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首页> 外文期刊>The APPEA Journal >SEISMIC EVIDENCE FOR REVERSE AND WRENCH FAULT TECTONICS—CLIFF HEAD OIL FIELD, PERTH BASIN
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SEISMIC EVIDENCE FOR REVERSE AND WRENCH FAULT TECTONICS—CLIFF HEAD OIL FIELD, PERTH BASIN

机译:反向和扳手断裂构造的地震证据—珀斯盆地斜顶油田

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摘要

Seismic interpretation of the Cliff Head oil field has shown it to be structurally complex with reverse faults, wrench faults and listric faults mapped at both field and reservoir scale within the Permo-Triassic section. The Cliff Head field overlies the Abrolhos Transfer Zone and has strong similarity to the progressive evolution, internal structure and rhomboid map geometry in experimental models of restraining stepovers in strike-slip systems. It is concluded that the Cliff Head oil field is a pop-up structure formed during the Permian and early Cretaceous within a restrained convergent wrench system—the result of sinistral transpression. A similar style of faulting could be applied when mapping seismic data in other offshore areas and especially the onshore Perth Basin with its poorer seismic data quality. Interpretation of prospects with a strong reverse or wrench component has implications for the timing of hydrocarbon emplacement and the potential for seal breach and leakage. Furthermore, paleo-structural style will determine fracture density and orientation and may be critical in determining optimum design of producer and injection wells during field development. It is recommended that interpreters of seismic data in the Perth Basin treat the fault patterns and structural trends of the Permian and early Cretaceous as different structural packages. The two should only be linked when it is very clear that there is a strong early Cretaceous overprint.
机译:对克利夫黑德油田的地震解释表明,它在二叠纪-三叠纪剖面内在油田和储层范围内都具有反向断裂,扳手断裂和李斯特断裂的构造复杂。 Cliff Head场覆盖了Abrolhos转移带,并且与走滑系统中抑制跨步的实验模型中的渐进式演化,内部结构和菱形图几何形状非常相似。结论是,悬崖头油田是二叠纪和白垩纪早期在受约束的会聚扳手系统中形成的弹出结构,这是左旋压迫的结果。当在其他近海地区,尤其是地震数据质量较差的珀斯陆上盆地绘制地震数据时,可以应用类似的断层样式。用强力的反向作用或扳手作用来解释远景对烃的注入时间以及密封件破裂和泄漏的可能性都有影响。此外,古构造样式将决定裂缝的密度和方向,并且对于确定油田开发期间生产井和注入井的最佳设计可能至关重要。建议珀斯盆地的地震数据解释者将二叠纪和早白垩世的断层样式和构造趋势视为不同的构造组合。只有在非常明显的早白垩世叠印很明显的情况下,才应将两者联系在一起。

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