Establishment and Application of Geological Data Base on Deep-water Channels in Angola Block

ZHANG WenBiao; LIU ZhiQiang; CHEN ZhiHai; XU HuaMing; LIN Yu; WANG JingWei

doi:10.14027/j.cnki.cjxb.2015.01.015

Volume 33 Issue 1

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ZHANG WenBiao, LIU ZhiQiang, CHEN ZhiHai, XU HuaMing, LIN Yu, WANG JingWei. Establishment and Application of Geological Data Base on Deep-water Channels in Angola Block[J]. Acta Sedimentologica Sinica, 2015, 33(1): 142-152. doi: 10.14027/j.cnki.cjxb.2015.01.015

Citation:

ZHANG WenBiao, LIU ZhiQiang, CHEN ZhiHai, XU HuaMing, LIN Yu, WANG JingWei. Establishment and Application of Geological Data Base on Deep-water Channels in Angola Block[J]. Acta Sedimentologica Sinica, 2015, 33(1): 142-152. doi: 10.14027/j.cnki.cjxb.2015.01.015

Establishment and Application of Geological Data Base on Deep-water Channels in Angola Block

doi: 10.14027/j.cnki.cjxb.2015.01.015

1.
Petroleum Exploration and Production Research Institute, SINOPEC, Beijing 100083;
2.
Research Centre of Reservoir Geophysics, BGP Inc. of CNPC, Zhuozhou, Hebei 072750

Received Date: 2014-03-07
Rev Recd Date: 2014-05-12
Publish Date: 2015-02-10

Abstract

To establish a quantitative geologic database at composite and single channel level for deep water slope channel systems in Angola, the characteristics and their quantitative relationships were carefully studied based on high frequency 3D seismic profile, slice and attribute data of shallow Pliocene deposits. The results indicate that the single channel activity pattern is somewhat similar to the point bar model in a meandering river. It migrates only in lateral direction (orthogonal to the paleocurrent direction) without "downstream sweep" component, and the lateral accretion composites form a "concentric half ring" shape in plane view, whereas the sandbodies fill in the axis by vertical accretion, and thinning towards channel edge. Good positive correlations can be widely observed between width and depth, meander-arc height and sinuosity in single channels. Based on the single channel activity pattern, the composite channel pattern can be classified into 3 types as (Ⅰ) lateral migration, (Ⅱ) inclined migration, and (Ⅲ) swing migration. Type (Ⅰ) develops in higher sinuosity section (sinuosity>1.3), whereas type (Ⅱ) and type (Ⅲ) develops mainly in lower sinuosity section (1
- deep-water channel,
- geological knowledge base,
- object-based modeling,
- Angola

References

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Establishment and Application of Geological Data Base on Deep-water Channels in Angola Block

1. Petroleum Exploration and Production Research Institute, SINOPEC, Beijing 100083;

2. Research Centre of Reservoir Geophysics, BGP Inc. of CNPC, Zhuozhou, Hebei 072750

Received Date: 2014-03-07

Rev Recd Date: 2014-05-12

Publish Date: 2015-02-10

Key words:

Abstract: To establish a quantitative geologic database at composite and single channel level for deep water slope channel systems in Angola, the characteristics and their quantitative relationships were carefully studied based on high frequency 3D seismic profile, slice and attribute data of shallow Pliocene deposits. The results indicate that the single channel activity pattern is somewhat similar to the point bar model in a meandering river. It migrates only in lateral direction (orthogonal to the paleocurrent direction) without "downstream sweep" component, and the lateral accretion composites form a "concentric half ring" shape in plane view, whereas the sandbodies fill in the axis by vertical accretion, and thinning towards channel edge. Good positive correlations can be widely observed between width and depth, meander-arc height and sinuosity in single channels. Based on the single channel activity pattern, the composite channel pattern can be classified into 3 types as (Ⅰ) lateral migration, (Ⅱ) inclined migration, and (Ⅲ) swing migration. Type (Ⅰ) develops in higher sinuosity section (sinuosity>1.3), whereas type (Ⅱ) and type (Ⅲ) develops mainly in lower sinuosity section (1

