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Thrust dip and thrust refraction in fault-bend folds: analogue models and theoretical predictions

机译:断层弯曲褶皱的推力倾角和推力折射:模拟模型和理论预测

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Analogue models made of two layers of loose sand separated by a thin layer of micro glass beads were shortened by a rigid emerging ramp dipping at either 30°or 45°and possessing a high, intermediate, or null surface friction. Shortening resulted in formation of closely spaced back thrusts in the sand layers. The dips of the back thrusts vary within a range of 30°depending on the ramp friction, and 7°depending on its dip. An increase in ramp friction, or, to a lesser extent, in ramp dip, decreases the thrust dips in the model. The second important observation is that, when friction is greater along the ramp than along the layer of glass beads, then the glass beads layer acts as a separate upper ramp above which the back thrusts steepen. The theory proposed to explain these observations predicts the thrust dips through a two-step procedure: first, global equilibrium of forces in the two layers is required to yield the mean forces at stake along the ramps and thrusts, second, the total dissipation is minimized with respect to the dips of the back thrusts. The relevant frictional properties of our analogue materials have been measured in stress conditions as close as possible to the experimental ones (below 1 kPa), and used with the theory to yield optimal back thrust dips that are all within 3°of the measured dips. This is a surprisingly good fit when considering that we did not take into account geometric changes, strain-softening, and dilatancy or compaction, due to slip on the thrusts. We conclude that this general two-step theoretical procedure is validated in the context of analogue frictional materials. We also propose a possible mechanism for thrust refraction and top-to-the-foreland sense of shear observed in the hanging walls of lower-flat to ramp transition in sedimentary piles that is based on the triggering of secondary upper ramps. Finally, this mechanical approach can also be seen as complementary to the kinematic models of fold-thrust structures which, by definition, cannot grasp the strong effects of friction on the kinematics.
机译:由两层由细微玻璃珠薄层隔开的松散沙子制成的模拟模型,由于在30°或45°处浸入的刚性新兴坡道而被缩短,并具有高,中度或零表面摩擦力。缩短导致在沙层中形成间隔很小的反推力。后推力的斜率在30°的范围内变化,具体取决于坡道摩擦力;在7°的范围内,取决于斜率。坡道摩擦的增加或坡道倾角的较小程度会减小模型中的推力倾角。第二个重要的观察结果是,当沿坡道的摩擦力大于沿玻璃珠层的摩擦力时,玻璃珠层将充当单独的上坡道,在该坡道上方,反推力会变陡。为解释这些观测结果而提出的理论通过两步过程来预测推力骤降:首先,需要两层力的全局平衡才能产生沿斜坡和推力的临界平均力,其次,总耗散最小化关于后推力的下降我们的模拟材料的相关摩擦性能已在尽可能接近实验条件(低于1 kPa)的应力条件下进行了测量,并与该理论一起用于产生最佳后推力倾角,该倾角均在所测倾角的3°以内。考虑到我们未考虑由于推力滑动而引起的几何变化,应变软化以及膨胀或压实,因此这是一个令人惊讶的良好拟合。我们得出的结论是,这种一般的两步理论程序已在模拟摩擦材料的范围内得到验证。我们还提出了一种可能的机制,该机制是基于次要上斜坡的触发,在沉积桩的下平面到斜坡过渡的悬挂壁中观察到的推力折射和从上到前的剪切感。最后,这种机械方法也可以看作是褶皱-推力结构运动学模型的补充,根据定义,该模型不能掌握摩擦力对运动学的强烈影响。

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