15 December 2024, Volume 38 Issue 4
    

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  • ZHENG Xue-gang, MA Xue-jun, Shamuhaer Yeerken, ZHAO Peng-bi
    Inland Earthquake. 2024, 38(4): 307-314. https://doi.org/10.16256/j.issn.1001-8956.2024.04.001
    Abstract ( ) Download PDF ( )   Knowledge map   Save
    For the determination of the focal depth of moderately strong earthquakes, the teleseismic converted wave depth phase pP and sP sounding is an effective method, and the depth accuracy can reach 2 km when the depth phase is clear. Teleseis program is used to fit the theoretical seismogram of the Maduo MS7.4 earthquake, and compared with the actual observation. The focal depth of the earthquake is measured, and the influence of the crustal velocity model on the teleseismic body wave depth phase pP sounding is analyzed and discussed. The results show that the initial rupture depth of the Maduo earthquake is 12 km, and the uncertainty of the Vp in the velocity model has a greater influence on the arrival time of the seismic phase in the theoretical seismogram.
  • ZHAO Peng, MIN Wei, SHU Peng, HE Kang
    Inland Earthquake. 2024, 38(4): 315-322. https://doi.org/10.16256/j.issn.1001-8956.2024.04.002
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    Through the field geological and geomorphological survey and trench excavation of the Danghe nanshan fault,it is found that multi-level fault scarps are developed along the north side of the fault, and the latest scarps break the floodplain of the gully, while the west section of the fault is accompanied by fold activity; The geological exploration trench excavated at the mouth of Dahonggou gully shows that the fault has dislocated a relatively new gravel layer. The sample test results show that the latest active age of the fault is at least the middle Holocene; Two trenches revealed the same seismic event, which occurred after (4.69±0.40) ka BP.
  • LI Bo, ZHANG Jing-yan, HE Huan, SONG Li-jun, HE Qiang
    Inland Earthquake. 2024, 38(4): 323-331. https://doi.org/10.16256/j.issn.1001-8956.2024.04.003
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    Based on the existing four-dimensional disaster volume mode, this study applied and analyzed the model by incorporating factors related to earthquake disasters. The disaster volume index of destructive earthquakes in Xinjiang from 2002 to 2022 was calculated to further classify disaster levels. To verify the accuracy of the model, the calculated results were compared with the results of a previously established three-dimensional disaster volume mode, and the disaster losses of the Wenchuan and Tangshan earthquakes, as well as other earthquakes, were calculated. The research results showed that under the consideration of richer disaster information, the calculation results of this model were more accurate and matched the actual situation of disaster losses.
  • LIAN Yin-chao, LI Xiao-dong, YAN Long, GUAN Dong-xiao, YAN Wei
    Inland Earthquake. 2024, 38(4): 332-339. https://doi.org/10.16256/j.issn.1001-8956.2024.04.004
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    To improve the earthquake monitoring equipment operations and maintenance security system construction, form operations personnel unified command, unified equipment management, unified scheduling, equipment operations efficient equipment support mechanism, improve the earthquake equipment operational response speed and the ability to solve practical problems, this paper is based on the cloud platform, use to server architecture design to realize the seismic equipment operational security system. Starting from the actual operation and maintenance of seismic equipment, the system strives to solve the deficiencies of poor management efficiency and low timeliness of operation and maintenance in the current operation and maintenance work, and realizes the digitization of troubleshooting, equipment management, data archiving and other functions of regional operation and maintenance work, which provides feasible reference for improving and supplementing the construction of regional operation and maintenance support system of seismic instruments and equipment.
