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断裂带内部结构指数构建及断层相定量地震解释

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断裂带的研究持续受到业界的关注,如何在地震资料上实现断裂带内部结构的定量解释是当前面临的重大挑战之一,本文聚焦利用地震资料实现断裂带内部三维空间非均质性的定量研究.该研究以海拉尔盆地乌尔逊凹陷南次凹为例,基于井上信息和地震资料建立了断裂带的地质模型并开展了地震正演模拟,确定不同产状、不同内部充填物的断裂带与地震反射波形的内在关系,构建了断裂带内部结构指数FIS,确定了断层相及背景围岩在FIS上的响应特征,实现了断裂带内部三维空间非均质性定量地震解释.研究发现:平面上,断裂带的FIS响应明显高于地层,FIS指数清晰地呈现了断裂带边界实现了断裂带与环境围岩的定量分离,即FIS大于26代表了断层相,FIS小于26则代表了围岩地层;沿断层走向方向具有分段特征,在断层倾向方向呈现分带性;在断层滑动面上,FIS指示了泥岩涂抹相的分布和低序级小尺度断层密集发育区的部位.油气勘探结果证实断裂带内部结构指数FIS用于定量预测断裂带的非均质性,可以指示断裂带内油气运移的有利部位,评价断层封闭性,是对断层相定量表征的探索.该方法在断块油气藏勘探开发、与断层有关的地质工程评价方面具有重要的应用价值.
Fault Interior Structure Index Construction and Quantitative Seismic Interpretation of Fault Facies
Fault zones have always drawn attention from the industry,and the performance of a quantitative interpretation of the fault interior structure on seismic data has remained as a big challenge.In this work,we focus on quantitatively populating the heterogeneity of the fault interior structure in a three-dimensional space on seismic data.To realize this goal,we take the South Wuerxun sub-depression in Hailar Basin as an example of a faulted basin.First,based on a heterogeneity analysis using the drilling and logging information from wells,we establish fault zone geologic models and perform seismic forward modeling to determine the relationship between different fault zone models with different fault dips,internal fillings,and P wave responses.Next,the fault interior structure index(FIS)is constructed,and the response features on the FIS from the fault facies and the host rock are observed.Finally,the FIS is applied to perform the quantitative interpretation and prediction of the heterogeneity in the FIS on seismic data.The results show that the FIS response from the fault zone is higher than that of the host rock in plane,indicating that the former is quantitatively separated from the surrounding host rocks.The FIS values greater than 26 represent the feedback from the fault facies,whereas those less than 26 represent the response from the host rocks.The FIS shows segmented features in the strike,banded in dip on plane.On the slip surface,the FIS indicates the shale smear zone and the location where low-graded and small-scaled faults are densely developed.The heterogeneity prediction result is proven by oil and gas exploration activities.The study results imply that the FIS could indicate a favorable path of the hydrocarbon migration in the fault zone and evaluate the fault sealing parts.The method can explore the quantitative characterization of fault facies and has essential popularization and application values in similar geological application fields,including hydrocarbon exploration,development of faulted reservoirs,and geological engineering evaluation related to faults.

fault interior structureFISfault faciesseismic forwardfaulted reservoirshydrocarbon migrationfault sealing

苏玉平、吕延防、马峰、张斌、谢明贤、陈广坡

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东北石油大学,大庆 163318

中国石油勘探开发研究院西北分院,兰州 730020

中国石油油藏描述重点实验室,兰州 730020

断裂带内部结构指数FIS 地震正演 断块油气藏 断层相 油气运移断层封闭性

2024

应用地球物理(英文版)
中国地球物理学会

应用地球物理(英文版)

影响因子:1.01
ISSN:1672-7975
年,卷(期):2024.21(4)