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3D Structural restoration and Geomechanical Forward Modeling in a visco- plastic medium to natural fracture prediction in a Malay producing field, offshore Malaysia

机译:三种结构恢复与地磁向前造型在马来西亚海岸生产领域自然骨折预测

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In order to ensure a successful drilling campaign,it was required to obtain knowledge of the possible location of natural fractures generated by different tectonic events affecting the Malay Basin through geological time to a high level of certainty. The acquired information would assist in the optimization of well trajectories to avoid these naturally fractured regions which would likely result in severe wellbore instability problems. The Malay Basin underwent an extensional phase during the Oligocene period with deposition of lacustrine source rocks.The Miocene was a time of fluvio-deltaic source and reservoir deposition and a compressional phase starting Early Miocene resulted in a positive structural inversion with a strong lateral component.A major unconformity underlined the peak of the tectonic inversion.The objective of the study was to model the heterogeneous paleo-stress and paleo-strain states by the construction of a geomechanical forward model in a visco-plastic medium using 3D restored model and then to relate the predicted strain and stresses in the fracture characterization process. The technique used to perform the restoration was based on the Finite Element Method,particularly suited for modeling complex geological structures.The paleo-stress was recovered from geomechanical forward modeling of restored structures at each geological time-step in order to calculate the internal stress condition and plastic strain distribution accumulated through geological time.
机译:为了确保成功的钻探运动,需要了解通过地质时间到高水平的地质时间影响马来盆地的不同构造事件产生的自然骨折的可能位置。所获得的信息将有助于优化井轨迹以避免这些自然骨折区域,这可能导致严重的井筒不稳定性问题。马来盆地在寡核苷酸期间经历了延伸期,寡烯源岩会沉积。中丙烯是氟化脲源和储层沉积的时间和储层沉积,并且一种具有强侧部组分的阳性结构反演的压缩阶段。一个主要的不整合强调了构造反转的峰值。该研究的目的是通过使用3D恢复模型的粘塑料介质的地质力学前向模型来建造异质古应力和古菌株状态。涉及裂缝表征过程中的预测应变和应力。用于执行恢复的技术基于有限元方法,特别适用于建模复杂的地质结构。从每个地质时间步骤中从恢复结构的地质力学向模型中回收古胁迫,以计算内部应力条件通过地质时间累积的塑料应变分布。

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