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Reference (42)

[1]	Bouma A H. Introduction to submarine fans and related turbidite systems[C]//Bouma H, Normark W R, Barnes N E. Submarine Fans and Related Turbidite Systems. New York: Springer-Verlag, 1985: 3-5.
[2]	Walker R G. Deep-water sandstone facies and ancient submarine fans: Models for exploration for stratigraphic traps[J]. AAPG Bulletin, 1978, 62(6): 932-966.
[3]	Mutti E, Normark W R. Comparing examples of modern and ancient turbidite systems: Problems and concepts[M]//Leggett J K, Zuffa G G. Marine Clastic Sedimentology. London: Graham and Trotman, 1987: 1-38.
[4]	BrocherayS, Cremer M, Zaragosi S, et al. 2000 years of frequent turbidite activity in the Capbreton Canyon (Bay of Biscay)[J]. Marine Geology, 2014, 347: 136-152
[5]	吕明,王颖,陈莹. 尼日利亚深水区海底扇沉积模式成因探讨及勘探意义[J]. 中国海上油气,2008,20(4):275-282.[Lü Ming, Wang Ying, Chen Ying. A discussion on origins of submarine fan deposition model and its exploration significance in Nigeria deep-water area[J]. China Offshore Oil and Gas, 20(4): 275-282.]
[6]	李磊,王英民,黄志超,等. 尼日尔三角洲深水区层序地层及地震相研究[J]. 沉积学报,2008, 26(3):407-416. [Li Lei, Wang Yingmin, Huang Zhichao, et al. Study on sequence stratigraphy and seismic facies in deep-water Niger Delta[J].Acta Sedimentologica Sinica, 2008, 26(3): 407-416.]
[7]	李胜利,于兴河,谢玉洪,等. 滨浅海泥流沟谷识别标志、类型及沉积模式——以莺歌海盆地东方1-1气田为例[J]. 沉积学报,2010,28(6):1076-1080.[Li Shengli, Yu Xinghe, Xie Yuhong, et al. Mud flow gully identification mark, type and deposition model in the littoral and neritic marine: A case study of Dongfang1-1 gas field in Yinggehai Basin[J]. Acta Sedimentologica Sinica, 2010, 28(6): 1076-1080.]
[8]	赵晓明,吴胜和,刘丽. 西非陆坡区深水复合水道沉积构型模式[J]. 中国石油大学学报:自然科学版,2012,36(6):1-5.[Zhao Xiaoming, Wu Shenghe, Liu Li. Sedimentary architecture model of deep-water channel complexes in slope area of West Africa[J]. Journal of China University of Petroleum, 2012, 36(6): 1-5.]
[9]	于水,程涛,陈莹. 尼日尔三角洲盆地深水沉积体系特征[J]. 地球科学,2012,37(4):763-770.[Yu Shui, Cheng Tao, Chen Ying. Depositional characteristics of deepwater systems in the Niger Delta Basin[J]. Earth Science, 2012, 37(4): 763-770.]
[10]	李胜利,于兴河,刘玉梅,等. 水道加朵体型深水扇形成机制与模式——以白云凹陷荔湾3-1地区珠江组为例[J]. 地学前缘,2012,19(2):32-40.[Li Shengli, Yu Xinghe, Liu Yumei, et al. Formation mechanism and pattern of deep-water fan with channel and lobe: A case study of the Zhujiang Formation in Liwan3-1 area, Baiyun depression [J]. Earth Science Frontiers, 2012, 19(2): 32-40.]
[11]	Clarke J D,Pickering K T. Submarine Channels: Processes and Architecture[M]. London: Vallis Press, 1996.
[12]	Sawyer D E, Flemings P B, Shipp R C,et al. Seismic geomorphology, lithology, and evolution of the Late Pleistocene Mars-Ursa turbidite region, Mississippi Canyon area, northern Gulf of Mexico[J]. AAPG Bulletin, 2007, 91(2): 215-234.