  • NAN Fang-fang, XIANG Yuan, ZHANG Feng, HUANG Shuai-tang, NIE Xiao-hong
    Inland Earthquake. 2024, 38(4): 340-348. https://doi.org/10.16256/j.issn.1001-8956.2024.04.005
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    In depth analysis of the activity characteristics, sequence parameters, and sequence types of the Wushi MS7.1 earthquake sequence on January 23, 2024 shows that the aftershock sequence of the Wushi MS7.1 earthquake is rich, and the intensity of seismic activity decays slowly, showing a fluctuating attenuation characteristic; The overall attenuation of earthquake frequency is relatively fast. The aftershocks are mainly distributed at the junction of the basin and mountains, with a length of about 200 km and a width of about 150 km, and are generally distributed in the NE direction. Before 4 strong aftershocks with MS>5.5, there was a certain degree of low p-values and h-values. Based on the analysis of the energy release ratio, b-value, and the difference in magnitude between the main shock and the maximum aftershock of the largest earthquake in the sequence, the Wushi MS7.1 earthquake sequence on January 23, 2024 belongs to the main shock aftershock type.
  • XIE Jiang-li, Alimujiang Yalikun, HUANG Shuai-tang, LI Bo
    Inland Earthquake. 2024, 38(4): 349-356. https://doi.org/10.16256/j.issn.1001-8956.2024.04.006
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    Using 131 destructive seismic events with intensity data, a total of 322 pairs of long and short axis data of intensity circle, the attenuation relationship of seismic intensity in different regions of Xinjiang is fitted by mathematical method. The seismic intensity attenuation models used in Xinjiang region are collected and sorted out. The long and short axis radii of each intensity zone of Wushi MS7.1 earthquake on January 23,2024 are simulated and calculated by using the model, and the absolute error analysis is carried out with the long and short axis radii of the actual survey intensity. The high intensity area of this earthquake is more than 40% larger than the high intensity area of the same magnitude in the past. The calculation results in the VII degree area are the closest to the actual value. The error in the long axis direction of the VI degree area is small, and the error in the short axis direction of the VI degree area is large. The intensity attenuation relationship used in the past may have a small epicenter distance in the high intensity area, and there is a large epicenter distance in the low intensity area. Therefore, when the intensity attenuation relationship is used to quickly evaluate the intensity impact field of earthquake disasters, special attention should be paid to the method of limiting the head and tail of the attenuation relationship to more accurately evaluate.
  • YANG Fen
    Inland Earthquake. 2024, 38(4): 357-365. https://doi.org/10.16256/j.issn.1001-8956.2024.04.007
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    Before the M6.4 earthquake inYangbi, Yunnan on May 21, 2021, the comprehensive probability values of the comprehensive prediction scheme of the MS≥5.0 earthquake in western Yunnan and the comprehensive probability values of the comprehensive prediction scheme of the MS≥6.0 earthquake in Yunnan breaking through the prediction threshold on January 28, 2021 and March 17, 2021 respectively, reaching the medium-term prediction index and meeting the first conditions of the prediction. Mercury and solid carbon dioxide in Xiaguan have also breaking through the forecast threshold, and the necessary conditions have been met. According to the hierarchical early warning model, the comprehensive prediction scheme of MS≥5.0 earthquake in western Yunnan and the comprehensive prediction scheme of MS≥6.0 earthquake in Yunnan have the conditions for short-term prediction on January 28, 2021 and March 17, 2021 respectively. Yangbi MS6.4 earthquake occurred on May 21, 2021 after 3.8 months and 2.1 months respectively.When both comprehensive schemes reach the short-term prediction index, the risk of MS≥6.0 strong earthquake in western Yunnan is enhanced.
  • LI Bing-ye, Ailixiati Yushan, LIU Dai-qin, CHEN Li, Abudutayier Yasen, Aerdake Kadeerbieke, ZHAO Lei
    Inland Earthquake. 2024, 38(4): 366-375. https://doi.org/10.16256/j.issn.1001-8956.2024.04.008
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    Using the mobile gravity observation data after Wushi MS7.1 earthquake in the South Tianshan area,the gravity field changes in the South Tianshan area before and after Wushi MS7.1 earthquake were obtained,and the 1-year and multi-year scale gravity changes before and after the earthquake in the area were studied. The results show that after the Wushi earthquake,the zero isoline of gravity change passes through the epicenter area and a high gradient zone of gravity change appears. In the area where the zero contour of gravity change appears,the material density is undergoing a transition process of increasing and decreasing. The difference in material increase and decrease leads to strong movement and energy accumulation. The gravity anomaly before strong earthquakes may last for a long time,and there may be a small change in the gravity field. Therefore,when extracting and analyzing the gravity anomaly signal before strong earthquakes,it is necessary to consider the gravity observation data with a long time span. The mobile gravity data observed after the earthquake can better reflect the stress release characteristics of the seismogenic fault,which is helpful to analyze the development trend of aftershocks.
