地质论评,2002,48(增刊4):31-35. [Zhou Jianxiong, Chen Zhenyu. A new Integrated method for dating minerals like zircon using electron microprobe and cathodoluminescence[J]. Geological Review, 2002, 48(Suppl.4): 31-35.]
[17]	Corfu F, Hanchar J M, Hoskin P W O, et al. Atlas of zircon textures[J]. Reviews in Mineralogy & Geochemistry, 2003, 53(1): 469-500.
[18]	移根旺. 锆石成因矿物学研究[J]. 中国水运,2008,8(6):259-260. [Yi Genwang. Genetic mineralogy research of zircon[J]. China Water Transport, 2008, 8(6): 259-260.]
[19]	陈道公,李彬贤,夏群科,等. 变质岩中锆石U-Pb计时问题评述——兼论大别造山带锆石定年[J]. 岩石学报,2001,17(1):129-138. [Chen Daogong, Li Binxian, Xia Qunke, et al. An evaluation of zircon U-Pb dating for metamorphic rocks and comments on zircon ages of Dabie orogen[J]. Acta Petrologica Sinica, 2001, 17(1): 129-138.]
[20]	Liu Yongsheng, Hu Zhaochu, Gao Shan, et al. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard[J]. Chemical Geology, 2008, 257(1/2): 34-43.
[21]	Liu Yongsheng, Gao Shan, Hu Zhaochu, et al. Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans-North China Orogen: U-Pb dating, Hf isotopes and trace elements in zircons of mantle xenoliths[J]. Journal of Petrology, 2010, 51(1/2): 537-571.
[22]	Liu Yongsheng, Hu Zhaochu, Zong Keqing, et al. Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS[J]. Chinese Science Bulletin, 2010, 55(15): 1535-1546.
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The Provenance Transformation and Sedimentary Filling Response of Paleogene Dongying Formation in Western Slope of Bozhong Sag

doi: 10.14027/j.cnki.cjxb.2015.01.004

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通讯作者: 陈斌, bchen63@163.com

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