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Determination of stress distribution on active fault by means of Casagrande method; an innovative approach

机译:用卡萨格兰德方法确定活动断层的应力分布;创新的方法

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The investigation deals with the stress distributions of undisturbed soil samples taken by preconsolidation press method from paleoseismological studies in the Gerede (Bolu) segment of the North Anatolian Fault System (NAPS), which is one of the most important intra-continental active transform faults in the world. Taking into consideration of the theoretical principal stress directions causing the faulting in the soil samples, consolidation experiments were carried out in different directions and the preconsolidation pressure values (PPV) of the samples were found by Casagrande method. Relations between the prime stress directions which are effective in the mechanism of fault formation and the values of PPV found by the Casagrande method were revealed. With all these calculations, the principal directions and magnitudes of the principal stresses causing faulting in the near-surface depths on the Gerede segment of the NAFS have been determined by a new method. The Gerede segment of the maximum principal stress (sigma 1) value at N 55.5 degrees W and N 60 degrees W was found 554.08 kPa and 327.54 kPa respectively. The maximum principal stress (sigma 1) direction of the fault was found to be N 55.5 degrees W and the angle value was 44.5 degrees.
机译:该研究处理的是采用预固结压榨法从北安那托利亚断裂系统(NAPS)的Gerede(Bolu)段进行的古地震学研究获得的未扰动土壤样品的应力分布,这是该州最重要的洲际活动转换断裂之一。世界。考虑到引起土壤样品断裂的理论主应力方向,进行了不同方向的固结试验,并通过卡萨格兰德方法求出了样品的预固结压力值(PPV)。揭示了对断层形成有效的主应力方向与卡萨格兰德方法测得的PPV值之间的关系。通过所有这些计算,已经通过一种新方法确定了导致NAFS Gerede段近表面深度断裂的主应力的主方向和大小。在N 55.5度和N 60度处发现最大主应力(sigma 1)值的Gerede区段分别为554.08 kPa和327.54 kPa。断层的最大主应力方向(σ1)为N 55.5度W,角度值为44.5度。

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