首页> 外文期刊>Journal of Asian earth sciences >Identification of a suspected Quaternary fault in eastern Korea: Proposal for a paleoseismic research procedure for the mapping of active faults in Korea
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Identification of a suspected Quaternary fault in eastern Korea: Proposal for a paleoseismic research procedure for the mapping of active faults in Korea

机译:鉴定朝鲜东部第四纪断层:拟定韩国活动断层古地震研究程序的建议

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In terms of seismic hazard in the Korean Peninsula, the occurrence of destructive earthquakes has long been overlooked because of no serious modern instrumental seismicity and lack of historical earthquake records of large earthquakes. In recent years, although the importance and uses of paleoseismological studies has significantly increased in seismic hazard assessments of critical facilities, there is still a huge lack of paleoseismological data to improve our knowledge for Korean active tectonics and relevant seismic hazards. In this study, we identified and characterized a suspected Quaternary fault in the eastern part of the Korea Peninsula based on lineament analyses, field observations, and trench surveys. We focus on a prominent lineament around the northern part of the previously reported, but not sufficiently studied, Maeup Fault. Firstly, a potential fault lineament is recognized by geomorphic expressions in a mountainous area from satellite and digital elevation model (DEM)-generated images. Then, fault-related geomorphic and hydrologic features, such as disconnected drainages, sag ponds, and asymmetric water leaking out on an artificial ditch, were observed along the lineament in the field studies. Finally, the existence of the fault is confirmed by an exposure of a 2.5 m wide fault core in trench surveys. The internal structures of the fault tore (i.e., slip surfaces, slickenlines, and S-C fabrics) indicate that the fault evolved via a series of slip events under a variety of tectonic settings, probably leading up to the current stress regime sustained during Quaternary. Thus our results suggest that the newly identified fault could be a Quaternary fault, and hence it is necessary to perform more paleoseismic investigations around the study region. This case study emphasizes the importance of the careful interpretation of tectonic landforms and fault zone structures in the study of active faults, and proposes a suitable research procedure for the identification of active faults in Korea. (C) 2015 Elsevier Ltd. All rights reserved.
机译:就朝鲜半岛的地震危险而言,破坏性地震的发生一直被忽视,因为它没有严重的现代仪器地震活动性,也没有大地震的历史地震记录。近年来,尽管在关键设施的地震危险性评估中,古地震学研究的重要性和用途已大大增加,但仍然缺少大量的古地震学数据来增进我们对韩国活跃构造和相关地震灾害的认识。在这项研究中,我们基于线性分析,现场观察和海沟调查,确定了朝鲜半岛东部的疑似第四纪断层并对其进行了特征化。我们专注于先前报道的但尚未充分研究的Maeup断层北部的突出地貌。首先,从卫星和数字高程模型(DEM)生成的图像中,通过山区的地貌表达式识别潜在的断层构造。然后,在野外研究中,沿断层观察到了断层相关的地貌和水文特征,例如不连续的排水系统,凹陷的池塘以及在人工沟渠中漏出的不对称水。最后,断层的存在可以通过在沟槽测量中暴露出2.5 m宽的断层芯来确认。断层撕裂的内部结构(即滑动面,光滑线和S-C织物)表明,在各种构造背景下,断层是通过一系列滑动事件演化而来的,可能导致第四纪持续的当前应力状态。因此,我们的结果表明,新发现的断层可能是第四纪断层,因此有必要在研究区域周围进行更多的古地震调查。本案例研究强调了对构造地貌和断层带结构进行仔细解释对活动断层研究的重要性,并提出了确定韩国活动断层的合适研究程序。 (C)2015 Elsevier Ltd.保留所有权利。

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