• Issue 3,2025 Table of Contents
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    • >Earthquake Engineering
    • Determination method for yield points in the design of self-centering braced structures

      2025, 47(3):501-511. DOI: 10.20000/j.1000-0844.20231026003

      Abstract (203) HTML (0) PDF 10.23 M (118) Comment (0) Favorites

      Abstract:Accurate determination of structural yield points is critical for developing constant-ductility elastic-plastic displacement response spectra. This study proposes a systematic method to identify design yield points for self-centering braced structures. Using the direct displacement-based design method (DDBD), three-story and five-story steel frame structures with self-centering buckling-restrained braces (SCBRB) were designed, and the impact of design yield points on the accuracy and outcomes of DDBD was thoroughly analyzed. The research results show that, for both low-rise and multi-story structures, the structural ductility capacity can achieve the target ductility demand using the proposed determination method for seismic design. Under an 8-degree earthquake, the maximum story drift ratio of structures designed with the proposed method is closer to the design goal of 2% compared to conventional determination approaches, and the initial design stiffness of SCBRB is also reduced. These results demonstrate the effectiveness of the proposed method in balancing safety and economy for SC-BRB structural systems.

    • Seismic damage assessment of damaged CFSST frame exterior joints strengthened by enveloped steel

      2025, 47(3):512-521. DOI: 10.20000/j.1000-0844.20231114003

      Abstract (126) HTML (0) PDF 11.77 M (60) Comment (0) Favorites

      Abstract:To evaluate the seismic damage of damaged concrete-filled steel square tubular (CFSST) frame exterior joints strengthened by enveloped steel, a numerical model was developed using finite element software ABAQUS based on prior experimental studies. Seismic damage was simulated using a material property reduction method, and an appropriate seismic damage model was employed to investigate the damage evolution mechanism of the joints. The study systematically examined the effects of enveloped steel's strength, thickness, and non-core zone reinforcement height on the seismic bearing capacity of CFSST frame exterior joints. Results indicate the following: (1) The material property reduction method accurately replicates the effects of seismic damage. (2) Strengthening lightly and moderately damaged specimens with enveloped steel restores or even surpasses their original seismic performance. (3) Increasing the enveloped steel material strength from Q235 to Q345, Q390, and Q420 increases the joint's ultimate load capacity by 6.27%, 10.57%, and 13.70%, respectively. Increasing the thickness of enveloped steel from 4 mm to 6 mm and 8 mm improved the ultimate load capacity by 4.02% and 9.68%, respectively. Extending the non-core zone reinforcement height of enveloped steel has a minimal effect on seismic capacity. Increasing the height from 200 mm to 400 mm improved the yield load and ultimate load by 0.86% and 4.56%, respectively.

    • Exact solution for the one-dimensional transient response of single-layer incompressible unsaturated porous media

      2025, 47(3):522-528. DOI: 10.20000/j.1000-0844.20230914001

      Abstract (120) HTML (0) PDF 4.26 M (52) Comment (0) Favorites

      Abstract:The exact solution for incompressible and unsaturated porous media has not been provided in the current literature. Thus, an exact solution was derived in the present study for the transient response of single-layer, incompressible, and unsaturated porous media in one-dimension conditions with typical boundary conditions based on the wave equations for unsaturated porous media proposed by Zienkiewicz. The inertial, viscous, and mechanical couplings were considered in the proposed solution. Taking the relative displacement of the liquid phase fluid as an independent variable, the dimensionless governing equations were first derived, and the eigenvalue and eigenfunction of the undamped system were given. Then, the original problem was transformed into the initial value problem for a set of second-order ordinary differential equations based on the constant-transform method and the orthogonality of eigenfunctions. The resulting problem was then solved using the state-space approach. Through this process, the exact solutions for displacement and stress of the original problem were obtained. The correctness of the solutions was verified by comparing them with the existing analytical and numerical results. Specifically, the analytical results indicate that only one type of compression wave exists in the incompressible unsaturated porous media. The compression wave with an opposite phase to the incident wave was generated at the fixed displacement boundary, whose response amplitude revealed a decreasing tendency with the increase of porous medium saturation.