  • JIA Yong-Bin, LIU Ping, WANG Bin, WANG Cheng-guo, DENG Ming-wen
    Inland Earthquake. 2024, 38(4): 376-386. https://doi.org/10.16256/j.issn.1001-8956.2024.04.009
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    By analyzing the characteristics of underground fluid anomalies and focal mechanism solutions before Changji MS4.8 earthquake on July 20,2022,the characteristics and distribution range of underground fluid anomalies before the earthquake were summarized.The analysis shows that the underground fluid anomaly of the Changji earthquake is within 80~140 km.From the perspective of the time from the earthquake,the underground fluid anomalies before the Changji earthquake can be divided into short-term anomalies and medium-term trend background anomalies, of which short-term anomalies are the main ones.Background anomaly of the medium-term trend shows that the dynamic water level of Xin 26 Spring decreases first and then increases.The short-term and impending anomalies are manifested as the rise of static water level in Xin 04 Well, the rise of static water level in Xin 20 Well and the rise of conductivity in Xin 15 Spring.The anomaly shows an EW distribution in space.The focal mechanism solution results show that the nodal plane I strikes 81°, the dip angle is 69°, and the slip angle is 174°.The nodal plane II has a strike of 173°, an inclination of 84°, and a sliding angle of 21°.The P-axis orientation is 305°, and the T-axis orientation is 39°, indicating that Changji MS4.8 earthquake was an earthquake event under the stress of NWW compression and NEE extension.The direction of the main compressive stress obtained from the focal mechanism solution of Changji earthquake is the same as that of anomaly distribution before the earthquake.
  • LIU Hai-yang, JIANG Zhi-ying, XU Yan-gang, JIA Dong-hui
    Inland Earthquake. 2024, 38(4): 387-393. https://doi.org/10.16256/j.issn.1001-8956.2024.04.010
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    Through five different pumping depth experiments at the depth of 5~105 cm at the Aksu fault hydrogen observation point in Xinjiang, it can be seen that there are great differences in the hydrogen background value, daily amplitude and dynamic characteristics of different pumping depths in the fault hydrogen observation.Due to the strong penetrability and low viscosity of hydrogen diffusion, hydrogen has obvious uneven zonality in the vertical direction of the observation hole. And because of the difference in the structural position of the observation point and the influence of meteorological factors, the hydrogen background value and the quality of the observation data are different. The pumping depth of 80 cm in the hanging wall of the fault at Aksu observation point, the mean square error and coefficient of variation of fault hydrogen data are significantly better than other depths, which can be used as the preferred depth of Aksu fault hydrogen observation.
  • YANG Shao-fu, SONG Chun-yan, SU Ping, ZHANG Sen, DENG Ming-wen
    Inland Earthquake. 2024, 38(4): 394-402. https://doi.org/10.16256/j.issn.1001-8956.2024.04.011
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    Observation data of three sets of VP broadband vertical pendulum tiltmeter at Korla station, Ruoqiang station and Qiemo station are selected, and the seismic noise level in the seismic frequency band is calculated by using the power spectral density analysis method. The results show that the background noise level of the instrument at Korla station is low due to the excellent observation conditions of the cavern and the small interference of the observation environment around the cavern. The noise level of the three sets of VP-type broadband vertical pendulum tiltmeter does not show obvious regularity in spatial distribution, but it shows the consistency that the NS component record is better than the EW component.
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