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Kinematic modeling of folding above listric propagating thrusts

机译:上链传播推力折叠的运动学模型

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We describe a kinematic approach to simulate folds above listric propagating thrusts. The model is based on a pre-defined circular thrust geometry with a maximum central angle beyond which the thrust is planar, inclined shear above the circular thrust, and trishear in front of the thrust Provided the trajectory of thrust propagation is established, the model can be run forward and backwards. We use this last feature to implement a global simulated annealing, inverse modeling strategy. This inverse modeling strategy is applied to synthetic folds as well as two real examples in offshore Venezuela and the Niger Delta toe-thrust system. These three examples illustrate the benefits of the algorithm, particularly in predicting the possible range of models that can fit the structures. Thrust geometry, depth to detachment level, and backlimb geometry have high impact in model parameters such as backlimb shear angle and fault slip; while forelimb geometry is critical to constrain parameters such as fault propagation to fault slip ratio and trishear angle. Steep to overturned beds in forelimb areas are often not imaged by seismic, so in the absence of additional well data, considering all possible thrust-fold geometries is critical for the modeling and whatever prediction (e.g. hydrocarbon trap integrity) is made from it.
机译:我们描述了一种运动学方法,可以模拟高于李斯特传播推力的褶皱。该模型基于预定义的圆形推力几何形状,该几何形状具有最大的中心角,超过该最大角度时,推力是平面的,圆形推力上方有倾斜剪切,推力前为三切线。如果已建立推力传播的轨迹,则该模型可以向前和向后跑。我们使用此最后一个功能来实现全局模拟退火,逆建模策略。这种逆建模策略适用于合成褶皱以及委内瑞拉近海和尼日尔三角洲脚趾-推力系统中的两个真实示例。这三个示例说明了该算法的优势,特别是在预测可以拟合结构的模型的可能范围方面。推力几何形状,深度至脱离水平以及后肢几何形状对模型参数(例如后肢剪切角和断层滑动)有很大影响;而前肢的几何形状对于约束诸如断层传播,断层滑移率和三剪切角等参数至关重要。前肢陡峭至倾覆的床层通常无法通过地震成像,因此在缺乏其他井眼数据的情况下,考虑所有可能的逆冲褶皱几何形状对于建模至关重要,并据此做出任何预测(例如油气藏完整性)。

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