    • Effect of lining thickness on the seismic response of tunnel side-crossing bridge pile system

      2025, 47(3):529-541. DOI: 10.20000/j.1000-0844.20230901001

      Abstract (113) HTML (0) PDF 31.70 M (55) Comment (0) Favorites

      Abstract:To investigate the influence of lining thickness on the tunnel side-crossing bridge pile system, this study takes an actual project in Dalian, Liaoning Province, as a case study. Then, using the combination of shaking table test and numerical simulation, this work investigates the influence of lining thickness on the seismic response of the tunnel side-crossing bridge pile system. The peak values of the structure's acceleration and internal forces (shear force, axial force, and bending moment), along with their change rate coefficients, were analyzed. The results show that the influence of lining thickness on the acceleration response of the ground surface is mainly in the range of approximately 70 m from the horizontal center. With the increase in lining thickness, the peak acceleration of the tunnel's upper section decreases, while that of the lower section increases, thus indicating an opposite acceleration response law. With the increase in the lining thickness, the peak internal force of the tunnel in the system rises, with maximum change rates of shear force and bending moment at 9.51% and 19.56%, respectively. At the same time, the peak shear force, axial force, and bending moment of the bridge pile decrease, with the maximum change rate of bending moment being 22.46%.

    • Deformation-damage mechanism and failure mode of creeping bedding rock landslides controlled by faults

      2025, 47(3):542-553. DOI: 10.20000/j.1000-0844.20231008003

      Abstract (137) HTML (0) PDF 18.92 M (65) Comment (0) Favorites

      Abstract:The stability of bedding rock slopes with weak interlayers is influenced by the combined effects of the weak interlayers and the surrounding rock mass. Owing to the poor physical and mechanical properties of weak interlayers, these slopes are highly susceptible to bedding landslide disasters. The instability mechanisms and failure modes of bedding rock slopes controlled by faults remain a critical concern in geotechnical engineering. This study investigates a bedding rock slope located at the right bank of a large hydropower project dam site in the upper Yellow River region based on field investigations. A finite element direct solution model was developed to analyze slope stability, incorporating interface elements employed to simulate the frictional sliding, opening, and closing of structural planes. The study examines the deformation characteristics, causative mechanisms, and stability of the slope under various conditions, focusing on creep-sliding deformation and failure controlled by the F27 fault. Results show that the potential sliding surface formed by bedding joints and the F27 fault is the dominant factor controlling slope stability. Under natural and rainstorm conditions, the slope transitions from a state of basic stability to marginal instability. Under seismic and extreme conditions, progressive extension and expansion of bedding joints and the F27 fault form a creeping bottom boundary. Tensile cracking deformation and failure occur at the trailing edge, leading to creep-tensile cracking failure along moderately to gently inclined structural planes. The slope instability poses severe threats to engineering safety, emphasizing the urgent need for targeted engineering treatments and slope reinforcement measures.

    • Mechanisms of highway slope failures induced by the Maerkang MS6.0 earthquake and post-earthquake secondary disaster effects

      2025, 47(3):554-565. DOI: 10.20000/j.1000-0844.20230705001

      Abstract (116) HTML (0) PDF 27.86 M (41) Comment (0) Favorites

      Abstract:On June 10, 2022, an MS6.0 earthquake occurred in Caodeng Township, Maerkang City, Sichuan Province, triggering widespread slope collapses and landslides along the newly constructed provincial highway S220 (Ribu-Muerzha Bridge section, K0+000-K56+059). Based on detailed post-earthquake investigations of slope failures in the engineering area, this study systematically summarizes the characteristics and mechanical mechanisms of earthquake-induced highway slope failures and discusses secondary disaster effects under alpine climate conditions. The slope failures induced by the Maerkang earthquake primarily manifested as localized rockfalls, individual landslide, isolated collapse, collapse zones, and high-altitude disasters (mainly soil landslides) exacerbated by topographic amplification of seismic waves in mountainous valleys. The mechanical mechanisms of highway slope failures in the epicentral area can be divided into five types: seismic cracking-damage type, bedding slip-tensile cracking type, toppling and cracking-collapse type, high-altitude debris flow type, and slope surface washout type. Seismic wave-induced tensile-shear damage to the rock and soil mass reduces slope stability, while gravitational potential energy in steep slopes drives instability and failure. Post-earthquake secondary disasters occurred in seismically damaged slopes under rainfall and freeze-thaw cycles in alpine environments, with disaster types varying according to damage severity and different geological conditions. For highway slope protection, it is recommended to reduce reliance on flexible measures and adopt rigid-flexible combined support systems. The results of this study provides theoretical foundations for refined slope protection design by elucidating distinct failure mechanisms.