[13]	McDonnell A, Loucks R G, Galloway W E. Paleocene to Eocene deep-water slope canyons, western Gulf of Mexico: Further insights for the provenance of deep-water offshore Wilcox Group plays[J]. AAPG Bulletin, 2008, 92(9):1169-1189.
[14]	Labourdette R, Bez M. Element migration in turbidite systems: Random or systematic depositional processes[J]. AAPG Bulletin, 2010, 94(3): 345-368.
[15]	Kolla V, Bourges P, Urruty J M, et al. Evolution of deep-water Tertiary sinuous channels offshore Angola (west Africa) and implications for reservoir architecture[J]. AAPG Bulletin, 2001, 85(8): 1373-1405.
[16]	Cross N E, Cunningham A, Cook R J,et al. Three-dimensional seismic geomorphology of a deep-water slope-channel system: The Sequoia field, offshore west Nile Delta, Egypt[J]. AAPG Bulletin, 2009, 93(8): 1063-1086.
[17]	赵晓明,吴胜和,刘丽. 尼日尔三角洲盆地Akpo油田新近系深水浊积水道储层构型表征[J]. 石油学报,2012,33(6):1049-1058.[Zhao Xiaoming, Wu Shenghe, Liu Li. Characterization of reservoir architectures for Neogene deepwater turbidity channels of Akpo oilfield, Niger Delta Basin[J]. Acta Petrolei Sinica, 2012, 33(6): 1049-1058.]
[18]	Lin Yu, Wu Shenghe, Wang Xing, et al. Composite sandbodies architecture of deep-water turbidite channels in the Niger Delta Basin[J]. Acta Geologica Sinica, 2014, 88(5):1801-1803.
[19]	李宇鹏,吴胜和,岳大力. 现代曲流河道宽度与点坝长度的定量关系[J]. 大庆石油地质与开发,2008,27(6):19-22. [Li Yupeng, Wu Shenghe, Yue Dali. Quantitative relation of the channel width and point-bar length of modern meandering river[J]. Petroleum Geology and Oil Development in Daqing, 2008, 27(6): 19-22.]
[20]	薛培华. 河流点坝相储层模式概论[M]. 北京:石油工业出版社,1991:51-63. [Xue Peihua. An Introduction to Reservoir Models of Point Bar Facies[M]. Beijing: Petroleum Industry Press, 1991: 51-63.]
[21]	张昌民,尹太举,朱永进,等. 浅水三角洲沉积模式[J]. 沉积学报,2010,28(5):933-944.[Zhang Changmin, Yin Taiju, Zhu Yongjin, et al. Shallow water deltas and models[J]. Acta Sedimentologica Sinica, 2010, 28(5): 933-944.]
[22]	尹太举,张昌民,樊中海,等.双河油田井下地质知识库的建立[J]. 石油勘探与开发,1997,24(6):95-98.[Yin Taiju, Zhang Changmin, Fan Zhonghai, et al. Founding subsurface geological data bank for Shuanghe oil field[J]. Petroleum Exploration & Development,1997, 24(6): 95-98.]
[23]	贾爱林,穆龙新,陈亮,等.扇三角洲储层露头精细研究方法[J]. 石油学报,2000,21(4):105-108.[Jia Ailin, Mu Longxin, Chen Liang, et al. Approach for detailed study of reservoir outcrop[J]. Acta Petrolei Sinica, 2000, 21(4): 105-108.]
[24]	于兴河,马兴祥,穆龙新,等. 辫状河储层地质模式及层次界面分析[M]. 北京:石油工业出版社,2004:60-106.[Yu Xinghe, Ma Xingxiang, Mu Longxin, et al. Geological Model and Hierarchical Interface Analysis of Braided River[M]. Beijing: Petroleum Industry Press, 2004: 60-106.]
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Establishment and Application of Geological Data Base on Deep-water Channels in Angola Block

doi: 10.14027/j.cnki.cjxb.2015.01.015

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通讯作者: 陈斌, bchen63@163.com

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