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Rock Mechanics and Rock Engineering

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30.03.2019 | Technical Note

New Insights Into The Current Stress Field Around the Yishu Fault Zone, Eastern China

verfasst von: Peng Li, Mei-feng Cai, Sheng-jun Miao, Qi-feng Guo

Erschienen in: Rock Mechanics and Rock Engineering | Ausgabe 10/2019

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The Yishu fault zone, also known as the Shandong segment of the Tan–Lu fault zone, is part of the middle segment of the Tan–Lu fault zone and is a large NNE striking (N10°–25°E) fault zone (Fig. 1). The fault zone stretches from the southern Tancheng area to the northern Laizhou Bay with a total length of approximately 350 km, and the fault zone is located between the western Shandong block and Jiaodong block or Sulu orogenic belt. During long-term development and the evolutionary process, the fault zone was characterized by distinct segment difference activities in space and multistage activities in time (Zhang et al. 2015). The fault zone is an important geotectonic boundary that controls and affects the stratigraphic framework, tectonic movement, magmatism and mineral distribution in the Shandong region. More importantly, the fault zone is a strong seismically active belt and obviously controls the strong earthquakes in both the Shandong region and North China; many moderate and strong earthquakes have occurred around the fault zone in the past (Zhu et al. 2018). The geological and seismological data show that the fault zone are still active (e.g., Lin et al. 1998; Yan et al. 2014; Jiang et al. 2017). Thus, the Yishu fault zone and its adjacent areas are the regions with high seismic activity frequencies in eastern China, which have always been highly concerning and have been designated as key seismic defense areas. …

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Titel: New Insights Into The Current Stress Field Around the Yishu Fault Zone, Eastern China
verfasst von: Peng Li
Mei-feng Cai
Sheng-jun Miao
Qi-feng Guo
Publikationsdatum: 30.03.2019
Verlag: Springer Vienna
Erschienen in: Rock Mechanics and Rock Engineering / Ausgabe 10/2019
Print ISSN: 0723-2632
Elektronische ISSN: 1434-453X
DOI: https://doi.org/10.1007/s00603-019-01792-x

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