    • Experimental study on the seismic behavior of cross-slanted corrugated steel plate shear walls

      2025, 47(3):566-577. DOI: 10.20000/j.1000-0844.20230508001

      Abstract (108) HTML (0) PDF 24.55 M (38) Comment (0) Favorites

      Abstract:To address the issue of out-of-plane buckling in flat steel plate shear walls, this paper proposes a new type of cross-slanted corrugated steel plate shear wall (CCSPW) with enhanced out-of-plane buckling-restrained performance. The study aims to investigate the influence of the corrugation angle on its seismic performance. To this end, three 1/3-scaled CCSPW specimens were designed and manufactured. The experimental study was conducted using the MTS loading system, focusing on various seismic performance indicators, such as initial stiffness, bearing capacity, failure process and form, energy consumption capacity, and ductility under low cyclic loading. The results show that CCSPWs can effectively prevent out-of-plane bulging under low cyclic loading, showcasing excellent lateral bearing capacity. The cross-slanted corrugated steel plates, subject to a joint force of tension and pressure, effectively improve the initial stiffness of specimens. Notably, the CCSPW specimen with an oblique angle of 60° exhibits the greatest initial stiffness. The specimen with an oblique angle of 45° shows a bearing capacity that is 5.5% and 10% higher than those of the other two specimens, along with the highest ductility coefficient and superior ductility. Additionally, the specimen with an oblique angle of 60° displays the largest equivalent viscous damping coefficient, ranging from 2% to 5% higher than those of the other two specimens, indicating excellent energy dissipation capacity.

    • 3D seismic response characteristics of valley sites based on real terrain

      2025, 47(3):578-589. DOI: 10.20000/j.1000-0844.20230906003

      Abstract (125) HTML (0) PDF 13.51 M (53) Comment (0) Favorites

      Abstract:To investigate the seismic response characteristics of typical valley sites, a three-dimensional finite element numerical model was developed based on the real terrain of a representative valley site in the North Tianshan region. The model was used to analyze the response characteristics of the valley site displacements, accelerations, and spectral accelerations under pulse-like and non-pulse-like ground motions. The results reveal that the dynamic response of the site is evidently influenced by the terrain, with surface displacement and acceleration being amplified as elevation increases. The displacement response in narrow valley areas is stronger than that in wide valley areas, whereas the acceleration response is weaker. A protruding mountain spur can amplify local displacement and acceleration responses, with a more pronounced effect under non-pulse-like earthquakes and a less evident impact under pulse-like earthquakes. Site displacement and acceleration responses increase as the depth of the rock and soil mass decreases. The amplification effect of shallow rock and soil mass on displacement is weakened, whereas that on acceleration is notably enhanced. The difference in surface displacement responses between the two types of earthquakes is remarkable, whereas the difference in acceleration responses is relatively small. As the PGA of the input ground motion increases, site displacement and acceleration responses increase linearly. Short-period spectral acceleration in high-altitude regions, such as mountain peaks, is significantly higher than in low-altitude areas, such as valleys. Conversely, long-period spectral acceleration is higher in low-altitude regions than in high-altitude areas. In narrow valley areas, long-period spectral acceleration is notably higher than in wide valley areas. Therefore, when planning engineering construction in valley sites, reasonable planning and layout should be carried out according to the characteristics of the building structures.

    • Hysteretic behavior analysis of steel reinforced concrete columns using segment fiber model

      2025, 47(3):590-597. DOI: 10.20000/j.1000-0844.20231209001

      Abstract (102) HTML (0) PDF 8.82 M (37) Comment (0) Favorites

      Abstract:

      Accurately predicting the elastoplastic behavior of steel reinforced concrete (SRC) members is essential for evaluating the collapse performance of SRC structures. This study develops a segment fiber model for SRC members (SRC-SFM) based on the discrete element method (DEM). Key innovations include (1) a uniaxial steel constitutive model that incorporates material softening and (2) a method for calculating concrete compressive constitutive parameters for an equivalent single-section, which accounts for dual confinement effects from structural steel and stirrups. This approach allows for the direct implementation of standard concrete models within the SRC-SFM framework. The proposed model was integrated into the DEM-based structural collapse discrete element computation program developed by the research team. Simulation analyses were performed to evaluate the hysteretic performance of H-section SRC columns with varying parameters under low-cycle reversed loading. The results confirm that the SRC-SFM, enhanced with a softening steel model and improved concrete constitutive parameter calculation method, accurately replicates the hysteretic behavior of flexural-compression members. These results establish a reliable foundation for subsequent studies on fracture mechanisms and collapse process simulations of SRC members.

