Control of the Strike-Slip Fault to the Source-to-Sink System of the Paleogene in Bohai Sea Area
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摘要: 走滑断裂在渤海海域广泛分布，深刻影响着沉积盆地的形成与演化，同时也深刻影响着源－汇体系的形成和演化.在对渤海海域大量钻井资料和地震资料分析的基础上，认为走滑断裂对渤海古近系源－汇体系的控制作用主要表现在：走滑断裂压扭作用控制了局部物源体系的形成；走滑断裂的张扭作用控制了沟谷低地的形成；走滑断裂的水平运动控制源－汇体系的横向迁移.走滑断裂带源－汇体系发育模式十分复杂，渤海古近系常见的主要有S型走滑断裂带源－汇体系模式、叠覆型走滑断裂带源－汇体系模式、帚状走滑断裂带源－汇体系模式、共轭走滑带源－汇体系模式.开展走滑断裂带源－汇体系特征及其控砂模式的探讨，对含油气盆地的储层预测具有重要的意义.Abstract: The strike slip faults are widely distributed in Bohai sea area and they play an important role in the formation and evolution of the sedimentary basin and the Source-to-Sink system. According to the principles of Source-to-Sink system analysis, this paper focuses on the study of control of the strike slip fault over the Source-to-Sink system of the Paleogene in Bohai on the basis of a large number of drilling data and seismic data analysis. It is found that the transpression of the strike slip faults controls the formation of local provenance system. and the transtension of the strike slip faults controls the formation of eroded ravines and valleys. The horizontal movement of the strike-slip fault controls the lateral migration of Source-to-Sink system. The Source-to-Sink system in the strike slip fault zone is more complex than that of the simple extension fault zone. There are four kinds of common Source-to-Sink system of strike slip faults in Paleogene in Bohai including S type strike slip fault source sink system mode, en echelon type strike slip fault source sink system mode, brush strike slip fault source sink system mode, and conjugate strike slip fault source sink system mode. The study on the characteristics of Source-to-Sink system and its sand control pattern of strike slip fault zone is very important for reservoir prediction in petroliferous basin.
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Key words:
- strike-slip fault /
- Source-to-Sink system /
- mode /
- Paleogene /
- Bohai sea area /
- petroleum geology
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图 1 渤海海域区域地质图与走滑断裂分布
Fig. 1. Regional geological map of Bohai sea area and strike-slip faults distrubution map
图 2 渤海海域走滑断裂带应力发育模式
a.右旋S型走滑断裂；b.左旋S型走滑断裂；c.右旋帚状走滑断裂；d.左旋帚状走滑断裂；e.右旋叠覆型走滑断裂；f.左旋叠覆型走滑断裂；g.右旋双重型走滑断裂；h.左旋双重型走滑断裂；i.共轭型走滑断裂
Fig. 2. Stress mode of strike-slip fault zones in Bohai sea area
图 3 锦州20-3地区右旋左阶S型走滑断裂控制的局部物源与近源辫状三角洲沉积
Fig. 3. The local provenance and proximal braided river delta controlled by dextral left step strike slip fault in JZ20-3 area
图 4 渤中34-9油田右旋右阶叠覆型走滑断裂控制的沟谷低地与辫状河三角洲沉积
Fig. 4. Valley and proximal braided river delta controlled by dextral right step strike slip fault in BZ34-9 oilfield
图 5 金县1-1地区走滑断裂水平位移与辫状河三角洲“鱼跃式”迁移
Fig. 5. Horizontal displacements of strike slip fault and braided river delta fish jumping migrate in JX1-1 area
图 6 辽东凸起中北段S型走滑带源－汇体系发育模式
Fig. 6. type strike slip fault source sink system mode in the middle-north section of Liaodong uplift
图 7 锦州25-1地区叠覆型走滑断裂带源－汇体系发育模式
T4代表沙二段顶面；T5代表沙二段底面
Fig. 7. En echelon type strike slip fault source sink system mode in JZ25-1 area
图 8 辽西低凸起北段锦州20-2北地区帚状走滑带源－汇体系发育模式
Fig. 8. Brush strike slip fault source sink system mode in JZ20-2N area of the north section of Liaoxi low uplift
图 9 曹妃甸6-4油田共轭走滑带源－汇体系发育模式
Fig. 9. Conjugate strike slip fault source sink system mode in CFD6-4 oilfield
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