Results 151 to 160 of about 381 (185)
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Temporal evolution of strain rate before the 2021 Mw 7.4 Maduo Earthquake.
The development of geodetic tools, such as Interferometric Synthetic Aperture Radar (InSAR), has revolutionized our exploration of earthquake physics and the assessment of seismic hazard. Over the past 20 years, InSAR has been increasingly used to determine the interseismic strain rate across major seismogenic faults.Conor Rutland +4 more
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Study on the Heterogeneity of the Stress Field in the Maduo Earthquake Fault Zone
Seismological Research LettersAbstract The 2021 Maduo earthquake sequence occurred on the Jiangcuo fault zone in Qinghai, China. However, the earthquake sequence did not occur along a straight fault. Aftershocks in the southeast section deflected the aftershocks in the southeast section to the east, when the aftershocks in the northwest section bifurcated.
Zhaoxuan Guan +3 more
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Unveiling the Activity of a Young Fault: Insights from the 2021 Maduo Earthquake
Faults grow through fault lengthening and slip accumulation, which are episodic processes related to the repetition of earthquakes. It is most often recorded in geomorphology. Meanwhile, the activity and seismic hazard of the ‘slow-moving’ faults are often overlooked due to their weak imprints in landforms, especially at their ...Wenqian Yao +10 more
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Sand liquefaction during the 2021 M 7.4 Maduo earthquake, China
Natural Hazards, 2022openaire +1 more source
Study regarding typical liquefaction damage during the 2021 Maduo Ms7.4 earthquake in China
Earthquake Engineering and Engineering Vibration, 2023Jinyuan Yuan +6 more
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Integrative oncology: Addressing the global challenges of cancer prevention and treatment
Ca-A Cancer Journal for Clinicians, 2022Jun J Mao,, Msce +2 more
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BEHAVIOR ANALYSIS OF YEMATAN BRIDGE ABUTMENT IN THE 2021 MADUO EARTHQUAKE AT QINGHAI, CHINA
On May 22, 2021, an M7.4 earthquake occurred in Maduo county, Qinghai, China, which caused significant damage to several bridges. Among them, the Yematan Bridge, a 25-span simply supported girder bridges experienced the most severe damage characterized by multi-span deck collapse and abutment failure. The abutment backwall fractured, departing from theopenaire +1 more source
Postseismic deformation occurs due to stress relaxation following large earthquakes and has been widely captured by space geodetic observations. For some earthquakes, afterslip has been inferred to take place in the fault barriers surrounding the areas of coseismic asperities.
Yuan Gao +5 more
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Yuan Gao +5 more
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