    • >Earthquake Research
    • Seismic response calculation results of soils based on strong motion records: a case study of SMASS

      2025, 47(3):598-609. DOI: 10.20000/j.1000-0844.20231024001

      Abstract (123) HTML (0) PDF 29.52 M (64) Comment (0) Favorites

      Abstract:This study examines the discrepancies between calculated results from one-dimensional equivalent linearization soil seismic response analysis and actual strong motion records. The analysis uses data from the seismic monitoring array of site and structure (SMASS) operated by the Hebei Key Laboratory of Earthquake Disaster Prevention and Risk Assessment. Strong motion records from the Guye and Luanzhou earthquakes were analyzed, with a hypothetical bedrock input boundary set at a depth of 101 m. Ground motion results at depths of 65 and 30 m and the surface, calculated using the LSSRLI-1 program, were compared to observed data. Analysis results show the following: (1) Peak ground acceleration (PGA): While the calculated PGA trends generally match observed results, the amplification factor deviates more significantly as soil depth increases. Furthermore, the calculated soil response to ground motions with varying spectral characteristics differs from actual observations. (2) Response spectra: The difference between computed and actual response spectra increases with increasing soil depth. At 30 m depth, the computed spectra exhibit a distinct "triple-peak" anomaly not present in the observed data. (3) Characteristic periods: At shallow soil depths, the computed response spectrum shows a noticeably longer characteristic period compared to the observed spectrum. (4) Fourier spectra: Discrepancies between computed and actual Fourier spectra grow with increasing soil thickness. While both align in the low-frequency range, their trends and predominant frequencies diverge at higher frequencies.

    • Typical damage characteristics of school buildings caused by the Jishishan MS6.2 earthquake and implications for personnel evacuation

      2025, 47(3):610-620. DOI: 10.20000/j.1000-0844.20240811001

      Abstract (111) HTML (0) PDF 28.87 M (43) Comment (0) Favorites

      Abstract:On December 18, 2023, an MS6.2 earthquake occurred in Jishishan County, Gansu Province. A field investigation was conducted immediately on 15 frame structures and 24 masonry structures from nine primary/secondary schools and four educational annexes located at varying seismic intensity zones. Key findings include the following: (1) All 12 severely damaged buildings were single-story masonry structures with steel-wood roof trusses. (2) Most frame structures sustained only minor damage, whereas others exhibited moderate damage. (3) Significant damage to nonstructural components and ancillary structures was observed even in structurally intact buildings, posing risks to the evacuation safety of students and teachers. Based on an on-site investigation, this study systematically summarizes the common seismic damage patterns in educational facilities and identifies the potential safety hazards along evacuation pathways through four key zones: classrooms, corridors, staircases, and outdoor spaces. Consequently, practical recommendations are proposed, including seismic retrofitting of nonstructural components, equipment, and ancillary structures on campus to further enhance the safety and evacuation efficiency of personnel in schools after earthquakes.

    • Inversion of parameters for intense underground explosions using surface deformation monitoring with InSAR

      2025, 47(3):621-630. DOI: 10.20000/j.1000-0844.20230720004

      Abstract (104) HTML (0) PDF 23.37 M (42) Comment (0) Favorites

      Abstract:Conducting intense underground explosion tests is crucial for countries to develop, test, and evaluate strategic weapons. The resulting parameters are essential for evaluating weapon capabilities and ensuring national security. In this study, the surface deformation of the target area was monitored using DS-InSAR technology, applying 48 scenes of ERS-1/2 data collected from 1992 to 2001. Then, the Bayesian inversion framework was employed, proving effective in determining the parameters of underground intense explosions using the finite prolate spheroid model and the point compound dislocation model (pCDM). Finally, the accuracy and reliability of both models were analyzed and compared. The results indicate that DS-InSAR technology could effectively detect surface deformation resulting from intense underground explosions. The single-and dual-source finite prolate spheroid models, as well as the pCDM, provided a good fit to the InSAR observations, with the latter offering a superior fit. The results also demonstrate that parameter inversion of geological models based on InSAR data can provide valuable technical support for the study of underground intense explosion tests.

