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Evolution of Riedel-shear pop-up structures during cumulative strike-slip faulting: A case study in the Misayama-Godo area, Fujimi Town, central Japan

机译:累积走滑断层过程中Riedel剪切弹起结构的演化:以日本中部富士见町Misayama-Godo地区为例

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Strike-slip faulting often develops en echelon faulting resulting from Riedel shears. When faulted basement rocks are covered by thick unconsolidated deposits, this en echelon faulting leads to the subsequent evolution of a series of pop-ups along the fault during cumulative displacement. Although previous sandbox experiments and numerical simulations have examined the evolutionary processes for Riedel-shear pop-up structure formation, few field examples have been reported until now concerning (1) the time-series of evolutionary processes of pop-up structure generation and (2) time periods necessary to reach the stage of a "throughgoing fault zone". The Itoigawa-Shizuoka Tectonic Line (ISTL) fault zone is among the largest and fastest-slipping active fault zones in Japan, and a series of tectonic pop-ups related to left-lateral strike-slip displacement have developed in the Fujimi area in the central to southern part of the fault zone. This area is covered by thick (similar to 820 m) unconsolidated deposits, which have resulted in Riedel-shear pop-up structures. We conducted a geomorphic analysis, an extensive drilling survey, and pit excavation survey on a pop-up in the Misayama-Godo area of Fujimi, and concluded that (1) the pop-up structures in the Misayama-Godo area have been built up by two marginal faults between similar to 100 ka and similar to 10-20 ka, and (2) the fault displacement at depth has been concentrated on the faults that run across the pop-up structures (corresponding to the "throughgoing fault zone") since similar to 10-20 ka. One of the faults that run across the pop-up structures probably slipped during the most recent earthquake in the central to southern part of the ISTL fault zone. This study is presented as a robust field example of the evolution of Riedel-shear pop-up structures during cumulative strike-slip faulting. (C) 2018 Elsevier B.V. All rights reserved.
机译:滑移断裂常因里德尔剪切作用而发展成梯级断裂。当断层基底岩石被厚厚的未固结沉积物覆盖时,这种梯级断层将导致在累积位移过程中沿着断层的一系列弹跳的后续发展。尽管以前的沙盒实验和数值模拟已经检查了Riedel剪切弹起结构形成的演化过程,但到目前为止,几乎没有关于(1)弹起结构生成的演化过程的时间序列和(2)的现场实例的报道。 )到达“贯穿断层带”阶段所需的时间段。系鱼川静冈构造线(ISTL)断裂带是日本最大,滑移最快的活动断裂带之一,在富士见地区的富士见地区已经形成了一系列与左侧走滑位移有关的构造弹出窗口。断裂带中南部。该区域被厚厚的(约820 m)未固结沉积物覆盖,这导致了Riedel剪切弹起结构。我们对富士见的Misayama-Godo地区的一个弹窗进行了地貌分析,广泛的钻探调查和基坑开挖调查,得出的结论是(1)Misayama-Godo地区的弹窗结构已经建成大约100 ka和大约10-20 ka之间的两个边缘断层,以及(2)深处的断层位移一直集中在贯穿弹出结构的断层上(对应于“贯穿断层带” “),因为类似于10-20 ka。在ISTL断层带中南部的最近一次地震中,贯穿弹出结构的断层之一可能已经滑落。这项研究作为Riedel剪切弹起结构在累积走滑断裂过程中演化的可靠实例。 (C)2018 Elsevier B.V.保留所有权利。

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