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Confluence and intersection of interacting conjugate faults: A new concept based on analogue experiments

机译:相互作用共轭断层的汇合和交会:基于模拟实验的新概念

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Examination of the interaction area of conjugate faults yields evidence of a yet unknown structural pattern. Analogue experiments revealed the evolution of this pattern during the interaction process. A fault propagating towards the highly active section of another conjugate fault becomes increasingly deflected towards the obtuse angle side of the conjugate system while approaching until joining it. During this process, the tip of the curved propagating fault retains its shear sense until immediately before joining with the highly active fault-a process called "confluence" in this report. Under constant remote stress, the deflected fault now becomes dominant. A fault branch splits off at the point where deflection commences, propagating straight ahead of the original direction, and may dissect the former master fault. Alternating activity at both of the faults finally produces the known intersection patterns. Further studies of the proposed concept on natural examples are recommended due to the close geometric similarity of the evolutionary structural stages and natural fault patterns.
机译:共轭断层相互作用区域的检验产生了一个未知的结构模式的证据。模拟实验揭示了这种模式在相互作用过程中的演变。朝另一个共轭断层的高活性部分传播的断层逐渐趋向共轭系统的钝角侧,直到接近它为止。在此过程中,弯曲的传播断层的尖端一直保持其剪切力,直到即将与高度活跃的断层连接为止。在本报告中,这一过程称为“汇合”。在恒定的远程应力下,偏转的断层现在占主导地位。断层分支在开始偏转的点处​​分裂,直接在原始方向上传播,并可能解剖出原来的主断层。最终,两个断层的交变活动都产生了已知的相交模式。由于演化结构阶段和自然断层模式的紧密几何相似性,建议对自然实例提出的概念进行进一步研究。

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