    • Correlation between surface/borehole response spectral ratio and microtremor HVSR

      2025, 47(3):631-641. DOI: 10.20000/j.1000-0844.20231202001

      Abstract (96) HTML (0) PDF 9.69 M (39) Comment (0) Favorites

      Abstract:Despite the lack of a robust theoretical foundation, the horizontal-to-vertical spectral ratio (HVSR) method of microtremor Fourier amplitudes has become a widely used tool for estimating site parameters and analyzing seismic site effects. This study refines the microtremor HVSR approach and introduces a novel empirical method for estimating the surface/borehole acceleration spectral ratio (SBSRa) under ground motions. The proposed method facilitates the estimation of ground motion amplification factors using in situ microtremor observations, offering critical data for seismic site effect research. Drawing on 296 958 strong motion acceleration records from 699 stations in Japan's KiK-net network, stable microtremor HVSRs were extracted from pre-event microtremor data (prior to P-wave arrivals). Statistical analysis revealed a strong correlation between microtremor HVSR and SBSRa under weak ground motions, with their spectral shapes and predominant frequencies showing high consistency. Using a frequency normalization approach, empirical correction coefficients were derived for various types of microtremor HVSR, leading to the development of a practical method for predicting SBSRa based on microtremor HVSR. Reliability analyses demonstrated that the predicted SBSRa achieves engineering-level accuracy, with Jaccard similarity coefficients exceeding 0.58 for more than 75% of the stations. These results validate the effectiveness of microtremor HVSR as a reliable proxy for approximating SBSRa under weak ground motions.

    • Present-day locking degree and seismic hazard analysis of the Lintan-Tanchang fault

      2025, 47(3):642-651. DOI: 10.20000/j.1000-0844.20240131001

      Abstract (99) HTML (0) PDF 16.31 M (71) Comment (0) Favorites

      Abstract:Based on two periods of global navigation satellite system (GNSS) data (2009-2013 and 2015-2019), the Tdefnode negative dislocation method was employed to invert the locking degree and slip deficit rate of the Lintan-Dangchang fault before the Minxian-ZhangxianMS6.6 and Xiahe MS5.7 earthquakes. Combined with the spatial distribution of small earthquakes and GNSS profile results, this study analyzed the characteristics of small earthquake activity and horizontal crustal movement before the two earthquakes and evaluated the future seismic hazard of the Lintan-Tanchang fault. The results show the following: (1) The seismogenic zones of the fault exhibited strong locking states before both earthquakes, with inverted locking depths generally consistent with the focal depths, and the slip deficit rate of the fault was relatively low. (2) Combined with the spatial distribution of small earthquakes, seismic quiescence periods were observed before both earthquakes, and the duration of these quiescence periods was consistent with the aftershock distribution lengths. (3) GNSS profiles across the Lintan-Dangchang fault indicated that the fault currently exhibits thrust-dominated compression with sinistral strike-slip movement, and the fault slip rates were enhanced after the earthquake compared with those before the earthquake. Integrated analysis reveals stronger locking and high slip deficit rates in the eastern Lintan segment than in the Minxian-Dangchang segment and the eastern Hezuo segment. As these locked zones also experienced seismic quiescence periods, attention should be focused on these two regions in future endeavors.

    • Characteristics of earthquake damage caused by the 2023 MS5.2 earthquake in Longyang District, Baoshan City, Yunnan Province

