2020
DOI: 10.3389/feart.2020.588304
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Seismogenic Faulting of the 2016 Mw 6.0 Hutubi Earthquake in the Northern Tien Shan Region: Constraints From Near-Field Borehole Strain Step Observations and Numerical Simulations

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Cited by 4 publications
(4 citation statements)
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“…The Kuqa and southern Junggar FTBs are developed at its southern and northern flanks, respectively, where active thrusting and folding are pronounced (Charreau et al., 2020; Deng et al., 1996; Hubert‐Ferrari et al., 2007; Li, Rao, et al., 2020; Lu et al., 2019; Saint‐Carlier et al., 2016; Tang et al., 2017; Tapponnier & Molnar, 1979). In the northern piedmont, the 1906 M 8 Manas earthquake occurred along the HMT structural belt, where co‐seismic surface ruptures were found in the field (Figure 1b; Avouac et al., 1993; Deng et al., 1996; Stockmeyer et al., 2014), and the occurrence of the 2016 M 6.2 Hutubi earthquake reflects its associated recent seismicity (Li et al., 2018, 2021; Lu et al., 2018).…”
Section: Geological Backgroundmentioning
confidence: 99%
“…The Kuqa and southern Junggar FTBs are developed at its southern and northern flanks, respectively, where active thrusting and folding are pronounced (Charreau et al., 2020; Deng et al., 1996; Hubert‐Ferrari et al., 2007; Li, Rao, et al., 2020; Lu et al., 2019; Saint‐Carlier et al., 2016; Tang et al., 2017; Tapponnier & Molnar, 1979). In the northern piedmont, the 1906 M 8 Manas earthquake occurred along the HMT structural belt, where co‐seismic surface ruptures were found in the field (Figure 1b; Avouac et al., 1993; Deng et al., 1996; Stockmeyer et al., 2014), and the occurrence of the 2016 M 6.2 Hutubi earthquake reflects its associated recent seismicity (Li et al., 2018, 2021; Lu et al., 2018).…”
Section: Geological Backgroundmentioning
confidence: 99%
“…Unlike GTSM strainmeter such as the United States, which can produce high frequency data of 20 Hz, the data sampling rate of strainmeter in mainland China is minute sampling due to data storage and transmission technology. Using these minute data, scholars in mainland China have carried out a lot of research, including the tidal Variation and calibration technology (Qiu et al, 2015), abnormal changes of different earthquakes (Qiu et al, 2010;Liu et al, 2014), co-seismic strain steps (Gong et al, 2019;Li et al, 2020), free oscillation of the earth excited by large earthquakes (Tang et al, 2007;Tang et al, 2008;Qiu, 2017), and also studied and analyzed the influence of water level, air pressure, rainfall and other factors on borehole strain, and studied the data processing methods to identify and eliminate these influencing factors (Zhou et al, 2008;Zhang and Huang, 2011;Zhang et al, 2015). However, these studies are limited to longer period signals because of the low sampling rate.…”
Section: Introductionmentioning
confidence: 99%
“…As the technical management and planning team of the borehole strain network in Mainland China, we have upgraded and updated the high-sampling data collectors of 10 four-component borehole strainmeters which are producing high frequency data of 100 Hz since 2017, only one site could produce high-frequency data before. Using these data, the ability of four-component borehole strainmeters to record strain seismic waves of earthquakes of different magnitudes has been studied (Qiu et al, 2015;Tang et al, 2022), the study of determining the strain magnitude of seismic surface wave based on borehole strain seismic wave is carried out (Li et al, 2020), Shi et al (2021) studied the direct observation of co-seismic static stress deviation changes consistent with the theoretical prediction. These sites can record the seismic waves of earthquakes with M6.0 or above in the world (Tang et al, 2022), and can also record the local earthquakes in the area where the site is located.…”
Section: Introductionmentioning
confidence: 99%
“…(5)(6)(7) This method has been used to study plate movements, earthquakes, volcanoes, and many other geological phenomena. (8)(9)(10)(11)(12)(13)(14)(15) Previous borehole strainmeters used in mainland China include volumetric strainmeters and four-gauge borehole strainmeters (FGBSs). (5)(6)(7) An FGBS is generally installed in a borehole in bedrock at a depth of tens or hundreds of meters to observe changes in the horizontal strain in the shallow surface of the crust.…”
Section: Introductionmentioning
confidence: 99%