      2025, 47(3):652-662. DOI: 10.20000/j.1000-0844.20230522001

      Abstract (119) HTML (0) PDF 36.13 M (36) Comment (0) Favorites

      Abstract:An MS5.2 earthquake occurred in Longyang District (24.91°N, 99.26°E), Baoshan City, Yunnan Province, on May 2, 2023, disrupting the relative seismic calm in Baoshan City, which had not experienced any MS≥5.0 earthquakes since 2015. Based on field investigations of disaster losses and the collection of disaster data, this study provides a detailed analysis of the seismogenic geological structure, focal mechanism, spatial distribution of seismic intensity, and the earthquake damage characteristics and causes in buildings and engineering structures in the Longyang area. Additionally, the earthquake damage matrix for buildings in the affected area was compared with the damage characteristics of historical earthquakes of similar magnitude in Yunnan Province. Results show that the epicenter of Longyang MS5.2 earthquake is located in the middle segment of the Lancang River fault zone, with right-lateral strike-slip, which is consistent with the result of the focal mechanism solution. The maximum intensity is Ⅵ degree, and the affected area is approximately 600 km2. The intensity circle presents an irregular ellipse with a long axis of 37 km and a short axis of 21 km. The long axis direction of the isoseismic line is NNW, aligning with the strike of the Lancang River fault, which is closest to the epicenter of the earthquake. Nine people were slightly injured in the earthquake, a number higher than typically seen in historical earthquakes of similar magnitude in Yunnan Province. The seismic performance of civil structure houses was poor, with notable damage observed. Due to site effects and the fact that some brick-concrete and frame structures were not constructed in accordance with specifications, the damage to houses in the area where the Wayao Town Government is located reached a severity level of VII. Traffic, communication, and water conservancy facilities were damaged to different degrees, with traffic infrastructure suffering the most severe damage. Given the extensive damage, high casualties, serious building destruction, and significant economic loss caused by this earthquake, the study offers emergency response recommendations. These suggestions aim to improve earthquake prevention, disaster reduction, and emergency rescue capabilities in western Yunnan, providing valuable reference for future preparedness and response strategies.

    • Construction of a visualization platform for field survey data acquisition based on an Android system

      2025, 47(3):663-670. DOI: 10.20000/j.1000-0844.20240118004

      Abstract (100) HTML (0) PDF 13.46 M (22) Comment (0) Favorites

      Abstract:To address practical challenges in current field surveys for earthquake monitoring, this study develops a visualization platform for field survey data acquisition. The platform, designed specifically for seismic monitoring workflows, enables field survey data collection of an Android mobile terminal using the Java language. It can consolidate heterogeneous data (e.g., measurements, images, and videos) into unified, standardized forms, enabling rapid transmission to centralized databases. Its implementation in the real-world field of earthquake monitoring shows that the system realizes comprehensive digital operation and reduces errors and repetitive work in traditional paper records, thus greatly improving the flexibility and timeliness of the collection work. These advancements provide a critical technical foundation for optimizing subsequent field monitoring tasks in seismology.

    • Construction and application of v S30 data in Sichuan Province: a case study of the Wenchuan MS8.0 earthquake

      2025, 47(3):671-679. DOI: 10.20000/j.1000-0844.20231201001

      Abstract (104) HTML (0) PDF 15.95 M (28) Comment (0) Favorites

      Abstract:As an important parameter for site classification, the average shear wave velocity at a depth of 30 m ( v S30 is widely used in domestic and international seismic design codes for buildings and structures, as well as in the correction of local site effects. However, the applicability of the v S30 data commonly used in China, which are provided by the United States Geological Survey (USGS), requires further verification. Based on the correlation between terrain slope in Sichuan Province and shallow average wave velocity, as well as the relationship between v S30 and shallow average shear wave velocity, this paper proposes a v S30 dataset for Sichuan Province paper. The dataset is then applied to the seismic intensity assessment of the Wenchuan MS8.0 earthquake. The results show that compared with the widely used v S30 data provided by USGS, the v S30 results for Sichuan Province obtained from this study are closer to the actual situation. The rapid seismic intensity assessment of the Wenchuan MS8.0 earthquake using the v S30 data in this study provides more accurate judgments of heavy and severe disaster areas. The results can improve the accuracy of seismic emergency outputs in Sichuan Province in the future, offering valuable first-hand reference materials for post-earthquake emergency command and rescue operations.

    • Adaptive quadtree downsampling method for InSAR data based on multifactor constraints

      2025, 47(3):680-689. DOI: 10.20000/j.1000-0844.20231128002

      Abstract (96) HTML (0) PDF 34.91 M (25) Comment (0) Favorites

      Abstract:Data compression of interferometric synthetic aperture radar (InSAR) deformation fields significantly enhances the inversion efficiency of coseismic slip distribution models and seismogenic structure parameters. However, traditional compression methods face challenges in balancing the removal of noise/redundant information and the preservation of global/local key deformation features. This study proposes a multifactor quadtree downsampling method constrained by variance, deformation gradient, and coherence for the downsampling processing of the InSAR coseismic deformation field. Significance and coherence coefficients were used to adaptively weigh various factors, and three strong earthquake events with different complexities were selected to verify the effectiveness and robustness of the method. Compared with existing methods, the multifactor quadtree downsampling method maintained balanced sampling rates and lower root mean square error across all cases, and the sampling results improved the resolution of fault slip distributions in three-dimensional slip inversions while reducing model residuals. The results suggest that the proposed method demonstrates low sampling rates, robust performance, effective elimination of low-coherence points, high retention of critical deformation details, and enhanced constraints on the linear distribution of deformation.

    • Potential seismic deformation of the Majiishan Grottoes induced by near-field active faults

      2025, 47(3):690-699. DOI: 10.20000/j.1000-0844.20250126004

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      Abstract:Multiple active faults are developed in the near field of the Majiishan Grottoes, with the northern margin fault zone of the West Qinling Mountains historically posing the greatest seismic threat. To investigate the impact of near-field seismogenic faults on the Majiishan grottoes, the seismic geological conditions and potential seismic hazards of the northern margin fault zone of the West Qinling Mountains were analyzed in this study. Combining the elastic dislocation theory and the three-dimensional finite element numerical simulation, the displacement and strain distribution patterns on the surface of the Majiishan Grottoes area during left-lateral strike-slip activities along the Tianshui—Baoji segment of the northern margin fault zone of the West Qinling Mountains under M 7.0 and M 7.5 earthquakes were examined. The results reveal that seismic deformation of the Tianshui—Baoji fault is dominated by horizontal shear, with localized secondary vertical deformation. Higher magnitudes significantly increase the magnitude and spatial extent of displacement and strain. In the Majiishan Grottoes area, seismic displacement, normal strain, and shear strain increase with the increase of magnitude. The southeastern direction of the grottoes exhibits the most critical displacement under future earthquakes, with shear strain posing the primary risk for potential rock mass dislocation or localized shear failure. Additionally, fault plane dimensions influence computational results: surface deformation stabilizes when the fault plane depth reaches 15 km, which can serve as a reference value for seismic simulations of the Tianshui-Baoji fault. This study provides critical insights for seismic risk assessment and mitigation of the Majiishan Grottoes.

    • Causes of damage to residential buildings during the Dingri MS6.8 earthquake in Xizang

      2025, 47(3):700-708. DOI: 10.20000/j.1000-0844.20250113001

      Abstract (127) HTML (0) PDF 23.17 M (38) Comment (0) Favorites

      Abstract:On January 7, 2025, an MS6.8 earthquake occurred in Cuoguo Township, Dingri County, Shigatse City, Xizang Autonomous Region, with a focal depth of 10 km. The epicenter was located in a high-altitude frigid region along the Shenza-Dingjie rift within the Lhasa block of the Qinghai-Xizang Plateau. The Dengmo fault, the seismogenic fault of the earthquake, is characterized by normal faulting, with a maximum coseismic displacement of approximately 3 m. Using results from a survey of residential building structures in the earthquake-prone regions of Xizang prior to the earthquake, this paper provides a summary of significant destructive earthquakes that occurred in Xizang from 1980 to 2024. The seismogenic structure of the Dingri MS6.8 earthquake and seismic damages to local residential buildings are also analyzed. The research results indicate that the Dingri MS6.8 earthquake is an earthquake with large magnitude, high intensity, and serious casualties compared with the earthquakes that occurred in Xizang over the years. Most residential buildings in the local area are wall-lifted beam structures. The earthquake damages include the peeling or even collapse of self-supporting walls, external wall cracking, house collapse due to overweight roofs, broken wooden columns or beam-column joints, and the fall of nonstructural components. Finally, a comprehensive analysis is conducted to identify the factors contributing to the severe casualties in this earthquake.

    • Relationship between aeromagnetic anomalies and fault structures in the capital area of China

      2025, 47(3):709-715. DOI: 10.20000/j.1000-0844.20240127001

      Abstract (116) HTML (0) PDF 15.21 M (37) Comment (0) Favorites

      Abstract:The capital area of China, located at a tectonic transition zone between the Yanshan uplift and the North China Plain, is characterized by complex structural settings. Using large-scale aeromagnetic anomaly data, horizontal and vertical first-order derivations at 0°, 45°, 90°, and 135° directions were calculated. Then, the fault structure was interpreted in detail, and a total of 39 NE-and NW-trending faults were identified in the capital area. The original aeromagnetic anomaly field shows disorganized high-amplitude anomalies in the Yanshan uplift in the north of the study area, indicating a multistage tectonic movement. High-gradient anomaly belts derived from the directional derivative map exhibit strong consistency with fault strikes. NE-and NW-trending faults in the Beijing depression display distinct linear features. Because of the negative anomaly traps in the Beijing depression, these faults can be considered “dry faults” with magmatic activity. Vertical derivatives highlight prominent high-anomaly gradient zones along the boundary of the Daxing uplift, Western Beijing uplift, and Beijing depression.

    • Activity of the southwest segment of the Huayingshan fault based on river terrace deformation

      2025, 47(3):716-726. DOI: 10.20000/j.1000-0844.20231027002

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      Abstract:In recent years, two moderate earthquakes of magnitude 6.0 occurred near the Huayingshan fault zone, a critical boundary fault within the Sichuan Basin. Therefore, it is crucial to study the activity characteristics of the Huayingshan fault. From the sedimentary history analysis of the study area, river terraces were first extracted using medium-resolution digital elevation models (DEMs). These terraces were then validated using high-resolution DEM from unmanned aerial vehicles and field surveys. Finally, the spatial distribution characteristics of terraces along the Minjiang River, Jinsha River, Yangtze River, and Tuojiang River in the southwest segment of the Huayingshan fault were systematically obtained. On the basis of the deformation characteristics and formation ages of the stratified geomorphic surfaces, the southwest segment of the Huayingshan fault exhibited significant activity during the Middle Pleistocene but weakened or ceased activity in the Late Pleistocene. These findings provide critical insights for seismic hazard assessment of the southwest segment of the Huayingshan fault and the identification of seismogenic structures of recent moderate earthquakes.

    • Detection and analysis of very low frequency earthquakes before the 2022 Luding MS6.8 earthquake

      2025, 47(3):727-740. DOI: 10.20000/j.1000-0844.20240130001

      Abstract (105) HTML (0) PDF 23.08 M (38) Comment (0) Favorites

      Abstract:On September 5, 2022, an MS6.8 earthquake struck Luding County, Ganzi Prefecture, Sichuan Province. Slow earthquakes manifested as very low frequency earthquakes occurring in the source region before the Luding earthquake hold significant implications for understanding the source physical processes of the mainshock. This study employs the Hilbert transform and short-time Fourier transform (STFT) to detect very low frequency earthquakes preceding the mainshock, with preliminary analyses of their recording stations, spectral characteristics, and temporal features. The results indicate the following: (1) A total of 14 very low frequency earthquakes were detected before the mainshock, and their vertical and horizontal components could be effectively detected, with superior detection performance in the vertical component. (2) Events with large amplitudes and long durations were better identified using the Hilbert transform, whereas those with small amplitudes, short durations, and overlapping waveforms were effectively detected using STFT. (3) A total of 67.7% of the stations successfully recorded all events, demonstrating strong observational reliability. The very low frequency earthquakes exhibited distinct spectral peaks within a relatively low-frequency range (0.06-0.16 Hz), markedly differing from the frequency bands of natural earthquakes. The event with the largest amplitude occurred 18 h before the mainshock, followed by an increasing frequency of events accompanied by heightened small earthquake activity. This pattern may reflect a gradual release of crustal stress through very low frequency earthquakes and minor earthquakes until the occurrence of the mainshock.

    • Design and implementation of an earthquake disaster risk assessment and service system in Sichuan Province

      2025, 47(3):741-750. DOI: 10.20000/j.1000-0844.20231024002

      Abstract (110) HTML (0) PDF 17.54 M (28) Comment (0) Favorites

      Abstract:The current focus of earthquake disaster prevention and mitigation work has shifted from postdisaster emergency rescue to predisaster risk prevention and control and from passive prevention of earthquake disasters to active reduction of earthquake disaster risks. The construction of earthquake disaster risk assessment and service systems can provide strong support for reducing earthquake disaster risks and enhancing the ability to prevent earthquake disasters. This paper started with the earthquake disaster risk situation of Sichuan Province, which was characterized by high risks of seismic and geological hazards, high exposure of disaster-bearing bodies, and significant differences in vulnerability of disaster-bearing bodies. Based on the needs and objectives of earthquake disaster risk prevention and control, it focused on earthquake disaster risk assessment, zonation, and information service. The overall framework, function, and business process of the earthquake disaster risk assessment and service system in Sichuan Province were designed and developed using big data, cloud computing, spatial information, and other technologies. The system integrated multisource heterogeneous earthquake disaster risk data, thus promoting the process of earthquake disaster risk assessment and further improving the information service capability for earthquake disaster risk prevention and control.

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